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1

Development Of 2-Meter Soil Temperature Probes And Results Of...  

Open Energy Info (EERE)

Meter Soil Temperature Probes And Results Of Temperature Survey Conducted At Desert Peak, Nevada, Usa Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference...

2

Shallow (2-meter) temperature surveys in Colorado  

SciTech Connect (OSTI)

Citation Information: Originator: Geothermal Development Associates, Reno, Nevada Publication Date: 2012 Title: Colorado 2m Survey Edition: First Publication Information: Publication Place: Reno Nevada Publisher: Geothermal Development Associates, Reno, Nevada Description: Shallow temperature surveys are useful in early-stage geothermal exploration to delineate surface outflow zones, with the intent to identify the source of upwelling, usually a fault. Detailed descriptions of the 2-meter survey method and equipment design can be found in Coolbaugh et al. (2007) and Sladek et al. (2007), and are summarized here. The survey method was devised to measure temperature as far below the zone of solar influence as possible, have minimal equilibration time, and yet be portable enough to fit on the back of an all-terrain vehicle (ATV); Figure 2). This method utilizes a direct push technology (DPT) technique where 2.3 m long, 0.54” outer diameter hollow steel rods are pounded into the ground using a demolition hammer. Resistance temperature devices (RTD) are then inserted into the rods at 2-meter depths, and allowed to equilibrate for one hour. The temperatures are then measured and recorded, the rods pulled out of the ground, and re-used at future sites. Usually multiple rods are planted over the course of an hour, and then the sampler returns back to the first station, measures the temperatures, pulls the rods, and so on, to eliminate waiting time. At Wagon Wheel Gap, 32 rods were planted around the hot springs between June 20 and July 1, 2012. The purpose was to determine the direction of a possible upflow fault or other structure. Temperatures at 1.5m and 2m depths were measured and recorded in the attribute table of this point shapefile. Several anomalous temperatures suggest that outflow is coming from a ~N60W striking fault or shear zone that contains the quartz-fluorite-barite veins of the adjacent patented mining claims. It should be noted that temperatures at 2m depth vary according to the amount of solar heating from above, as well as possible geothermal heating from below. Spatial Domain: Extent: Top: 4490310.560635 m Left: 150307.008238 m Right: 433163.213617 m Bottom: 4009565.915398 m Contact Information: Contact Organization: Geothermal Development Associates, Reno, Nevada Contact Person: Richard “Rick” Zehner Address: 3740 Barron Way City: Reno State: NV Postal Code: 89511 Country: USA Contact Telephone: 775-737-7806 Spatial Reference Information: Coordinate System: Universal Transverse Mercator (UTM) WGS’1984 Zone 13N False Easting: 500000.00000000 False Northing: 0.00000000 Central Meridian: -105.00000000 Scale Factor: 0.99960000 Latitude of Origin: 0.00000000 Linear Unit: Meter Datum: World Geodetic System 1984 (WGS ’1984) Prime Meridian: Greenwich Angular Unit: Degree Digital Form: Format Name: Shape file

Zehner, Richard E.

2012-02-01T23:59:59.000Z

3

Use of Rapid Temperature Measurements at a 2-Meter Depth to Augment...  

Open Energy Info (EERE)

Measurements at a 2-Meter Depth to Augment Deeper Temperature Gradient Drilling Jump to: navigation, search OpenEI Reference LibraryAdd to library Conference Paper: Use of Rapid...

4

Development Of 2-Meter Soil Temperature Probes And Results Of Temperature  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 NoPublic Utilities Address:011-DNA Jump to:52c8ff988c1Dering Harbor, New York: EnergyEnergyguaGet involvedSurvey

5

Soil temperature, soil moisture and thaw depth, Barrow, Alaska, Ver. 1  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

This dataset consists of field measurements of soil properties made during 2012 and 2013 in areas A-D of Intensive Site 1 at the Next-Generation Ecosystem Experiments (NGEE) Arctic site near Barrow, Alaska. Included are i) weekly measurements of thaw depth, soil moisture, presence and depth of standing water, and soil temperature made during the 2012 and 2013 growing seasons (June - September) and ii) half-hourly measurements of soil temperature logged continuously during the period June 2012 to September 2013.

Sloan, V.L.; J.A. Liebig; M.S. Hahn; J.B. Curtis; J.D. Brooks; A. Rogers; C.M. Iversen; R.J. Norby

6

Soil temperature, soil moisture and thaw depth, Barrow, Alaska, Ver. 1  

SciTech Connect (OSTI)

This dataset consists of field measurements of soil properties made during 2012 and 2013 in areas A-D of Intensive Site 1 at the Next-Generation Ecosystem Experiments (NGEE) Arctic site near Barrow, Alaska. Included are i) weekly measurements of thaw depth, soil moisture, presence and depth of standing water, and soil temperature made during the 2012 and 2013 growing seasons (June - September) and ii) half-hourly measurements of soil temperature logged continuously during the period June 2012 to September 2013.

Sloan, V.L.; J.A. Liebig; M.S. Hahn; J.B. Curtis; J.D. Brooks; A. Rogers; C.M. Iversen; R.J. Norby

2014-01-10T23:59:59.000Z

7

CO2 CH4 flux Air temperature Soil temperature and Soil moisture, Barrow, Alaska 2013 ver. 1  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

This dataset consists of field measurements of CO2 and CH4 flux, as well as soil properties made during 2013 in Areas A-D of Intensive Site 1 at the Next-Generation Ecosystem Experiments (NGEE) Arctic site near Barrow, Alaska. Included are i) measurements of CO2 and CH4 flux made from June to September (ii) Calculation of corresponding Gross Primary Productivity (GPP) and CH4 exchange (transparent minus opaque) between atmosphere and the ecosystem (ii) Measurements of Los Gatos Research (LGR) chamber air temperature made from June to September (ii) measurements of surface layer depth, type of surface layer, soil temperature and soil moisture from June to September.

Margaret Torn

8

Soil organic matter stability and the temperature sensitivity of soil respiration   

E-Print Network [OSTI]

Soil respiration is an important source of atmospheric CO2, with the potential for large positive feedbacks with global warming. The size of these feedbacks will depend on the relative sensitivity to temperature of very ...

Burns, Nancy Rosalind

2012-11-29T23:59:59.000Z

9

SCS-2005-17 Soil Temperatures for Cotton Planting  

E-Print Network [OSTI]

SCS-2005-17 6-05 Soil Temperatures for Cotton Planting Randy Boman, Ph.D., Associate Professor and Extension Agronomist-Cotton Robert Lemon, Ph.D., Professor and Extension Agronomist-Cotton C otton can and leaves. The cotton seed also has two cotyledons, or seed leaves. These cotyledons are storage tissues

Mukhtar, Saqib

10

Temperature-associated increases in the global soil respiration record  

SciTech Connect (OSTI)

Soil respiration (RS), the flux of CO2 from the soil surface to the atmosphere, comprises the second-largest terrestrial carbon flux, but its dynamics are incompletely understood, and the global flux remains poorly constrained. Ecosystem warming experiments, modelling analyses, and biokinetics all suggest that RS should change with climate. This has been difficult to confirm observationally because of the high spatial variability of RS, inaccessibility of the soil medium, and inability of remote sensing instruments to measure large-scale RS fluxes. Given these constraints, is it possible to discern climate-driven changes in regional or global RS fluxes in the extant four-decade record of RS chamber measurements? Here we use a database of worldwide RS observations, matched with high-resolution historical climate data, to show a previously unknown temporal trend in the RS record after accounting for mean annual climate, leaf area, nitrogen deposition, and changes in CO2 measurement technique. Air temperature anomaly (deviation from the 1961-1990 mean) is significantly and positively correlated with changes in RS fluxes; both temperature and precipitation anomalies exert effects in specific biomes. We estimate that the current (2008) annual global RS flux is 98±12 Pg and has increased 0.1 Pg yr-1 over the last 20 years, implying a global RS temperature response (Q10) of 1.5. An increasing global RS flux does not necessarily constitute a positive feedback loop to the atmosphere; nonetheless, the available data are consistent with an acceleration of the terrestrial carbon cycle in response to global climate change.

Bond-Lamberty, Benjamin; Thomson, Allison M.

2010-03-25T23:59:59.000Z

11

DVS5.2 METERS 8 METERS OCR507, STOR-X DATA LOGGER  

E-Print Network [OSTI]

DVS5.2 METERS 10 METERS 8 METERS OCR507, STOR-X DATA LOGGER 16" BATTERY HOUSING TC INVERTED5 METERS 1" SAS INDUCTIVE CABLE BREAKOUT RADAR REFLECTOR OS PAPA RECOVERY HANDLE 1 METER-SBE 37 MICROCAT TC HUMIDITY (FLEX) CTD/GTD/O2 4 METERS WETLabs FLNTUSB FLUOROMETER DOUBLE NUT AND TORQUE ALL LOAD CELL NUTS

12

Temperature effects on decomposition rates of soil organic matter with differing proportions of labile and  

E-Print Network [OSTI]

favorable energy source. Labile soil organic matter is sugar, starch, and carbohydrates. An alternative energy source is recalcitrant carbon, which is harder to decompose soil organic matter such as lignin energy source (Nabu, 2009). With increasing global temperatures, it is important to understand how soil

Vallino, Joseph J.

13

Use of Rapid Temperature Measurements at a 2-Meter Depth to Augment Deeper  

Open Energy Info (EERE)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home5b9fcbce19 No revisionEnvReviewNonInvasiveExplorationUT-gTagusparkCalculator JumpUnitedBeowawe Geothermal Field | Open

14

Soil moisture surpasses elevated CO2 and temperature as a control on soil carbon dynamics in a multi-factor climate change experiment  

SciTech Connect (OSTI)

Some single-factor experiments suggest that elevated CO2 concentrations can increase soil carbon, but few experiments have examined the effects of interacting environmental factors on soil carbon dynamics. We undertook studies of soil carbon and nitrogen in a multi-factor (CO2 x temperature x soil moisture) climate change experiment on a constructed old-field ecosystem. After four growing seasons, elevated CO2 had no measurable effect on carbon and nitrogen concentrations in whole soil, particulate organic matter (POM), and mineral-associated organic matter (MOM). Analysis of stable carbon isotopes, under elevated CO2, indicated between 14 and 19% new soil carbon under two different watering treatments with as much as 48% new carbon in POM. Despite significant belowground inputs of new organic matter, soil carbon concentrations and stocks in POM declined over four years under soil moisture conditions that corresponded to prevailing precipitation inputs (1,300 mm yr-1). Changes over time in soil carbon and nitrogen under a drought treatment (approximately 20% lower soil water content) were not statistically significant. Reduced soil moisture lowered soil CO2 efflux and slowed soil carbon cycling in the POM pool. In this experiment, soil moisture (produced by different watering treatments) was more important than elevated CO2 and temperature as a control on soil carbon dynamics.

Garten Jr, Charles T [ORNL; Classen, Aimee T [ORNL; Norby, Richard J [ORNL

2009-01-01T23:59:59.000Z

15

Clemson final report: High temperature formulations for SRS soils  

SciTech Connect (OSTI)

This study was undertaken to demonstrate the application of a DC arc melter to in-situ vitrification of SRS soils. The melter that was available at the DOE/Industrial Vitrification Laboratory at Clemson University was equipped with opposing solid electrodes. To simulate field conditions, two hollow electrode configurations were evaluated which allowed fluxes to be injected into the melter while the soils were being vitrified. the first 4 runs utilized pre-blended flux (two runs) and attempted flux injection (two runs). These runs were terminated prematurely due to offgas sampling problems and melt freezing. The remaining four runs utilized a different electrode geometry, and the runs were not interrupted to change out the offgas sampling apparatus. These runs were conducted successfully.

Schumacher, R.F. [Westinghouse Savannah River Company, AIKEN, SC (United States)

1997-03-11T23:59:59.000Z

16

Validation of Noah-simulated Soil Temperature in the North American Land Data Assimilation System Phase 2  

SciTech Connect (OSTI)

Soil temperature can exhibit considerable memory from weather and climate signals and is among the most important initial conditions in numerical weather and climate models. Consequently, a more accurate long-term land surface soil temperature dataset is needed to improve weather and climate simulation and prediction, and is also important for the simulation of agricultural crop yield and ecological processes. The North-American Land Data Assimilation (NLDAS) Phase 2 (NLDAS-2) has generated 31-years (1979-2009) of simulated hourly soil temperature data with a spatial resolution of 1/8o. This dataset has not been comprehensively evaluated to date. Thus, the ultimate purpose of the present work is to assess Noah-simulated soil temperature for different soil depths and timescales. We used long-term (1979-2001) observed monthly mean soil temperatures from 137 cooperative stations over the United States to evaluate simulated soil temperature for three soil layers (0-10 cm, 10-40 cm, 40-100 cm) for annual and monthly timescales. We used short-term (1997-1999) observed soil temperature from 72 Oklahoma Mesonet stations to validate simulated soil temperatures for three soil layers and for daily and hourly timescales. The results showed that the Noah land surface model (Noah LSM) generally matches observed soil temperature well for different soil layers and timescales. At greater depths, the simulation skill (anomaly correlation) decreased for all time scales. The monthly mean diurnal cycle difference between simulated and observed soil temperature revealed large midnight biases in the cold season due to small downward longwave radiation and issues related to model parameters.

Xia, Youlong; Ek, Michael; Sheffield, Justin; Livneh, Ben; Huang, Maoyi; Wei, Helin; Song, Feng; Luo, Lifeng; Meng, Jesse; Wood, Eric

2013-02-25T23:59:59.000Z

17

An example of remediation of mercury impacted soil using high vacuum low temperature thermal desorption  

SciTech Connect (OSTI)

The purpose of this paper is to describe a high vacuum, low temperature thermal desorption (LTTD) technology which has been used to remediate soil impacted with elemental mercury and to present the results of pre-treatment and post-treatment soil sampling. The general operating principles of this high vacuum LTTD technology, the IRHV-200, are: (a) depression of the boiling points of the target compounds by lowering the ambient pressure within the treatment chamber using a vacuum pump; (b) use of infrared radiation to generate a thermal gradient in the top several inches of non-liquid material contained within the treatment chamber and use of a carrier gas to transport the desorbed contaminants from the treatment chamber to a pollution control system. The overall effect of these parameters is a batch treatment system capable of desorbing target contaminants from soil under anaerobic conditions and low temperature such that the desorbed contaminants do not degrade and generate thermal or oxidative by-products. Essentially, the desorbed contaminants undergo a reversible phase change from liquid to vapor in the treatment chamber and are condensed back to liquid in the pollution control system. Results of bench top testing are compared to full scale remediations of significant volumes of soil to demonstrate remediation of mercury impacted soil. This technology is also applicable for soils impacted with other higher boiling point organics, such as, PCP, PCBs, PAHs, PNAs, pesticides and herbicides.

Dagdigian, J.V. [McLaren/Hart, Irvine, CA (United States)

1997-12-31T23:59:59.000Z

18

Importance of moisture transport, snow cover and soil freezing to ground temperature predictions  

E-Print Network [OSTI]

foundation may also be explicitly calculated. For buildings utilizing ground source heat pump systems of the annual outdoor and indoor air temperatures. Then periodic heat transfer coefficients and phase lags with significant earth contact. A numerical model for heat and moisture transfer in partially frozen soils has been

19

Plant-soil interactions and acclimation to temperature of microbial-mediated soil respiration may affect predictions of soil CO2 efflux  

E-Print Network [OSTI]

shifts in microbial communities due to soil warming.Soil Sci Soc Am J 61:475–481to an important portion of soil CO 2 ef?ux (Hanson et al.

Curiel Yuste, J.; Ma, S.; Baldocchi, D. D.

2010-01-01T23:59:59.000Z

20

Soil carbon sensitivity to temperature and carbon use efficiency compared across microbial-ecosystem models of varying complexity  

SciTech Connect (OSTI)

Global ecosystem models may require microbial components to accurately predict feedbacks between climate warming and soil decomposition, but it is unclear what parameters and levels of complexity are ideal for scaling up to the globe. Here we conducted a model comparison using a conventional model with first-order decay and three microbial models of increasing complexity that simulate short- to long-term soil carbon dynamics. We focused on soil carbon responses to microbial carbon use efficiency (CUE) and temperature. Three scenarios were implemented in all models: constant CUE (held at 0.31), varied CUE ( 0.016 C 1), and 50 % acclimated CUE ( 0.008 C 1). Whereas the conventional model always showed soil carbon losses with increasing temperature, the microbial models each predicted a temperature threshold above which warming led to soil carbon gain. The location of this threshold depended on CUE scenario, with higher temperature thresholds under the acclimated and constant scenarios. This result suggests that the temperature sensitivity of CUE and the structure of the soil carbon model together regulate the long-term soil carbon response to warming. Equilibrium soil carbon stocks predicted by the microbial models were much less sensitive to changing inputs compared to the conventional model. Although many soil carbon dynamics were similar across microbial models, the most complex model showed less pronounced oscillations. Thus, adding model complexity (i.e. including enzyme pools) could improve the mechanistic representation of soil carbon dynamics during the transient phase in certain ecosystems. This study suggests that model structure and CUE parameterization should be carefully evaluated when scaling up microbial models to ecosystems and the globe.

Li, Jianwei [University of Oklahoma] [University of Oklahoma; Wang, Gangsheng [ORNL] [ORNL; Allison, Steven D. [University of California, Irvine] [University of California, Irvine; Mayes, Melanie [ORNL] [ORNL; Luo, Yiqi [University of Oklahoma] [University of Oklahoma

2014-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


21

Soil respiration at mean annual temperature predicts annual total across vegetation types and biomes  

E-Print Network [OSTI]

3.0 License. Biogeosciences Soil respiration at mean annualI. L. , and Carvalho, J. E. M. : Effects of soil watercontent on soil res- piration in forests and cattle pastures

2010-01-01T23:59:59.000Z

22

Experiment evidence on the temperature dependence of desiccation cracking behavior of clayey soils  

E-Print Network [OSTI]

induced by shrinkage also create weak zones in a soil body with reduced overall mechanical strength soils Chao-Sheng Tang1, 2 , Yu-Jun Cui2* , Anh-Minh Tang2 , Bin Shi1 , 1 School of Earth Sciences;2 Abstract: When drying a clayey soil, shrinkage and then cracking on soil surface occur due to water loss

Boyer, Edmond

23

Impact of Hillslope-Scale Organization of Topography, Soil Moisture, Soil Temperature, and Vegetation on Modeling Surface Microwave Radiation Emission  

E-Print Network [OSTI]

Microwave radiometry will emerge as an important tool for global remote sensing of near-surface soil moisture in the coming decade. In this modeling study, we find that hillslope-scale topography (tens of meters) influences ...

Flores, Alejandro N.

24

Novel Phytase from Pteris vittata Resistant to Arsenate, High Temperature, and Soil Deactivation  

E-Print Network [OSTI]

, Florida 32611, United States State Key Lab of Pollution Control and Resource Reuse, School Jason T. Lessl, Lena Q. Ma,*,, Bala Rathinasabapathi,§ and Charles Guy Soil and Water Science Department, § Horticultural Sciences, and Environmental Horticulture, University of Florida, Gainesville

Ma, Lena

25

Distribution of Soil Temperature Regimes and Climate Change in the Mojave Desert Region  

E-Print Network [OSTI]

precipitation, and water vapor on diurnal temperature range.Idaho, United States. Water Resour. Res. 37: 2843-2846.and J. Bouma. 1994. Modelling water and chemical fluxes as

Bai, Yanying

2009-01-01T23:59:59.000Z

26

Department of Crop and Soil Sciences PhD Graduate Research Assistantship: Soil Science/Soil Quality/Soil Physics  

E-Print Network [OSTI]

Department of Crop and Soil Sciences PhD Graduate Research Assistantship: Soil Science/Soil Quality/Soil Physics Position Summary: Plastic mulches are used in agriculture to conserve water, suppress weeds, and increase soil temperatures. However, plastic mulches need to be disposed off at the end

Flury, Markus

27

E-Print Network 3.0 - annual soil respiration Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Sciences and Ecology 4 Summary Soil respiration is controlled by soil temperature, soil water, fine roots, microbial activity, and soil physical and Summary: into the model; and...

28

In-situ vitrification of soil  

DOE Patents [OSTI]

A method of vitrifying soil at or below a soil surface location. Two or more conductive electrodes are inserted into the soil for heating of the soil mass between them to a temperature above its melting temperature. Materials in the soil, such as buried waste, can thereby be effectively immobilized.

Brouns, Richard A. (Kennewick, WA); Buelt, James L. (Richland, WA); Bonner, William F. (Richland, WA)

1983-01-01T23:59:59.000Z

29

Original article Soil CO2 efflux in a beech forest: dependence on soil  

E-Print Network [OSTI]

Original article Soil CO2 efflux in a beech forest: dependence on soil temperature and soil water 1998) Abstract - Our objective was to quantify the annual soil carbon efflux in a young beech forest in north-eastern France (Hesse Forest, Euroflux site FR02) from measurements of soil CO, efflux. Soil CO

Paris-Sud XI, Université de

30

Surface Soil  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Surface Soil Surface Soil We compare local soil samples with samples collected from northern New Mexico locations that are beyond the range of potential influence from normal...

31

Soil moisture and soil-litter mixing effects on surface litter decomposition: A controlled environment assessment  

E-Print Network [OSTI]

temperature and radiant energy levels and soil-litter mixing. Temperature and radiant energy effects on litterSoil moisture and soil-litter mixing effects on surface litter decomposition: A controlled University, Las Cruces, NM 88003, USA c Department of Plant and Soil Sciences, University of Kentucky

Archer, Steven R.

32

ARM - Measurement - Soil surface temperature  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May JunDatastreamsmmcrcalgovInstrumentsruc Documentation RUC : XDCResearch Relatedcontentcharacteristics ARM Data Discovery

33

KSInglett Page 1 MATH FOR SOIL SCIENTISTS  

E-Print Network [OSTI]

skills that are most relevant to graduate courses in environmental science including Soil and Water transport 9. Soil temperature, heat capacity and conductivity Unit 3 PROBLEM SOLVING IN SOIL BIOCHEMISTRY 10 and gas fluxes Unit 5 PROBLEM SOLVING IN SOIL CHEMISTRY, FERTILITY, and MANAGEMENT (optional) 19. p

Ma, Lena

34

Soil Profile CO2 concentrations in forested and clear cut sites in Nova Scotia, Canada  

E-Print Network [OSTI]

concentration; Forest management; Soil temperature; Soil moisture; Soil texture 1. Introduction Subsurface2 production and transport caused by the complex interactions between biotic and environmental content, and soil physical characteristics (transport factors) mainly determine the variability

Beltrami, Hugo

35

Soils Soil Series  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmosphericNuclear Security Administrationcontroller systemsBiSite CulturalDepartment ofat HomeAssurance: DOESoil0 Soils Soil

36

Soil moisture in complex terrain: quantifying effects on atmospheric boundary layer flow and providing improved surface boundary conditions for mesoscale models  

E-Print Network [OSTI]

74 ii Soil Moisture Sensors: Decagon ECH2O Capacitance133 A.10 Soil types corresponding to each75 Soil Moisture and Temperature Probe

Daniels, Megan Hanako

2010-01-01T23:59:59.000Z

37

Soil Quality Information Sheet Rangeland Soil Quality--Soil Biota  

E-Print Network [OSTI]

powerhouse of soil, include an incredible diversity of organisms. Tons of soil biota, including micro

38

Soil respiration in perennial grass and shrub ecosystems: Linking environmental controls with plant and microbial sources on seasonal and diel timescales  

E-Print Network [OSTI]

R. Vargas (2008), Automated soil respiration measure- ments:and J. M. Wraith (2007), Diurnal hysteresis between soil CO2 and soil temperature is controlled by soil water content,

Carbone, Mariah S; Winston, Gregory C; Trumbore, Susan E

2008-01-01T23:59:59.000Z

39

Managing Soil Salinity  

E-Print Network [OSTI]

This publication explains soil salinity, factors that contribute to it, and methods of correcting saline soils....

Provin, Tony; Pitt, John L.

2001-07-13T23:59:59.000Z

40

APBI 402 / SOIL 502 SUSTAINABLE SOIL MANAGEMENT  

E-Print Network [OSTI]

1 APBI 402 / SOIL 502 SUSTAINABLE SOIL MANAGEMENT TERM 1 - 2014/15 Lead Instructors*: Maja Krzic indicators to assess sustainability of land management practices. Characterize the soil chemical environment 402-Sustainable Soil Management SOIL 502-Advanced Sustainable Soil Management Final exam 35% Final

Farrell, Anthony P.

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


41

IMPORTED SOIL OR SOIL-FORMING MATERIALS  

E-Print Network [OSTI]

IMPORTED SOIL OR SOIL-FORMING MATERIALS PLACEMENT BPG NOTE 5 Best Practice Guidance for Land of heavy industry. Soil material initially present on a site may have been removed or stored in bunds the original soil that has been stored or importing a soil from elsewhere or using a soil-forming material

42

A mathematical model for variation in water-retention curves among sandy soils  

E-Print Network [OSTI]

activity in soil varies with water content, soil texture and structure, temperature, energy and nutrientA mathematical model for variation in water-retention curves among sandy soils H.W. HUNT1 *, A@nrel.colostate.edu Abstract: Equations were developed to predict soil matric potential as a function of soil water content

Wall, Diana

43

Representing the effects of alpine grassland vegetation cover on the simulation of soil thermal dynamics by ecosystem  

E-Print Network [OSTI]

hourly time steps, soil surface temperature is calculated by iteratively solving the energy balanceRepresenting the effects of alpine grassland vegetation cover on the simulation of soil thermal] Soil surface temperature is a critical boundary condition for the simulation of soil temperature

Ickert-Bond, Steffi

44

Soils and Environment Soil fertility and soil processes  

E-Print Network [OSTI]

be removed without blasting. Definition of soil #12; Land use planning, urbanization, timber management, landslides, and earthquakes Soils often carry a climatic signal Soil properties related to environmental soil. The fertile soils formed on glacial deposits in the mid-western United States are transported

Pan, Feifei

45

Soil Quality Information Sheet Rangeland Soil Quality--  

E-Print Network [OSTI]

Soil Quality Information Sheet Rangeland Soil Quality-- Physical and Biological Soil Crusts USDA, Natural Resources Conservation Service May 2001 Rangeland Sheet 7 What are soil crusts? A physical crust is a thin layer with reduced porosity and increased density at the surface of the soil. A biological crust

46

Spatial Variation of Soil Type and Soil Moisture in the Regional Atmospheric Modeling System  

SciTech Connect (OSTI)

Soil characteristics (texture and moisture) are typically assumed to be initially constant when performing simulations with the Regional Atmospheric Modeling System (RAMS). Soil texture is spatially homogeneous and time-independent, while soil moisture is often spatially homogeneous initially, but time-dependent. This report discusses the conversion of a global data set of Food and Agriculture Organization (FAO) soil types to RAMS soil texture and the subsequent modifications required in RAMS to ingest this information. Spatial variations in initial soil moisture obtained from the National Center for Environmental Predictions (NCEP) large-scale models are also introduced. Comparisons involving simulations over the southeastern United States for two different time periods, one during warmer, more humid summer conditions, and one during cooler, dryer winter conditions, reveals differences in surface conditions related to increases or decreases in near-surface atmospheric moisture con tent as a result of different soil properties. Three separate simulation types were considered. The base case assumed spatially homogeneous soil texture and initial soil moisture. The second case assumed variable soil texture and constant initial soil moisture, while the third case allowed for both variable soil texture and initial soil moisture. The simulation domain was further divided into four geographically distinct regions. It is concluded there is a more dramatic impact on thermodynamic variables (surface temperature and dewpoint) than on surface winds, and a more pronounced variability in results during the summer period. While no obvious trends in surface winds or dewpoint temperature were found relative to observations covering all regions and times, improvement in surface temperatures in most regions and time periods was generally seen with the incorporation of variable soil texture and initial soil moisture.

Buckley, R.

2001-06-27T23:59:59.000Z

47

Original article Effect of tillage on bare soil energy balance  

E-Print Network [OSTI]

Original article Effect of tillage on bare soil energy balance and thermal regime: an experimental; accepted 26 May 1998) Abstract - The effects of tillage on the energy balance and temperature of bare soil were studied using three plots that had different soil structures due to different times of seedbed

Paris-Sud XI, Université de

48

Soil Organic Carbon Degradation, Barrow, 2013-2014  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

This dataset provides information about soil organic carbon decomposition in Barrow soil incubation studies. The soil cores were collected from low-center polygon (Area A) and were incubated in the laboratory at different temperatures for up to 60 days. Transformations of soil organic carbon were characterized by UV and FT-IR, and small organic acids in water-soluble carbons were quantified by ion chromatography during the incubation

Baohua Gu; Ziming Yang

49

Water Transfer from Soil to the Atmosphere as Related to Climate and Soil Properties  

E-Print Network [OSTI]

Facilities and Systems - Design of the lysimetric facility of the project began in 1966. During 1967, soil cores were taken for the lysimeters, and in 1968 an unforseen temperature problem in the lysimeters was solved. A total of 9 undisturbed soil...

Wendt, C. W.

50

Soil Science Society of America Journal Soil Sci. Soc. Am. J. 76:17281740  

E-Print Network [OSTI]

. Temporal Variability of Nitrous Oxide from Fertilized Croplands: Hot Moment Analysis Soil&Water. Abrupt rises in both temperature and soil moisture appeared to trigger major hot moments, whereas high temporal variability. Measured N2O emissions from fertilized cropland fall within a wide range: 0

51

ORIGINAL ARTICLE Sensible and latent heat flux response to diurnal variation in soil  

E-Print Network [OSTI]

of the soil, but also the energy/water exchanges between the land surface and atmosphere (Li et al. 2002) dueORIGINAL ARTICLE Sensible and latent heat flux response to diurnal variation in soil surface temperature and moisture under different freeze/thaw soil conditions in the seasonal frozen soil region

52

ORIGINAL ARTICLE Sensible and latent heat flux response to diurnal variation in soil  

E-Print Network [OSTI]

condition of the soil, but also the energy/water exchanges between the land surface and atmosphere (Li et alORIGINAL ARTICLE Sensible and latent heat flux response to diurnal variation in soil surface temperature and moisture under different freeze/thaw soil conditions in the seasonal frozen soil region

53

Evaluation of the Hydro-Thermodynamic Soil Vegetation Scheme and implementation of a new numerical scheme  

E-Print Network [OSTI]

ii Evaluation of the Hydro-Thermodynamic Soil Vegetation Scheme and implementation of a new.S. Fairbanks, Alaska August 2005 #12;iii Abstract The Hydro-Thermodynamic Soil-Vegetation Scheme (HTSVS........................................................................................................................... 24 Evaluation of snow depth and soil temperatures predicted by the Hydro- Thermodynamic Soil

Moelders, Nicole

54

Soil Series  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmosphericNuclear Security Administrationcontroller systemsBiSite CulturalDepartment ofat HomeAssurance: DOE NSoftwareSoil0

55

Building Fertile Soil  

E-Print Network [OSTI]

A Backyard Guide to Healthy Soil and Higher Yields, by JohnInstitute. Start with the Soil, by Grace Gershuny. Emmaus,Institute. 1993. The Soul of Soil: A Guide to Ecological

Lindsey, Ann

2008-01-01T23:59:59.000Z

56

Rapid reconnaissance of geothermal prospects using shallow temperature...  

Open Energy Info (EERE)

Using a preliminary model and analysis of the Coso data, the importance of measuring soil thermal diffusivity data at each temperature probe site was shown. Corrected 2-m...

57

Using electrical resistance tomography to map subsurface temperatures  

DOE Patents [OSTI]

A method is provided for measuring subsurface soil or rock temperatures remotely using electrical resistivity tomography (ERT). Electrical resistivity measurements are made using electrodes implanted in boreholes driven into the soil and/or at the ground surface. The measurements are repeated as some process changes the temperatures of the soil mass/rock mass. Tomographs of electrical resistivity are calculated based on the measurements using Poisson's equation. Changes in the soil/rock resistivity can be related to changes in soil/rock temperatures when: (1) the electrical conductivity of the fluid trapped in the soil's pore space is low, (2) the soil/rock has a high cation exchange capacity and (3) the temperature changes are sufficiently high. When these three conditions exist the resistivity changes observed in the ERT tomographs can be directly attributed to changes in soil/rock temperatures. This method provides a way of mapping temperature changes in subsurface soils remotely. Distances over which the ERT method can be used to monitor changes in soil temperature range from tens to hundreds of meters from the electrode locations. 1 fig.

Ramirez, A.L.; Chesnut, D.A.; Daily, W.D.

1994-09-13T23:59:59.000Z

58

Using electrical resistance tomography to map subsurface temperatures  

DOE Patents [OSTI]

A method is provided for measuring subsurface soil or rock temperatures remotely using electrical resistivity tomography (ERT). Electrical resistivity measurements are made using electrodes implanted in boreholes driven into the soil and/or at the ground surface. The measurements are repeated as some process changes the temperatures of the soil mass/rock mass. Tomographs of electrical resistivity are calculated based on the measurements using Poisson's equation. Changes in the soil/rock resistivity can be related to changes in soil/rock temperatures when: (1) the electrical conductivity of the fluid trapped in the soil's pore space is low, (2) the soil/rock has a high cation exchange capacity and (3) the temperature changes are sufficiently high. When these three conditions exist the resistivity changes observed in the ERT tomographs can be directly attributed to changes in soil/rock temperatures. This method provides a way of mapping temperature changes in subsurface soils remotely. Distances over which the ERT method can be used to monitor changes in soil temperature range from tens to hundreds of meters from the electrode locations.

Ramirez, Abelardo L. (Pleasanton, CA); Chesnut, Dwayne A. (San Francisco, CA); Daily, William D. (Livermore, CA)

1994-01-01T23:59:59.000Z

59

Influence of soil physicochemical properties on hydrology and restoration response in Carolina Bay wetlands.  

SciTech Connect (OSTI)

Carolina Bays are shallow depression wetlands found in the southeast US that have been severely altered by human activity. The need to restore these complex and diverse systems is well established, but our understanding of basic wetland hydrological processes is limited, hence our ability to predict the need for and/or assess the effectiveness of bay restorations is hindered. Differing physicochemical properties of soils within bay interiors may control bay hydrology. However, previous efforts to establish relationships between soil characteristics and bay hydrology have been inconclusive and the question still remains as to why some bays are ponded throughout the year while others, within a similar landscape unit, are predominantly dry. An assessment of soil and hydrologic characteristics was initiated in restored and unrestored control bays to determine if a relationship exists. Soil morphology was described and permanent monitoring wells were installed at each site. Soil samples were collected by horizon to a depth of 2 meters at the topographic center of each site, and then analyzed. After three years, multiple regression analysis (stepwise backward and forward) was used to establish relationships between the soil physicochemical characteristics and bay hydroperiod in the undisturbed sites. Results from surface soils indicated that exchangeable acidity (EA) was the best single predictor of hydrology. The best double predictor was EA and total N and EA, total N and total C as the best triple predictor. A significant relationship (r2 = 0.96) between hydroperiod and clay content in the argillic horizon (Bt) was also observed. Subsequently, this relationship was utilized to predict hydrologic response using pre-restoration hydroperiod data. The model accurately identified sites that did not need hydrologic restoration (too wet), and effectively showed sites that responded well to restoration activities.

Barton, C. D.; Andrews, D.M.; Kolka, R.K.

2006-04-01T23:59:59.000Z

60

CROP & SOIL SCIENCES Soybean Breeding  

E-Print Network [OSTI]

CROP & SOIL SCIENCES Soybean Breeding Committee Membership Dr. Joseph Bouton - committee chair Dr. Brian Schwartz Department of Crop & Soil Sciences Department of Crop & Soil Sciences University & Soil Sciences Department of Crop & Soil Sciences University of Georgia University of Georgia Center

Arnold, Jonathan

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


61

CROP & SOIL SCIENCES Forage Breeding  

E-Print Network [OSTI]

CROP & SOIL SCIENCES Forage Breeding Committee Membership Dr. Joseph Bouton - committee chair Dr. Brian Schwartz Department of Crop & Soil Sciences Department of Crop & Soil Sciences University & Soil Sciences Department of Crop & Soil Sciences University of Georgia University of Georgia Center

Arnold, Jonathan

62

Environmental Soil Chemistry Second Edition Environmental Soil Chemistry illustrates fundamental principles of soil  

E-Print Network [OSTI]

Environmental Soil Chemistry Second Edition Environmental Soil Chemistry illustrates fundamental principles of soil chemistry with respect to environmental reactions between soils and other natural contemporary training in the basics of soil chemistry and applications to real-world environmental concerns

Sparks, Donald L.

63

Effects of soil solarization on yields of celery, pepper, onion, control of soil-borne pathogens, and chemical changes in the soil  

E-Print Network [OSTI]

of sublethal temperatures or a combination of thermal and biological control (36). In some of the same experiments, Fusarium spp. were also controlled by solarization (36, 67). Katan et al. (36) found that preheating the soil 45 to 50'C, allowing it to cool... (16) . Effective disease control is correlated with a corresponding reduction in inoculum density of pathogenic fungal propagules in solari zed soil (27, 32, 36, 71, 49, 3, 67, 22 ) . The reduction in inoculum density in solarized soil by thermal...

Avila, Francisco Antonio

1989-01-01T23:59:59.000Z

64

Soil Testing and Research  

E-Print Network [OSTI]

Soil Testing and Research Analytical Laboratory Copyright © 2014 University of Minnesota Soil Testing and Research Analytical Laboratory Department of Soil, Water and Climate College of Food payable to the University of Minnesota We also accept the following credit cards: Soil Testing

Ciocan-Fontanine, Ionut

65

Indiana Soil and Landscape  

E-Print Network [OSTI]

Indiana Soil and Landscape Evaluation Manual Version 1.0 D.P. Franzmeier G.C. Steinhardt D soil scientists to be the state soil. The scale on the gray panel is in decimeters and feet. The upper 18 inches (46 cm) of the soil formed in Wisconsinan age loess, and the lower part formed

Holland, Jeffrey

66

Rapid reconnaissance of geothermal prospects using shallow temperature...  

Open Energy Info (EERE)

using shallow temperature surveys. Semi-annual technical report Abstract Shallow (2-m) soil temperature data have been collected at 27 sites at Long Valley, California, and at 102...

67

american temperature record: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

temperature, pressure, cloud, humidity and wind. The calibrated soil temperature data recorded at 1 foot30 cm and 4 foot100 cm depth 125 Call for Papers NEW Graduate...

68

1.8.2001 31.12.2004 SOIL-FROST AND SNOW METAMORPHISM SIMULATIONS FOR THE BALTEX-  

E-Print Network [OSTI]

assimilation, 4DVAR, water and energy fluxes, BALTEX 1. Summary Modules to consider soil-frost and snow-metamorphism and the depth of snow regulate soil freezing with implications for soil hydraulic properties, energy, water in freezing or thawing and a release of latent heat or consumption of energy, again altering soil temperature

Moelders, Nicole

69

Homeowner Soil Sample Information Form  

E-Print Network [OSTI]

Homeowners should submit this form with their soil samples when requesting a soil test from the Texas A&M Soil Testing Laboratory....

Provin, Tony

2007-04-11T23:59:59.000Z

70

Responses of soil respiration to elevated CO2, air warming, and changing soil water availability in an old-field grassland  

SciTech Connect (OSTI)

Responses of soil respiration to atmospheric and climatic change will have profound impacts on ecosystem and global C cycling in the future. This study was conducted to examine effects on soil respiration of the concurrent driving factors of elevated atmospheric CO2 concentration, rising temperature, and changing precipitation in a constructed old-field grassland in eastern Tennessee, USA. Model ecosystems of seven old-field species in 12 open-top chambers (4 m in diameter) were treated with two CO2 (ambient and ambient plus 300 ppm) and two temperature (ambient and ambient plus 3 C) levels. Two split plots with each chamber were assigned with high and low soil moisture levels. During the 19-month experimental period from June 2003 to December 2004, higher CO2 concentration and soil water availability significantly increased mean soil respiration by 35.8% and 15.7%, respectively. The effects of air warming on soil respiration varied seasonally from small reductions to significant increases to no response, and there was no significant main effect. In the wet side of elevated CO2 chambers, air warming consistently caused increases in soil respiration, whereas in other three combinations of CO2 and water treatments, warming tended to decrease soil respiration over the growing season but increase it over the winter. There were no interactive effects on soil respiration among any two or three treatment factors irrespective of testing time period. Temperature sensitivity of soil respiration was reduced by air warming, lower in the wet than the dry side, and not affected by CO2 treatment. Variations of soil respiration responses with soil temperature and soil moisture ranges could be primarily attributable to the seasonal dynamics of plant growth and its responses to the three treatments. Using a conceptual model to interpret the significant relationships of treatment-induced changes in soil respiration with changes in soil temperature and moisture observed in this study, we conclude that elevated CO2, air warming, and changing soil water availability had both direct and indirect effects on soil respiration via changes in the three controlling factors: soil temperature, soil moisture, and C substrate. Our results demonstrate that the response of soil respiration to climatic warming should not be represented in models as a simple temperature response function. A more mechanistic understanding of the direct and indirect impacts of concurrent global change drivers on soil respiration is needed to facilitate the interpretation and projection of ecosystem and global C cycling in response to atmospheric and climate change.

Wan, Shiqiang [Chinese Academy of Sciences; Norby, Richard J [ORNL; Childs, Joanne [ORNL; Weltzin, Jake [University of Tennessee, Knoxville (UTK)

2007-01-01T23:59:59.000Z

71

Soil Test P vs. Total P in Wisconsin Soils  

E-Print Network [OSTI]

Soil Test P vs. Total P in Wisconsin Soils Larry G. Bundy & Laura W. Good Department of Soil Science University of Wisconsin-Madison #12;Introduction · Soil test P is often measured · Little information is available on total P content of soils · Why do we care about total P now? ­ Soil total P

Balser, Teri C.

72

Extractable soil phosphorus in Blackland Prairie soils  

E-Print Network [OSTI]

The Texas Agricultural Extension Service (TAEX) Soil Testing Laboratory currently utilizes a single phosphorus (P) extractant consisting of 1.43 M NH4OAc, 1. 0 M HCl, and 0.025 M EDTA-PH 4.2 to estimate plant available P for all soils in Texas...

Byrd, Robert Claude

2012-06-07T23:59:59.000Z

73

Nitrification in Texas Soils.  

E-Print Network [OSTI]

have a high nitrificati is the balmcing of these extremes which redlices the average le between acid ancl non-acid soils. C03TPOSITION OF SOILS TVITFI LOW AND HIGH NITRIFIC-4TION. Table 11 contains the chemical composition of soils having low nitl... are subsoils. Subsoils thus possess nnu~nally high and unusually low nitrification. Table 11.-Chemical composition of soils with nitrification below 10 . I Average .............................. Nitri- fication 7164 7090 4596' 5710 4645 3976 3657 3...

Fraps, G. S. (George Stronach)

1920-01-01T23:59:59.000Z

74

Overview of different aspects of climate change effects on soils.  

SciTech Connect (OSTI)

Climate change [i.e., high atmospheric carbon dioxide (CO2) concentrations (?400 ppm); increasing air temperatures (2-4°C or greater); significant and/or abrupt changes in daily, seasonal, and inter-annual temperature; changes in the wet/dry cycles; intensive rainfall and/or heavy storms; extended periods of drought; extreme frost; heat waves and increased fire frequency] is and will significantly affect soil properties and fertility, water resources, food quantity and quality, and environmental quality. Biotic processes that consume atmospheric CO2 and create organic carbon (C) that is either reprocessed to CO2 or stored in soils, are the subject of active current investigations with great concern over the influence of climate change. In addition, abiotic C cycling and its influence on the inorganic C pool in soils is a fundamental global process in which acidic atmospheric CO2 participates in the weathering of carbonate and silicate minerals, ultimately delivering bicarbonate and Ca2+ or other cations that precipitate in the form of carbonates in soils or are transported to the rivers, lakes, and oceans. Soil responses to climate change will be complex, and there are many uncertainties and unresolved issues. The objective of the review is to initiate and further stimulate a discussion about some important and challenging aspects of climate-change effects on soils, such as accelerated weathering of soil minerals and resulting C and elemental fluxes in and out of soils, soil/geo-engineering methods used to increase C sequestration in soils, soil organic matter (SOM) protection, transformation and mineralization, and SOM temperature sensitivity. This review reports recent discoveries and identifies key research needs required to understand the effects of climate change on soils.

Qafoku, Nikolla

2014-08-01T23:59:59.000Z

75

UNSATURATED SOIL MECHANICS IMPLEMENTATION  

E-Print Network [OSTI]

UNSATURATED SOIL MECHANICS IMPLEMENTATION DURING PAVEMENT CONSTRUCTION QUALITY ASSURANCE Mn !! Performance Based Construction QA !! Unsaturated Soil Mechanics !! What We've Learned !! Next Steps #12.6-6.0 5 - 7 19 0.8 5 7 - 9 24 1.1 4 9 - 11 28 1.2 4 #12;Unsaturated Soil Mechanics #12;Fundamentals

Minnesota, University of

76

Experimental unsaturated soil mechanics  

E-Print Network [OSTI]

In this general report, experimental systems and procedures of investigating the hydro-mechanical behaviour of unsaturated soils are presented. The water retention properties of unsaturated soils are commented and linked to various physical parameters and properties of the soils. Techniques of controlling suction are described together with their adaptation in various laboratory testing devices. Some typical features of the mechanical behaviour of unsaturated soils are presented within an elasto-plastic framework. An attempt to describe the numerous and significant recent advances in the investigation of the behaviour of unsaturated soils, including the contributions to this Conference, is proposed.

Delage, Pierre

2008-01-01T23:59:59.000Z

77

Pressure &Pressure & TemperatureTemperature  

E-Print Network [OSTI]

to measure atmospheric pressure, and thermometer toprobe to measure atmospheric pressure, and thermometer toprobe to measure atmospheric pressure, and thermometer toprobe to measure atmospheric pressure, and thermometer to measure air temperature.measure air temperature.measure air temperature.measure air temperature

California at Santa Cruz, University of

78

Soil Quality Information Sheet Rangeland Soil Quality--Introduction  

E-Print Network [OSTI]

Soil Quality Information Sheet Rangeland Soil Quality--Introduction USDA, Natural Resources of the soil, the vegetation, the water, and the air as well as the ecological processes of the rangeland ecosystem are balanced and sustained. What is soil? Soil is a dynamic resource that supports plants

79

Soil Horizons Some Noteworthy Soil Science in Wisconsin  

E-Print Network [OSTI]

Soil Horizons Some Noteworthy Soil Science in Wisconsin Alfred E. Hartemink The impact and benefits of soil science have only partly been documented. Here I highlight four noteworthy soil science achievements from the state of Wisconsin that took place between 1870 and the early 1980s: (i) the first soil

Mladenoff, David

80

SOIL TEST INTERPRETATIONS RECOMMENDATIONS HANDBOOK  

E-Print Network [OSTI]

1 SOIL TEST INTERPRETATIONS AND RECOMMENDATIONS HANDBOOK Originally written 1983 By Daryl D..................................................20 SOIL ACIDITY AND LIMESTONE...............................................27 EXCHANGEABLE MAGNESIUM No. Page No. I. Nitrogen rate adjustments based upon soil texture, organic matter, and time of major

Noble, James S.

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


81

Soil and Water Conservation (Virginia)  

Broader source: Energy.gov [DOE]

Soil and water conservation districts (SWCDs) were established in the 1930s to develop comprehensive programs and plans to conserve soil resources, control and prevent soil erosion, prevent floods...

82

Soil and Water Conservation (Texas)  

Broader source: Energy.gov [DOE]

The Texas State Soil and Water Conservation Board is established to encourage and oversee soil-conserving land-use practices, and to provide for the conservation of soil and related resources and...

83

Soil metagenomics and carbon cycling  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Soil metagenomics and carbon cycling Soil metagenomics and carbon cycling Establishing a foundational understanding of the microbial and ecosystem factors that control carbon...

84

Soil and Water Conservation (Indiana)  

Broader source: Energy.gov [DOE]

The Indiana Association of Soil and Water Conservation Districts is an association of the 92 soil and water conservation districts, each representing one of the 92 Indiana counties.

85

Soil Conservation Districts Law (Iowa)  

Broader source: Energy.gov [DOE]

This legislation establishes a soil and water conservation division within the Iowa Department of Agriculture, as well as local soil and water conservation districts. The regulations accompanying...

86

On-Farm Soil Monitoring for Water  

E-Print Network [OSTI]

. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11 Soil quality and soil management resources the air which helps build soil organic matter and tilth, and sustains the soil resource for future generations and other species. Improving and protecting soil quality can help support sustainable crop

Holland, Jeffrey

87

In situ formation of phosphate barriers in soil  

DOE Patents [OSTI]

Reactive barriers and methods for making reactive barriers in situ in soil for sequestering soil ontaminants including actinides and heavy metals. The barrier includes phosphate, and techniques are disclosed for forming specifically apatite barriers. The method includes injecting dilute reagents into soil in proximity to a contamination plume or source such as a waste drum to achieve complete or partial encapsulation of the waste. Controlled temperature and pH facilitates rapid formation of apatite, for example, where dilute aqueous calcium chloride and dilute aqueous sodium phosphate are the selected reagents. Mixing of reagents to form precipitate is mediated and enhanced through movement of reagents in soil as a result of phenomena including capillary action, movement of groundwater, soil washing and reagent injection pressure.

Moore, Robert C. (Edgewood, NM)

2002-01-01T23:59:59.000Z

88

Temperature System  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmosphericNuclear Security AdministrationcontrollerNanocrystallineForeignTechnology-Selection-Process SignL.Ted Donat1 Soil Water

89

Soil Quality Information Sheet Rangeland Soil Quality--  

E-Print Network [OSTI]

roots, rills, gullies, wind scours, and soil deposition reflect such processes as runoff and erosion. Waterflow patterns X X 3. Pedestals and/or terracettes X X 4. Bare ground X X 5. Gullies X X 6. Wind. Compaction layer X X X 12. Functional/structural groups X 13. Plant mortality/ decadence X 14. Litter amount

90

Soils in the Riparian Incorporating Soil Dynamics into  

E-Print Network [OSTI]

deposits or upland slope wash · Soil particle size reflect the energy (velocity) of depositionalSoils in the Riparian Complex Incorporating Soil Dynamics into Ecological Site Descriptions Kenneth F. Scheffe, SSS August 16, 2007 #12;Water Changes Everything · Water is the trump card over soils

91

Soil Quality Information Sheet Rangeland Soil Quality--Compaction  

E-Print Network [OSTI]

Soil Quality Information Sheet Rangeland Soil Quality--Compaction USDA, Natural Resources Conservation Service May 2001 Rangeland Sheet 4 What is compaction? Soil compaction occurs when moist or wet soil aggregates are pressed together and the pore space between them is reduced. Compaction changes

92

Soil Quality Information Sheet Rangeland Soil Quality--Wind Erosion  

E-Print Network [OSTI]

Soil Quality Information Sheet Rangeland Soil Quality--Wind Erosion USDA, Natural Resources of the earth's surface by wind. Wind erosion removes and redistributes soil. Small blowout areas may, fence rows, and roadbanks. In many cases the fine soil particles and organic matter are blown offsite

93

Soil Quality Information Sheet Rangeland Soil Quality--Water Erosion  

E-Print Network [OSTI]

Soil Quality Information Sheet Rangeland Soil Quality--Water Erosion USDA, Natural Resources and removal of soil material by water. The process may be natural or accelerated by human activity. The rate of erosion may be very slow to very rapid, depending on the soil, the local landscape, and weather conditions

94

Beth Brockett SOIL 502 Soil Quality Analysis -Chemistry Case Study  

E-Print Network [OSTI]

Beth Brockett SOIL 502 Soil Quality Analysis - Chemistry Case Study "Sustainability Street are represented by the Podzolic Order, and more specifically form part of the Bose Soil Management Group) with a limited decomposer community dominated by fungi. Any remnants of native soil at the Sustainability Street

95

CROP & SOIL SCIENCES Irrigation Specialist  

E-Print Network [OSTI]

CROP & SOIL SCIENCES Irrigation Specialist Committee Membership Dr. John Beasley - committee chair Dr. Jared Whitaker Department of Crop & Soil Sciences Department of Crop & Soil Sciences University: (229) 386-7308 Fax: (912) 681-0376 Dr. Robert Carrow Dr. Mark Risse Department of Crop & Soil Sciences

Arnold, Jonathan

96

Digital Soil Mapping: Interactions with  

E-Print Network [OSTI]

Chapter 21 Digital Soil Mapping: Interactions with and Applications for Hydropedology J.A. Thompson,1, * S. Roecker,2 S. Grunwald3 and P.R. Owens4 ABSTRACT Spatial information on soils, particularly hydrologic and hydromorphic soil properties, is used to understand and assess soil water retention, flooding

Grunwald, Sabine

97

CROP & SOIL SCIENCES Quantitative Genomics  

E-Print Network [OSTI]

CROP & SOIL SCIENCES Quantitative Genomics Committee Membership Dr. Scott Jackson - committee chair Dr. Peng-Wah Chee Department of Crop & Soil Sciences Department of Crop & Soil Sciences University of Horticulture Department of Crop & Soil Sciences University of Georgia University of Georgia 2360 Rainwater Rd

Arnold, Jonathan

98

Husnjak et al., 2004. Soil inventory and soil classification in Croatia ISRIC World Soil Information Country Series  

E-Print Network [OSTI]

Husnjak et al., 2004. Soil inventory and soil classification in Croatia Page 1 ISRIC World Soil Information Country Series Soil inventory and soil classification in Croatia: historical review, current classification in Croatia Page 2 Summary An historical overview of soil survey and soil classification activities

Rossiter, D G "David"

99

Tree Fertilization Soil Analysis  

E-Print Network [OSTI]

, increase root density, maintain tree health #12;#12;pH ­ effects nutrient availability · Symptoms of high pHTree Fertilization #12;Soil Analysis vs. Foliar Analysis #12;Macronutrients N P K Mg S Ca

100

Soil Erosion (Minnesota)  

Broader source: Energy.gov [DOE]

The Board of Water and Soil Resources has adopted a model ordinance to serve as the minimum standard for local governments, which are asked to implement standards and administrative procedures...

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


101

Automated soil gas monitoring chamber  

DOE Patents [OSTI]

A chamber for trapping soil gases as they evolve from the soil without disturbance to the soil and to the natural microclimate within the chamber has been invented. The chamber opens between measurements and therefore does not alter the metabolic processes that influence soil gas efflux rates. A multiple chamber system provides for repetitive multi-point sampling, undisturbed metabolic soil processes between sampling, and an essentially airtight sampling chamber operating at ambient pressure.

Edwards, Nelson T.; Riggs, Jeffery S.

2003-07-29T23:59:59.000Z

102

Saving our soils  

E-Print Network [OSTI]

when we consider how important the world’s soils are to human civilization. Within the next several decades, about 9–10 billion people will increasingly require food, timber, fiber, and bioenergy, as well as related ecosystem ser- vices... producers, motivated by short-term finances, increase inputs of fertilizers and pesticides to maximize yields, frequently with adverse environmental impacts. Subsistence farmers coax decreasing crop yields from soils that can no longer be managed sustainably...

Grandy, A. Stuart; Billings, Sharon A.; Richter Dan

2010-05-01T23:59:59.000Z

103

Soil Biology & Biochemistry 38 (2006) 22922299 Modifications of degradation-resistant soil organic matter by soil  

E-Print Network [OSTI]

Soil Biology & Biochemistry 38 (2006) 2292­2299 Modifications of degradation-resistant soil organic matter by soil saprobic microfungi Veronika R eza´ c ova´ a,b,Ă, Hana Hrs elova´ a , Hana Gryndlerova in their solutions and in sterile soil by microfungal species and two well-known HA degraders were studied

Miksik, Ivan

2006-01-01T23:59:59.000Z

104

Crop and Soil Science Degree Checklist Name: ____________________________  

E-Print Network [OSTI]

and Soil Science Degree Checklist Name: ____________________________ ID Intensive (SOIL 325) (3) _______ HHS 231 ­ Lifetime Fitness for Health (2. Global Issues (3) (*soil science electives meeting requirement) _______ Science

Grünwald, Niklaus J.

105

Jennifer Learned, Dana Nakase, Enrique Vivoni, and Sharon J . Hall. Arizona State University, PO Box 874501, Tempe AZ 85287-4501. Background: Plant growth in arid ecosystems is water limited. Soil water  

E-Print Network [OSTI]

Box 874501, Tempe AZ 85287-4501. Background: Plant growth in arid ecosystems is water limited. Soil and temperature sensors were installed at 7 cm. · Atmospheric temperature & humidity sensors were deployed in the soil box via sensors. · Simulations in Hydrus 2D were run to match soil box experiments. · Model output

Hall, Sharon J.

106

Remote Sensing of Soils, Minerals, and Geomorphology  

E-Print Network [OSTI]

,Remote Sensing of Soils, Minerals, and GeomorphologyMinerals, and Geomorphology · Soil is unconsolidated material). ·· SoilSoil is unconsolidated material at the surface of the Earth thatis unconsolidated material

107

1 INTRODUCTION Researches in unsaturated soil mechanics  

E-Print Network [OSTI]

1 INTRODUCTION Researches in unsaturated soil mechanics considerably developed in the past decades exchanges during shearing were also monitored, and Experimental unsaturated soil mechanics Pierre Delage- mechanical behaviour of unsaturated soils are presented. The water retention properties of unsaturated soils

Paris-Sud XI, Université de

108

soils.ifas.ufl.edu Soil & Water Science Department  

E-Print Network [OSTI]

interested in courses that emphasize sustainability, resource management, valuation of ecosystem servicessoils.ifas.ufl.edu UF/IFAS Soil & Water Science Department DISTANCE EDUCATION GRADUATE PROGRAMS #12;SOIL AND WATER SCIENCE DEPARTMENT The Soil and Water Science Department at the University of Florida

Watson, Craig A.

109

Plasma treatment of INEL soil contaminated with heavy metals  

SciTech Connect (OSTI)

INEL soil spiked with inorganic salts of chromium, lead, mercury, silver, and zinc was melted in a 150 kW plasma furnace to produce a glassy slag product. This glassy slag is an environmentally safe waste form. In order to reduce the melting temperature of the soil, sodium carbonate was added to half of the test batches. Random sample from each batch of glassy slag product were analyzed by an independent laboratory for total metals concentration and leachability of metals via the Environmental Protection Agency (EPA) toxicity characterization leaching procedure (RCLP) tests. These tests showed the residual metals were very tightly bound to the slag matrix and were within EPA TCLP limits under these test conditions. Additionally, scanning electron microscopy (SEM) and emissions dispersive spectroscopy (EDS) analysis of the vitrified soil also confirmed that the added metals present in the vitrified soil were totally contained in the crystalline phase as distinct oxide crystallites.

Detering, B.A.; Batdorf, J.A.

1992-01-01T23:59:59.000Z

110

POST OAK SAVANNA IN TRANSITION: JUNIPER ENCROACHMENT AND CLIMATE CHANGE ALTER GRASSLAND SOIL RESPIRATION  

E-Print Network [OSTI]

The amount of carbon flux from soils on a global scale is estimated at over 75 x 1015 g C yr-1. Climate change is projected to affect regional environmental conditions, raising temperatures and altering precipitation patterns. The semi...

Thompson, Bennie

2011-08-08T23:59:59.000Z

111

Identifying soils with potential of expanding sulfate mineral formation using electromagnetic induction  

E-Print Network [OSTI]

, moisture, salinity, and temperature (Doerge et al., 2003). Soil properties such as cation exchange capacity, solum depth and pore continuity may also be extrapolated from apparent EC measurements. Currently, the two most popular commercial instruments...

Fox, Miranda Lynn

2004-11-15T23:59:59.000Z

112

Soil and Water Conservation (Florida)  

Broader source: Energy.gov [DOE]

Florida’s 62 Soil and Water Conservation Districts were established in 1937 under Chapter 582 Florida Statutes. The law was based on federal model legislation to establish Soil and Water...

113

Residential construction on expansive soils  

E-Print Network [OSTI]

Residences founded on expansive soils experience billions of dollars each year in damage caused by the heaving and shrinking of the foundation soils. It is thought that stiffening the foundation, while increasing the cost of the home, will save...

Phipps, James Frederick

1993-01-01T23:59:59.000Z

114

Miamisburg Environmental Management Project Archived Soil & Groundwate...  

Office of Environmental Management (EM)

Miamisburg Environmental Management Project Archived Soil & Groundwater Master Reports Miamisburg Environmental Management Project Archived Soil & Groundwater Master Reports...

115

Fernald Environmental Management Project Archived Soil & Groundwater...  

Office of Environmental Management (EM)

Fernald Environmental Management Project Archived Soil & Groundwater Master Reports Fernald Environmental Management Project Archived Soil & Groundwater Master Reports Fernald...

116

Intergrating Magnetotellurics, Soil Gas Geochemistry and Structural...  

Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

Intergrating Magnetotellurics, Soil Gas Geochemistry and Structural Analysis to Identify Hidden, High Enthalpy, Extensional Geothermal Systems Intergrating Magnetotellurics, Soil...

117

Review and model-based analysis of factors influencing soil carbon sequestration beneath switchgrass (Panicum virgatum)  

SciTech Connect (OSTI)

Abstract. A simple, multi-compartment model was developed to predict soil carbon sequestration beneath switchgrass (Panicum virgatum) plantations in the southeastern United States. Soil carbon sequestration is an important component of sustainable switchgrass production for bioenergy because soil organic matter promotes water retention, nutrient supply, and soil properties that minimize erosion. A literature review was included for the purpose of model parameterization and five model-based experiments were conducted to predict how changes in environment (temperature) or crop management (cultivar, fertilization, and harvest efficiency) might affect soil carbon storage and nitrogen losses. Predictions of soil carbon sequestration were most sensitive to changes in annual biomass production, the ratio of belowground to aboveground biomass production, and temperature. Predictions of ecosystem nitrogen loss were most sensitive to changes in annual biomass production, the soil C/N ratio, and nitrogen remobilization efficiency (i.e., nitrogen cycling within the plant). Model-based experiments indicated that 1) soil carbon sequestration can be highly site specific depending on initial soil carbon stocks, temperature, and the amount of annual nitrogen fertilization, 2) response curves describing switchgrass yield as a function of annual nitrogen fertilization were important to model predictions, 3) plant improvements leading to greater belowground partitioning of biomass could increase soil carbon sequestration, 4) improvements in harvest efficiency have no indicated effects on soil carbon and nitrogen, but improve cumulative biomass yield, and 5) plant improvements that reduce organic matter decomposition rates could also increase soil carbon sequestration, even though the latter may not be consistent with desired improvements in plant tissue chemistry to maximize yields of cellulosic ethanol.

Garten Jr, Charles T [ORNL

2012-01-01T23:59:59.000Z

118

Beamline Temperatures  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr MayAtmospheric Optical Depth (AOD)ProductssondeadjustsondeadjustAboutScience ProgramBackground8.0.1 PrintTemperatures Energy: 3.0000 GeV

119

GUIDE TO GRADUATE SOIL SCIENCE  

E-Print Network [OSTI]

GUIDE TO GRADUATE PROGRAMS in AGRONOMY and SOIL SCIENCE Updated July 2011 THE DEPARTMENT OF CROP AND SOIL SCIENCES THE PENNSYLVANIA STATE UNIVERSITY UNIVERSITY PARK, PA #12;iiii Guide to Graduate Programs in Agronomy and Soil Science Table of Contents Introduction

Guiltinan, Mark

120

5, 95145, 2008 Soil parameter  

E-Print Network [OSTI]

tools to sim- ulate mass and energy fluxes within the soil vegetation atmosphere continuum for nu, linking the water and energy fluxes at the land surface. An appropriate parameterisation of soil hydraulicHESSD 5, 95­145, 2008 Soil parameter inversion ­ potential and limits A. Loew and W. Mauser Title

Paris-Sud XI, Université de

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


121

LUNAR SOIL SIMULATION TRAFFICABILITY PARAMETERS  

E-Print Network [OSTI]

LUNAR SOIL SIMULATION and TRAFFICABILITY PARAMETERS by W. David Carrier, III Lunar Geotechnical.0 RECOMMENDED LUNAR SOIL TRAFFICABILITY PARAMETERS Table 9.14 in the Lunar Sourcebook (Carrier et al. 1991, p. 529) lists the current recommended lunar soil trafficability parameters: bc = 0.017 N/cm2 bN = 35° K

Rathbun, Julie A.

122

Soil Remediation Test  

SciTech Connect (OSTI)

Soils contaminated with petroleum by-products can now be effectively remediated using a variety of technologies. Among these are in-situ bioremediation, land farming, and landfill/replacing of soil. The range of efficiencies and cost effectiveness of these technologies has been well documented. Exsorbet Plus is showing promise as an in-situ bioremediation agent. It is made of naturally grown Spaghnum Peat Moss which has been activated for encapsulation and blended with nitrogen-rich fertilizer. In its initial field test in Caracas, Venezuela, it was able to remediate crude oil-contaminated soil in 90 days at less than half of the cost of competing technologies. Waste Solutions, Corp and the US Department of Energy signed a Cooperative Research and Development Agreement to test Exsorbet Plus at the Rocky Mountain Oilfield Testing Center near Casper, Wyoming. As part of the test, soil contaminated with crude oil was treated with Exsorbet Plus to aid the in-situ bioremediation process. Quantitative total petroleum hydrocarbon (TPH) measurements were acquired comparing the performance of Exsorbet Plus with an adjacent plot undergoing unaided in-situ bioremediation.

Manlapig, D. M.; Williamsws

2002-04-01T23:59:59.000Z

123

Demonstration testing and evaluation of in situ soil heating. Revision 1, Demonstration system design  

SciTech Connect (OSTI)

Over the last nine years IIT Research Institute (IITRI) has been developing and testing the in situ heating and soil decontamination process for the remediation of soils containing hazardous organic contaminants. In this process the soil is heated in situ using electrical energy. The contaminants are removed from the soil due to enhanced vaporization, steam distillation and stripping. The vaporized contaminants, water vapor and air are recovered from the heated zone by means of a vacuum manifold system which collects gases from below surface as well as from the soil surface. A vapor barrier is used to prevent fugitive emissions of the contaminants and to control air infiltration to minimize dilution of the contaminant gases and vapors. The recovered gases and vapors are conveyed to an on site vapor treatment system for the clean up of the vent gases. Electrical energy is applied to the soil by forming an array of electrodes in the soil which are electrically interconnected and supplied with power. The electrodes are placed in drilled bore holes which are made through the contaminated zone. There are two versions of the in situ heating and soil treatment process: the f irst version is called the In Situ Radio Frequency (RF) Soil Decontamination Process and the second version is called the In Situ Electromagnetic (EM) Soil Decontamination Process. The first version, the RF Process is capable of heating the soil in a temperature range of 100{degrees} to 400{degrees}C. The soil temperature in the second version, the EM Process, is limited to the boiling point of water under native conditions. Thus the soil will be heated to a temperature of about 85{degrees} to 95{degrees}C. In this project IITRI will demonstrate the EM Process for in situ soil decontamination at K-25 Site due to the fact that most of the contaminants of concern are volatile organics which can be removed by heating the soil to a temperature range of 85{degrees} to 95{degrees}C.

Dev, H.

1994-08-16T23:59:59.000Z

124

Pneumatic soil removal tool  

DOE Patents [OSTI]

A soil removal tool is provided for removing radioactive soil, rock and other debris from the bottom of an excavation, while permitting the operator to be located outside of a containment for that excavation. The tool includes a fixed jaw, secured to one end of an elongate pipe, which cooperates with a movable jaw pivotably mounted on the pipe. Movement of the movable jaw is controlled by a pneumatic cylinder mounted on the pipe. The actuator rod of the pneumatic cylinder is connected to a collar which is slidably mounted on the pipe and forms part of the pivotable mounting assembly for the movable jaw. Air is supplied to the pneumatic cylinder through a handle connected to the pipe, under the control of an actuator valve mounted on the handle, to provide movement of the movable jaw. 3 figs.

Neuhaus, J.E.

1992-10-13T23:59:59.000Z

125

Pneumatic soil removal tool  

DOE Patents [OSTI]

A soil removal tool is provided for removing radioactive soil, rock and other debris from the bottom of an excavation, while permitting the operator to be located outside of a containment for that excavation. The tool includes a fixed jaw, secured to one end of an elongate pipe, which cooperates with a movable jaw pivotably mounted on the pipe. Movement of the movable jaw is controlled by a pneumatic cylinder mounted on the pipe. The actuator rod of the pneumatic cylinder is connected to a collar which is slidably mounted on the pipe and forms part of the pivotable mounting assembly for the movable jaw. Air is supplied to the pneumatic cylinder through a handle connected to the pipe, under the control of an actuator valve mounted on the handle, to provide movement of the movable jaw.

Neuhaus, John E. (Newport News, VA)

1992-01-01T23:59:59.000Z

126

Effects of soil moisture on the responses of soil temperatures to climate change in cold regions  

E-Print Network [OSTI]

and the Commu- nity Earth System Model 1 (CESM1) (http://poorly simulated by current earth system models. A number of

Subin, Z.M.

2014-01-01T23:59:59.000Z

127

Procedures to predict vertical differential soil movement for expansive soils  

E-Print Network [OSTI]

OF TABLES Table Page 1. Soil profile considered in all sample calculations, 2. Gardner's coefficient. 3. Measured suction profile values. 4. Summary of vertical differential soil movements for Appendix C. . . . 50 . . . 54 70 . . . . 74 LIST... OF FIGURES Figure 1. United States map of expansive soils after Wiggins. 2. Center lift distortion mode Page 3. Edge lift distortion mode. 4. The structure of kaolinite (a) atomic structure (b) symbolic structure. . . 5. The structure of serpentine (a...

Naiser, Donald David

1997-01-01T23:59:59.000Z

128

High Temperatures & Electricity Demand  

E-Print Network [OSTI]

High Temperatures & Electricity Demand An Assessment of Supply Adequacy in California Trends.......................................................................................................1 HIGH TEMPERATURES AND ELECTRICITY DEMAND.....................................................................................................................7 SECTION I: HIGH TEMPERATURES AND ELECTRICITY DEMAND ..........................9 BACKGROUND

129

Compacted Soil Liner Interface Strength Importance  

E-Print Network [OSTI]

Case Study Compacted Soil Liner Interface Strength Importance Timothy D. Stark, F.ASCE1 ; Hangseok interface is not the geomembrane (GM)/compacted low-permeability soil liner (LPSL) but a soil­soil interface placing the cover soil from bottom to top. DOI: 10.1061/(ASCE)GT.1943-5606 .0000556. © 2012 American

130

CROP & SOIL SCIENCES Water Policy and Management  

E-Print Network [OSTI]

CROP & SOIL SCIENCES Water Policy and Management Committee Membership Dr. David Radcliffe - committee chair Dr. George Vellidis Department of Crop & Soil Sciences Department of Crop & Soil Sciences & Soil Sciences Department of Crop & Soil Sciences University of Georgia University of Georgia Stripling

Arnold, Jonathan

131

Occurrence of Nitrites in Soils.  

E-Print Network [OSTI]

capacity for producing nitrates may form large amounts of nitrites. Nitrites may persist in the soil or in soil extracts for several weeks. Magnesium carbonate and calcium car- bonate may favor the formation of nitrites. Water equivaIent to 50 per cent... ............................................. Method of work 5 Nitrites in soils without additions of nitrogenous materials ........ 6 Nitrification capacity as measured by nitric nitrogen alone. and by nitric and nitrous nitrogen combined ....................... 6...

Fraps, G. S. (George Stronach); Sterges, A. J.

1930-01-01T23:59:59.000Z

132

The Basicity of Texas Soils.  

E-Print Network [OSTI]

chemical prob- lems connected with the investigations of cotton root rot being made by the Division of Plant Pathology and Physiology. Lab- oratory methods were needed for estimating the amounts of acid or sulphur required to bring experimental soils... approxi- mately to a desired degree of acidity. Information was needed regarding the amounts of acid or sulphur required to make acid various kinds of soil. This Bulletin discusses the basicity of Texas soils, and the amounts of acid or sulphur...

Fraps, G. S. (George Stronach); Carlyle, E. C. (Elmer Cardinal)

1929-01-01T23:59:59.000Z

133

Soil structure interaction for shrink-swell soils a new design procedure for foundation slabs on shrink-swell soils  

E-Print Network [OSTI]

diffusion soil volume change model starts with proposing a new laboratory test to determine the coefficient of unsaturated diffusivity for intact soils. Then, it introduces the development of a cracked soil diffusion factor, provides a chart for it...

Abdelmalak, Remon Melek

2009-05-15T23:59:59.000Z

134

Plant and Soil VIII, no. 3 March 1957 PROBLEMS OF SOIL TESTING  

E-Print Network [OSTI]

Plant and Soil VIII, no. 3 March 1957 PROBLEMS OF SOIL TESTING ON CALCAREOUS SOILS by DAN H. YAALON The Hebrew University of Jerusalem, Israel Chemically and mineralogically the soils of arid and semiarid of limestone, most of the soils are calcareous. Extensive leaching may have removed the CaCO3 from the soil

Ahmad, Sajjad

135

Soil Tillage Influences on Soil Mineral Nitrogen and Nitrate Leaching in  

E-Print Network [OSTI]

Soil Tillage Influences on Soil Mineral Nitrogen and Nitrate Leaching in Swedish Arable Soils Ĺsa Myrbeck Faculty of Natural Resources and Agricultural Sciences Department of Soil and Environment Uppsala field experiment, Paper III. (photo: J. Arvidsson) #12;Soil Tillage Influences on Soil Mineral Nitrogen

136

Recommended Academic Plan for the Environmental Resource Management -Soil Science Option (E R M/SOIL)  

E-Print Network [OSTI]

Recommended Academic Plan for the Environmental Resource Management - Soil Science Option (E R M/SOIL of Calculus I or MATH 140* (GQ) Calculus With Analytic Geometry I 4 SOILS 101 (GN) Introductory Soil Science 3 AG 150S (First-Year Seminar) Be a Master Student! 2 SOILS 102 Introductory Soil Science Laboratory 1

Omiecinski, Curtis

137

Long-term soil warming and Carbon Cycle Feedbacks to the Climate System  

SciTech Connect (OSTI)

The primary objective of the proposed research was to quantify and explain the effects of a sustained in situ 5oC soil temperature increase on net carbon (C) storage in a northeastern deciduous forest ecosystem. The research was done at an established soil warming experiment at the Harvard Forest in central Massachusetts – Barre Woods site established in 2001. In the field, a series of plant and soil measurements were made to quantify changes in C storage in the ecosystem and to provide insights into the possible relationships between C-storage changes and nitrogen (N) cycling changes in the warmed plots. Field measurements included: 1) annual woody increment; 2) litterfall; 3) carbon dioxide (CO2) efflux from the soil surface; 4) root biomass and respiration; 5) microbial biomass; and 6) net N mineralization and net nitrification rates. This research was designed to increase our understanding of how global warming will affect the capacity of temperate forest ecosystems to store C. The work explored how soil warming changes the interactions between the C and N cycles, and how these changes affect land-atmosphere feedbacks. This core research question framed the project – What are the effects of a sustained in situ 5oC soil temperature increase on net carbon (C) storage in a northeastern deciduous forest ecosystem? A second critical question was addressed in this research – What are the effects of a sustained in situ 5{degrees}C soil temperature increase on nitrogen (N) cycling in a northeastern deciduous forest ecosystem?

Melillo, Jerry M.

2014-04-30T23:59:59.000Z

138

Saxton soil remediation project  

SciTech Connect (OSTI)

The Saxton Nuclear Experimental Facility (SNEF) consists of a 23-MW(thermal) pressurized light water thermal reactor located in south central Pennsylvania. The Saxton Nuclear Experimental Corporation (SNEC), a wholly owned subsidiary of the General Public Utilities (GPU) Corporation, is the licensee for the SNEF. Maintenance and decommissioning activities at the site are conducted by GPU Nuclear, also a GPU subsidiary and operator of the Three Mile Island and Oyster Creek nuclear facilities. The remediation and radioactive waste management of contaminated soils is described.

Holmes, R.D. [GPU Nuclear Corporation, Middletown, PA (United States)

1995-12-31T23:59:59.000Z

139

A Study of Heat Sink Performance in Air and Soil for Use in a Thermoelectric Energy Harvesting Device  

E-Print Network [OSTI]

A Study of Heat Sink Performance in Air and Soil for Use in a Thermoelectric Energy Harvesting of a thermoelectric generator is to exploit the natural temperature difference between the air and the soil to generate small amounts of electrical energy. Since the conversion efficiency of even the best

140

Evaluation of MM5 Simulations With HTSVS With and Without Inclusion of Soil-Frost Parameterization  

E-Print Network [OSTI]

things soil freezing and thawing. Reanalysis of temperature, wind vector, specific humidity-frost. For precipitation, the wind vector, and in the mid-troposphere for temperature, the improvement index-frost into the European Centre for Medium-Range Weather Forecasts (ECMWF) model improved the simulation of annual

Moelders, Nicole

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


141

Soil Conservation Districts Law (North Dakota)  

Broader source: Energy.gov [DOE]

This chapter aims to provide for the conservation of the soil and soil resources of this state and for the control and prevention of soil erosion, and to preserve the state's natural resources,...

142

Soil Insulation For Barrier Layer Protection In Landfill Covers  

E-Print Network [OSTI]

Landfill covers are designed to isolate waste from the environment by incorporating low-permeability barrier layers. The barrier layer minimizes and controls gas escaping from the waste and the amount of infiltrating moisture available for leachate generation. Barrier layers are typically designed and constructed of a thick layer of compacted fine-grain native soil material or a manufactured geosynthetic clay liner. The barrier layer must be protected from frost damage. Freezing of a compacted soil layer has been shown to cause quick and irreversible degradation. Large increases in permeability have been demonstrated in compacted clay barriers subjected to a minimum number of freezing and thawing cycles. Design methods to protect the barrier layer from frost damage have not been addressed in the research literature. A design procedure is addressed in this paper that determines the thickness of soil required to protect a barrier layer. The procedure is based on sitespecific temperature ...

Gregory Smith Roy

143

Remote sensing of soil radionuclide fluxes in a tropical ecosystem  

SciTech Connect (OSTI)

We are using a transponding geostationary satellite to collect surface environmental data to describe the fate of soil-borne radionuclides. The remote, former atomic testing grounds at the Eniwetok and Bikini Atolls present a difficult environment in which to collect continuous field data. Our land-based, solar-powered microprocessor and environmental data systems remotely acquire measurements of net and total solar radiation, rain, humidity, temperature, and soil-water potentials. For the past year, our water flux model predicts wet season plant transpiration rates nearly equal to the 6 to 7 mm/d evaporation pan rate, which decreases to 2 to 3 mm/d for the dry season. Radioisotopic analysis confirms the microclimate-estimated 1:3 to 1:20 soil to plant /sup 137/Cs dry matter concentration ratio. This ratio exacerbates the dose to man from intake of food plants. Nephelometer measurements of airborne particulates presently indicate a minimum respiratory radiological dose.

Clegg, B.; Koranda, J.; Robinson, W.; Holladay, G.

1980-11-06T23:59:59.000Z

144

Examining the Relationship between Antecedent Soil Moisture and Summer Precipitation in the U.S. Great Plains  

E-Print Network [OSTI]

This dissertation focuses on examining the relationship between antecedent soil moisture and summer precipitation in the U.S. Great Plains (GP). The influence of Nino sea surface temperatures (SSTs) on summer precipitation has also been investigated...

Meng, Lei

2010-01-14T23:59:59.000Z

145

Technical Note Engineering Soils Maps  

E-Print Network [OSTI]

Technical Note Engineering Soils Maps PAUL M. SANTI Department of Geology and Geological database. In this technique, rose-pie charts provide an overall assessment of soils hazards structures such as pipelines, power lines, and roads; and regional evaluations of sources of ag- gregate

146

How Soil Organic Matter Composition Controls Hexachlorobenzene-Soil-Interactions: Adsorption Isotherms and Quantum Chemical Modelling  

E-Print Network [OSTI]

Hazardous persistent organic pollutants (POPs) interact in soil with the soil organic matter (SOM) but this interaction is insufficiently understood at the molecular level. We investigated the adsorption of hexachlorobenzene (HCB) on soil samples with systematically modified SOM. These samples included the original soil, the soil modified by adding a hot water extract (HWE) fraction (soil+3 HWE and soil+6 HWE), and the pyrolyzed soil. The SOM contents increased in the order pyrolyzed soil soil soil+3 HWE soil+6 HWE. For the latter three samples this order was also valid for the HCB adsorption. The pyrolyzed soil adsorbed more HCB than the other samples at low initial concentrations, but at higher concentrations the HCB adsorption became weaker than in the samples with HWE addition. This adsorption behaviour combined with the differences in the chemical composition between the soil samples suggested that alkylated aromatic, phenol, and lignin monomer compounds contributed most to the HC...

Ahmed, Ashour; Kühn, Oliver

2013-01-01T23:59:59.000Z

147

Evaluation of soil washing for radiologically contaminated soils  

SciTech Connect (OSTI)

Soil washing has been applied internationally to decontaminate soils due to the widespread increase in environmental awareness manifested in the United States by promulgation of the Comprehensive Environmental Response, Compensation and Liability Act, yet we continue to lack understanding on why the technique works in one application and not in another. A soil washing process typically integrates a variety of modules, each designed to decontaminate the matrix by destroying a particular phase or segregating a particle size fraction in which the contaminants are concentrated. The more known about how the contaminants are fixed, the more likely the process will succeed. Much can be learned from bioavailability studies on heavy metals in soils. Sequential extraction experiments designed to destroy one fixation mechanism at a time can be used to determine how contaminants are bound. This knowledge provides a technical basis for designing a processing strategy to efficiently decontaminate soil while creating a minimum of secondary wastes. In this study, a soil from the Idaho National Engineering Laboratory was physically and chemically characterized, then sequentially extracted to determine if soil washing could be effectively used to remove cesium, cobalt and chromium.

Gombert, D. II

1994-03-01T23:59:59.000Z

148

Non-Traditional Soil Additives: Can They Improve Crop Production?  

E-Print Network [OSTI]

Non-traditional soil additives include soil conditioners such as organic materials and minerals, soil activators that claim to stimulate soil microbes or inoculate soil with new beneficial organisms, and wetting agents that may be marketed...

McFarland, Mark L.; Stichler, Charles; Lemon, Robert G.

2002-06-26T23:59:59.000Z

149

Demonstration testing and evaluation of in situ soil heating. Health and safety plan (Revision 2)  

SciTech Connect (OSTI)

This document is the Health and Safety Plan (HASP) for the demonstration of IITRI`s EM Treatment Technology. In this process, soil is heated in situ by means of electrical energy for the removal of hazardous organic contaminants. This process will be demonstrated on a small plot of contaminated soil located in the Pit Area of Classified Burial Ground K-1070-D, K-25 Site, Oak Ridge, TN. The purpose of the demonstration is to remove organic contaminants present in the soil by heating to a temperature range of 85{degrees} to 95{degrees}C. The soil will be heated in situ by applying 60-Hz AC power to an array of electrodes placed in boreholes drilled through the soil. In this section a brief description of the process is given along with a description of the site and a listing of the contaminants found in the area.

Dev, H.

1994-12-28T23:59:59.000Z

150

The soil reference shrinkage curve  

E-Print Network [OSTI]

A recently proposed model showed how a clay shrinkage curve is transformed to the soil shrinkage curve at the soil clay content higher than a critical one. The objective of the present work was to generalize this model to the soil clay content lower a critical one. I investigated (i) the reference shrinkage curve, that is, one without cracks; (ii) the superficial layer of aggregates, with changed pore structure compared with the intraaggregate matrix; and (iii) soils with sufficiently low clay content where there are large pores inside the intraaggregate clay (so-called lacunar pores). The methodology is based on detail accounting for different contributions to the soil volume and water content during shrinkage. The key point is the calculation of the lacunar pore volume variance at shrinkage. The reference shrinkage curve is determined by eight physical soil parameters: (1) oven-dried specific volume; (2) maximum swelling water content; (3) mean solid density; (4) soil clay content; (5) oven-dried structural porosity; (6) the ratio of aggregate solid mass to solid mass of intraaggregate matrix; (7) the lacunar factor that characterizes the rate of the lacunar pore volume change with water content; and (8) oven-dried lacunar pore volume. The model was validated using available data. The model predicted value of the slope of the reference shrinkage curve in the basic shrinkage area is equal to unity minus the lacunar factor value, and is between unity and zero in the agreement with observations.

V. Y. Chertkov

2014-03-11T23:59:59.000Z

151

Soil protection major Prof. Dani Or  

E-Print Network [OSTI]

and energy fluxes in soils (water, air, nutrients and pollutants) · provide solutions for sustainable land1 Soil protection major Prof. Dani Or Soil and Terrestrial Environmental Physics CHN F 29.1 Universitätstrasse 16 8092 Zürich dani.or@env.ethz.ch +41 44 633 60 15 Objectives of soil protection major

Giger, Christine

152

CROP & SOIL SCIENCES Extension Peanut Agronomist  

E-Print Network [OSTI]

CROP & SOIL SCIENCES Extension Peanut Agronomist Committee Membership Dr. J. Michael Moore - committee chair Dr. Clint Waltz Department of Crop & Soil Sciences Department of Crop & Soil Sciences-7300 Fax: (229) 386-7308 Fax: (770) 412-4734 Dr. Eric Prostko Dr. Guy Collins Department of Crop & Soil

Arnold, Jonathan

153

CROP & SOIL SCIENCES Small Grain Breeding  

E-Print Network [OSTI]

CROP & SOIL SCIENCES Small Grain Breeding Committee Membership Dr. Paul Raymer - committee chair Dr. Scott Jackson Department of Crop & Soil Sciences Department of Crop & Soil Sciences University & Soil Sciences Department of Horticulture University of Georgia University of Georgia 2360 Rainwater Rd

Arnold, Jonathan

154

Soil and Water Conservation Spring 2014  

E-Print Network [OSTI]

of the interconnectedness of soil and water conservation. The course focusses on soil and water management as it relates to relevant issues surrounding agriculture and sustainability. Concepts include current soil and water and societal issues. Course Goals: Understand the basic principles of soil and water management

Ma, Lena

155

SOIL QUALITY AND CROP Dick Wolkowski  

E-Print Network [OSTI]

#12;WHAT IS SOIL QUALITY DEPENDS ON WHO YOU ARE: Farmer: Highly productive, sustainable media Soil test and pH "Artificial" drainage Residue management Microbial activity Salts #12;Soil biology factors into an index #12;Pennsylvania #12;A SOIL MANAGEMENT ASSESSMENT FRAMEWORK (Andrews et al., 2004

Balser, Teri C.

156

Soil and Water Conservation Spring 2014  

E-Print Network [OSTI]

focusses on soil and water management as it relates to relevant issues surrounding agriculture and sustainability. Concepts include current soil and water resources, historical erosion and sedimentation problems principles of soil and water management and conservation. 2. Discuss strategies for soil or water

Ma, Lena

157

Productive soil must be fertile physical fertility  

E-Print Network [OSTI]

, structure, drainage, tilth · chemical fertility ­ nutrient supply · soil testing #12;#12;Soil formation-'weathering' · physical ­freezing, thawing, wetting, drying, organisms · chemical ­dissolved minerals moved in water ­soil · improve by adding organic residues ­ decay: 90% CO2 + H2O #12;#12;#12;Problem: `heavy' soil · aggregates

Balser, Teri C.

158

Soil as natural capital Ecosystem services and  

E-Print Network [OSTI]

threats Decline in: Lead to: soil carbon soil erosion biological ac2 tool box Information on sustainable soil use incentives After Daiily et al 2009 "decision loop" #12;Soil is a natural capital Ecosystem services Nutrient retention Carbon storage Water retention

159

CROP & SOIL SCIENCES Cotton Physiologist Tifton campus  

E-Print Network [OSTI]

CROP & SOIL SCIENCES Cotton Physiologist ­ Tifton campus Committee Membership Dr. Stanley Culpepper

Arnold, Jonathan

160

MICHIGAN'S SOIL NITRATE TEST FOR CORN MSU SOIL AND PLANT NUTRIENT LAB  

E-Print Network [OSTI]

MICHIGAN'S SOIL NITRATE TEST FOR CORN MSU SOIL AND PLANT NUTRIENT LAB Michigan State University Extension Crop and Soil Sciences Department Michigan State University WHY TEST SOIL FOR NITRATES Nitrate testing of soil is an excellent and inexpensive way of evaluating the available nitrogen (N) status

Isaacs, Rufus

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


161

RESEARCH ARTICLE A novel soil organic C model using climate, soil type  

E-Print Network [OSTI]

RESEARCH ARTICLE A novel soil organic C model using climate, soil type and management data-Verlag, France 2012 Abstract This report evidences factors controlling soil or- ganic carbon at the national scale by modelling data of 2,158 soil samples from France. The global soil carbon amount, of about 1

Paris-Sud XI, Université de

162

REGULAR ARTICLE Impact of biological soil crusts and desert plants on soil  

E-Print Network [OSTI]

REGULAR ARTICLE Impact of biological soil crusts and desert plants on soil microfaunal community plants and biological soil crusts on desert soil nematode and protozoan abundance and community composition. In the first experiment, biological soil crusts were removed by physical trampling. Treatments

Neher, Deborah A.

163

Impact of Soil Type and Compaction Conditions on Soil Water Characteristic  

E-Print Network [OSTI]

Impact of Soil Type and Compaction Conditions on Soil Water Characteristic C. J. Miller, M.ASCE1 the variation of water content and pore water suction for compacted clayey soils. The soils had varying amounts of clay fraction with plasticities ranging from low to high plasticity. The unsaturated soil behavior

Yu, Sheng-Tao

164

Part I. Ecological Sites and Soil Part II. A Framework for Soil and  

E-Print Network [OSTI]

Part I. Ecological Sites and Soil Survey Part II. A Framework for Soil and Vegetation Dynamics Arlene Tugel, Soil Scientist Liaison to ARS, USDA-NRCS Las Cruces, NM and the Soils-ESD Advisory Group #12;What makes a site a site? Soil forming factors: climate, parent, material, biotic factors

165

Soil Test Report The following information is being provided for farmers. For consumer soil test report  

E-Print Network [OSTI]

Soil Test Report The following information is being provided for farmers. For consumer soil test fertility status of the soil in each field can invest wisely in fertilizer and lime to produce the most economical crop yields. A soil test provides the needed information about soil pH, lime need and available

Isaacs, Rufus

166

Soil drainage as an active agent of recent soil evolution: a David Montagnea,b  

E-Print Network [OSTI]

1 Soil drainage as an active agent of recent soil evolution: a review* David Montagnea,b , Sophie on pedogenesis mainly focuses on the long-term soil formation and most often neglects recent soil evolution drainage on soil evolution. Artificial drainage is considered as an example of the impact of recent changes

Boyer, Edmond

167

Soil Aggregate Size Affects Phosphorus Desorption from Highly Weathered Soils and Plant Growth  

E-Print Network [OSTI]

Soil Aggregate Size Affects Phosphorus Desorption from Highly Weathered Soils and Plant Growth X of P around soil aggregates (Gunary et al., 1964; Linquist etfrom soil, understanding P desorption from soils may improve the precision of P diagnosis and fertilization recommendations. Many al., 1997

van Kessel, Chris

168

Tree Species Effects on Soil Organic Matter Dynamics: The Role of Soil  

E-Print Network [OSTI]

Tree Species Effects on Soil Organic Matter Dynamics: The Role of Soil Cation Composition Sarah E the influence of tree species on soil carbon and nitrogen (N) dynamics in a common garden of replicated substantial divergence in foliar and soil base cation concentrations and soil pH among spe- cies, we

Minnesota, University of

169

Global Soil Change: Land Use, Soil and Water SWS4231C, SWS5234  

E-Print Network [OSTI]

of the soil system to withstand global-scale perturbations (e.g., climate or land use change, spread Properties 4. Land Use Change Impacts on Soils 5. Land Use and Agriculture (Irrigation and Fertilization In Soil) 6. Land Use and Soil Erosion 7. Climate Change Impacts on Soils 8. Land Use-Climate

Ma, Lena

170

Worldwide organic soil carbon and nitrogen data  

SciTech Connect (OSTI)

The objective of the research presented in this package was to identify data that could be used to estimate the size of the soil organic carbon pool under relatively undisturbed soil conditions. A subset of the data can be used to estimate amounts of soil carbon storage at equilibrium with natural soil-forming factors. The magnitude of soil properties so defined is a resulting nonequilibrium values for carbon storage. Variation in these values is due to differences in local and geographic soil-forming factors. Therefore, information is included on location, soil nitrogen content, climate, and vegetation along with carbon density and variation.

Zinke, P.J.; Stangenberger, A.G. [Univ. of California, Berkeley, CA (United States). Dept. of Forestry and Resource Management; Post, W.M.; Emanual, W.R.; Olson, J.S. [Oak Ridge National Lab., TN (United States)

1986-09-01T23:59:59.000Z

171

Selective leaching of uranium from uranium-contaminated soils: Progress report 1  

SciTech Connect (OSTI)

Three soils and a sediment contaminated with uranium were used to determine the effectiveness of sodium carbonate and citric acid leaching to decontaminated or remove uranium to acceptable regulatory levels. Two of the soils were surface soils from the DOE facility formerly called the Feed Materials Production Center (FMPC) at Fernald, Ohio. This facility is presently called the Femald Environmental Management Project (FEMP). Carbonate extractions generally removed from 70 to 90% of the uranium from the Fernald storage pad soil. Uranium was slightly more difficult to extract from the Fernald incinerator and the Y-12 landfarm soils. Very small amounts of uranium could be extracted from the storm sewer sediment. Extraction with carbonate at high solution-to-soil ratios were as effective as extractions at low solution-to-soil ratios, indicating attrition by the paddle mixer was not significantly different than that provided in a rotary extractor. Also, pretreatments such as milling or pulverizing the soil sample did not appear to increase extraction efficiency when carbonate extractions were carried out at elevated temperatures (60[degree]C) or long extraction times (23 h). Adding KMnO[sub 4] in the carbonate extraction appeared to increase extraction efficiency from the Fernald incinerator soil but not the Fernald storage pad soil. The most effective leaching rates (> 90 % from both Fernald soils) were obtained using a citrate/dithionite extraction procedure designed to remove amorphous (noncrystalline) iron/aluminum sesquioxides from surfaces of clay minerals. Citric acid also proved to be a very good extractant for uranium.

Francis, C.W.; Mattus, A.J.; Farr, L.L.; Elless, M.P.; Lee, S.Y.

1993-02-01T23:59:59.000Z

172

Selective leaching of uranium from uranium-contaminated soils: Progress report 1  

SciTech Connect (OSTI)

Three soils and a sediment contaminated with uranium were used to determine the effectiveness of sodium carbonate and citric acid leaching to decontaminated or remove uranium to acceptable regulatory levels. Two of the soils were surface soils from the DOE facility formerly called the Feed Materials Production Center (FMPC) at Fernald, Ohio. This facility is presently called the Femald Environmental Management Project (FEMP). Carbonate extractions generally removed from 70 to 90% of the uranium from the Fernald storage pad soil. Uranium was slightly more difficult to extract from the Fernald incinerator and the Y-12 landfarm soils. Very small amounts of uranium could be extracted from the storm sewer sediment. Extraction with carbonate at high solution-to-soil ratios were as effective as extractions at low solution-to-soil ratios, indicating attrition by the paddle mixer was not significantly different than that provided in a rotary extractor. Also, pretreatments such as milling or pulverizing the soil sample did not appear to increase extraction efficiency when carbonate extractions were carried out at elevated temperatures (60{degree}C) or long extraction times (23 h). Adding KMnO{sub 4} in the carbonate extraction appeared to increase extraction efficiency from the Fernald incinerator soil but not the Fernald storage pad soil. The most effective leaching rates (> 90 % from both Fernald soils) were obtained using a citrate/dithionite extraction procedure designed to remove amorphous (noncrystalline) iron/aluminum sesquioxides from surfaces of clay minerals. Citric acid also proved to be a very good extractant for uranium.

Francis, C.W.; Mattus, A.J.; Farr, L.L.; Elless, M.P.; Lee, S.Y.

1993-02-01T23:59:59.000Z

173

Numerical study on transient heat transfer under soil with plastic mulch in agriculture applications using a nonlinear finite element model  

E-Print Network [OSTI]

In this paper is developed a simple mathematical model of transient heat transfer under soil with plastic mulch in order to determine with numerical studies the influence of different plastic mulches on the soil temperature and the evolutions of temperatures at different depths with time. The governing differential equations are solved by a Galerkin Finite Element Model, taking into account the nonlinearities due to radiative heat exchange between the soil surface, the plastic mulch and the atmosphere. The model was validated experimentally giving good approximation of the model to the measured data. Simulations were run with the validated model in order to determine the optimal combination of mulch optical properties to maximize the soil temperature with a Taguchi's analysis, proving that the material most used nowadays in Colombia is not the optimal and giving quantitative results of the properties the optimal mulch must possess.

De Castro, Carlos Armando

2011-01-01T23:59:59.000Z

174

Soil Organic Matter of Natural and Restored Coastal Wetland Soils in Southern California  

E-Print Network [OSTI]

of natural and created marsh soils. J. Exp. Mar. Biol. Ecol.2007. Freshwater Input Structures Soil Properties, VerticalS.S. , Hoover, K.L. 1996. Soil properties of reference

Elgin, Barbara K.

2012-01-01T23:59:59.000Z

175

Organic soil phosphorus is plant-available but is neglected by routine soil-testing methods  

E-Print Network [OSTI]

microorganisms. Biol. Fertil. Soils 1988; 5: 308-312 Van derplant species and to evaluate different soil-testing methodsin measuring organic soil-P. Material and Methods This

Steffens, Diedrich; Leppin, Thomas; Schubert, Sven

2009-01-01T23:59:59.000Z

176

Consolidation theories for saturated-unsaturated soils and numerical simulation of residential buildings on expansive soils  

E-Print Network [OSTI]

and numerical techniques: different simulation methods for different boundary conditions such as tree, grass, and bare soils, coupled hydro-mechanical stress analysis to describe deformation of saturated-unsaturated soils, jointed elements simulation of soil...

Zhang, Xiong

2005-11-01T23:59:59.000Z

177

The prediction of root zone soil moisture with a water balance - microwave emission model  

E-Print Network [OSTI]

. T (1-) = T (I-) = T (I + e t &Rz) + ( T (I + e R. ) 8 e el I=2 ei i+ I (II-18) where -2a azi T =T. (1-e ) e. i 1 n = number of layers Rn =0 bz n To describe the brightness temperature above the soil sur face, the effective temperature of emi... and Groundtruth. Analysis of the Surface Flux Approach RADCON Model Scatter Due to Soil Variability . Selection of 21 cm Wavelength over 6 cm Wavelength. V CONCLUSION Summary of Results. Recommendations REFERENCES. 72 72 76 80 83 90 100 109 109...

Smith, Michael Robert

2012-06-07T23:59:59.000Z

178

Tensile creep of soil-cement and its relationship to fatigue  

E-Print Network [OSTI]

Creep curves at different temperatures. 19 Log (D(t)-Dz) vs. log t at different temperatures. 68 69 INTRODUCTION Portland cement is an extremely important stabilizing agent for a wide range of soil types. Because of its strength-enhancing property... Mechanics (LEFM) is applicable to the investigation and determination of realistic failure criteria of fine-grained soils stabilized with Portland cement [27]. This is due to the fact that the radius of curvature at the tip of a microcrack is small...

Kim, Youngsoo

1985-01-01T23:59:59.000Z

179

HVDC ground electrode heat dissipation in an N-layer soil  

SciTech Connect (OSTI)

The temperature distribution in an N-layer soil, due to High Voltage Direct Current (HVDC) injection via ground electrodes was computed using finite difference methods. The temperature profiles using various ground electrode shapes buried in a two-layer soil were computed using these same techniques. The results obtained were then compared with results obtained experimentally in a laboratory at Ecole Polytecnique. A sensitivity analysis was performed on the effect of the height of the top layer of a two-layer earth model and the results were tabulated.

Greiss, H.; Mukhedkar, D.; Houle, J.L.; Do, X.D.; Gervais, Y. (Ecole Polytechnique, Montreal, Quebec (CA))

1988-10-01T23:59:59.000Z

180

Developing a Soil Property Database for the Oklahoma Mesonet.  

E-Print Network [OSTI]

??The objective of this study was to create a comprehensive database of soil hydraulic and physical properties of the Oklahoma Mesonet station soils. Replicate soil… (more)

Scott, Bethany

2012-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


181

Heterotrophic Soil Respiration in Warming Experiments: Using Microbial Indicators to Partition Contributions from Labile and Recalcitrant Soil Organic Carbon. Final Report  

SciTech Connect (OSTI)

The central objective of the proposed work was to develop a genomic approach (nucleic acid-based) that elucidates the mechanistic basis for the observed impacts of experimental soil warming on forest soil respiration. The need to understand the mechanistic basis arises from the importance of such information for developing effective adaptation strategies for dealing with projected climate change. Specifically, robust predictions of future climate will permit the tailoring of the most effective adaptation efforts. And one of the greatest uncertainties in current global climate models is whether there will be a net loss of carbon from soils to the atmosphere as climate warms. Given that soils contain approximately 2.5 times as much carbon as the atmosphere, a net loss could lead to runaway climate warming. Indeed, most ecosystem models predict that climate warming will stimulate microbial decomposition of soil carbon, producing such a positive feedback to rising global temperatures. Yet the IPCC highlights the uncertainty regarding this projected feedback. The uncertainty arises because although warming-experiments document an initial increase in the loss of carbon from soils, the increase in respiration is short-lived, declining to control levels in a few years. This attenuation could result from changes in microbial physiology with temperature. We explored possible microbial responses to warming using experiments and modeling. Our work advances our understanding of how soil microbial communities and their activities are structured, generating insight into how soil carbon might respond to warming. We show the importance of resource partitioning in structuring microbial communities. Specifically, we quantified the relative abundance of fungal taxa that proliferated following the addition of organic substrates to soil. We added glycine, sucrose, cellulose, lignin, or tannin-protein to soils in conjunction with 3-bromo-deoxyuridine (BrdU), a nucleotide analog. Active microbes absorb BrdU from the soil solution; if they multiply in response to substrate additions, they incorporate the BrdU into their DNA. After allowing soils to incubate, we extracted BrdU-labeled DNA and sequenced the ITS regions of fungal rDNA. Fungal taxa that proliferated following substrate addition were likely using the substrate as a resource for growth. We found that the structure of active fungal communities varied significantly among substrates. The active fungal community under glycine was significantly different from those under other conditions, while the active communities under sucrose and cellulose were marginally different from each other and the control. These results indicate that the overall community structure of active fungi was altered by the addition of glycine, sucrose, and cellulose and implies that some fungal taxa respond to changes in resource availability. The community composition of active fungi is also altered by experimental warming. We found that glycine-users tended to increase under warming, while lignin-, tannin/protein-, and sucrose-users declined. The latter group of substrates requires extracellular enzymes for use, but glycine does not. It is possible that warming selects for fungal species that target, in particular, labile substrates. Linking these changes in microbial communities and resource partitioning to soil carbon dynamics, we find that substrate mineralization rates are, in general, significantly lower in soils exposed to long-term warming. This suggests that microbial use of organic substrates is impaired by warming. Yet effects are dependent on substrate identity. There are fundamental differences in the metabolic capabilities of the communities in the control and warmed soils. These differences might relate to the changes in microbial community composition, which appeared to be associated with groups specialized on different resources. We also find that functional responses indicate temperature acclimation of the microbial community. There are distinct seasonal patterns and to long-term soil warming, with

Bradford, M A; Melillo, J M; Reynolds, J F; Treseder, K K; Wallenstein, M D

2010-06-10T23:59:59.000Z

182

Detection of explosives in soils  

DOE Patents [OSTI]

An apparatus and method for detecting explosive-indicating compounds in subsurface soil. The apparatus has a probe with an adsorbent material on some portion of its surface that can be placed into soil beneath the ground surface, where the adsorbent material can adsorb at least one explosive-indicating compound. The apparatus additional has the capability to desorb the explosive-indicating compound through heating or solvent extraction. A diagnostic instrument attached to the probe detects the desorbed explosive-indicating compound. In the method for detecting explosive-indicating compounds in soil, the sampling probe with an adsorbent material on at least some portion of a surface of the sampling probe is inserted into the soil to contact the adsorbent material with the soil. The explosive-indicating compounds are then desorbed and transferred as either a liquid or gas sample to a diagnostic tool for analysis. The resulting gas or liquid sample is analyzed using at least one diagnostic tool selected from the group consisting of an ion-mobility spectrometer, a gas chromatograph, a high performance liquid chromatograph, a capillary electrophoresis chromatograph, a mass spectrometer, a Fourier-transform infrared spectrometer and a Raman spectrometer to detect the presence of explosive-indicating compounds.

Chambers, William B. (Edgewood, NM); Rodacy, Philip J. (Albuquerque, NM); Phelan, James M. (Bosque Farms, NM); Woodfin, Ronald L. (Sandia Park, NM)

2002-01-01T23:59:59.000Z

183

A soil moisture budget analysis of Texas using basic climatic data while assuming a possible warming trend across the state  

E-Print Network [OSTI]

of the slope (dashed lines) of the regression line of precipitation on mean temperature for the Lower Valley. 35. Isopleths of MTRANGE (in 'F) for Texas during August. 71 36. Percentage of monthly soil moisture (SM) for the High Plains for a O'F (control... are significant at the 95% confidence interval. 74 37. Percentage of monthly soil moisture (SM) for the High Plains for a O'F (control), I' F, 2'F, 3'F, and 4'F increase in the mean annual temperature of Texas. Mean monthly temperatures increase non...

Bjornson, Brian Matthew

1990-01-01T23:59:59.000Z

184

Changes in soil carbon and nitrogen associated with switchgrass production  

E-Print Network [OSTI]

.), other forage grasses, cultivated crops, and forest were collected seasonally at six locations. Soil organic C (SOC), total N, soil microbial biomass C (SMBC) and N (SMBN), soil mineralizable C and N, and basal soil respiration (BSR) were in general...

Lobo Alonzo, Porfirio Jose

2004-11-15T23:59:59.000Z

185

Major Nitrogen Loss Pathways in Upland Blueberry Soils  

E-Print Network [OSTI]

2 O production in an arable peat soil in Central KalimantanTateyama brown forest soil + peat moss (1:1), SC- Soil +the tropical and boreal peat soils have a wide fungal

Vano, Imre

2009-01-01T23:59:59.000Z

186

Soil samples at the APS  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE:1 First Use of Energy for All Purposes (Fuel and Nonfuel),Feet) Year Jan Feb Mar Apr May JunDatastreamsmmcrcalgovInstrumentsrucLas ConchasPassiveSubmittedStatus Tom Fletcher,Future | Department of HowSoftware speedsSoilSoil

187

Strings at finite temperature  

SciTech Connect (OSTI)

We obtain a semiclassical evaluation of the temperature for which the free energy of the strings of spontaneously broken scalar electrodynamics vanishes. We argue that, above this temperature, these objects should play a significant physical role.

Arago C. de; Bazeia, D.; Eboli, O.J.P.; Marques, G.C.

1985-12-15T23:59:59.000Z

188

Rainwater Harvesting: Soil Storage and Infiltration System  

E-Print Network [OSTI]

A soil storage and infiltration system collects rainfall runoff from the roofs of buildings and directs it underground where it infiltrates the soil. Such a system conserves water and protects it from surface pollution. This publication describes...

Mechell, Justin; Lesikar, Bruce J.

2008-08-11T23:59:59.000Z

189

Irrigation Monitoring with Soil Water Sensors  

E-Print Network [OSTI]

Monitoring soil water content is essential if growers want to optimize production, conserve water, reduce environmental impacts and save money. This publication illustrates how soil moisture monitoring can improve irrigation decisions and how...

Enciso, Juan; Porter, Dana; Peries, Xavier

2007-01-19T23:59:59.000Z

190

FINGERPRINTING SOILS – A PROOF OF CONCEPT  

E-Print Network [OSTI]

Forensic soil characterization is an under-explored field in the forensic sciences. One aspect of forensic sciences is Locard’s Exchange Principle, which states that every contact leaves a trace. As soil characterization technology improves...

Kobylinski, Catherine

2011-05-06T23:59:59.000Z

191

BIOCYCLE JUNE 2002 41 ETAL contaminated soils  

E-Print Network [OSTI]

where smelter emissions or mine wastes caused con- tamination and soils were acidic. Such metal toxic the location of the main lead smelter, over 2,000 yards of soils have been excavated and replaced with clean

Brown, Sally

192

Maryland Soil Conservation Districts Law (Maryland)  

Broader source: Energy.gov [DOE]

It is the policy of the state to conserve the soil, water, and related resources of the state through establishing regulations for land-use practices related to soil erosion. This legislation...

193

Probabilistic Analysis of the Compressibility of Soils  

E-Print Network [OSTI]

of surface loads or variable soil deposits. In current practice, the analysis to determine settlements is deterministic. It assumes that the soil profile at a site is uniform from location to location, and only allows limited consideration of the variations...

Jung, Byoung C.

2010-07-14T23:59:59.000Z

194

Soil Carbon Sequestration and the Greenhouse Effect  

E-Print Network [OSTI]

Soil Carbon Sequestration and the Greenhouse Effect Second edition Rattan Lal & Ronald F. Follett. Printed in the United States of America. #12;181 Soil Carbon Sequestration and the Greenhouse Effect, 2nd

Archer, Steven R.

195

Bioaugmentation of TNT-contaminated soil  

E-Print Network [OSTI]

Microbial transformation of trinitrotoluene (TNT) in phics. contaminated soil was investigated in this research. A Bacillus sp., isolated from soil obtained from an army ammunition facility, was used to enhance the rate of TNT removal over a 360 day...

Bokelmann, Annamarie

1999-01-01T23:59:59.000Z

196

Soil Quality Information Sheet Rangeland Soil Quality--Infiltration  

E-Print Network [OSTI]

programs.) Persons with disabilities who require alternative means for communication of program information by infiltration. The infiltration rate can be restricted by poor management. Under these conditions, the water) and the infiltration rate. These are affected by vegetation and many soil properties. Residence time The length of time

197

Centennial black carbon turnover observed in a Russia steppe soil  

E-Print Network [OSTI]

the zonal steppe soils of Russia. J. Plant Nutr. Soil Sci. ,CD-ROM "Land Resources of Russia", International Institute

Hammes, K.

2010-01-01T23:59:59.000Z

198

The effect of soil hydraulic properties vs. soil texture in land surface models  

E-Print Network [OSTI]

depths in the soil column controls the partitioning of the two key energy fluxes of concern in climateThe effect of soil hydraulic properties vs. soil texture in land surface models E. D. Gutmann and E and difficulties in scaling existing data. In particular, the spatial distribution of Soil Hydraulic Properties

Small, Eric

199

A dynamic organic soil biogeochemical model for simulating the effects of wildfire on soil environmental  

E-Print Network [OSTI]

of surface energy balance [Liu et al., 2005], soil thermal and hydrological regimes [MacKay, 1995; Burn, 1998A dynamic organic soil biogeochemical model for simulating the effects of wildfire on soil not comprehensively considered how interactions among fire disturbance, soil environmental conditions

Wagner, Diane

200

Managing Our Grandchildren's Forests: The Role of Soil Biology and Soil Ecology1  

E-Print Network [OSTI]

matter and energy, water and nutrients, organic matter, and gases. Soils within forest ecosystems supportManaging Our Grandchildren's Forests: The Role of Soil Biology and Soil Ecology1 James R. Boyle2 The papers of this volume provide some "nuggets" of insight into the complexity of soil biology and its

Standiford, Richard B.

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


201

Soil Biology & Biochemistry 39 (2007) 21382149 Heterogeneity of soil nutrients and subsurface biota  

E-Print Network [OSTI]

Author's personal copy Soil Biology & Biochemistry 39 (2007) 2138­2149 Heterogeneity of soil Laboratory, 999-W, Aiken, SC 29808, USA f Department of Plant & Soil Science, University of Vermont, Hills to have a highly heterogeneous distribution of nutrients and soil biota, with greater concentrations

Neher, Deborah A.

2007-01-01T23:59:59.000Z

202

UNL Microgravity: Team Fast Project: Lunar soil is much different from terrestrial soil,  

E-Print Network [OSTI]

UNL Microgravity: Team Fast Project: Lunar soil is much different from terrestrial soil, consisting of a large percentage of very fine particles. Lunar soil also contains very irregular and jagged particles formed from the sintering together of broked grains during micro-meteorite bombardment. NASA has soil

Farritor, Shane

203

Digital soil mapping: Towards a multiple-use Soil Information System D G Rossiter  

E-Print Network [OSTI]

Digital soil mapping: Towards a multiple-use Soil Information System D G Rossiter Senior University and remote sensing. However, mapping of soil types and characteristics has not fully shared in this revolution, because of the complexity of soil geography and the high cost of its direct obser- vation. None

Rossiter, D G "David"

204

Soil CO2 flux and photoautotrophic community composition in high-elevation, `barren' soil  

E-Print Network [OSTI]

Soil CO2 flux and photoautotrophic community composition in high-elevation, `barren' soil Kristen R of Colorado, Campus Box 450, Boulder, CO 80309, USA. Summary Soil-dominated ecosystems, with little-elevation, subnival zone soil (i.e. elevations higher than the zone of continuous vegetation), the structure

Hammerton, James

205

Differences in potassium forms between cutans and adjacent soil matrix in a Grey Clay Soil  

E-Print Network [OSTI]

Differences in potassium forms between cutans and adjacent soil matrix in a Grey Clay Soil Fan Liu1 , R. J. Gilkes, R. D. Hart, and A. Bruand2 Department of Soil Science and Plant Nutrition, Faculty are common fabric features in soil and represent foci of chemical and biological reactions. The influence

Boyer, Edmond

206

Holme et al. Soil Redox Sensor Networks RADIO FREQUENCY ENABLED SOIL REDOX POTENTIAL  

E-Print Network [OSTI]

Holme et al. Soil Redox Sensor Networks RADIO FREQUENCY ENABLED SOIL REDOX POTENTIAL SENSOR technologies that may be combined into a cost effective soil redox sensor network, discuss the merits of each as a component of said network, describe a prototype soil redox sensor network and perform basic laboratory

Rubinstein, Benjamin

207

Evaluating Soil Health Summary: Soil health can be measured, monitored and managed to increase sustainability and  

E-Print Network [OSTI]

Evaluating Soil Health Summary: Soil health can be measured, monitored and managed to increaseResourcesNonmedia, Producers, Web. From Sara Adlington, (406) 994-4602 Filename: Eval Soil Health PR2014 Web: Ag, Extension with Montana State University and MSU Extension have recommendations for growers on evaluating soil quality

Lawrence, Rick L.

208

Soil Biology & Biochemistry 38 (2006) 30013002 A synthesis of soil biodiversity and ecosystem functioning in  

E-Print Network [OSTI]

Soil Biology & Biochemistry 38 (2006) 3001­3002 Editorial A synthesis of soil biodiversity-free soils in Antarctica has exploded, drastically altering general perceptions about the diversity of life on this cold, dark and windy continent. In Victoria Land, Antarctica (701300 S to 78100S), where soil biota

Wall, Diana

2006-01-01T23:59:59.000Z

209

Bio-Char Soil Management on Highly Weathered Soils in the Humid Tropics  

E-Print Network [OSTI]

therefore have to be applied each year to sustain soil productivity. Management of black carbon (C36 Bio-Char Soil Management on Highly Weathered Soils in the Humid Tropics Johannes Lehmann1), ColombiaQ1 CONTENTS 36.1 Bio-Char Management and Soil Nutrient Availability

Lehmann, Johannes

210

Soil Science Society of America Journal Revealing Soil Structure and Functional Macroporosity  

E-Print Network [OSTI]

how fast water, greenhouse gases, vola- tile compounds, chemicals, and pollutants can enter and move ecosystem functions. In this study, soil physical measurements (soil-water retention and air permeability soil clay content, while significantly higher air permeability was observed for the l1 to l3 soils than

Wildenschild, Dorthe

211

Author's personal copy Soil total carbon analysis in Hawaiian soils with visible, near-infrared and  

E-Print Network [OSTI]

Author's personal copy Soil total carbon analysis in Hawaiian soils with visible, near-infrared reflectance spectroscopy Agriculture Hawaii Mid-infrared Soil carbon Visible near-infrared Accurate assessment of DRS for Ct prediction of Hawaiian ag- ricultural soils by creating visible, near-infrared (VNIR

Grunwald, Sabine

212

Kinetics of Ni Sorption in Soils: Roles of Soil Organic Matter and Ni Precipitation  

E-Print Network [OSTI]

sorption in soils may be controlled by different reaction mechanisms at various time scales be an important path for Ni sequestration in soils.9 The mechanisms of Ni-LDH formation have been investigatedKinetics of Ni Sorption in Soils: Roles of Soil Organic Matter and Ni Precipitation Zhenqing Shi

Sparks, Donald L.

213

Soil Science Society of America Journal Soil Sci. Soc. Am. J. 76:17191727  

E-Print Network [OSTI]

Soil Science Society of America Journal Soil Sci. Soc. Am. J. 76:1719­1727 doi:10.2136/sssaj2011.0303 Received 7 Sept. 2011. *Corresponding author (soils@msu.edu). © Soil Science Society of America, 5585 or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any

Schaetzl, Randall

214

6, 13011320, 2006 Temperature  

E-Print Network [OSTI]

ACPD 6, 1301­1320, 2006 Temperature climatology and trend estimates over Durban, South Africa H and Physics Discussions Temperature climatology and trend estimates in the UTLS region as observed over Commons License. 1301 #12;ACPD 6, 1301­1320, 2006 Temperature climatology and trend estimates over Durban

Boyer, Edmond

215

Critical shear stresses in cohesive soils  

E-Print Network [OSTI]

CRITICAL SHEAR STRESSES IN COHESIVE SOILS A Thesis By ROBERT JAMES REKTORIK Approved as to style and content by: (Committee hairm g- c& ( ead of epartm ( mber) (Member) January 1964 ACKNOWLEDGMENTS I wish to acknowledge the guidance..., and Dummy Soil Sample 17 Typical Soil Samples after Scour Test, San Saba Clay 25 Typical Soil Samples after Scour Test, Houston Black Clay, K177 Regression of Critical Shearing Force on Per Cent Moisture . 31 10. Regression of Critical Shearing Force...

Rektorik, Robert James

1964-01-01T23:59:59.000Z

216

Oxidation of Organic Compounds in the Soil.  

E-Print Network [OSTI]

.................... ltudy by Means of Carbon Dioxide Formed 8 ............................... lomparison of . Various Materials 9 ...................................... lffect of Nature of Soil 14 ..................................... Ixidation of Soil Carbon 18... was drawn to take out the carbon dioxide. Althongl~ such experi- ments are well adapted to estimate carbon cliosicle, obviously, such con- ditions do not prevail in the soil, and while it is possible that Wollnp's conclusions may appl~r to the soil uncler...

Fraps, G. S. (George Stronach)

1915-01-01T23:59:59.000Z

217

Soil-Geomorphic Change during Desertification  

E-Print Network [OSTI]

soils mesquite coppice dunes #12;1750 1850 1950 2050 mesquite black grama Sandy Basin Floor Site #12

218

Ice-lens formation and geometrical supercooling in soils and other colloidal materials  

E-Print Network [OSTI]

We present a new, physically-intuitive model of ice-lens formation and growth during the freezing of soils and other dense, particulate suspensions. Motivated by experimental evidence, we consider the growth of an ice-filled crack in a freezing soil. At low temperatures, ice in the crack exerts large pressures on the crack walls that will eventually cause the crack to split open. We show that the crack will then propagate across the soil to form a new lens. The process is controlled by two factors: the cohesion of the soil, and the geometrical supercooling of the water in the soil; a new concept introduced to measure the energy available to form a new ice lens. When the supercooling exceeds a critical amount (proportional to the cohesive strength of the soil) a new ice lens forms. This condition for ice-lens formation and growth does not appeal to any ad hoc, empirical assumptions, and explains how periodic ice lenses can form with or without the presence of a frozen fringe. The proposed mechanism is in good agreement with experiments, in particular explaining ice-lens pattern formation, and surges in heave rate associated with the growth of new lenses. Importantly for systems with no frozen fringe, ice-lens formation and frost heave can be predicted given only the unfrozen properties of the soil. We use our theory to estimate ice-lens growth temperatures obtaining quantitative agreement with the limited experimental data that is currently available. Finally we suggest experiments that might be performed in order to verify this theory in more detail. The theory is generalizable to complex natural-soil scenarios, and should therefore be useful in the prediction of macroscopic frost heave rates.

Robert W. Style; Stephen S. L. Peppin; Alan C. F. Cocks; John S. Wettlaufer

2011-09-09T23:59:59.000Z

219

PayneOklahoma SOIL SURVEY OF PAYNE COUNTY, OKLAHOMA  

E-Print Network [OSTI]

SOIL SURVEY OF PAYNE COUNTY, OKLAHOMA OSURR Headquarters 0 700 1,400 2,100 2,800350 Feet 0 200 400100 Meters Web Soil Survey 1.1 National Cooperative Soil Survey 5/7/2007 Page 1 of 4 #12;MAP INFORMATION SOIL Web Soil Survey URL: http://websoilsurvey.nrcs.usda.gov Coordinate System: UTM Zone 14 Soil Survey

Ghajar, Afshin J.

220

11:776:413 Soil Quality S. Murphy Page 1  

E-Print Network [OSTI]

: Soil Management & Sustainability, best management practices Week 4 Soil Degradation and resulting's dependence on soil To understand society's impact on soil and need for educated management To increase sequestration. Managing soil to build/maintain organic matter. Week 6 Chemical Indicators: soil pH, buffering

Chen, Kuang-Yu

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


221

Measurement Scheduling for Soil Moisture Sensing  

E-Print Network [OSTI]

energy consumption is presented; the paper is grounded in the physics of soil moisture. By David I Shuman off some inaccuracy in estimating soil moisture evolution for a significant reduction in energyINVITED P A P E R Measurement Scheduling for Soil Moisture Sensing: From Physical Models to Optimal

Mahajan, Aditya

222

Soil Properties That Distinguish Ecological Sites  

E-Print Network [OSTI]

Soil Properties That Distinguish Ecological Sites Mike Duniway USGS-Southwest Biological Science of vegetation? Why do sites differ in response to disturbance & management? #12;Ecological Sites & Soil Properties · Within a climatic zone (e.g. MLRA), differentiation of ecological sites based on soil

223

Common Questions Why should I soil test?  

E-Print Network [OSTI]

Common Questions Why should I soil test? Soil testing is an important diagnostic tool to evaluate nutrient imbalances and understand plant growth. The most important reason to soil test is to have a basis for intelligent application of fertilizer and lime. Testing also allows for growers and homeowners to maintain

Isaacs, Rufus

224

DIVISION S-6--SOIL & WATER MANAGEMENT & CONSERVATION  

E-Print Network [OSTI]

DIVISION S-6--SOIL & WATER MANAGEMENT & CONSERVATION Soil Organic Carbon Sequestration Rates soil column within 20 yr following culti- Carbon sequestration rates, with a change from CT to NT, can in approximately 40 to and returning to the original land cover or other peren- 60 yr. Carbon sequestration rates

225

The Needs of Texas Soils for Lime.  

E-Print Network [OSTI]

Department of Agriculture. STS PAGE ............................................. What lime does 5 ............................................. Acidity of soils 7 ............................................. Sources of lime 8... of Texas soils for lime, as far as our present information permits. WHST LIME DOES Lime performs sereral functions in the soil, some of which are favor- able to increased crops and the maintenance of fertility, some favorable to certain crops...

Fraps, G. S. (George Stronach)

1919-01-01T23:59:59.000Z

226

Rangeland Sheet 6 Soil Quality Information Sheet  

E-Print Network [OSTI]

decomposition. Chemically stable organic matter gives soil its dark color and is generally the largest pool. Increasing levels of organic matter promote a higher water- holding capacity, which results in increasedRangeland Sheet 6 Soil Quality Information Sheet Rangeland Soil Quality--Organic Matter USDA

227

4, 38293862, 2007 Mechanisms of soil  

E-Print Network [OSTI]

BGD 4, 3829­3862, 2007 Mechanisms of soil carbon storage S. Steinbeiss et al. Title Page Abstract Biogeosciences Discussions is the access reviewed discussion forum of Biogeosciences Mechanisms of soil carbon­3862, 2007 Mechanisms of soil carbon storage S. Steinbeiss et al. Title Page Abstract Introduction

Boyer, Edmond

228

Sulfate induced heave in lime stabilized soil  

E-Print Network [OSTI]

The addition of hydrated lime to clay soils is one of the most common methods of soil stabilization. However, when sulfates are present in the soil, the calcium in the lime reacts with the sulfates to form ettringite, an expandable mineral...

Bredenkamp, Sanet

1994-01-01T23:59:59.000Z

229

9, 1443714473, 2012 Soil carbon drivers  

E-Print Network [OSTI]

BGD 9, 14437­14473, 2012 Soil carbon drivers and benchmarks in Earth system models K. E. O. Todd if available. Causes of variation in soil carbon predictions from CMIP5 Earth system models and comparison #12;BGD 9, 14437­14473, 2012 Soil carbon drivers and benchmarks in Earth system models K. E. O. Todd

Ickert-Bond, Steffi

230

Agricultural Management Practices And Soil Quality  

E-Print Network [OSTI]

Agricultural Management Practices And Soil Quality: Measuring, assessing, and comparing laboratory and field test kit indicators of soil quality attributes. Publication 452-400 #12;Agricultural Management Associate, respectively, Crop and Soil Environmental Sciences, Virginia Tech #12;1 Introduction What makes

Liskiewicz, Maciej

231

Soil phosphorus status and fertilizer use in select agricutural soils in Nicaragua  

E-Print Network [OSTI]

SOIL PHOSPHORUS STATUS AND FERTILIZER USE IN SELECT AGRICULTURAL SOILS IN NICARAGUA A Thesis by PATRICK G. NIEMEYER Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree... of MASTER OF SCIENCE August 2001 Major Subject: Soil Science SOIL PHOSPHORUS STATUS AND FERTILIZER USE IN SELECT AGRICULTURAL SOILS IN NICARAGUA A Thesis by PATRICK G. NIEMEYER Submitted to Texas A&M University in partial fulfillment...

Niemeyer, Patrick G

2001-01-01T23:59:59.000Z

232

Temperature compensated photovoltaic array  

DOE Patents [OSTI]

A temperature compensated photovoltaic module comprises a series of solar cells having a thermally activated switch connected in parallel with several of the cells. The photovoltaic module is adapted to charge conventional batteries having a temperature coefficient differing from the temperature coefficient of the module. The calibration temperatures of the switches are chosen whereby the colder the ambient temperature for the module, the more switches that are on and form a closed circuit to short the associated solar cells. By shorting some of the solar cells as the ambient temperature decreases, the battery being charged by the module is not excessively overcharged at lower temperatures. PV module is an integrated solution that is reliable and inexpensive. 2 figs.

Mosher, D.M.

1997-11-18T23:59:59.000Z

233

Temperature compensated photovoltaic array  

DOE Patents [OSTI]

A temperature compensated photovoltaic module (20) comprised of a series of solar cells (22) having a thermally activated switch (24) connected in parallel with several of the cells (22). The photovoltaic module (20) is adapted to charge conventional batteries having a temperature coefficient (TC) differing from the temperature coefficient (TC) of the module (20). The calibration temperatures of the switches (24) are chosen whereby the colder the ambient temperature for the module (20), the more switches that are on and form a closed circuit to short the associated solar cells (22). By shorting some of the solar cells (22) as the ambient temperature decreases, the battery being charged by the module (20) is not excessively overcharged at lower temperatures. PV module (20) is an integrated solution that is reliable and inexpensive.

Mosher, Dan Michael (Plano, TX)

1997-11-18T23:59:59.000Z

234

Black Carbon in the Soil Carbon Cycle: Is it an Oxidation Resistant End-Product?  

E-Print Network [OSTI]

for different materials and combustion temperatures. It is less than 1% for thermally altered biomass at combusBlack Carbon in the Soil Carbon Cycle: Is it an Oxidation Resistant End-Product? Simone resistant product of incomplete combustion, and consists out of a range of combustion products such as char

Fischlin, Andreas

235

Soil Science Minor To earn a Soil Science minor, students must complete the following courses to total 27 credits  

E-Print Network [OSTI]

Soil Science Minor To earn a Soil Science minor, students must complete the following courses to total 27 credits: I. Soil Core A. ______SOIL 205.Soil Science (4) or ____ CSS 305. Principles of Soil Science (4) [Taught at EOU La Grande campus only

Grünwald, Niklaus J.

236

Soil microbial biomass: an estimator of soil development in reclaimed lignite mine soil  

E-Print Network [OSTI]

A two-year study was conducted at the Big Brown lignite mine in Fairfield, Texas, to determine the rate and extent of recovery of the soil microbial biomass (SMB) in mixed overburden. The relationships between SMB carbon (SMBC), basal respiration...

Swanson, Eric Scott

1996-01-01T23:59:59.000Z

237

Automatic temperature adjustment apparatus  

DOE Patents [OSTI]

An apparatus for increasing the efficiency of a conventional central space heating system is disclosed. The temperature of a fluid heating medium is adjusted based on a measurement of the external temperature, and a system parameter. The system parameter is periodically modified based on a closed loop process that monitors the operation of the heating system. This closed loop process provides a heating medium temperature value that is very near the optimum for energy efficiency.

Chaplin, James E. (66 Overlook Rd., Bloomingdale, NJ 07403)

1985-01-01T23:59:59.000Z

238

Vitrification testing of soil fines from contaminated Hanford 100 Area and 300 Area soils  

SciTech Connect (OSTI)

The suitability of Hanford soil for vitrification is well known and has been demonstrated extensively in other work. The tests reported here were carried out to confirm the applicability of vitrification to the soil fines (a subset of the Hanford soil potentially different in composition from the bulk soil) and to provide data on the performance of actual, vitrified soil fines. It was determined that the soil fines were generally similar in composition to the bulk Hanford soil, although the fraction <0.25 mm in the 100 Area soil sample appears to differ somewhat from the bulk soil composition. The soil fines are readily melted into a homogeneous glass with the simple additions of CaO and/or Na{sub 2}O. The vitrified waste (plus additives) occupies only 60% of the volume of the initial untreated waste. Leach testing has shown the glasses made from the soil fines to be very durable relative to natural and man-made glasses and has demonstrated the ability of the vitrified waste to greatly reduce the release of radionuclides to the environment. Viscosity and electrical conductivity measurements indicate that the soil fines will be readily processable, although with levels of additives slightly greater than used in the radioactive melts. These tests demonstrate the applicability of vitrification to the contaminated soil fines and the exceptional performance of the waste form resulting from the vitrification of contaminated Hanford soils.

Ludowise, J.D.

1994-05-01T23:59:59.000Z

239

Temperature and RH Targets  

Broader source: Energy.gov [DOE]

Presented by Vishal O Mittal of the Florida Solar Energy Center at the High Temperature Membrane Working Group Meeting, San Francisco, September 14, 2006.

240

Review of soil contamination guidance  

SciTech Connect (OSTI)

A review of existing and proposed radioactive soil contamination standards and guidance was conducted for United Nuclear Corporation (UNC), Office of Surplus Facilities Management. Information was obtained from both government agencies and other sources during a literature survey. The more applicable standards were reviewed, evaluated, and summarized. Information pertaining to soil contamination for both facility operation and facility decommissioning was obtained from a variety of sources. These sources included: the Code of Federal Regulations, regulatory guides, the Federal Register, topical reports written by various government agencies, topical reports written by national laboratories, and publications from the American National Standards Institute (ANSI). It was difficult to directly compare the standards and guidance obtained from these sources since each was intended for a specific situation and different units or bases were used. However, most of the information reviewed was consistent with the philosophy of maintaining exposures at levels as low as reasonably achievable (ALARA).

Mueller, M.A.; Kennedy, W.E. Jr.; Soldat, J.K.

1981-08-01T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


241

An investigation of soil-tool interaction theories as they apply to a Lunar soil simulant  

E-Print Network [OSTI]

developed for finding the force required to fail soil with a blade, given the appropriate parameters of the blade, the soil, and their interaction. The properties of interest in the Lunar soil are presented in this thesis. Then the parameters of a... terrestrial analog of the true Lunar soil is determined. Given these, the predictive models are implemented to predict the required force to fail the Lunar soil simulant with a flat blade. An apparatus is developed to fail the prepared Lunar soil simulant...

Willman, Brian Michael

1992-01-01T23:59:59.000Z

242

A new method for the experimental heating of intact soil profiles for application to climate change experiments  

SciTech Connect (OSTI)

Advanced facilities are needed to evaluate the response of complex ecosystems to projected unique climate conditions not observable in the context of current natural variation or through the use of climate gradients. A next-generation, experimental system for simulating future belowground temperature increases was conceived, simulated, constructed and tested in a temperate deciduous forest in Oak Ridge, Tennessee, USA. The new system uses low-wattage, 3-m deep, circumferentially-installed heaters surrounding a defined soil volume to both add the necessary energy to support a set-point soil temperature differential within the treatment area and to add exterior energy inputs equal to that which might be lost from lateral heat conduction. This approach, which is designed to work in conjunction with aboveground heated chambers, requires only two control positions, (1) aboveground air temperatures at 1 m and (2) belowground temperatures at 0.8 m. The approach is capable of achieving in situ target temperature differentials in the tested range of +4.0 0.5 C for soils to a measured depth of -2 m located within the aboveground boundary for air heating. These differentials were sustained throughout 2009, and both diurnal and seasonal cycles at all soil depths were retained using this simple heating approach. Measured mean energy inputs required to sustain the target heating level of +4 C over the 7.1 m2 target area were substantial: 21.1 kW h d-1 m-2 for aboveground heating but 16 times lower for belowground heaters at 1.3 kW h d-1 m-2. Observations of soil CO2 efflux from the surface of the target soil volumes showed CO2 losses throughout 2009 that were elevated above the temperature response curve for control CO2 losses at levels greater than have been reported in previous soil warming studies. Stimulation of biological activity of previously undisturbed deep-soil carbon stocks is the expected source. Long-term research programs may be able to apply similar experimental systems to address uncertainties in process-level responses of microbial, plant, and animal communities in whole, intact ecosystems using this new heating method that capture expected future warming and temperature dynamics throughout the soil profile.

Hanson, Paul J [ORNL; Childs, Kenneth W [ORNL; Wullschleger, Stan D [ORNL; Riggs, Jeffery S [ORNL; Thomas, Warren Kyle [ORNL; Todd Jr, Donald E [ORNL; Warren, Jeffrey [ORNL

2011-01-01T23:59:59.000Z

243

Fiber optic temperature sensor  

SciTech Connect (OSTI)

Our fiber optic temperature measurement sensor and system is a major improvement over methods currently in use in most industrial processes, and it delivers all of the attributes required simplicity, accuracy, and cost efficiency-to help improve all of these processes. Because temperature is a basic physical attribute of nearly every industrial and commercial process, our system can eventually result in significant improvements in nearly every industrial and commercial process. Many finished goods, and the materials that go into them, are critically dependent on the temperature. The better the temperature measurement, the better quality the goods will be and the more economically they can be produced. The production and transmission of energy requires the monitoring of temperature in motors, circuit breakers, power generating plants, and transmission line equipment. The more reliable and robust the methods for measuring these temperature, the more available, stable, and affordable the supply of energy will become. The world is increasingly realizing the threats to health and safety of toxic or otherwise undesirable by products of the industrial economy in the environment. Cleanup of such contamination often depends on techniques that require the constant monitoring of temperature in extremely hazardous environments, which can damage most conventional temperature sensors and which are dangerous for operating personnel. Our system makes such monitoring safer and more economical.

Rabold, D.

1995-12-01T23:59:59.000Z

244

High temperature probe  

DOE Patents [OSTI]

A high temperature probe for sampling, for example, smokestack fumes, and is able to withstand temperatures of 3000.degree. F. The probe is constructed so as to prevent leakage via the seal by placing the seal inside the water jacket whereby the seal is not exposed to high temperature, which destroys the seal. The sample inlet of the probe is also provided with cooling fins about the area of the seal to provide additional cooling to prevent the seal from being destroyed. Also, a heated jacket is provided for maintaining the temperature of the gas being tested as it passes through the probe. The probe includes pressure sensing means for determining the flow velocity of an efficient being sampled. In addition, thermocouples are located in various places on the probe to monitor the temperature of the gas passing there through.

Swan, Raymond A. (Fremont, CA)

1994-01-01T23:59:59.000Z

245

Thermal Removal Of Tritium From Concrete And Soil To Reduce Groundwater Impacts  

SciTech Connect (OSTI)

Legacy heavy-water moderator operations at the Savannah River Site (SRS) have resulted in the contamination of equipment pads, building slabs, and surrounding soil with tritium. At the time of discovery the tritium had impacted the shallow (< 3-m) groundwater at the facility. While tritium was present in the groundwater, characterization efforts determined that a significant source remained in a concrete slab at the surface and within the associated vadose zone soils. To prevent continued long-term impacts to the shallow groundwater a CERCLA non-time critical removal action for these source materials was conducted to reduce the leaching of tritium from the vadose zone soils and concrete slabs. In order to minimize transportation and disposal costs, an on-site thermal treatment process was designed, tested, and implemented. The on-site treatment consisted of thermal detritiation of the concrete rubble and soil. During this process concrete rubble was heated to a temperature of 815 deg C (1,500 deg F) resulting in the dehydration and removal of water bound tritium. During heating, tritium contaminated soil was used to provide thermal insulation during which it's temperature exceeded 100 deg C (212 deg F), causing drying and removal of tritium. The thermal treatment process volatiles the water bound tritium and releases it to the atmosphere. The released tritium was considered insignificant based upon Clean Air Act Compliance Package (CAP88) analysis and did not exceed exposure thresholds. A treatability study evaluated the effectiveness of this thermal configuration and viability as a decontamination method for tritium in concrete and soil materials. Post treatment sampling confirmed the effectiveness at reducing tritium to acceptable waste site specific levels. With American Recovery and Reinvestment Act (ARRA) funding three additional treatment cells were assembled utilizing commercial heating equipment and common construction materials. This provided a total of four units to batch treat concrete rubble and soil. Post treatment sampling verified that the activity in the treated soil and concrete met the treatment standards for each medium which allowed the treated concrete rubble and soil to be disposed of on site as backfill. During testing and operations a total of 1,261-m{sup 3} (1,650-yd{sup 3}) of contaminated concrete and soils were treated with an actual incurred cost of $3,980,000. This represents a unit treatment cost of $3,156/m{sup 3} ($2,412/yd{sup 3}). In 2011 the project was recognized with an e-Star Sustainability Award by DOE's Office of Environmental Management.

Jackson, Dennis G.; Blount, Gerald C.; Wells, Leslie H.; Cardoso-Neto, Joao E.; Kmetz, Thomas F.; Reed, Misty L.

2012-12-04T23:59:59.000Z

246

Thermal Removal of Tritium from Concrete and Soil to Reduce Groundwater Impacts - 13197  

SciTech Connect (OSTI)

Legacy heavy-water moderator operations at the Savannah River Site (SRS) have resulted in the contamination of equipment pads, building slabs, and surrounding soil with tritium. At the time of discovery the tritium had impacted the shallow (< 3-m) groundwater at the facility. While tritium was present in the groundwater, characterization efforts determined that a significant source remained in a concrete slab at the surface and within the associated vadose zone soils. To prevent continued long-term impacts to the shallow groundwater a CERCLA non-time critical removal action for these source materials was conducted to reduce the leaching of tritium from the vadose zone soils and concrete slabs. In order to minimize transportation and disposal costs, an on-site thermal treatment process was designed, tested, and implemented. The on-site treatment consisted of thermal detritiation of the concrete rubble and soil. During this process concrete rubble was heated to a temperature of 815 deg. C (1,500 deg. F) resulting in the dehydration and removal of water bound tritium. During heating, tritium contaminated soil was used to provide thermal insulation during which it's temperature exceeded 100 deg. C (212 deg. F), causing drying and removal of tritium. The thermal treatment process volatiles the water bound tritium and releases it to the atmosphere. The released tritium was considered insignificant based upon Clean Air Act Compliance Package (CAP88) analysis and did not exceed exposure thresholds. A treatability study evaluated the effectiveness of this thermal configuration and viability as a decontamination method for tritium in concrete and soil materials. Post treatment sampling confirmed the effectiveness at reducing tritium to acceptable waste site specific levels. With American Recovery and Reinvestment Act (ARRA) funding three additional treatment cells were assembled utilizing commercial heating equipment and common construction materials. This provided a total of four units to batch treat concrete rubble and soil. Post treatment sampling verified that the activity in the treated soil and concrete met the treatment standards for each medium which allowed the treated concrete rubble and soil to be disposed of on-site as backfill. During testing and operations a total of 1,261-m{sup 3} (1,650-yd{sup 3}) of contaminated concrete and soils were treated with an actual incurred cost of $3,980,000. This represents a unit treatment cost of $3,156/m{sup 3} ($2,412/yd{sup 3}). In 2011 the project was recognized with an e-Star Sustainability Award by DOE's Office of Environmental Management. (authors)

Jackson, Dennis G. [Savannah River National Laboratory, Building 773-42A, Aiken, South Carolina 29808 (United States)] [Savannah River National Laboratory, Building 773-42A, Aiken, South Carolina 29808 (United States); Blount, Gerald C. [Savannah River Nuclear Solutions (United States)] [Savannah River Nuclear Solutions (United States); Wells, Leslie H.; Cardoso, Joao E.; Kmetz, Thomas F.; Reed, Misty L. [U.S Department of Energy-Savannah River Site (United States)] [U.S Department of Energy-Savannah River Site (United States)

2013-07-01T23:59:59.000Z

247

Soil Erosion and Sediment Control Act, Soil and Water Conservation District, and Council on Soil and Water Conservation Regulations (Connecticut)  

Broader source: Energy.gov [DOE]

These regulations establish Soil and Water Conservation Districts throughout the State of Connecticut. Each district has its own Board of Directors; membership and election procedures are defined...

248

Leaf water potential in Pinus taeda L. as related to fluctuating soil water and atmospheric conditions  

E-Print Network [OSTI]

growing on Bienville loamy fine sand near Rusk, Texas. The average available water storage capacity was 9. 50 inches in the 8-foot profile. Siruiltaneous measurements of leaf water potential and environmental variables were made weekly at two hour... pressure 2 deficit, temperature, and wind (R 0. 78). A regression equation relating total daily water stress to only vapor pressure deficit and soil water content in the 0- to 4-foot soil layer was also signifi- 2= cant (R = 0. 76). The total daily...

Ellison, Stanley Lee

1969-01-01T23:59:59.000Z

249

Age-dating implications from the morphologic, petrologic, and isotopic investigations of a calcic soil, Terrell County, Texas  

E-Print Network [OSTI]

previously used to estimate local ambient temperatures from calcic soils, where the isotopic temperature derived from recent pedogenic carbonate m soils on the Fort Bliss military reserve in Texas and New Mexico closely matched the area's average annual... on the Stockton Plateau and for Roswell, NM (NOAA, 1991). Location Fort Stockton TX Sanderson TX Rostsctt NM Mean Annual Temp ('F) Mean Annual Precip. (in) Mean January Temp. ('1') Mean August. Temp ('F) 64. 1 12 21 44. 4 79. 8 65 7 12. 56 45 4 80. 4...

Jolley, Darren Manning

1994-01-01T23:59:59.000Z

250

The behavior of soil-applied cyclotri- and cyclotetraphosphate in Texas soils  

E-Print Network [OSTI]

Cyclotriphosphate (C3P) is of interest to soil scientists because it demonstrates little or no retention by soil constituents. Non-sorption is desirable in the development of mobile P fertilizers. Work was expanded to include cyclotetraphosphate...

Trostle, Calvin Lewie

2012-06-07T23:59:59.000Z

251

Soil macroaggregate dynamics in a mountain spatial climate gradient  

E-Print Network [OSTI]

Soil macroaggregate dynamics in a mountain spatial climate gradient Lauric Cécillon1,2,* , Nilvania://lauric.cecillon.free.fr/ Key words: Mountain soils; Climate change; Soil aggregation; Soil organic matter; Near infrared reflectance spectroscopy; Soil threats Biogeochemistry 97: 31-43 (2010) http://dx.doi.org/10.1007/s10533

Paris-Sud XI, Université de

252

Soil maps of Wisconsin Alfred E. Hartemink a,  

E-Print Network [OSTI]

Soil maps of Wisconsin Alfred E. Hartemink a, , Birl Lowery a , Carl Wacker b a University of Wisconsin-Madison, Department of Soil Science, FD Hole Soils Lab, 1525 Observatory Drive, Madison, WI 53706 May 2012 Accepted 15 May 2012 Available online xxxx Keywords: Soil maps Historical maps Digital soil

Mladenoff, David

253

CROP & SOIL SCIENCES Statewide Variety Testing Program Coordinator  

E-Print Network [OSTI]

CROP & SOIL SCIENCES Statewide Variety Testing Program Coordinator Committee Membership Dr. Jerry Johnson - committee chair Dr. Paul Raymer Department of Crop & Soil Sciences Department of Crop & Soil Department of Crop & Soil Sciences Department of Crop & Soil Sciences University of Georgia University

Arnold, Jonathan

254

Expanded Course Description for 11:776:413 Soil Quality  

E-Print Network [OSTI]

Soil Quality: soil management & sustainability, concept of best management practices (BMPs) Soil and restoration of desirable properties will be addressed. Management of our soil resource to maintain or improve soil quality and maximize ecosystem sustainability will be emphasized. Learning Goals: To gain full

Chen, Kuang-Yu

255

SOIL QUALITY (SWS 6134) 3 Credits-Fall 2014  

E-Print Network [OSTI]

with basic concepts, principles, components, measurements, and evaluation of soil quality and its management for sustainable agriculture. Soil quality is the capacity of the soil to function within the ecosystem boundaries. In this course, state-of-the-art studies on soil quality and the principles, assessment and management of soil

Ma, Lena

256

The Chemical Composition of Some Texas Soils.  

E-Print Network [OSTI]

TEXAS AGRICULTURAL ESPERlMENT STATIONS. ______-_________- _-__---- - -. - _ _._ __ BULLETlN NO. 100. Chemical Section, Dec., 1907. The Chemical Composition of Some Texas Soils BY G. S. FRAPS, 'Ph. D., Chemist. POSTOFFICE COLLEGE STATION.... The postoffice address is College, Station, Texas. Reports and bulletins are sent free upon application to the Director. THE CHEMICAL COMPOSITION OF SOME TEXAS SOILS. BY G. S. FRAPS. This bulletin is a popular account of a study of a nnmber of Texas soils...

Fraps, G. S. (George Stronach)

1907-01-01T23:59:59.000Z

257

Water as a Reagent for Soil Remediation  

SciTech Connect (OSTI)

SRI International conducted experiments in a two-year, two-phase process to develop and evaluate hydrothermal extraction technology, also known as hot water extraction (HWE) technology, for remediating petroleum-contaminated soils. The bench-scale demonstration of the process has shown great promise, and the implementation of this technology will revolutionize the conventional use of water in soil remediation technologies and provide a standalone technology for removal of both volatile and heavy components from contaminated soil.

Jayaweera, Indira S.; Marti-Perez, Montserrat; Diaz-Ferrero, Jordi; Sanjurjo, Angel

2003-03-06T23:59:59.000Z

258

High Temperature Capacitor Development  

SciTech Connect (OSTI)

The absence of high-temperature electronics is an obstacle to the development of untapped energy resources (deep oil, gas and geothermal). US natural gas consumption is projected to grow from 22 trillion cubic feet per year (tcf) in 1999 to 34 tcf in 2020. Cumulatively this is 607 tcf of consumption by 2020, while recoverable reserves using current technology are 177 tcf. A significant portion of this shortfall may be met by tapping deep gas reservoirs. Tapping these reservoirs represents a significant technical challenge. At these depths, temperatures and pressures are very high and may require penetrating very hard rock. Logistics of supporting 6.1 km (20,000 ft) drill strings and the drilling processes are complex and expensive. At these depths up to 50% of the total drilling cost may be in the last 10% of the well depth. Thus, as wells go deeper it is increasingly important that drillers are able to monitor conditions down-hole such as temperature, pressure, heading, etc. Commercial off-the-shelf electronics are not specified to meet these operating conditions. This is due to problems associated with all aspects of the electronics including the resistors and capacitors. With respect to capacitors, increasing temperature often significantly changes capacitance because of the strong temperature dependence of the dielectric constant. Higher temperatures also affect the equivalent series resistance (ESR). High-temperature capacitors usually have low capacitance values because of these dielectric effects and because packages are kept small to prevent mechanical breakage caused by thermal stresses. Electrolytic capacitors do not operate at temperatures above 150oC due to dielectric breakdown. The development of high-temperature capacitors to be used in a high-pressure high-temperature (HPHT) drilling environment was investigated. These capacitors were based on a previously developed high-voltage hybridized capacitor developed at Giner, Inc. in conjunction with a unique high-temperature electrolyte developed during the course of the program. During this program the feasibility of operating a high voltage hybridized capacitor at 230oC was demonstrated. Capacitor specifications were established in conjunction with potential capacitor users. A method to allow for capacitor operation at both ambient and elevated temperatures was demonstrated. The program was terminated prior to moving into Phase II due to a lack of cost-sharing funds.

John Kosek

2009-06-30T23:59:59.000Z

259

Metal behavior during fluidized bed thermal treatment of soil  

SciTech Connect (OSTI)

The Superfund dumpsites are frequently composed of soils contaminated with hazardous organic constituents and toxic heavy metals. While thermal treatment is an effective method of remediating the contaminated soils, the major environmental concerns are the emissions of toxic metal fumes during the treatment and the leaching of metals from the treated soil. The US EPA has reported that metals can account for almost all of the identified cancer risks from waste incineration systems. Research leading to better understanding of their behavior and better controlling of their emissions is urgently needed. In this study, the behavior of metals during the fluidized bed thermal treatment of artificially prepared metal-contaminated clay was experimentally and theoretically investigated. The objective of the study was to evaluate the effects of operating conditions on metal volatilization and metal leachability associated with the process. Metal experiments were carried out in a well instrumented 76 mm (3 inch) i.d. fluidized bed incinerator. The metals involved were compounds of lead and cadmium and the operating parameters included metal concentration, air flow rate, treatment temperature and treatment duration. The observed results indicated that metal volatilization is mainly a function of treatment temperature and treatment duration. The degree of volatilization was observed to range from 5 to 40% depending on the operating conditions. Cadmium leachability was observed to be relatively high compared to that of lead. In addition to the experimental study, a theoretical model based on the laws of heat and mass transfer operations and reaction kinetics was derived to simulate the metal volatilization process. The derived model was found to predict reasonably well the experimental observations.

Ho, T.C.; Lee, H.T.; Shiao, C.C.; Hopper, J.R. [Lamar Univ., Beaumont, TX (United States). Dept. of Chemical Engineering] [Lamar Univ., Beaumont, TX (United States). Dept. of Chemical Engineering; Bostick, W.D. [Martin Marietta Energy Systems, Inc., Oak Ridge, TN (United States). Chemistry Dept.] [Martin Marietta Energy Systems, Inc., Oak Ridge, TN (United States). Chemistry Dept.

1995-12-31T23:59:59.000Z

260

Performance evaluation soil samples utilizing encapsulation technology  

DOE Patents [OSTI]

Performance evaluation soil samples and method of their preparation uses encapsulation technology to encapsulate analytes which are introduced into a soil matrix for analysis and evaluation by analytical laboratories. Target analytes are mixed in an appropriate solvent at predetermined concentrations. The mixture is emulsified in a solution of polymeric film forming material. The emulsified solution is polymerized to form microcapsules. The microcapsules are recovered, quantitated and introduced into a soil matrix in a predetermined ratio to form soil samples with the desired analyte concentration. 1 fig.

Dahlgran, J.R.

1999-08-17T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


261

Performance evaluation soil samples utilizing encapsulation technology  

DOE Patents [OSTI]

Performance evaluation soil samples and method of their preparation using encapsulation technology to encapsulate analytes which are introduced into a soil matrix for analysis and evaluation by analytical laboratories. Target analytes are mixed in an appropriate solvent at predetermined concentrations. The mixture is emulsified in a solution of polymeric film forming material. The emulsified solution is polymerized to form microcapsules. The microcapsules are recovered, quantitated and introduced into a soil matrix in a predetermined ratio to form soil samples with the desired analyte concentration.

Dahlgran, James R. (Idaho Falls, ID)

1999-01-01T23:59:59.000Z

262

Microbial and Mineralogical Characterizations of Soils Collected...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

gold mines. Citation: Rastogi G, S Osman, RK Kukkadapu, MH Engelhard, PA Vaishampayan, GL Andersen, and RK Sani.2010."Microbial and Mineralogical Characterizations of Soils...

263

Tank farm backlog soil sample analysis plan  

SciTech Connect (OSTI)

This document describes the measures to collect samples, perform testing on samples, and make decisions to obtain a Contained- in Determination for tank farms backlog soil.

Ahlers, J.D., Westinghouse Hanford

1996-07-17T23:59:59.000Z

264

Pullman Soils: Distribution, Importance, Variability, and Management.  

E-Print Network [OSTI]

soils in Texas is bounded by the New Mexico-Texas state line on the west, the Canadian River on the north, and the caprock escarpment at the High Plains-Rolling Plains boundary on the east. A catena of loamy soils extending from Farwell to near...). The portions of different counties occupied by Pullman soil range from about 0.1 to 70 percent (Table 2). The area of Pullman soils is bounded by the New Mexico- Texas state line on the west, the caprock escarpment at the Canadian River on the north...

Unger, Paul W.; Pringle, Fred B

1981-01-01T23:59:59.000Z

265

Elevated CO2 stimulates grassland soil respiration by increasing carbon inputs rather than by enhancing soil  

E-Print Network [OSTI]

Elevated CO2 stimulates grassland soil respiration by increasing carbon inputs rather than It is not clear whether the consistent positive effect of elevated CO2 on soil respiration (soil carbon flux, SCF) results from increased plant and microbial activity due to (i) greater C availability through CO2-induced

Minnesota, University of

266

Applied Soil Ecology 21 (2002) 7188 Soil invertebrate and microbial communities, and decomposition  

E-Print Network [OSTI]

Applied Soil Ecology 21 (2002) 71­88 Soil invertebrate and microbial communities, and decomposition. Spongberg Department of Earth, Ecological and Environmental Sciences, University of Toledo, Toledo, OH 43606 for quantification of ecological impact of chemical contamination of soils. This study examined the effects

Neher, Deborah A.

267

Soil Science Society of America Journal Soil Sci. Soc. Am. J. 76:23272341  

E-Print Network [OSTI]

Soil Science Society of America Journal Soil Sci. Soc. Am. J. 76:2327­2341 doi:10.2136/sssaj2012.0043 Received 3 Feb. 2012. *Corresponding author (sabgru@ufl.edu). © Soil Science Society of America, 5585 or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any

Grunwald, Sabine

268

Soil compaction: track induced soil stress isn't so positive in comparison with tyre  

E-Print Network [OSTI]

Soil compaction: track induced soil stress isn't so positive in comparison with tyre Ingeniors presence and the overall higher load of the track system. Conversely, tyres distribute uniformly the load the easy to obtain contact area surface of the track -or tyre- with the soil, the interface pressure

Boyer, Edmond

269

Part I. Ecological Sites and Soil Part II. A Framework for Soil and  

E-Print Network [OSTI]

on management (states) (1) (2) (3) (4) (6) (5) #12;State and transition models, by definition, include soil #12;Part II. Ecological sites and state and transition models: A framework for soil and vegetation dynamics and management #12;The soil survey is the foundation of the ecological site inventory process

270

Soil Science Society of America Journal Soil Sci. Soc. Am. J. 78:14581468  

E-Print Network [OSTI]

. Ithaca, NY 14853 John J. Battles Dep. of Environmental Science, Policy and Management Univ. of California was transported downward through the forest floor and upper mineral soil in a progressive fashion. By Year 11Soil Science Society of America Journal Soil Sci. Soc. Am. J. 78:1458­1468 doi:10.2136/sssaj2014

Battles, John

271

EFFECTS OF COMPOST AND LIME APPLICATION ON SOIL CHEMICAL PROPERTIES, SOIL MICROBIAL COMMUNITY, AND FUSARIUM WILT IN  

E-Print Network [OSTI]

1 EFFECTS OF COMPOST AND LIME APPLICATION ON SOIL CHEMICAL PROPERTIES, SOIL MICROBIAL COMMUNITY compost as an antagonistic suppression approach to combat soil-borne disease effects on crop yields the effect of compost and lime on soil chemical properties, the soil microbial community (including Fusarium

Ma, Lena

272

Low temperature cryoprobe  

DOE Patents [OSTI]

A portable, hand held probe usable within a small confine to produce a point source of nitrogen or helium at a relatively constant temperatures of 77 degrees Kelvin, is discussed. 3 figs.

Sungaila, Z.F.

1988-04-12T23:59:59.000Z

273

High-Temperature Superconductivity  

ScienceCinema (OSTI)

Like astronomers tweaking images to gain a more detailed glimpse of distant stars, physicists at Brookhaven National Laboratory have found ways to sharpen images of the energy spectra in high-temperature superconductors ? materials that carry electrical c

Peter Johnson

2010-01-08T23:59:59.000Z

274

Elevated temperature crack propagation  

SciTech Connect (OSTI)

This paper is a summary of two NASA contracts on high temperature fatigue crack propagation in metals. The first evaluated the ability of fairly simple nonlinear fracture parameters to correlate crack propagation. Hastelloy-X specimens were tested under isothermal and thermomechanical cycling at temperatures up to 980 degrees C (1800 degrees F). The most successful correlating parameter was the crack tip opening displacement derived from the J-integral. The second evaluated the ability of several path-independent integrals to correlate crack propagation behavior. Inconel 718 specimens were tested under isothermal, thermomechanical, temperature gradient, and creep conditions at temperatures up to 650 degrees C (1200 degrees F). The integrals formulated by Blackburn and by Kishimoto correlated the data reasonably well under all test conditions.

Orange, T.W.

1994-02-01T23:59:59.000Z

275

Penrose Well Temperatures  

SciTech Connect (OSTI)

Penrose Well Temperatures Geothermal waters have been encountered in several wells near Penrose in Fremont County, Colorado. Most of the wells were drilled for oil and gas exploration and, in a few cases, production. This ESRI point shapefile utilizes data from 95 wells in and around the Penrose area provided by the Colorado Oil and Gas Conservation Commission (COGCC) database at http://cogcc.state.co.us/ . Temperature data from the database were used to calculate a temperature gradient for each well. This information was then used to estimate temperatures at various depths. Projection: UTM Zone 13 NAD27 Extent: West -105.224871 East -105.027633 North 38.486269 South 38.259507 Originators: Colorado Oil and Gas Conservation Commission (COGCC) Karen Christopherson

Christopherson, Karen

2013-03-15T23:59:59.000Z

276

High temperature pressure gauge  

DOE Patents [OSTI]

A high temperature pressure gauge comprising a pressure gauge positioned in fluid communication with one end of a conduit which has a diaphragm mounted in its other end. The conduit is filled with a low melting metal alloy above the diaphragm for a portion of its length with a high temperature fluid being positioned in the remaining length of the conduit and in the pressure gauge.

Echtler, J. Paul (Pittsburgh, PA); Scandrol, Roy O. (Library, PA)

1981-01-01T23:59:59.000Z

277

Evaluation of Snow Depth and Soil Temperatures Predicted by the HydroThermodynamic SoilVegetation Scheme Coupled with the  

E-Print Network [OSTI]

. Discrepancies between predicted and observed snow- depth changes relate to the coupling. Enhanced water supply to the atmosphere, which results from water that was assumed to be open in MM5 but was actually ice covered also lead to snowfall where none occurred. For heavy snowfall the performance of the coupled model

Moelders, Nicole

278

Soil-landscape model helps predict potassium supply in vineyards  

E-Print Network [OSTI]

for making and inter- preting soil surveys (2nd ed. ). USDA-K S, V, K Depth inches Color* moist soil Sand Silt Clay Claymineralogy† pH CEC cmol(+)/kg soil‡ Exchangeable K K

O'Geen, Anthony T; Pettygrove, Stuart; Southard, Randal; Minoshima, Hideomi; Verdegaal, Paul S.

2008-01-01T23:59:59.000Z

279

Storage and turnover of organic matter in soil  

E-Print Network [OSTI]

of organic carbon from peat soils. Nature 412 , 785. Fried,Plant Litter. Standard Soil Methods for Long-Term Ecological2007). Role of proteins in soil carbon and nitrogen storage:

Torn, M.S.

2009-01-01T23:59:59.000Z

280

Soils Management, Site Productivity and Forest Nutrition: Nutrient Balance  

E-Print Network [OSTI]

;#12;1) principals 2) strategies 3) implementation Sustainable Soil Management: #12;- maintenance of fertility soil management Strategies: #12;Examples of adaptive management models used for achieving sustainableSoils Management, Site Productivity and Forest Nutrition: Nutrient Balance and Availability

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


281

Soil Hydraulic Characteristics of a Small Southwest Oregon Watershed Following  

E-Print Network [OSTI]

--------------------------------------------- Soil Hydraulic Characteristics of a Small Southwest by a high-intensity burn over areas of steep topography. The areal distribution of soil hydraulic of infiltration capacity, saturated hydraulic conductivity, and soil moisture characteristics. Also, measures

Standiford, Richard B.

282

Experiment Hazard Class 15.2 - USDA Soil Permit  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

shipment, and disposal of regulated soil samples. A copy of the current APS USDA Soil Permit must accompany all samples. A copy of the home institution's soil permit is required...

283

Acid soil fertility at the Cinzana station, Mali, West Africa  

E-Print Network [OSTI]

that may be associated with acid soil infertility include biological organisms (nematodes, termites), restrictive subsoil layers (claypans, ironpans, silt pans, plow pans, etc. ), soil erosion, zones of low soil moisture retention, and other physical...

Doumbia, Mamadou Diosse

1990-01-01T23:59:59.000Z

284

Manoj Shukla Assistant Professor of Environmental Soil Physics,  

E-Print Network [OSTI]

Manoj Shukla Assistant Professor of Environmental Soil Physics, Plant and Environmental Sciences University, India Professional Experience 2005-Present Assistant Professor of Environmental Soil Physics, New Interests Assessment and modeling of chemical fate and transport and physical, chemical properties of soil

Johnson, Eric E.

285

Using soil sensing technology to examine interactions and controls between ectomycorrhizal growth and environmental factors on soil CO2 dynamics  

E-Print Network [OSTI]

Plant Soil (2010) 331:17–29 DOI 10.1007/s11104-y REGULAR ARTICLE Using soil sensing technology to examineand environmental factors on soil CO 2 dynamics Niles J.

Hasselquist, Niles J.; Vargas, Rodrigo; Allen, Michael F.

2010-01-01T23:59:59.000Z

286

Accumulation and replacement of exchangeable sodium in soils of Southeast Texas under turfgrass and its effect on soil infiltration rate  

E-Print Network [OSTI]

in soils of this area. This study assessed the degree of Na accumulation on cation exchange sites as affected by gypsum treatments in soils that support turfgrass (bermudagrass) and the response of soil infiltration rate to different rates of gypsum...

Aydemir, Salih

2012-06-07T23:59:59.000Z

287

Relating the Expression of Soil Redoximorphic Features to Soil Texture, pH, and Cation Exchange Capacity  

E-Print Network [OSTI]

Three laboratory studies were performed to elucidate the influence of soil texture, pH, and cation exchange capacity (CEC) on the concentration of ferrous Fe in soil solution and the resulting expression of soil redoximorphic features...

Mersmann, Ryan S.

2010-01-14T23:59:59.000Z

288

19th World Congress of Soil Science, Soil solutions for a changing world, Brisbane, Australia 1-6 August 2010  

E-Print Network [OSTI]

). The investigated ES were climate regulation through carbon sequestration in soil and biomass, soil conservation of these results are discussed. Key Words Land use change, socioeconomic drivers, carbon sequestration, soil

Boyer, Edmond

289

Process for removing polychlorinated biphenyls from soil  

DOE Patents [OSTI]

The present invention relates to a method of removing polychlorinated biphenyls from soil. The polychlorinated biphenyls are extracted from the soil by employing a liquid organic solvent dispersed in water in the ratio of about 1:3 to 3:1. The organic solvent includes such materials as short-chain hydrocarbons including kerosene or gasoline which are immiscible with water and are nonpolar. The organic solvent has a greater affinity for the PCB's than the soil so as to extract the PCB's from the soil upon contact. The organic solvent phase is separated from the suspended soil and water phase and distilled for permitting the recycle of the organic solvent phase and the concentration of the PCB's in the remaining organic phase. The present process can be satisfactorily practiced with soil containing 10 to 20% petroleum-based oils and organic fluids such as used in transformers and cutting fluids, coolants and the like which contain PCB's. The subject method provides for the removal of a sufficient concentration of PCB's from the soil to provide the soil with a level of PCB's within the guidelines of the Environmental Protection Agency.

Hancher, C.W.; Saunders, M.B.; Googin, J.M.

1984-11-16T23:59:59.000Z

290

CSMRI Bagged Soil Disposal Summary Report  

E-Print Network [OSTI]

of radioactive/metals-contaminated soils and similar soils to a solid waste landfill in a letter dated August 26 Radioactive Materials License No. 1094-01. This document serves to provide a summary of the disposal as well. During the 2004 remediation work, approximately 1,870 cubic yards (cy) of radioactive

291

Forests and soil UK Forestry Standard Guidelines  

E-Print Network [OSTI]

; forestry; soil; sustainable forest management; UK Forestry Standard. FCGL006/FC-GB(MMJ)/JCTP-2.5K/NOV11 for sustainable forest management Good forestry practice requirement Element of SFM Reference number LegalForests and soil UK Forestry Standard Guidelines #12;Key to symbols UKFS Requirements

292

Carbon and Nitrogen Dynamics in Agricultural Soils  

E-Print Network [OSTI]

support in a precision farming context. Keywords: Carbon balances, carbon sequestration, decompositionCarbon and Nitrogen Dynamics in Agricultural Soils Model Applications at Different Scales in Time Print: SLU Service/Repro, Uppsala 2012 #12;Carbon and Nitrogen Dynamics in Agricultural Soils. Model

293

Analysis of large soil samples for actinides  

SciTech Connect (OSTI)

A method of analyzing relatively large soil samples for actinides by employing a separation process that includes cerium fluoride precipitation for removing the soil matrix and precipitates plutonium, americium, and curium with cerium and hydrofluoric acid followed by separating these actinides using chromatography cartridges.

Maxwell, III; Sherrod L. (Aiken, SC)

2009-03-24T23:59:59.000Z

294

NNSS Soils Monitoring: Plutonium Valley (CAU366)  

SciTech Connect (OSTI)

The U.S. Department of Energy (DOE) National Nuclear Security Administration (NNSA), Nevada Site Office (NSO), Environmental Restoration Soils Activity has authorized the Desert Research Institute (DRI) to conduct field assessments of potential sediment transport of contaminated soil from Corrective Action Unit (CAU) 366, Area 11 Plutonium Valley Dispersion Sites Contamination Area (CA) during precipitation runoff events.

Miller Julianne J.,Mizell Steve A.,Nikolich George, Campbell Scott

2012-02-01T23:59:59.000Z

295

DIGITAL SOIL RESOURCE INVENTORIES: STATUS AND PROSPECTS  

E-Print Network [OSTI]

DIGITAL SOIL RESOURCE INVENTORIES: STATUS AND PROSPECTS D G Rossiter Department of Earth Systems an inventory of digital soils data and supporting information available or publicized on the World Wide Web-scale inventories, especially using the SOTER methodology. Large-scale digital data are limited to the USA, Canada

Rossiter, D G "David"

296

CCA Training : Soil and Water Management  

E-Print Network [OSTI]

dry 25,000,000 acresa Includes both external surfaces and surfaces between crystal plates. #12;The and nutrient transformations · Associated with soil porosity #12;Soil Physical Properties: Structure Properties: Structure · Structure type = aggregation has different shape and varies with depth ­Granular

Balser, Teri C.

297

Soil and Groundwater Cleanup - In-Situ Grouting, Lessons Learned...  

Energy Savers [EERE]

Soil and Groundwater Cleanup - In-Situ Grouting, Lessons Learned (Post CD-4), Environmental Management Cleanup, May 2011 Soil and Groundwater Cleanup - In-Situ Grouting, Lessons...

298

Rocky Flats Environmental Technology Site Archived Soil & Groundwater...  

Office of Environmental Management (EM)

Rocky Flats Environmental Technology Site Archived Soil & Groundwater Master Reports Rocky Flats Environmental Technology Site Archived Soil & Groundwater Master Reports Rocky...

299

Microbial communities acclimate to recurring changes in soil...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

communities acclimate to recurring changes in soil redox potential status. Microbial communities acclimate to recurring changes in soil redox potential status. Abstract: Rapidly...

300

Contingency in the Direction and Mechanics of Soil Organic Matter...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Contingency in the Direction and Mechanics of Soil Organic Matter Responses to Increased Rainfall. Contingency in the Direction and Mechanics of Soil Organic Matter Responses to...

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


301

Persistence of soil organic matter in eroding versus depositional...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Persistence of soil organic matter in eroding versus depositional landform positions. Persistence of soil organic matter in eroding versus depositional landform positions....

302

Vadose Zone Soil Moisture Wicking Using Super Absorbent Polymers...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Vadose Zone Soil Moisture Wicking Using Super Absorbent Polymers. Vadose Zone Soil Moisture Wicking Using Super Absorbent Polymers. Abstract: Super-absorbent polymers (SAPs) have...

303

Effects of Soil Texture on Belowground Carbon and Nutrient  

E-Print Network [OSTI]

to 1-m depth. The quantity of labile soil P, the soil C:N ratio, and live and dead fine root biomass

Neff, Jason

304

agricultural peat soil: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

components and hydraulic properties of peat soils Boyer, Edmond 4 Agricultural Soil Carbon Sequestration: Economic Issues and Research Needs Environmental Sciences and...

305

agricultural peat soils: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

components and hydraulic properties of peat soils Boyer, Edmond 4 Agricultural Soil Carbon Sequestration: Economic Issues and Research Needs Environmental Sciences and...

306

acid forest soils: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Forest Succession Biology and Medicine Websites Summary: K7L 3N6, Canada ABSTRACT Carbon sequestration in soils that have previously beendepletedoforganic the soil carbon...

307

acid forest soil: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Forest Succession Biology and Medicine Websites Summary: K7L 3N6, Canada ABSTRACT Carbon sequestration in soils that have previously beendepletedoforganic the soil carbon...

308

Mechanisms controlling soil carbon turnover and their potential...  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

controlling soil carbon turnover and their potential application for enhancing carbon sequestration . Mechanisms controlling soil carbon turnover and their potential application...

309

acidic soil isolates: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Soil pH indicates its alkalinity or acidity. This property influences soil chemistry and crop production. A low maintenance ROSS Ultra Triodeguarantees accurate measurement of...

310

Temperature initiated passive cooling system  

DOE Patents [OSTI]

A passive cooling system for cooling an enclosure only when the enclosure temperature exceeds a maximum standby temperature comprises a passive heat transfer loop containing heat transfer fluid having a particular thermodynamic critical point temperature just above the maximum standby temperature. An upper portion of the heat transfer loop is insulated to prevent two phase operation below the maximum standby temperature.

Forsberg, Charles W. (Oak Ridge, TN)

1994-01-01T23:59:59.000Z

311

Temperature initiated passive cooling system  

DOE Patents [OSTI]

A passive cooling system for cooling an enclosure only when the enclosure temperature exceeds a maximum standby temperature comprises a passive heat transfer loop containing heat transfer fluid having a particular thermodynamic critical point temperature just above the maximum standby temperature. An upper portion of the heat transfer loop is insulated to prevent two phase operation below the maximum standby temperature. 1 fig.

Forsberg, C.W.

1994-11-01T23:59:59.000Z

312

High temperature thermometric phosphors  

DOE Patents [OSTI]

A high temperature phosphor consists essentially of a material having the general formula LuPO{sub 4}:Dy{sub x},Eu{sub y} wherein: 0.1 wt % {<=} x {<=} 20 wt % and 0.1 wt % {<=} y {<=} 20 wt %. The high temperature phosphor is in contact with an article whose temperature is to be determined. The article having the phosphor in contact with it is placed in the environment for which the temperature of the article is to be determined. The phosphor is excited by a laser causing the phosphor to fluoresce. The emission from the phosphor is optically focused into a beam-splitting mirror which separates the emission into two separate emissions, the emission caused by the dysprosium dopant and the emission caused by the europium dopant. The separated emissions are optically filtered and the intensities of the emission are detected and measured. The ratio of the intensity of each emission is determined and the temperature of the article is calculated from the ratio of the intensities of the separate emissions. 2 figs.

Allison, S.W.; Cates, M.R.; Boatner, L.A.; Gillies, G.T.

1999-03-23T23:59:59.000Z

313

High temperature thermometric phosphors  

DOE Patents [OSTI]

A high temperature phosphor consists essentially of a material having the general formula LuPO.sub.4 :Dy.sub.(x),Eu.sub.y) wherein: 0.1 wt %.ltoreq.x.ltoreq.20 wt % and 0.1 wt %.ltoreq.y.ltoreq.20 wt %. The high temperature phosphor is in contact with an article whose temperature is to be determined. The article having the phosphor in contact with it is placed in the environment for which the temperature of the article is to be determined. The phosphor is excited by a laser causing the phosphor to fluoresce. The emission from the phosphor is optically focused into a beam-splitting mirror which separates the emission into two separate emissions, the emission caused by the dysprosium dopant and the emission caused by the europium dopent. The separated emissions are optically filtered and the intensities of the emission are detected and measured. The ratio of the intensity of each emission is determined and the temperature of the article is calculated from the ratio of the intensities of the separate emissions.

Allison, Stephen W. (Knoxville, TN); Cates, Michael R. (Oak Ridge, TN); Boatner, Lynn A. (Oak Ridge, TN); Gillies, George T. (Earlysville, VA)

1999-03-23T23:59:59.000Z

314

Temperature Data Evaluation  

SciTech Connect (OSTI)

Groundwater temperature is sensitive to the competing processes of heat flow from below the advective transport of heat by groundwater flow. Because groundwater temperature is sensitive to conductive and advective processes, groundwater temperature may be utilized as a tracer to further constrain the uncertainty of predictions of advective radionuclide transport models constructed for the Nevada Test Site (NTS). Since heat transport, geochemical, and hydrologic models for a given area must all be consistent, uncertainty can be reduced by devaluing the weight of those models that do not match estimated heat flow. The objective of this study was to identify the quantity and quality of available heat flow data at the NTS. One-hundred-forty-five temperature logs from 63 boreholes were examined. Thirteen were found to have temperature profiles suitable for the determination of heat flow values from one or more intervals within the boreholes. If sufficient spatially distributed heat flow values are obtained, a heat transport model coupled to a hydrologic model may be used to reduce the uncertainty of a nonisothermal hydrologic model of the NTS.

Gillespie, David

2003-03-01T23:59:59.000Z

315

The summer soil institute provides a unique opportunity to gain a funda-  

E-Print Network [OSTI]

of managing our soil resources sustainably. A u n iq u e e du c at ion al e x p e r i e n c e soil of critical is sues in soil sustainability. Instructors and topics Thomas Borch: Environmental Soil Chemistry Stromberger: Soil Microbiology Diana Wall: Soil Sustainability, Soil Fauna Matthew Wallenstein: Soil

Wall, Diana

316

Measuring spatial variability in soil characteristics  

DOE Patents [OSTI]

The present invention provides systems and methods for measuring a load force associated with pulling a farm implement through soil that is used to generate a spatially variable map that represents the spatial variability of the physical characteristics of the soil. An instrumented hitch pin configured to measure a load force is provided that measures the load force generated by a farm implement when the farm implement is connected with a tractor and pulled through or across soil. Each time a load force is measured, a global positioning system identifies the location of the measurement. This data is stored and analyzed to generate a spatially variable map of the soil. This map is representative of the physical characteristics of the soil, which are inferred from the magnitude of the load force.

Hoskinson, Reed L. (Rigby, ID); Svoboda, John M. (Idaho Falls, ID); Sawyer, J. Wayne (Hampton, VA); Hess, John R. (Ashton, ID); Hess, J. Richard (Idaho Falls, ID)

2002-01-01T23:59:59.000Z

317

High-temperature Pump Monitoring - High-temperature ESP Monitoring...  

Broader source: Energy.gov (indexed) [DOE]

7 4.4.4 High-temperature Pump Monitoring - High-temperature ESP Monitoring Presentation Number: 018 Investigator: Dhruva, Brindesh (Schlumberger Technology Corp.) Objectives: To...

318

Temperature and Microbial Activity Effects on Trace Element Leaching from Metalliferous Peats  

E-Print Network [OSTI]

Temperature and Microbial Activity Effects on Trace Element Leaching from Metalliferous PeatsDue to geochemical processes, peat soils often have elevated con- sulfides (Cannon, 1955). The maximum Zn concentra as high as 10 g kg 1 . Theperatures to vary microbial activity in two metalliferous peats (M7 acidic peat

Walter, M.Todd

319

Fluorescent temperature sensor  

DOE Patents [OSTI]

The present invention is a fluorescent temperature sensor or optical thermometer. The sensor includes a solution of 1,3-bis(1-pyrenyl)propane within a 1-butyl-1-1-methylpyrrolidinium bis(trifluoromethylsulfonyl)imide ionic liquid solvent. The 1,3-bis(1-pyrenyl)propane remains unassociated when in the ground state while in solution. When subjected to UV light, an excited state is produced that exists in equilibrium with an excimer. The position of the equilibrium between the two excited states is temperature dependent.

Baker, Gary A [Los Alamos, NM; Baker, Sheila N [Los Alamos, NM; McCleskey, T Mark [Los Alamos, NM

2009-03-03T23:59:59.000Z

320

Temperature differential detection device  

DOE Patents [OSTI]

A temperature differential detection device for detecting the temperature differential between predetermined portions of a container wall is disclosed as comprising a Wheatstone bridge circuit for detecting resistance imbalance with a first circuit branch having a first elongated wire element mounted in thermal contact with a predetermined portion of the container wall, a second circuit branch having a second elongated wire element mounted in thermal contact with a second predetermined portion of a container wall with the wire elements having a predetermined temperature-resistant coefficient, an indicator interconnected between the first and second branches remote from the container wall for detecting and indicating resistance imbalance between the first and second wire elements, and connector leads for electrically connecting the wire elements to the remote indicator in order to maintain the respective resistance value relationship between the first and second wire elements. The indicator is calibrated to indicate the detected resistance imbalance in terms of a temperature differential between the first and second wall portions. 2 figs.

Girling, P.M.

1986-04-22T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


321

Low Temperature Performance Characterization  

Broader source: Energy.gov (indexed) [DOE]

0.0036 0.0038 0.004 0.0042 Inverse Temperature, 1K Gen2 Electrodes and 1.2M LiPF6 in EC:EMC (3:7 ww) (BID 1935), 4.1V, 3 Sep. Gen2 Electrodes and 1.2M LiPF6 in EC:EMC (3:7 ww)...

322

Innovative vitrification for soil remediation  

SciTech Connect (OSTI)

The objective of this DOE demonstration program is to validate the performance and operation of the Vortec Cyclone Melting System (CMS{trademark}) for the processing of LLW contaminated soils found at DOE sites. This DOE vitrification demonstration project has successfully progressed through the first two phases. Phase 1 consisted of pilot scale testing with surrogate wastes and the conceptual design of a process plant operating at a generic DOE site. The objective of Phase 2, which is scheduled to be completed the end of FY 95, is to develop a definitive process plant design for the treatment of wastes at a specific DOE facility. During Phase 2, a site specific design was developed for the processing of LLW soils and muds containing TSCA organics and RCRA metal contaminants. Phase 3 will consist of a full scale demonstration at the DOE gaseous diffusion plant located in Paducah, KY. Several DOE sites were evaluated for potential application of the technology. Paducah was selected for the demonstration program because of their urgent waste remediation needs as well as their strong management and cost sharing financial support for the project. During Phase 2, the basic nitrification process design was modified to meet the specific needs of the new waste streams available at Paducah. The system design developed for Paducah has significantly enhanced the processing capabilities of the Vortec vitrification process. The overall system design now includes the capability to shred entire drums and drum packs containing mud, concrete, plastics and PCB`s as well as bulk waste materials. This enhanced processing capability will substantially expand the total DOE waste remediation applications of the technology.

Jetta, N.W.; Patten, J.S.; Hart, J.G.

1995-12-01T23:59:59.000Z

323

Effect of soiling in CPV systems  

SciTech Connect (OSTI)

The effect of soiling in flat PV modules has been already studied, causing a reduction of the electrical output of 4% on average. For CPV's, as far as soiling produces light scattering at the optical collector surface, the scattered rays should be definitively lost because they cannot be focused onto the receivers again. While the theoretical study becomes difficult because soiling is variable at different sites, it becomes easier to begin the monitoring of the real field performance of concentrators and then raise the following question: how much does the soiling affect to PV concentrators in comparison with flat panels?' The answers allow to predict the PV concentrator electrical performance and to establish a pattern of cleaning frequency. Some experiments have been conducted at the IES-UPM and CSES-ANU sites, consisting in linear reflective concentration systems, a point focus refractive concentrator and a flat module. All the systems have been measured when soiled and then after cleaning, achieving different increases of I{sub SC}. In general, results show that CPV systems are more sensitive to soiling than flat panels, accumulating losses in I{sub SC} of about 14% on average in three different tests conducted at IES-UPM and CSES-ANU test sites in Madrid (Spain) and Canberra (Australia). Some concentrators can reach losses up to 26% when the system is soiled for 4 months of exposure. (author)

Vivar, M.; Herrero, R.; Anton, I.; Martinez-Moreno, F.; Moreton, R.; Sala, G. [Instituto de Energia Solar, UPM, Ciudad Universitaria S/N, 28040 Madrid (Spain); Blakers, A.W.; Smeltink, J. [Centre for Sustainable Energy Systems, Australian National University, Canberra 0200 (Australia)

2010-07-15T23:59:59.000Z

324

A petroleum contaminated soil bioremediation facility  

SciTech Connect (OSTI)

The amount of petroleum contaminated soil (PCS) at the Savannah River site (SRS) that has been identified, excavated and is currently in storage has increased several fold during the last few years. Several factors have contributed to this problem: (1) South Carolina Department of Health ad Environmental control (SCDHEC) lowered the sanitary landfill maximum concentration for total petroleum hydrocarbons (TPH) in the soil from 500 to 100 parts per million (ppm), (2) removal and replacement of underground storage tanks at several sites, (3) most recently SCDHEC disallowed aeration for treatment of contaminated soil, and (4) discovery of several very large contaminated areas of soil associated with leaking underground storage tanks (LUST), leaking pipes, disposal areas, and spills. Thus, SRS has an urgent need to remediate large quantities of contaminated soil that are currently stockpiled and the anticipated contaminated soils to be generated from accidental spills. As long as we utilize petroleum based compounds at the site, we will continue to generate contaminated soil that will require remediation.

Lombard, K.; Hazen, T.

1994-06-01T23:59:59.000Z

325

100 Area soil washing treatability test plan  

SciTech Connect (OSTI)

This test plan describes specifications, responsibilities, and general methodology for conducting a soil washing treatability study as applied to source unit contamination in the 100 Area. The objective ofthis treatability study is to evaluate the use of physical separation systems and chemical extraction methods as a means of separating chemically and radioactively contaminated soil fractions from uncontaminated soil fractions. The purpose of separating these fractions is to minimize the volume of soil requiring permanent disposal. It is anticipated that this treatability study will be performed in two phases of testing, a remedy screening phase and a remedy selection phase. The remedy screening phase consists of laboratory- and bench-scale studies performed by Battelle Pacific Northwest laboratories (PNL) under a work order issued by Westinghouse Hanford Company (Westinghouse Hanford). This phase will be used to provide qualitative evaluation of the potential effectiveness of the soil washing technology. The remedy selection phase, consists of pilot-scale testing performed under a separate service contract to be competitively bid under Westinghouse Hanford direction. The remedy selection phase will provide data to support evaluation of the soil washing technology in future feasibility studies for Interim Remedial Measures (IRMs) or final operable unit (OU) remedies. Performance data from these tests will indicate whether applicable or relevant and appropriate requirements (ARARs) or cleanup goals can be met at the site(s) by application of soil washing. The remedy selection tests wig also allow estimation of costs associated with implementation to the accuracy required for the Feasibility Study.

Not Available

1993-03-01T23:59:59.000Z

326

WATER AS A REAGENT FOR SOIL REMEDIATION  

SciTech Connect (OSTI)

SRI International conducted experiments in a two-year, two-phase process to develop and evaluate hydrothermal extraction technology, also known as hot water extraction (HWE) technology, to separate petroleum-related contaminants and other hazardous pollutants from soil and sediments. In this process, water with added electrolytes (inexpensive and environmentally friendly) is used as the extracting solvent under subcritical conditions (150-300 C). The use of electrolytes allows us to operate reactors under mild conditions and to obtain high separation efficiencies that were hitherto impossible. Unlike common organic solvents, water under subcritical conditions dissolves both organics and inorganics, thus allowing opportunities for separation of both organic and inorganic material from soil. In developing this technology, our systematic approach was to (1) establish fundamental solubility data, (2) conduct treatability studies with industrial soils, and (3) perform a bench-scale demonstration using a highly contaminated soil. The bench-scale demonstration of the process has shown great promise. The next step of the development process is the successful pilot demonstration of this technology. Once pilot tested, this technology can be implemented quite easily, since most of the basic components are readily available from mature technologies (e.g., steam stripping, soil washing, thermal desorption). The implementation of this technology will revolutionize the conventional use of water in soil remediation technologies and will provide a stand-alone technology for removal of both volatile and heavy components from contaminated soil.

Indira S. Jayaweera; Montserrat Marti-Perez; Jordi Diaz-Ferrero; Angel Sanjurjo

2001-11-12T23:59:59.000Z

327

Localized temperature stability of low temperature cofired ceramics  

DOE Patents [OSTI]

The present invention is directed to low temperature cofired ceramic modules having localized temperature stability by incorporating temperature coefficient of resonant frequency compensating materials locally into a multilayer LTCC module. Chemical interactions can be minimized and physical compatibility between the compensating materials and the host LTCC dielectrics can be achieved. The invention enables embedded resonators with nearly temperature-independent resonance frequency.

Dai, Steven Xunhu

2013-11-26T23:59:59.000Z

328

Potential dentrification rates of Texas soils  

E-Print Network [OSTI]

of depleting soil nitrogen by volatilization has been known for many years. It is the reduction of nitrate (NO ) or nitrite (N02 ) forms of nitrogen to gases. The principal deni . rifica. tion products are nitrogen (N2) and nitrous oxide (N20). The losses... gases evolved from Texas soils and relate it to soil organic mat*er content. Hopefully *he results of the study will be useful in increasing the efficiency of fertilizer usage in Texas and at the same time provide some of the insight needed for main...

Hsu, Shu-Chun Dolores

1975-01-01T23:59:59.000Z

329

Acuff Soils: Distribution, Importance, Variability, and Management.  

E-Print Network [OSTI]

at the High Plains Rolling Plains boundary on the southeast, and a catena of sandy soils extending from Stanton, Texas, to Clovis, New Mexico, on the west. Within this roughly crescent-shaped area, Acuff soils occupy about 21 percent of the land surface.... The area of Acuff soils ranges from aboutl01?lOmin. to 103?50 min. west longitude and from about 32?10 min. to 35?40 min. north latitude Eleva tion of the surface ranges from abou t 2,500 to 4,200 feet above mean sea level. The area is in a subhumid...

Unger, Paul W.; Pringle, Fred B.; Blackstock, Dan A.

1993-01-01T23:59:59.000Z

330

Assessing inhalation exposure from airborne soil contaminants  

SciTech Connect (OSTI)

A method of estimation of inhalation exposure to airborne soil contaminants is presented. this method is derived from studies of airborne soil particles with radioactive tags. The concentration of contaminants in air (g/m{sup 3}) can be derived from the product of M, the suspended respirable dust mass concentration (g/m{sup 3}), S, the concentration of contaminant in the soil (g/g), and E{sub f}, an enhancement factor. Typical measurement methods and values of M, and E{sub f} are given along with highlights of experiences with this method.

Shinn, J.H.

1998-04-01T23:59:59.000Z

331

Climate-Soil-Vegetation Control on Groundwater Table Dynamics and its Feedbacks in a Climate Model  

SciTech Connect (OSTI)

Among the three dynamically linked branches of the water cycle, including atmospheric, surface, and subsurface water, groundwater is the largest reservoir and an active component of the hydrologic system. Because of the inherent slow response time, groundwater may be particularly relevant for long time-scale processes such as multi-years or decadal droughts. This study uses regional climate simulations with and without surface water – groundwater interactions for the conterminous U.S. to assess the influence of climate, soil, and vegetation on groundwater table dynamics, and its potential feedbacks to regional climate. Analysis shows that precipitation has a dominant influence on the spatial and temporal variations of groundwater table depth (GWT). The simulated GWT is found to decrease sharply with increasing precipitation. Our simulation also shows some distinct spatial variations that are related to soil porosity and hydraulic conductivity. Vegetation properties such as minimum stomatal resistance, and root depth and fraction are also found to play an important role in controlling the groundwater table. Comparing two simulations with and without groundwater table dynamics, we find that groundwater table dynamics mainly influences the partitioning of soil water between the surface (0 – 0.5 m) and subsurface (0.5 – 5 m) rather than total soil moisture. In most areas, groundwater table dynamics increases surface soil moisture at the expense of the subsurface, except in regions with very shallow groundwater table. The change in soil water partitioning between the surface and subsurface is found to strongly correlate with the partitioning of surface sensible and latent heat fluxes. The evaporative fraction (EF) is generally higher during summer when groundwater table dynamics is included. This is accompanied by increased cloudiness, reduced diurnal temperature range, cooler surface temperature, and increased cloud top height. Although both convective and non-convective precipitation are enhanced, the higher EF changes the partitioning to favor more non-convective precipitation, but this result could be sensitive to the convective parameterization used. Compared to simulations without groundwater table dynamics, the dry bias in the summer precipitation is slightly reduced over the central and eastern U.S. Groundwater table dynamics can provide important feedbacks to atmospheric processes, and these feedbacks are stronger in regions with deeper groundwater table, because the interactions between surface and subsurface are weak when the groundwater table is deep. This increases the sensitivity of surface soil moisture to precipitation anomalies, and therefore enhances land surface feedbacks to the atmosphere through changes in soil moisture and evaporative fraction. By altering the groundwater table depth, land use change and groundwater withdrawal can alter land surface response and feedback to the climate system.

Leung, Lai-Yung R.; Huang, Maoyi; Qian, Yun; Liang, Xu

2010-01-29T23:59:59.000Z

332

November 2000 No. 2 --2000 Soil Erosion and Productivity1/  

E-Print Network [OSTI]

the forces of nature move vulnerable soil toward the sea. Very simply put wind and water provide the energy needed to detach soil particles and transport them until their energy decreases and the particles mph can splash soil particles as far as 5 feet. The raindrop energy also compacts and seals the soil

Balser, Teri C.

333

LittleRockCreek SOIL SURVEY OF ATOKA COUNTY, OKLAHOMA  

E-Print Network [OSTI]

3800600 3800600 3800800 3800800 3801000 3801000 3801200 3801200 3801400 3801400 SOIL SURVEY OF ATOKA 200 400100 Meters Web Soil Survey 1.1 National Cooperative Soil Survey 3/17/2007 Page 1 of 3 #12;MAP INFORMATION SOIL SURVEY OF ATOKA COUNTY, OKLAHOMA Wes Watkins Agricultural Research and Extension Center

Ghajar, Afshin J.

334

SOIL SURVEY OF PAYNE COUNTY, OKLAHOMA OSURR Section 17  

E-Print Network [OSTI]

66 26 76 26 26 26 SOIL SURVEY OF PAYNE COUNTY, OKLAHOMA OSURR Section 17 0 300 600 900 1,200150 Feet 0 100 20050 Meters Web Soil Survey 1.1 National Cooperative Soil Survey 5/7/2007 Page 1 of 3 #12;MAP INFORMATION SOIL SURVEY OF PAYNE COUNTY, OKLAHOMA OSURR Section 17 Source of Map: Natural Resources

Ghajar, Afshin J.

335

TITLE SOIL SUITABILITY EVALUATION FOR TOBACCO BASED ON GREY CLUSTER  

E-Print Network [OSTI]

TITLE SOIL SUITABILITY EVALUATION FOR TOBACCO BASED ON GREY CLUSTER ANALYSIS GAO Rui QIAO Hong Abstract: Suitability evaluation of soil for tobacco is the base of spatial analysis and optimization disposition. It provides scientific basis for reasonable development of soil for tobacco. Taking soil in San

Paris-Sud XI, Université de

336

Method for treatment of soils contaminated with organic pollutants  

DOE Patents [OSTI]

A method for treating soil contaminated by organic compounds wherein an ozone containing gas is treated with acid to increase the stability of the ozone in the soil environment and the treated ozone applied to the contaminated soil to decompose the organic compounds. The soil may be treated in situ or may be removed for treatment and refilled.

Wickramanayake, Godage B. (Cranbury, NJ)

1993-01-01T23:59:59.000Z

337

Enrichment of Heavy Metals in Sediment Resulting from Soil  

E-Print Network [OSTI]

, Harpenden, Hertfordshire AL5 2JQ, U.K. Heavy metal pollution of soil and water is often associated of water erosion in detaching and transporting sediment-associated heavy metals from agri- cultural soils to surface waters has been overlooked. Heavy metals in arable soils are derived from the soil parent material

Quinton, John

338

Applicability of CS616 Soil Water Sensors for South  

E-Print Network [OSTI]

site water balance Image from: (Migliaccio 2007) #12;Background ­ Soil Water Sensors Time DomainApplicability of CS616 Soil Water Sensors for South Florida Urban Soils Kevin Koryto Water: Determine if CS616 soil water sensors are functioning adequately at field site. Hypothesis: Presence of air

Migliaccio, Kati White

339

Is Gypsum Application Beneficial to Soil? Francisco J. Arriaga  

E-Print Network [OSTI]

). · Response to calcium application unlikely even in soils testing low or very low, except when growing S demand (alfalfa, canola and brassicas), in sandy soils and soils low in organic matter. · Soils with low or medium potential for sulfate retention (sands and loamy sands), and with no recent manure applications

Balser, Teri C.

340

On-Site Wastewater Treatment Systems: Soil Particle Analysis Procedure  

E-Print Network [OSTI]

Soil is an important component of an on-site wastewater treatment system. This publication explains the composition of soils, the sizing of soil particles, and the ways soil particles are analyzed to determine whether a site is suitable for a...

Lesikar, Bruce J.

2005-08-18T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


341

Soils of Amazonia with particular reference to the RAINFOR sites  

E-Print Network [OSTI]

they develop over unconsolidated weathering materials ofthin soils derived from unconsolidated material and lacking

Quesada, C. A; Lloyd, J.; Anderson, L. O; Fyllas, N. M; Schwarz, M.; Czimczik, C. I

2011-01-01T23:59:59.000Z

342

The Role of Micro-Mechanics in Soil Mechanics  

E-Print Network [OSTI]

The Role of Micro-Mechanics in Soil Mechanics M.D.Bolton CUED/D-Soils/TR313 September 2000;1 The Role of Micro-Mechanics in Soil Mechanics Malcolm Bolton Summary It is suggested that observations of the changing microstructure of soils will permit the selection and refinement of relevant micro-mechanisms

Bolton, Malcolm

343

Analysis of flow patterns and flow mechanisms in soils  

E-Print Network [OSTI]

Analysis of flow patterns and flow mechanisms in soils Dissertation Co-directed by the University mechanism or changing soil physical properties (stratification). Thus, in stratified soil, we restricted was prepared at the Department of Soil Physics, University of Bayreuth, and at the Hydrogeological Laboratory

Avignon et des Pays de Vaucluse, Université de

344

www.VadoseZoneJournal.org Soil Architecture and  

E-Print Network [OSTI]

www.VadoseZoneJournal.org Soil Architecture and Physicochemical Func ons: An Introduc on Soils func engineers with the best educa on possible. The 16 papers in this special sec on on soil architecture measurement, visualiza on, and modeling of soil structure (architecture) and physical, chemical

Wildenschild, Dorthe

345

High Temperature Membrane Working Group  

Broader source: Energy.gov [DOE]

This presentation provides an overview of the High Temperature Membrane Working Group Meeting in May 2007.

346

Engine Cylinder Temperature Control  

DOE Patents [OSTI]

A method and apparatus for controlling a temperature in a combustion cylinder in an internal combustion engine. The cylinder is fluidly connected to an intake manifold and an exhaust manifold. The method and apparatus includes increasing a back pressure associated with the exhaust manifold to a level sufficient to maintain a desired quantity of residual exhaust gas in the cylinder, and varying operation of an intake valve located between the intake manifold and the cylinder to an open duration sufficient to maintain a desired quantity of fresh air from the intake manifold to the cylinder, wherein controlling the quantities of residual exhaust gas and fresh air are performed to maintain the temperature in the cylinder at a desired level.

Kilkenny, Jonathan Patrick (Peoria, IL); Duffy, Kevin Patrick (Metamora, IL)

2005-09-27T23:59:59.000Z

347

Manufacturing High Temperature Systems  

Office of Energy Efficiency and Renewable Energy (EERE) Indexed Site

AFDC Printable Version Share this resource Send a link to EERE: Alternative Fuels Data Center Home Page to someone by E-mail Share EERE: Alternative Fuels Data Center Home Page on Facebook Tweet about EERE: Alternative Fuels Data Center Home Page on Twitter Bookmark EERE: Alternative Fuels Data Center Home Page on Google Bookmark EERE: Alternative Fuels Data Center Home Page on Delicious RankCombustion | Department of Energy Low-TemperatureEnergyAll ManufacturingFoodOctoberto DOE

348

Don't guess -soil test! Get your Home Lawn and Garden Soil Test kit today  

E-Print Network [OSTI]

-application of phosphorous or nitrogen fertilizers. ·Cost savings. Why apply what you don't need? Soil test results provide

349

Growth of Phymatotrichum omnivorum in Branyon and Weswood soils: and its interactions with other soil microorganisms  

E-Print Network [OSTI]

The Pathogen vi vi I xiv Control of Phymatotr ichum omnivorum Interactions with Competitive Microflora Interactions wi th Antagonistic Micruflora Suppr essive Soils Survival of Antagonists 10 MATERIALS AND METHODS Selection of Soil 14 Source... 10 cm from the inoculum. Trial 1 67 14. P1ycel i a) growth in ster i le ( top ) and nonster i le & bottom & Br anyon clay pr i or to coming in contact with chitin-amended soil. Notice the browning of the mycelium in the nonsterile soil 69 15...

Powell, Rebecca Lynn

1987-01-01T23:59:59.000Z

350

THE SOIL SCOOP by Clain Jones, Montana State University Extension Soil Fertility Specialist, and Kathrin Olson-Rutz, Research Associate  

E-Print Network [OSTI]

of energy for soil microorganisms.Although SOC makes up roughly 60% of SOM, only a portion the water solubleTHE SOIL SCOOP by Clain Jones, Montana State University Extension Soil Fertility Specialist, and Kathrin Olson-Rutz, Research Associate Evaluating Soil Quality and Health rate cycling timing

Lawrence, Rick L.

351

Soil Security: Solving the Global Soil Crisis Andrea Koch, Alex McBratney, Mark Adams, Damien Field, Robert Hill,  

E-Print Network [OSTI]

, climate change and energy sustainability. Soil science has not been sufficiently translated to policySoil Security: Solving the Global Soil Crisis Andrea Koch, Alex McBratney, Mark Adams, Damien Field England Michael Zimmermann University of Natural Resources and Life Sciences Vienna Abstract Soil

Grunwald, Sabine

352

Soil Biology & Biochemistry 38 (2006) 30653082 Soil carbon turnover in the McMurdo Dry Valleys, Antarctica  

E-Print Network [OSTI]

Soil Biology & Biochemistry 38 (2006) 3065­3082 Soil carbon turnover in the McMurdo Dry Valleys Valleys are among the most inhospitable soil environments on Earth due to climate and substrate because likely sources of organic matter are 102 ­104 yrs old and in situ soil respiration is typically

Wall, Diana

2006-01-01T23:59:59.000Z

353

Soil nematode communities are ecologically more mature beneath late-than early-successional stage biological soil crusts  

E-Print Network [OSTI]

Soil nematode communities are ecologically more mature beneath late- than early-successional stage biological soil crusts Brian J. Darby a,*, Deborah A. Neher a , Jayne Belnap b a Department of Plant and Soil; accepted 12 April 2006 Abstract Biological soil crusts are key mediators of carbon and nitrogen inputs

Neher, Deborah A.

354

Effects of Soil Organic Matter on the Kinetics and Mechanisms of Pb(II) Sorption and Desorption in Soil  

E-Print Network [OSTI]

Effects of Soil Organic Matter on the Kinetics and Mechanisms of Pb(II) Sorption and Desorption in Soil Daniel G. Strawn* and Donald L. Sparks ABSTRACT make better predictions about the mobility and threat from Pb contami- and desorption behavior on soil be understood, as wellnated soil, it is critical

Sparks, Donald L.

355

What Happens to Nitrogen in Soils?  

E-Print Network [OSTI]

This publication explains the chemistry of nitrogen, the processes by which nitrogen is added to and removed from the soil, and methods of preventing nitrogen losses on agricultural lands....

Provin, Tony; Hossner, L. R.

2001-07-09T23:59:59.000Z

356

Collection Policy: Crop and Soil Sciences Introduction  

E-Print Network [OSTI]

production systems, sustainable agroecosystem management, and linkages between agriculture and environmental and less on soils. Newer research programs focus on sustainability, landscape systems, weeds Organic agriculture and weed management, sustainable local food systems o The nitrogen cycle in native

Angenent, Lars T.

357

Adsorption and transport of pyrithiobac in soils  

E-Print Network [OSTI]

adsorbents (Gonzales bentonite, Georgia kaolinite, goethite, and Michigan peat) and four soils (Houston Black c, Hidalgo sl, Orelia scl, and Ships sic) having a wide range of physical and chemical properties. Adsorption isotherms were developed...

Matocha, Christopher John

1996-01-01T23:59:59.000Z

358

Soil Building as a Climate Mitigation Strategy  

E-Print Network [OSTI]

capacity? Promote soil formation Prevent erosion (increase cohesion, shield water and wind energy, The City College of New York nkrakauer@ccny.cuny.edu #12;"drought may become so widespread and so severe

Krakauer, Nir Y.

359

Soil phosphorus status in potato fields  

E-Print Network [OSTI]

P deficiency in irrigated potatoes. Can. J. Plant Sci. 68,soil test P levels in these potato fields. References He,Introduction The potato crop requires substantial amounts of

He, Z.; Honeycutt, C. W.; Zhang, H.

2009-01-01T23:59:59.000Z

360

Soil Erosion and Sediment Control (Maryland)  

Broader source: Energy.gov [DOE]

The Departments of the Environment and Natural Resources are authorized to develop regulations to combat soil erosion and control the addition of sediment to waters of the state. As part of the...

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


361

Soil and Water Conservation Policy (Minnesota)  

Broader source: Energy.gov [DOE]

This statute establishes that it is the responsibility of land occupiers to implement practices that conserve soil and water resources, and the policy of the state encourages them to do so.

362

Soil and Water Conservation Districts (South Carolina)  

Broader source: Energy.gov [DOE]

Soil and Water Conservation Districts are local governmental subdivisions of the state of South Carolina, established to provide for land and water conservation and prevent erosion in the state....

363

The Soil Moisture Active Passive (SMAP) Mission  

E-Print Network [OSTI]

The Soil Moisture Active Passive (SMAP) mission is one of the first Earth observation satellites being developed by NASA in response to the National Research Council's Decadal Survey. SMAP will make global measurements of ...

Entekhabi, Dara

364

SOIL SURVEY OF PAYNE COUNTY, OKLAHOMA OSURR Section 5  

E-Print Network [OSTI]

21 76 11 25 61 49 2 11 65 25 74 25 25 25 6125 65 25 40 11 W 26 25 32 W 54 3 11 65 11 74 11 74 SOIL Soil Survey 1.1 National Cooperative Soil Survey 5/7/2007 Page 1 of 3 #12;MAP INFORMATION SOIL SURVEY OF PAYNE COUNTY, OKLAHOMA OSURR Section 5 Source of Map: Natural Resources Conservation Service Web Soil

Ghajar, Afshin J.

365

The Composition and Properties of Some Texas Soils.  

E-Print Network [OSTI]

AS AGRICULTURAL EXPERIMENT BULLETIN NO. 99. December, 1907. The Composition and Properties of Some Texas Soils BY G. S. FRAPS, Chemist. Postoffice, COLLEGE STATION, BRAZOS COUNTY, TEXAS- TEXAS AGRICULTURAL EXPERIMENT STATlON ICERS...- isms, (bacteria) which aid in maintaining a supply of active plant food in the soil. The organic matter makes the soil more retentive of moisture, and has a favorable effect upon the physical character of the soil, rendering clay soils less stiff...

Fraps, G. S. (George Stronach)

1907-01-01T23:59:59.000Z

366

The moisture retention characteristic of four soils from Niger  

E-Print Network [OSTI]

of air at the surface is relatively facile. Hydraulic Conductivity Redistribution of soil water affects plant growth, and the rate and duration of internal moisture flow determines 19 effective soil water storage. This is important to remember when... in sorption (wetting). This characteristic of wetting versus drying for a soil is known as the hysteresis effect (Lal 1979a). Hillel (1980) notes that hysteresis is important for coarse-textured soils in the process of redistribution of soil water...

Landeck, Jonathon Keith

1984-01-01T23:59:59.000Z

367

A study of cellulose gasification in a fluidized bed using a high-temperature solar furnace  

SciTech Connect (OSTI)

A 4.2-meter solar furnace was used to study the gasification of cellulose with steam in a fluidized bed. The heating value of the high-temperature equilibrium products is about twenty percent higher than that of the reactants. The increase represents stored solar energy; and the product, synthesis gas, is valuable as a chemical feedstock or pipeline gas. All experiments were performed at atmospheric pressure. Pure tabular alumina as well as crushed automotive exhaust was used as a bed material. Microcrystalline {alpha}-cellulose, entrained in argon, entered the fluidized bed just above the distributor. Steam heated to the operating temperature in a 10 cm packed bed section below the fluidized bed. In all cases, the process ran with more steam than required to produce an equimolar mixture of carbon monoxide and hydrogen. We used a quartz reactor between 1100 and 1430 K; a steel reactor at 1500 K and an Inconel reactor at 1600 K. Reactor inside diameter, nominally 5 cm, varied slightly; the bed height was adjusted to keep the gas residence time constant. Hydrogen production rate was measured before and after experiments with steam alone, with this amount subtracted. Equilibrium mixtures were not achieved. Catalysts improved hydrogen yields with higher than expected concentrations of carbon monoxide, methane and lighter hydrocarbons such as ethylene and acetylene. Experiments performed without catalyst at 1300 K, achieved a mixture (dry, argon-free) of 46 mole% CO, 30% H{sub 2} 14% CH{sub 4} 5% CO{sub 2} and 5% C{sub 2}H{sub 4}. An equilibrium mixture at this temperature would have contained 39% CO, 30% H{sub 2} 7% CO{sub 2} and no CH{sub 4} or C{sub 2}H{sub 4}. With the catalyst, the CO and CH{sub 4} decreased to 40% and 2% respectively, the H{sub 2} increased to 47%, and CO{sub 2} remained the same. No ethylene was formed. The hydrocarbon-rich mixtures achieved are typical of rapid-pyrolysis processes.

Murray, J.P.

1989-01-01T23:59:59.000Z

368

The behavior of piles in cohesionless soils  

E-Print Network [OSTI]

and the load- settlement behavior of single piles in cohesionless soils is addressed. The available data on instrumerted piles load-tested vertically in sands is collected and analyzed to determine the load transfer characteristics of the soil. A... the distribution of residual stresses in the piles, and methods of obtaining residual stresses from load test results are discussed. Correlations with the results of the Standard Penetration Test are presented and are used to develop a new design procedure which...

Tucker, Larry Milton

1983-01-01T23:59:59.000Z

369

Response of rice to soil phosphorus levels  

E-Print Network [OSTI]

RESPORSE OF RICE TO SOIL PHOSPHORUS LEVELS MOHJQRiD JL ~ QUDDUS Submitted te the Graduate Sohool of the kgrloultural and Mechanical College of Texas im partial fulfillment of the requirements for the legree of IGLSTER OF SCIENCE Luguet~ 1962... Eager Sub)cot& Agronomy RESPONSE OF RICE TO SOIL PHOSPHORUS LEVELS A Thesis KIHAMNAD Ae QUDDUS Approwed as to style and content by& Chairman of Committee Cpt r Head of Department August, 1962 ACKNOWLEDGMENTS The author wishes to express his...

Quddus, Mohammad Abdul

1962-01-01T23:59:59.000Z

370

Procedures for sampling radium-contaminated soils  

SciTech Connect (OSTI)

Two procedures for sampling the surface layer (0 to 15 centimeters) of radium-contaminated soil are recommended for use in remedial action projects. Both procedures adhere to the philosophy that soil samples should have constant geometry and constant volume in order to ensure uniformity. In the first procedure, a ''cookie cutter'' fashioned from pipe or steel plate, is driven to the desired depth by means of a slide hammer, and the sample extracted as a core or plug. The second procedure requires use of a template to outline the sampling area, from which the sample is obtained using a trowel or spoon. Sampling to the desired depth must then be performed incrementally. Selection of one procedure over the other is governed primarily by soil conditions, the cookie cutter being effective in nongravelly soils, and the template procedure appropriate for use in both gravelly and nongravelly soils. In any event, a minimum sample volume of 1000 cubic centimeters is recommended. The step-by-step procedures are accompanied by a description of the minimum requirements for sample documentation. Transport of the soil samples from the field is then addressed in a discussion of the federal regulations for shipping radioactive materials. Interpretation of those regulations, particularly in light of their application to remedial action soil-sampling programs, is provided in the form of guidance and suggested procedures. Due to the complex nature of the regulations, however, there is no guarantee that our interpretations of them are complete or entirely accurate. Preparation of soil samples for radium-226 analysis by means of gamma-ray spectroscopy is described.

Fleischhauer, H.L.

1985-10-01T23:59:59.000Z

371

Organic Phosphoric Acid of the Soil.  

E-Print Network [OSTI]

TEXAS AGRICULTURAL EXPERIMENT STATIONS BULLETIN NO. +6CT /36 CHEMICAL SECTION, FEBRUARY, 191 1 I TECHNICAL BULLETIN Organic Phosphoric Acid of the Soil BY G. S. FRAPS, Chemist POSTOFFICE College Station, Brazos County, 'Texas. ,\\ustin... . ................................................ introduction 5 .............................. hmmonia-Soluble Phosphoric Acid 5 ................ Solubility of Phosphates in Ammonia 6 I Fixation of Phosphoric Acid from Ammonia .......... 7 Effect of Ratio of Soil to Solvent in Extraction of Phos- I I...

Fraps, G. S. (George Stronach)

1911-01-01T23:59:59.000Z

372

Survival of Salmonella typhimurium in soil  

E-Print Network [OSTI]

~th' in Soil. (August 1975) Larry Marvin Zibilskes B. S. , Texas AAM University Chairman of Advisory Committee: Dr. Richard Lleaver Land application is a desirable alternative for the disposal and utilization of cattle manure because nutri- ents... in the manure may be used by plants for growth. This practice may constitute a health hazard to animals coming into contact with manured soil. Salmonella ~t h- imurium is a commonly encountered intestinal bacterium which is pathogenic for warm...

Zibilske, Larry Marvin

1975-01-01T23:59:59.000Z

373

Soil Fumigation for Plant Disease Control.  

E-Print Network [OSTI]

satisfactory results were secured wikh xylene, ethylene dichloride, sodium cyanide and formaldehyde. Paper impregnated wit11 hoof-and-horn glue, casein glue, or vegetttble paste, and adequately sealed at the edges, was most satisfactory for con- fining... of a system of electrically heated units in the plant bed or soil box has been developed. Liquid soil drenches with disinfecting chemicals such as mercuric chlo- ride, formaldehyde, various organic mercury compounds, cyanide compounds, sulphuric...

Young, P. A. (Paul Allen); Godfrey, G. H. (George Harold)

1943-01-01T23:59:59.000Z

374

Soil degradation, global warming and climate impacts  

E-Print Network [OSTI]

will demonstrate one methodology for assessing the potential large-scale impacts of soil degradation on African climates and water resources. In addition it will compare and contrast these impacts to those expected from global warming and compare impacts for differ...- ent watershed regions on the continent. 2. METHODS In order to make a similar comparison between pro- jected climate change scenarios due to global warming © Inter-Research 2001 *E-mail: feddema@ku.edu Soil degradation, global warming and climate...

Feddema, Johannes J.; Freire, Sergio Carneiro

2001-01-01T23:59:59.000Z

375

Possibilities of Sulphur as a Soil Amendment.  

E-Print Network [OSTI]

TEXAS AGRICULTURAL EXPERIMENT STATION A. B. CONNER, DIRECTOR COLLEGE STATION, BRAZOS COUNTY, TEXAS BULLETIN NO. 414 AUGUST, 1930 DIVISION OF CHEMISTRY POSSIBILITIES OF SULPHUR AS A - SOIL AMENDMENT AGRICULTURAL AND MECHANICAL COLLEGE OF TEXAS... . --- Agronomist B. C. LANGLEY,'B. S., Assistant in Soils PUBLICATIONS: A. D. JACKSON, Chief VETERINARY SCIENCE: *M. FRANCIS, D. V. M., Chief. H SCHMIDT D V M Veferznarian E: JUNGHE~R, D. V. M.. Veterinarran W T HARDY D V RI., Veterinnrian F.'E.'CARROL;, D...

Fraps, G. S. (George Stronach)

1930-01-01T23:59:59.000Z

376

Remediating pesticide contaminated soils using solvent extraction  

SciTech Connect (OSTI)

Bench-scale solvent extraction studies were performed on soil samples obtained from a Superfund site contaminated with high levels of p,p{prime}-DDT, p,p{prime}-DDE and toxaphene. The effectiveness of the solvent extraction process was assessed using methanol and 2-propanol as solvents over a wide range of operating conditions. It was demonstrated that a six-stage methanol extraction using a solvent-to-soil ratio of 1.6 can decrease pesticide levels in the soil by more than 99% and reduce the volume of material requiring further treatment by 25 times or more. The high solubility of the pesticides in methanol resulted in rapid extraction rates, with the system reaching quasi-equilibrium state in 30 minutes. The extraction efficiency was influenced by the number of extraction stages, the solvent-to-soil ratio, and the soil moisture content. Various methods were investigated to regenerate and recycle the solvent. Evaporation and solvent stripping are low cost and reliable methods for removing high pesticide concentrations from the solvent. For low concentrations, GAC adsorption may be used. Precipitating and filtering pesticides by adding water to the methanol/pesticide solution was not successful when tested with soil extracts. 26 refs., 10 figs., 6 tabs.

Sahle-Demessie, E.; Meckes, M.C.; Richardson, T.L. [National Management Research Lab., Cincinnati, OH (United States)

1996-12-31T23:59:59.000Z

377

The influence of soluble anions upon some physical and physico-chemical properties of soils  

E-Print Network [OSTI]

Miller soil and solutions of various sodium salts ..................... ..................... . 22 Figure 2. Breaking strength of artificial soil crusts made from Miller soil and solutions of various potassium SaltS .................. ......... 23... Figure 3, Breaking strength of artificial soil crusts made from Lake Charles soil and solutions of various sodium salts ....................................... 24 Figure 4. Breaking strength of artificial soil crusts made from Lake Charles soil...

Longenecker, Donald Edwin

1957-01-01T23:59:59.000Z

378

Thermionic converter temperature controller  

DOE Patents [OSTI]

A method and apparatus for controlling the temperature of a thermionic reactor over a wide range of operating power, including a thermionic reactor having a plurality of integral cesium reservoirs, a honeycomb material disposed about the reactor which has a plurality of separated cavities, a solid sheath disposed about the honeycomb material and having an opening therein communicating with the honeycomb material and cavities thereof, and a shell disposed about the sheath for creating a coolant annulus therewith so that the coolant in the annulus may fill the cavities and permit nucleate boiling during the operation of the reactor.

Shaner, Benjamin J. (McMurray, PA); Wolf, Joseph H. (Pittsburgh, PA); Johnson, Robert G. R. (Trafford, PA)

2001-04-24T23:59:59.000Z

379

Thermionic Converter Temperature Controller  

SciTech Connect (OSTI)

A method and apparatus for controlling the temperature of a thermionic reactor over a wide range of operating power, including a thermionic reactor having a plurality of integral cesium reservoirs, a honeycomb material disposed about the reactor which has a plurality of separated cavities, a solid sheath disposed about the honeycomb material and having an opening therein communicating with the honeycomb material and cavities thereof, and a shell disposed about the sheath for creating a coolant annulus therewith so that the coolant in the annulus may fill the cavities and permit nucleate boiling during the operation of the reactor.

Shaner,B. J.; Wolf, Joseph H.; Johnson, Robert G. R.

1999-08-23T23:59:59.000Z

380

Drexel University Temperature Sensors  

SciTech Connect (OSTI)

This document summarizes background information and presents results related to temperature measurements in the Advanced Test Reactor (ATR) National Scientific User Facility (NSUF) Drexel University Project 31091 irradiation. The objective of this test was to assess the radiation performance of new ceramic materials for advanced reactor applications. Accordingly, irradiations of transition metal carbides and nitrides were performed using the Hydraulic Shuttle Irradiation System (HSIS) in the B-7 position and in static capsules inserted into the A-3 and East Flux Trap Position 5 locations of the ATR.

K. L. Davis; D. L. Knudson; J. L. Rempe; B. M. Chase

2014-09-01T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


381

NON-DESTRUCTIVE SOIL CARBON ANALYZER.  

SciTech Connect (OSTI)

This report describes the feasibility, calibration, and safety considerations of a non-destructive, in situ, quantitative, volumetric soil carbon analytical method based on inelastic neutron scattering (INS). The method can quantify values as low as 0.018 gC/cc, or about 1.2% carbon by weight with high precision under the instrument's configuration and operating conditions reported here. INS is safe and easy to use, residual soil activation declines to background values in under an hour, and no radiological requirements are needed for transporting the instrument. The labor required to obtain soil-carbon data is about 10-fold less than with other methods, and the instrument offers a nearly instantaneous rate of output of carbon-content values. Furthermore, it has the potential to quantify other elements, particularly nitrogen. New instrumentation was developed in response to a research solicitation from the U.S. Department of Energy (DOE LAB 00-09 Carbon Sequestration Research Program) supporting the Terrestrial Carbon Processes (TCP) program of the Office of Science, Biological and Environmental Research (BER). The solicitation called for developing and demonstrating novel techniques for quantitatively measuring changes in soil carbon. The report includes raw data and analyses of a set of proof-of-concept, double-blind studies to evaluate the INS approach in the first phase of developing the instrument. Managing soils so that they sequester massive amounts of carbon was suggested as a means to mitigate the atmospheric buildup of anthropogenic CO{sub 2}. Quantifying changes in the soils' carbon stocks will be essential to evaluating such schemes and documenting their performance. Current methods for quantifying carbon in soil by excavation and core sampling are invasive, slow, labor-intensive and locally destroy the system being observed. Newly emerging technologies, such as Laser Induced Breakdown Spectroscopy and Near-Infrared Spectroscopy, offer soil-carbon analysis; however, these also are invasive and destructive techniques. The INS approach permits quantification in a relatively large volume of soil without disrupting the measurement site. The technique is very fast and provides nearly instantaneous results thereby reducing the cost, and speeding up the rate of analysis. It also has the potential to cover large areas in a mobile scanning mode. These capabilities will significantly advance the tracking carbon sequestration and offer a tool for research in agronomy, forestry, soil ecology and biogeochemistry.

WIELOPOLSKI,L.MITRA,S.HENDREY,G.ORION,I.ROGERS,H.TORBERT,A.PRIOR,S.RUNION,B.

2004-02-01T23:59:59.000Z

382

Crowdsourcing urban air temperatures from smartphone battery?temperatures  

E-Print Network [OSTI]

Accurate air temperature observations in urban areas are important for meteorology and energy demand planning. They are indispensable to study the urban heat island effect and the adverse effects of high temperatures on ...

Overeem, A.

383

E-Print Network 3.0 - affecting soil erosion Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

the soil to deteriorate. Soil erosion by water, and the impact of sediment... or control soil water ... Source: Iowa State University, Office of Biorenewables Programs Collection:...

384

E-Print Network 3.0 - alentejo soils surface Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

mineral soil surface. humus form: A group of soil horizons located at or near... on the soil surface in ... Source: Collection: Renewable Energy 35 Chapter 1 Introduction Page...

385

E-Print Network 3.0 - air soil water Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

iii. Soil-Plant Relationships iv. Cation exchange IV. Pollution of Water, Soil, and Air: (Lecture... unsaturated unsteady water flow X. Gaseous Phase of Soils (Hillel pages...

386

E-Print Network 3.0 - air water soil Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

iii. Soil-Plant Relationships iv. Cation exchange IV. Pollution of Water, Soil, and Air: (Lecture... unsaturated unsteady water flow X. Gaseous Phase of Soils (Hillel pages...

387

E-Print Network 3.0 - acids soils ph Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Improve Landscape Tree Performance Summary: Engineering Urban Soils to Improve Landscape Tree Performance P. Eric Wiseman, Ph.D. Assistant... Soil - Crusting 12;Urban Soil -...

388

E-Print Network 3.0 - affected granular soils Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

platy, prismlike, and blocklike (see Figure 3... ). Soil structure affects soil water movement when a soil is saturated with water. Water can move quickly... between...

389

E-Print Network 3.0 - abandoned pasture soils Sample Search Results  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

studies do report losses of soil carbon in pastures due to their heavy use. Soil... of Carbon Sequestration in Soils ... Source: Marn-Spiotta, Erika - Department of Geography,...

390

INTERANNUAL VARIABILITY IN GLOBAL SOIL RESPIRATION (1980-1994) Interannual Variability in Global Soil  

E-Print Network [OSTI]

INTERANNUAL VARIABILITY IN GLOBAL SOIL RESPIRATION (1980-1994) NDP-081 Interannual Variability in Global Soil Respiration on a 0.5 Degree Grid Cell Basis (1980-1994) Contributed by: James W. Raich 1, Tennessee 37831-6335. The ORNL is managed by UT-Battelle, LLC for the U.S. DEPARTMENT OF ENERGY under

391

The effects of soil type and chemical treatment on nickel speciation in refinery enriched soils  

E-Print Network [OSTI]

The effects of soil type and chemical treatment on nickel speciation in refinery enriched soils Aerial deposition of Ni from a refinery in Port Colborne, Ontario, Canada has resulted in the enrichment in vegetable crops grown in the vicinity of the refinery. Conversely, dolomitic lime- stone additions resulted

392

UNCORRECTEDPROOF 1 Towards deterministic downscaling of SMOS soil moisture using MODIS derived soil  

E-Print Network [OSTI]

of environmental applications including meteor- 33 ology, hydrology, water resource management and climatology. 34UNCORRECTEDPROOF 1 Towards deterministic downscaling of SMOS soil moisture using MODIS derived soil Kerr b 4 a Civil and Environmental Engineering, The University of Melbourne, Australia 5 b Centre d

Boyer, Edmond

393

Eect of sludge-processing mode, soil texture and soil pH on metal mobility in undisturbed soil columns under accelerated loading  

E-Print Network [OSTI]

Eect of sludge-processing mode, soil texture and soil pH on metal mobility in undisturbed soil 8 September 1999 Abstract The eect of sludge processing (digested dewatered, pelletized, alkaline (Lamellic Hapludalf), at initial pH levels of 5 and 7. Sludges were applied during four accelerated cropping

Walter, M.Todd

394

Electrokinetic electrode system for extraction of soil contaminants from unsaturated soils  

DOE Patents [OSTI]

An electrokinetic electrode assembly is described for use in extraction of soil contaminants from unsaturated soil in situ. The assembly includes a housing for retaining a liquid comprising an electrolyte solution, pure water, and soil water, the housing being in part of porous material capable of holding a vacuum. An electrode is mounted in the housing. The housing is provided with a vacuum orifice for effecting a vacuum within the housing selectively to control flow of soil water through the housing into the chamber and to control outflow of the liquid from the chamber. The assembly further includes conduit means for removing the liquid from the housing and returning the electrolyte solution to the housing, and a conduit for admitting pure water to the housing. An electrode system and method are also revealed for extraction of soil contaminants. The system and method utilize at least two electrode assemblies as described above. 5 figs.

Lindgren, E.R.; Mattson, E.D.

1995-07-25T23:59:59.000Z

395

Electrokinetic electrode system for extraction of soil contaminants from unsaturated soils  

DOE Patents [OSTI]

There is presented an electrokinetic electrode assembly for use in extraction of soil contaminants from unsaturated soil in situ. The assembly includes a housing for retaining a liquid comprising an electrolyte solution, pure water, and soil water, the housing being in part of porous material capable of holding a vacuum. An electrode is mounted in the housing. The housing is provided with a vacuum orifice for effecting a vacuum within the housing selectively to control flow of soil water through the housing into the chamber and to control outflow of the liquid from the chamber. The assembly further includes conduit means for removing the liquid from the housing and returning the electrolyte solution to the housing, and a conduit for admitting pure water to the housing. There is further presented an electrode system and method for extraction of soil contaminants, the system and method utilizing at least two electrode assemblies as described above.

Lindgren, Eric R. (Albuquerque, NM); Mattson, Earl D. (Albuquerque, NM)

1995-01-01T23:59:59.000Z

396

Soil type: Metabasic soils have 50 to 80 percent more mineralizable C than granitic soils. The same soils appear to more efficiently retain TN and some TOC at greater depths. Very low DOC in both soils indicate efficient C utilization and incorporation in  

E-Print Network [OSTI]

Soil type: Metabasic soils have 50 to 80 percent more mineralizable C than granitic soils. The same indicate efficient C utilization and incorporation in microbial or SOM pools. Greater mineral N in granite percent. There is not evidence of the impact of increased available C on TOC in granitic soils. Soil

Norton, Jay B.

397

Philosophy 26 High Temperature Superconductivity  

E-Print Network [OSTI]

Philosophy 26 High Temperature Superconductivity By Ohm's Law, resistance will dim. Low temperature superconductivity was discovered in 1911 by Heike was explained by BCS theory. BCS theory explains superconductivity microscopically

Callender, Craig

398

The Greenhouse Effect Temperature Equilibrium  

E-Print Network [OSTI]

The Greenhouse Effect #12;Temperature Equilibrium The Earth is in equilibrium with the Sun temperature is about 14C, or 287K. The 40K difference is due to the greenhouse effect. Essentially all

Walter, Frederick M.

399

Energy Savings with High Temperature Water Generation Systems  

E-Print Network [OSTI]

fuel costs ency but as shown the steam system requires from steam systems are wasting a lot of ener~y and 18.1 to 44.8 more energy at the boiler than HTW dollars. I since the losses are realized in getting the steam to the user. To further compare....21 4 12.00 2.0 85 630 545 7.41 6 14.00 2.5 98 703 605 7.17 8 17.50 2.5 115 763 648 6.63 10 18.00 2.5 136 822 686 6.04 Assumptions: a. Heating medium temperature: 400 0 F c. Average pipe/conduit buried depth 4ft. b. Average soil temperature: 52...

Manicke, A. C.

1982-01-01T23:59:59.000Z

400

Dynamic properties of subgrade soils, including environmental effects  

E-Print Network [OSTI]

-up, Showing Endcaps With the Induction Coils and Psychrometers . . . . 39 Photograph of Calibration Device 41 27 Schematic of Layered Systems Used to Determine Stresses 44 28 Compaction Curve for the Moscow Soil Showing th~ Soil Suction Contours (in psi..., 1 psi = 6. 9 kN/m ) . 47 Compaction Curve for the Floydada Soil Showing the Soil Suction Contours (in psi, 1 psi 6. 9 kN/mZ) 3O Compaction Curve for the Allenfarm Soil Showing the Soil Suction Contours (in psi, 1 psi 6. 9 kN/mZ) 49 Typical...

Edris, Earl Victor

1976-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


401

Battery system with temperature sensors  

DOE Patents [OSTI]

A battery system to monitor temperature includes at least one cell with a temperature sensing device proximate the at least one cell. The battery system also includes a flexible member that holds the temperature sensor proximate to the at least one cell.

Wood, Steven J.; Trester, Dale B.

2012-11-13T23:59:59.000Z

402

Measuring soil moisture with imaging radars  

SciTech Connect (OSTI)

An empirical algorithm for the retrieval of soil moisture content and surface Root Mean Square (RMS) height from remotely sensed radar data was developed using scatterometer data. The algorithm is optimized for bare surfaces and requires two copolarized channels at a frequency between 1.5 and 11 GHz. It gives best results for kh {le} 2.5, {mu}{sub {upsilon}}{le}35%, and {theta}{ge}30{degree}. Omitting the usually weaker hv-polarized returns makes the algorithm less sensitive to system cross-talk and system noise, simplify the calibration process and adds robustness to the algorithm in the presence of vegetation. However, inversion results indicate that significant amounts of vegetation (NDVI>0.4) cause the algorithm to underestimate soil moisture and overestimate RMS height. A simple criteria based on the {sigma}{sub hv}{sup 0}/{sigma}{sub vv}{sup 0} ratio is developed to select the areas where the inversion is not impaired by the vegetation. The inversion accuracy is assessed on the original scatterometer data sets but also on several SAR data sets by comparing the derived soil moisture values with in-situ measurements collected over a variety of scenes between 1991 and 1994. Both spaceborne (SIR-C) and airborne (AIRSAR) data are used in the test. Over this large sample of conditions, the RMS error in the soil moisture estimate is found to be less than 4.2% soil moisture.

Dubois, P.C.; Zyl, J. van [California Inst. of Tech., Pasadena, CA (United States). Jet Propulsion Lab.] [California Inst. of Tech., Pasadena, CA (United States). Jet Propulsion Lab.; Engman, T. [NASA Goddard Space Flight Center, Greenbelt, MD (United States)] [NASA Goddard Space Flight Center, Greenbelt, MD (United States)

1995-07-01T23:59:59.000Z

403

Hot Pot Contoured Temperature Gradient Map  

SciTech Connect (OSTI)

Temperature gradient contours derived from Oski temperature gradient hole program and from earlier published information.

Lane, Michael

2013-06-28T23:59:59.000Z

404

Hot Pot Contoured Temperature Gradient Map  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Temperature gradient contours derived from Oski temperature gradient hole program and from earlier published information.

Lane, Michael

405

Effect of soil temperature on resistance of rice to seedling blight caused by Sclerotium rolfsii Sacc  

E-Print Network [OSTI]

I":". . -"';-'. , ;::::, RP9?C2 '|GZ - GGt'W "ZR%Zh&'~I'Tgfi *" zo?: 3~Gh'&IPWI|tG! Eh QZ 'BXCAK. - TQ '-, ';: ?' ! ', -':;, i", , ;. :;?-i;'!:G :. BGGZZIIG BBIZGGG, ':G"G", Kl'GZ' h il 'ZZZIIGXIIXGLGZGBZZ;::"BGG. ''::, . :":G ';"', . '?'i... ''' ' ', ' '' ? ' ', , ' ZZ " I AVP~' . ' I. , X Z?Z" '' 1 ?''. .. l~;t, , I. h 3R'kCK6I;"'VIh'. Z-hg~Z, ' ', '?" l;, I, ', 'hhh ~~i Z'. zZ, , *, ~~;". ?', BGIGI. ' 'I, . ; =, '-. ?::-";, ':. "?::. . ":-, :, :;. ";, . "', '-'-. -'::;:, :. ; T5@-', : jjyft8i:-. W4%es, , :pi...

Weerapat, Praphas

1964-01-01T23:59:59.000Z

406

Soil fungicides in relation to cotton seedling disease at various temperature levels  

E-Print Network [OSTI]

to obtain controlled spacing an4 4epth of seed ?hon ylanting, ~, , ~ 18 Xllnotration of seedling disease grades. Xi No evidence of diseases' energed 2 Sprouted' no e?L'donee of disease; no ssLergenoe. 5 Lesion less than three nao in length? 4i Lesion... of disease. 2, Emerged; lesion lees than three nn. long. ~Eaepgedj le&oh learn Qlall I%a ss, 10$$, gl aineb io the non proprietary nano ef sino ?thglene bi sdithiooarhanate. 4. Knerged~ sevorelF lesiono4, but not girdle4. 5? Energed~ dea4 or girdling...

Ranney, Carleton David

1955-01-01T23:59:59.000Z

407

Soil carbon sensitivity to temperature and carbon use efficiency compared across microbial-ecosystem models  

E-Print Network [OSTI]

, accounting for the response of microbial communities to environmental parameters in Earth system models may

German, Donovan P.

408

Low-Temperature Soil Heating Using Renewable Energy Anthony J. Rossman1  

E-Print Network [OSTI]

was harvested with a hybrid photovoltaic/wind electric system. The electrical energy generated by the hybrid with a lower potential environmental impact than traditional strategies and can be cost effective at sites contaminant volatility, diffusion, desorption, and microbiological activity. Direct and indirect solar energy

Vermont, University of

409

Seasonality of soil CO2 efflux in a temperate forest: Biophysical effects of snowpack and spring freeze–thaw cycles  

SciTech Connect (OSTI)

Changes in characteristics of snowfall and spring freeze–thaw-cycle (FTC) events under the warming climate make it critical to understand biophysical controls on soil CO2 efflux (RS) in seasonally snow-covered ecosystems. We conducted a snow removal experiment and took year-round continuous automated measurements of RS, soil temperature (T5) and soil volumetric water content at the 5 cm depth (W5) with a half-hour interval in a Chinese temperate forest in 2010–2011. Our objectives were to: (1) develop statistical models to describe the seasonality of RS in this forest; (2) quantify the contribution of seasonal RS to the annual budget; (3) examine biophysical effects of snowpack on RS; and (4) test the hypothesis that an FTC-induced enhancement of RS is jointly driven by biological and physical processes.

Wang, Chuankuan; Han, Yi; Chen, Jiquan; Wang, Xingchang; Zhang, Quanzhi; Bond-Lamberty, Benjamin

2013-08-15T23:59:59.000Z

410

Site monitoring from soil sample analysis  

SciTech Connect (OSTI)

Soil samples have been collected for the past three years as part of a long range monitoring program. The program was designed to provide information on possible migration of plutonium in soil and to provide data for comparison with the EPA proposed guidance on transuranium elements in the environment. Samples have been collected at six locations west of Indiana Street within the eastern boundaries of the Rocky Flats Plant site. The EPA comparison study has been performed at five sites and the plutonium migration study is underway at the sixth site. The data on plutonium analyses will be compared to the EPA screening level of 0.20 ..mu..Ci/m/sup 2/ (74 x 10/sup 8/ Bq/km/sup 2/) in the five boundary sites. Possible migration trends will be examined for the plutonium data on soils from the other site.

Illsley, C.T.

1982-01-01T23:59:59.000Z

411

Chemotactic selection of pollutant degrading soil bacteria  

DOE Patents [OSTI]

A method is described for identifying soil microbial strains which may be bacterial degraders of pollutants. This method includes: Placing a concentration of a pollutant in a substantially closed container; placing the container in a sample of soil for a period of time ranging from one minute to several hours; retrieving the container and collecting its contents; microscopically determining the identity of the bacteria present. Different concentrations of the pollutant can be used to determine which bacteria respond to each concentration. The method can be used for characterizing a polluted site or for looking for naturally occurring biological degraders of the pollutant. Then bacteria identified as degraders of the pollutant and as chemotactically attracted to the pollutant are used to innoculate contaminated soil. To enhance the effect of the bacteria on the pollutant, nutrients are cyclicly provided to the bacteria then withheld to alternately build up the size of the bacterial colony or community and then allow it to degrade the pollutant.

Hazen, T.C.

1991-03-04T23:59:59.000Z

412

Quantum Chemistry at Finite Temperature  

E-Print Network [OSTI]

In this article, we present emerging fields of quantum chemistry at finite temperature. We discuss its recent developments on both experimental and theoretical fronts. First, we describe several experimental investigations related to the temperature effects on the structures, electronic spectra, or bond rupture forces for molecules. These include the analysis of the temperature impact on the pathway shifts for the protein unfolding by atomic force microscopy (AFM), the temperature dependence of the absorption spectra of electrons in solvents, and the temperature influence over the intermolecular forces measured by the AFM. On the theoretical side, we review advancements made by the author in the coming fields of quantum chemistry at finite temperature. Starting from the Bloch equation, we have derived the sets of hierarchy equations for the reduced density operators in both canonical and grand canonical ensembles. They provide a law according to which the reduced density operators vary in temperature for the identical and interacting many-body systems. By taking the independent particle approximation, we have solved the equations in the case of a grand canonical ensemble, and obtained an energy eigenequation for the molecular orbitals at finite temperature. The explicit expression for the temperature-dependent Fock operator is also given. They form a mathematical foundation for the examination of the molecular electronic structures and their interplay with finite temperature. Moreover, we clarify the physics concerning the temperature effects on the electronic structures or processes of the molecules, which is crucial for both theoretical understanding and computation. Finally, ....

Liqiang Wei

2006-05-23T23:59:59.000Z

413

Soil Testing Following Flooding, Overland Flow of Wastewater and other Freshwater Disasters  

E-Print Network [OSTI]

Freshwater flooding can seriously affect soil fertility and the physical and chemical properties of soil. This publication explains how to reclaim flooded soil. Having the soil tested for microbes, pesticides, hydrocarbons and other contaminants...

Provin, Tony; Feagley, Sam E.; Pitt, John L.; McFarland, Mark L.

2009-05-26T23:59:59.000Z

414

SOIL MOISTURE RETENTION CHARACTERISTICS AND HYDRAULIC CONDUCTIVITY FOR DIFFERENT AREAS IN INDIA IN SELECTED STATES  

E-Print Network [OSTI]

SOIL MOISTURE RETENTION CHARACTERISTICS AND HYDRAULIC CONDUCTIVITY FOR DIFFERENT AREAS IN INDIA systems require knowledge of the relationships between soil moisture content (), soil water pressure (h) and unsaturated hydraulic conductivity (K). This study involved field and laboratory determination of soil

Kumar, C.P.

415

Soil community composition and ecosystem processes Comparing agricultural ecosystems with natural ecosystems  

E-Print Network [OSTI]

Soil community composition and ecosystem processes Comparing agricultural ecosystems with natural, nitrogen, pesticides Abstract. Soil organisms play principal roles in several ecosystem functions, i decomposition, and acting as an environmental buffer. Agricultural soils would more closely resemble soils

Neher, Deborah A.

416

CONTRIBUTION TO THE KNOWLEDGE OF SOIL ALGAE OF TWO ABANDONED INDUSTRIAL  

E-Print Network [OSTI]

CONTRIBUTION TO THE KNOWLEDGE OF SOIL ALGAE OF TWO ABANDONED INDUSTRIAL SEDIMENTATION BASINS Sixty three species of soil algae and Cyanoprocaryota were recovered from eight investigated sites sites in Chvaletice suggests soil toxicity of these biotopes. Keywords Soil algae, Chlorophyta

417

In situ removal of contamination from soil  

DOE Patents [OSTI]

A process of remediation of cationic heavy metal contamination from soil utilizes gas phase manipulation to inhibit biodegradation of a chelating agent that is used in an electrokinesis process to remove the contamination. The process also uses further gas phase manipulation to stimulate biodegradation of the chelating agent after the contamination has been removed. The process ensures that the chelating agent is not attacked by bioorganisms in the soil prior to removal of the contamination, and that the chelating agent does not remain as a new contaminant after the process is completed. 5 figs.

Lindgren, E.R.; Brady, P.V.

1997-10-14T23:59:59.000Z

418

In situ removal of contamination from soil  

DOE Patents [OSTI]

A process of remediation of cationic heavy metal contamination from soil utilizes gas phase manipulation to inhibit biodegradation of a chelating agent that is used in an electrokinesis process to remove the contamination, and further gas phase manipulation to stimulate biodegradation of the chelating agent after the contamination has been removed. The process ensures that the chelating agent is not attacked by bioorganisms in the soil prior to removal of the contamination, and that the chelating agent does not remain as a new contaminant after the process is completed.

Lindgren, Eric R. (Albuquerque, NM); Brady, Patrick V. (Albuquerque, NM)

1997-01-01T23:59:59.000Z

419

Sherm Soils - Distribution, Importance, Variability, and Management.  

E-Print Network [OSTI]

from about 101 0 30' to 1030 30' west longitude and from about 35 0 40' to 360 40' north latitude. This area is bounded by the breaks above the North Canadian River on the north, the caprock escarpment at the Cana dian River on the south..., the caprock escarpment at the High Plains Rolling Plains boundary on the east, and a catena of loamy soils extending from Kerrick to Channing on the west. Within the area of occurrence, Sherm soils occupy about 75 percent of the land surface. Elevation...

Unger, Paul W.; Pringle, Fred B.

1986-01-01T23:59:59.000Z

420

Olton Soils - Distribution, Importance Variability and Management.  

E-Print Network [OSTI]

from about 101 ?10' to 103?50' West longitude and about 32?50' to 35?40' North latitude. Elevation of the sur face of Olton soils ranges from about 2,600 to 4 ,200 feet above mean sea level. The area is in a semiarid climatic zone where average.... The depth to a strong calcic horizon averages about 49 inches. The CaC03 content ofthis layer ranges from 35 to 56 percent and averages about 45 percent. The primary area of occurrence for Olton soils includes the area south and west of a line...

Unger, Paul W.; Pringle, Fred B.

1998-01-01T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


421

Biochar amendment and greenhouse gas emissions from agricultural soils   

E-Print Network [OSTI]

The aim of this study was to investigate the effects of biochar amendment on soil greenhouse gas (GHG) emissions and to elucidate the mechanisms behind these effects. I investigated the suppression of soil carbon dioxide ...

Case, Sean Daniel Charles

2013-11-28T23:59:59.000Z

422

Testing Your Soil: How to Collect and Send Samples  

E-Print Network [OSTI]

Soil tests can be used to estimate the kinds and amounts of soil nutrients available to plants and as aids in determining fertilizer needs. This publication covers the three-step procedure for obtaining sample bags and instructions, collecting...

Provin, Tony; Pitt, John L.

2002-06-26T23:59:59.000Z

423

Review of soil water models with respect to savanna hydrology   

E-Print Network [OSTI]

Effective management leading towards sustainable rangeland production in arid and semi-arid regions will stem from effective soil water management and comprehension of the hydrological properties of the soil in relation to pastoralism. However...

Derry, Julian F; Russell, Graham; Liedloff, Adam C

2006-07-21T23:59:59.000Z

424

Scaling hydraulic properties of a macroporous soil Binayak P. Mohanty  

E-Print Network [OSTI]

Scaling hydraulic properties of a macroporous soil Binayak P. Mohanty U.S. Salinity Laboratory, Riverside, California Abstract. Macroporous soils exhibit significant differences in their hydraulic properties for different pore domains. Multimodal hydraulic functions may be used to describe

Mohanty, Binayak P.

425

Variations in microbial community composition through two soil depth profiles  

E-Print Network [OSTI]

35% of the total quantity of microbial biomass found in the top 2 m of soil is found below a depth: Microbial diversity; Phospholipid fatty acid; Soil profile; Community composition; Microbial biomass 1

Fierer, Noah

426

Ground-based measurements of soil water storage in Texas  

E-Print Network [OSTI]

Landslides EROSION Dust Weak SOIL STRENGTH Hard Latent heat SOLAR ENERGY Sensible heat Energy Stevens' HydraProbe Soil T, q, and ECapparent ADVANTAGES Lower initial cost Spatial distribution SDI

Yang, Zong-Liang

427

Investigation of Soil Moisture - Vegetation Interactions in Oklahoma  

E-Print Network [OSTI]

, but not well understood climate factor. This study examines soil moisture-vegetation health interactions using both in situ observations and land surface model simulations. For the observational study, soil moisture is taken from 20 in situ Oklahoma Mesonet...

Ford, Trenton W.

2013-03-06T23:59:59.000Z

428

Agricultural soil and its conservation in Mexico as percei  

E-Print Network [OSTI]

natural and human causes as somewhat major causes of agricultural soil degradation in Mexico, with human causes being more of a cause than natural causes. 3. Students felt that soil conservation efforts are needed; these efforts should...

Revello, Valerie Ann

1995-01-01T23:59:59.000Z

429

Earth pressures and deformations in civil infrastructure in expansive soils  

E-Print Network [OSTI]

This dissertation includes the three major parts of the study: volume change, and lateral earth pressure due to suction change in expansive clay soils, and design of civil infrastructure drilled pier, retaining wall and pavement in expansive soils...

Hong, Gyeong Taek

2008-10-10T23:59:59.000Z

430

The spatial and temporal organization of soil moisture  

E-Print Network [OSTI]

Runoff, infiltration, evaporation and transpiration and-at climatic scales-precipitation are hydrologic processes that strongly depend on soil moisture. From a descriptive viewpoint, soil moisture is. characterized by an extremely high degree...

Vogel, Gregor Klaus

1995-01-01T23:59:59.000Z

431

Soil moisture modeling and scaling using passive microwave remote sensing  

E-Print Network [OSTI]

Soil moisture in the shallow subsurface is a primary hydrologic state governing land-atmosphere interaction at various scales. The primary objectives of this study are to model soil moisture in the root zone in a distributed manner and determine...

Das, Narendra N.

2007-04-25T23:59:59.000Z

432

aggregate soil samples: Topics by E-print Network  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

and questionnaires for your own identification. Directions for obtaining soil samples Norton, Jay B. 35 Testing Your Soil: How to Collect and Send Samples Texas A&M University...

433

Application of Polymeric Agents for Improved Soil Decontamination  

SciTech Connect (OSTI)

The objectives of the Thrust II project include optimization of the technology for PO Mayak soils, identification of clean up requirements, design and construction of a mobile production-scale process system, installation and deployment of the soil washing technology.

Heiser, John

2008-09-30T23:59:59.000Z

434

The Farmer's Conundrum: Income from Biofuels or Protect the Soil...  

Broader source: Energy.gov (indexed) [DOE]

The Farmer's Conundrum: Income from Biofuels or Protect the Soil? The Farmer's Conundrum: Income from Biofuels or Protect the Soil? July 1, 2010 - 11:39am Addthis Lindsay Gsell...

435

Onsite Wastewater Treatment Systems: Septic Tank/Soil Absorption Field  

E-Print Network [OSTI]

For septic tank and soil absorption systems to work properly, homeowners must choose the right kind of system for their household size and soil type, and they must maintain them regularly. This publication explains the treatment, design, operation...

Lesikar, Bruce J.

2008-10-23T23:59:59.000Z

436

Modeling, estimation, and control of robot-soil interactions  

E-Print Network [OSTI]

This thesis presents the development of hardware, theory, and experimental methods to enable a robotic manipulator arm to interact with soils and estimate soil properties from interaction forces. Unlike the majority of ...

Hong, Won, 1971-

2001-01-01T23:59:59.000Z

437

An Open Source Simulation Model for Soil and Sediment Bioturbation  

E-Print Network [OSTI]

An Open Source Simulation Model for Soil and Sediment Bioturbation Katja Schiffers1 *¤a , Lorna (2011) An Open Source Simulation Model for Soil and Sediment Bioturbation. PLoS ONE 6(12): e28028. doi

Paris-Sud XI, Université de

438

High temperature interfacial superconductivity  

DOE Patents [OSTI]

High-temperature superconductivity confined to nanometer-scale interfaces has been a long standing goal because of potential applications in electronic devices. The spontaneous formation of a superconducting interface in bilayers consisting of an insulator (La.sub.2CuO.sub.4) and a metal (La.sub.1-xSr.sub.xCuO.sub.4), neither of which is superconducting per se, is described. Depending upon the layering sequence of the bilayers, T.sub.c may be either .about.15 K or .about.30 K. This highly robust phenomenon is confined to within 2-3 nm around the interface. After exposing the bilayer to ozone, T.sub.c exceeds 50 K and this enhanced superconductivity is also shown to originate from a 1 to 2 unit cell thick interfacial layer. The results demonstrate that engineering artificial heterostructures provides a novel, unconventional way to fabricate stable, quasi two-dimensional high T.sub.c phases and to significantly enhance superconducting properties in other superconductors. The superconducting interface may be implemented, for example, in SIS tunnel junctions or a SuFET.

Bozovic, Ivan (Mount Sinai, NY); Logvenov, Gennady (Port Jefferson Station, NY); Gozar, Adrian Mihai (Port Jefferson, NY)

2012-06-19T23:59:59.000Z

439

Removal of uranium from uranium-contaminated soils -- Phase 1: Bench-scale testing. Uranium in Soils Integrated Demonstration  

SciTech Connect (OSTI)

To address the management of uranium-contaminated soils at Fernald and other DOE sites, the DOE Office of Technology Development formed the Uranium in Soils Integrated Demonstration (USID) program. The USID has five major tasks. These include the development and demonstration of technologies that are able to (1) characterize the uranium in soil, (2) decontaminate or remove uranium from the soil, (3) treat the soil and dispose of any waste, (4) establish performance assessments, and (5) meet necessary state and federal regulations. This report deals with soil decontamination or removal of uranium from contaminated soils. The report was compiled by the USID task group that addresses soil decontamination; includes data from projects under the management of four DOE facilities [Argonne National Laboratory (ANL), Los Alamos National Laboratory (LANL), Oak Ridge National Laboratory (ORNL), and the Savannah River Plant (SRP)]; and consists of four separate reports written by staff at these facilities. The fundamental goal of the soil decontamination task group has been the selective extraction/leaching or removal of uranium from soil faster, cheaper, and safer than current conventional technologies. The objective is to selectively remove uranium from soil without seriously degrading the soil`s physicochemical characteristics or generating waste forms that are difficult to manage and/or dispose of. Emphasis in research was placed more strongly on chemical extraction techniques than physical extraction techniques.

Francis, C. W.

1993-09-01T23:59:59.000Z

440

Active cooling-based surface confinement system for thermal soil treatment  

DOE Patents [OSTI]

A thermal barrier is disclosed for surface confinement with active cooling to control subsurface pressures during thermal remediation of shallow (5-20 feet) underground contaminants. If steam injection is used for underground heating, the actively cooled thermal barrier allows the steam to be injected into soil at pressures much higher (20-60 psi) than the confining strength of the soil, while preventing steam breakthrough. The rising steam is condensed to liquid water at the thermal barrier-ground surface interface. The rapid temperature drop forced by the thermal barrier drops the subsurface pressure to below atmospheric pressure. The steam and contaminant vapors are contained by the thermal blanket, which can be made of a variety of materials such as steel plates, concrete slabs, membranes, fabric bags, or rubber bladders. 1 fig.

Aines, R.D.; Newmark, R.L.

1997-10-28T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


441

Active cooling-based surface confinement system for thermal soil treatment  

DOE Patents [OSTI]

A thermal barrier is disclosed for surface confinement with active cooling to control subsurface pressures during thermal remediation of shallow (5-20 feet) underground contaminants. If steam injection is used for underground heating, the actively cooled thermal barrier allows the steam to be injected into soil at pressures much higher (20-60 psi) than the confining strength of the soil, while preventing steam breakthrough. The rising steam is condensed to liquid water at the thermal barrier-ground surface interface. The rapid temperature drop forced by the thermal barrier drops the subsurface pressure to below atmospheric pressure. The steam and contaminant vapors are contained by the thermal blanket, which can be made of a variety of materials such as steel plates, concrete slabs, membranes, fabric bags, or rubber bladders.

Aines, Roger D. (Livermore, CA); Newmark, Robin L. (Pleasanton, CA)

1997-01-01T23:59:59.000Z

442

Soil surface modification in the Trans-Pecos region of Texas  

E-Print Network [OSTI]

higher on unplowed areas, but deep soils contained more soil water when root plowed on Upton gravelly loams. Deep Reagan silty clay loam soils contained more soil water after treatment than did untreated areas. Brush cover was significantly reduced... Deep Soil, Reagan Silty Clay Loam. Deep Soil, Upton Gravelly Loam . Total Grass Production. Forbs Shallow Soil, Reagan Silty Clay Loam Shallow Soil, Upton Gravelly Loam. Total Herbaceous Production Total Grass Production Forbs iv vii 14 14...

Merrill, Clifton Edwards

1983-01-01T23:59:59.000Z

443

2000): Soil carbon sequestration and land-use change: processes and potential  

E-Print Network [OSTI]

matter dynamics that may result in enhanced soil carbon sequestration with changes in land-use and soil

W. M. Post; K. C. Kwon

444

SOIL SURVEY OF PAYNE COUNTY, OKLAHOMA OSURR Section 4  

E-Print Network [OSTI]

25 6 4 11 25 41 72 25 74 49 74 11 51 4926 26 74 26 26 26 SOIL SURVEY OF PAYNE COUNTY, OKLAHOMA OSURR Section 4 0 400 800 1,200 1,600200 Feet 0 100 20050 Meters Web Soil Survey 1.1 National Cooperative Soil Survey 5/7/2007 Page 1 of 3 #12;MAP INFORMATION SOIL SURVEY OF PAYNE COUNTY, OKLAHOMA OSURR Section 4

Ghajar, Afshin J.

445

Arsenic distribution in soils surrounding the Utah copper smelter  

SciTech Connect (OSTI)

We investigated the extent of arsenic contamination from a Utah copper smelter as reflected by arsenic residue accumulated in the surface soil. The highest arsenic concentrations occurred within 3 km of the smelter. Arsenic soil contamination was evident up to 10 km from the smelter, with the major transport direction being ESE. Data from the subsurface soil samples indicated that arsenic has also leached through the soil.

Ball, A.L. (Univ. of Utah Coll. of Engineering, Salt Lake City); Rom, W.N.; Glenne, B.

1983-05-01T23:59:59.000Z

446

Comparison of methods for determining soil hydraulic characteristics  

E-Print Network [OSTI]

). Soil cores were centrifuged and the redistribution of water was measured as change in weight with time. Inconsistent results and limited data obtained with this method, consequently, prevented ade- quate conclusions from being made. Hydraulic... storage capacity of a soil is determined by infiltration, redistribution and drainage processes which also rely on knowledge of soil moisture movement. Three approaches used to determine the relevant hydraulic properties utitilized in describing soil...

Byrd Humphreys, Kathryn

1979-01-01T23:59:59.000Z

447

Systematic Variability of Soil Hydraulic Conductivity Across Three Vertisol Catenas  

E-Print Network [OSTI]

of soil measured on small samples is log-normally distributed and related to physical properties of that soil sample (Mapa, 1995; Reynolds and Zebchuk, 1996; Lin et al., 1998; Baldock and Nelson, 2000). The United States Department of Agriculture (USDA... structure and water content for clayey soils (Mapa, 1995; Baldock and Nelson, 2000). 6 Measurement Methods A variety of laboratory and field methods of measuring Ks are available. Laboratory measurements are typically conducted on undisturbed soil...

Rivera, Leonardo Daniel

2011-10-21T23:59:59.000Z

448

Measurement of thermodynamic temperature of high temperature fixed points  

SciTech Connect (OSTI)

The paper is devoted to VNIIOFI's measurements of thermodynamic temperature of the high temperature fixed points Co-C, Pt-C and Re-C within the scope of the international project coordinated by the Consultative Committee for Thermometry working group 5 'Radiation Thermometry'. The melting temperatures of the fixed points were measured by a radiance mode radiation thermometer calibrated against a filter radiometer with known irradiance spectral responsivity via a high temperature black body. This paper describes the facility used for the measurements, the results and estimated uncertainties.

Gavrilov, V. R.; Khlevnoy, B. B.; Otryaskin, D. A.; Grigorieva, I. A.; Samoylov, M. L.; Sapritsky, V. I. [All-Russian Research Institute for Optical and Physical Measurements (VNIIOFI), 46 Ozernaya St., Moscow 119361 (Russian Federation)] [All-Russian Research Institute for Optical and Physical Measurements (VNIIOFI), 46 Ozernaya St., Moscow 119361 (Russian Federation)

2013-09-11T23:59:59.000Z

449

High-temperature Pump Monitoring - High-temperature ESP Monitoring...  

Broader source: Energy.gov (indexed) [DOE]

Report Detecting Fractures Using Technology at High Temperatures and Depths - Geothermal Ultrasonic Fracture Imager (GUFI); 2010 Geothermal Technology Program Peer Review Report...

450

Historic climate change impacts on soil frost in the Mid-Western  

E-Print Network [OSTI]

#12;4 Why do we care about soil frost ? · Effects energy and water balance fluxes · Snowmelt events and significance of soil frost in the past century · To study how soil frost effects regional water and energy;17 Effects of soil frost on water & energy balance Differences = Frozen Soil ON ­ Frozen Soil OFF Runoff (RO

Cherkauer, Keith

451

Department of Crop and Soil Sciences Dr. Markus Flury, Professor  

E-Print Network [OSTI]

& Environmental Engineering, Chem- ical Engineering, Soil Science (with Soil Physics or Soil Chemistry emphasis, Engineering Science, or Biological Systems Engineering. The candidate will receive salary, health insurance eligibility verification as required by the US Citizenship and Immigration Services. PO Box 646420, Pullman

Flury, Markus

452

The Composition of the Soils of the Texas Panhandle.  

E-Print Network [OSTI]

. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5 Soil Types by Counties. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6 Armstrong County . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6 Briecoe County... BY COUNTIES. The following is a list of the types of soils found in the varwus counties accoTding to maps published by the Bureau of Soils. Armstrong County. Amarillo silty clay loam. Amarillo loam. Amarillo sands. Rough broken land. Vernon loam...

Fraps, G. S.

1915-01-01T23:59:59.000Z

453

Use of passive microwave remote sensing to monitor soil moisture  

E-Print Network [OSTI]

January 1998) Abstract - Surface soil moisture is a key variable to describe the water and energy soil layer) is a key variable in the water and energy exchanges at the land surfaceReview Use of passive microwave remote sensing to monitor soil moisture Jean-Pierre Wignerona

Paris-Sud XI, Université de

454

Sponsored by: Texas Soil Observation Network (TxSON)  

E-Print Network [OSTI]

Sponsored by: Texas Soil Observation Network (TxSON) A Program for Monitoring SOIL MOISTURE Across the State of Texas Refined soil moisture satellite data products for operational use and improved to meet water, wind, and energy demands Real-time emergency response data for natural disasters

Yang, Zong-Liang

455

Soil sampling kit and a method of sampling therewith  

DOE Patents [OSTI]

A soil sampling device and a sample containment device for containing a soil sample is disclosed. In addition, a method for taking a soil sample using the soil sampling device and soil sample containment device to minimize the loss of any volatile organic compounds contained in the soil sample prior to analysis is disclosed. The soil sampling device comprises two close fitting, longitudinal tubular members of suitable length, the inner tube having the outward end closed. With the inner closed tube withdrawn a selected distance, the outer tube can be inserted into the ground or other similar soft material to withdraw a sample of material for examination. The inner closed end tube controls the volume of the sample taken and also serves to eject the sample. The soil sample containment device has a sealing member which is adapted to attach to an analytical apparatus which analyzes the volatile organic compounds contained in the sample. The soil sampling device in combination with the soil sample containment device allow an operator to obtain a soil sample containing volatile organic compounds and minimizing the loss of the volatile organic compounds prior to analysis of the soil sample for the volatile organic compounds.

Thompson, Cyril V. (Knoxville, TN)

1991-01-01T23:59:59.000Z

456

Soil sampling kit and a method of sampling therewith  

DOE Patents [OSTI]

A soil sampling device and a sample containment device for containing a soil sample is disclosed. In addition, a method for taking a soil sample using the soil sampling device and soil sample containment device to minimize the loss of any volatile organic compounds contained in the soil sample prior to analysis is disclosed. The soil sampling device comprises two close fitting, longitudinal tubular members of suitable length, the inner tube having the outward end closed. With the inner closed tube withdrawn a selected distance, the outer tube can be inserted into the ground or other similar soft material to withdraw a sample of material for examination. The inner closed end tube controls the volume of the sample taken and also serves to eject the sample. The soil sample containment device has a sealing member which is adapted to attach to an analytical apparatus which analyzes the volatile organic compounds contained in the sample. The soil sampling device in combination with the soil sample containment device allows an operator to obtain a soil sample containing volatile organic compounds and minimizing the loss of the volatile organic compounds prior to analysis of the soil sample for the volatile organic compounds. 11 figures.

Thompson, C.V.

1991-02-05T23:59:59.000Z

457

In-Situ Thermal Remediation of Contaminated Soil1  

E-Print Network [OSTI]

as follows. Over a period of several weeks, electrical energy is introduced to the contaminated soil usingChapter 1 In-Situ Thermal Remediation of Contaminated Soil1 Written by Huaxiong Huang,2 Serguei Lapin and Rex Westbrook 1.1 Background Recently, a method for removing contaminants from soil (several

Lapin, Sergey

458

Soil and human health: an epidemiological review R. L. HOUGH  

E-Print Network [OSTI]

Soil and human health: an epidemiological review R. L. HOUGH The Macaulay Institute, Craigiebuckler, Aberdeen AB15 8QH, UK Summary Two different approaches have been used to study relationships between soil in the geosciences and broadly relates spatial soil characteristics to geographic incidence of disease. However

Ahmad, Sajjad

459

Soil Properties, Surveys, and Applications GEOG 3220 Fall 2009  

E-Print Network [OSTI]

Soil Properties, Surveys, and Applications GEOG 3220 Fall 2009 Dr. Scott Lecce Office: A-235, Elements of the Nature and Properties of Soils Course Description: The purpose of this course is to provide a general introduction to soil science for students interested in environmental studies. It is taught from

Lecce, Scott A.

460

Soil erosion and agricultural sustainability David R. Montgomery*  

E-Print Network [OSTI]

Soil erosion and agricultural sustainability David R. Montgomery* Department of Earth and Space conventionally plowed agricultural fields average 1­2 orders of magnitude greater than rates of soil production indicates that, considered globally, hill- slope soil production and erosion evolve to balance geologic

Montgomery, David R.

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


461

Labile Soil Phosphorus as Influenced by Methods of  

E-Print Network [OSTI]

Labile Soil Phosphorus as Influenced by Methods of Applying Radioactive Phosphorus Vilma V. Selvaratnam, Senay Siimer, A. J. Andersen, J. D. Thomsen and G. Gissel Nielsen #12;RISŘ-R-409 LABILE SOIL barley, ijuckwheat, and rye grass for the L- value determination. The four soils differed greatly

462

vendredi 7 dcembre 2012 Benchmarking of Excavated Soil  

E-Print Network [OSTI]

vendredi 7 décembre 2012 Benchmarking of Excavated Soil Reuse Management in Europe & Development · Implementation at a National Level: different options, different tools > Challenge with Excavated Soil Reuse from some experienced countries. vendredi 7 décembre 2012 D3E / DG > 2 Benchmarking of Excavated Soil

Paris-Sud XI, Université de

463

A soil test can provide information on the  

E-Print Network [OSTI]

A soil test can provide information on the proper amount of lime and fertilizer to apply to your is saved, and plant health is optimized. Soil testing can also be used to diagnose common nutrient deficien- cies for plants that are growing poorly. The reliability of the soil test, however, can be no bet- ter

Liskiewicz, Maciej

464

Relation of Soil Nitrogen, Nitrification and Ammonification to Pot Experiments.  

E-Print Network [OSTI]

............................................ 6 Relation of the Crops to the Total Nitrogen of the Soil ........... 7 Relation of the Different Crops ................................. 8 Relation of Surface Soil to Subsoil ............................. 13 Acid Soils Compared with Non-Acid... of Production of Nitrates to the Results of the Pot Ex- periments ................................................ 21 Extensive Work ............................................ 24 Relation of Nitric Nitrogen to Nitrogen Removed by First Crop .... 24...

Fraps, G. S. (George Stronach)

1921-01-01T23:59:59.000Z

465

Unsaturated hydraulic conductivity function based on a soil fragmentation process  

E-Print Network [OSTI]

Unsaturated hydraulic conductivity function based on a soil fragmentation process Shmuel Assouline-parameter expression for relative hydraulic conductivity (RHC) of partially saturated soils. It is based on the premise. This assumption allows us to derive hydraulic properties of soils (water retention curves and unsaturated

Tartakovsky, Daniel M.

466

Spatial and Temporal Variability of Microbes in Selected Soils at  

E-Print Network [OSTI]

the soil prior to dis- posal is required to minimize the quantity of disposed soil. Many of the Pu, microbial species diversity and biomass varies more in deserts than in other ecosystems (Kieft 1991 to determine baseline microbial activity and biomass in soils prior to decontamination. Information from

467

Soil to plant transfer of 238 Th on a uranium  

E-Print Network [OSTI]

Soil to plant transfer of 238 U, 226 Ra and 232 Th on a uranium mining-impacted soil from species grown in soils from southeastern China contaminated with uranium mine tailings were analyzed The radioactive waste (e.g. tailings) produced by uranium mining activities contains a series of long

Hu, Qinhong "Max"

468

Mechanisms of DNA Adsorption to Soil Particles Student: Maline Elumelu  

E-Print Network [OSTI]

1 Mechanisms of DNA Adsorption to Soil Particles Student: Maline Elumelu Advisor: Dr. Michael), Swiss Federal Institute of Technology (ETH), Zurich Abstract It has been found that DNA adsorbed to soil particles can be partially protected against enzymatic degradation. Soils are a very heterogeneous matrix

Fischlin, Andreas

469

Analysis of flow patterns and flow mechanisms in soils  

E-Print Network [OSTI]

Analysis of flow patterns and flow mechanisms in soils Dissertation Co-directed by the University of paths, varying flow mechanism or changing soil physical properties (stratification). Thus, in stratified-28Jan2010 #12;This doctoral thesis was prepared at the Department of Soil Physics, University

Paris-Sud XI, Université de

470

Soil Disturbance from an Integrated Mechanical Forest Fuel Reduction  

E-Print Network [OSTI]

Soil Disturbance from an Integrated Mechanical Forest Fuel Reduction Operation in Southwest Oregon1. This paper reports results of soil disturbance generated from an integrated forest harvesting/mechanical, mechanical harvesting, soil strength Introduction Currently, there is a lack of information concerning

Bolding, M. Chad

471

Agricultural Soil Carbon Sequestration: Economic Issues and Research Needs  

E-Print Network [OSTI]

Agricultural Soil Carbon Sequestration: Economic Issues and Research Needs Draft paper Bruce A Mc............................................................................................................. 5 2 Why Consider Promoting Agricultural Soil Carbon Sequestration?...................... 6 2 Agricultural Soil Carbon Sequestration....... 11 3.1 What is the cost of GHGE offsets arising from large

McCarl, Bruce A.

472

THE UNPREDICTABILITY OF SOIL FERTILITY ACROSS SPACE AND TIME  

E-Print Network [OSTI]

on Precision Agriculture and Other Resource Management, at least 20 presenters discussed soil spatial to describe and manage this soil spatial variability by the use of Management Zones while 18 presenters discussed other means of Managing Variability in the soil (Robert el al., 2000). Additionally, the temporal

Obradovic, Zoran

473

Sidewall tensiometer and method of determining soil moisture potential in below-grade earthen soil  

DOE Patents [OSTI]

A sidewall tensiometer to in situ determine below-grade soil moisture potential of earthen soil includes, a) a body adapted for insertion into an opening in earthen soil below grade, the body having lateral sidewalls; b) a laterally oriented porous material provided relative to the body lateral sidewalls, the laterally oriented porous material at least in part defining a fluid chamber within the body; c) a pressure a sensor in fluid communication with the fluid chamber; and d) sidewall engaging means for engaging a portion of a sidewall of an earth opening to laterally urge the porous material into hydraulic communication with earthen soil of another portion of the opening sidewall. Methods of taking tensiometric measurements are also disclosed.

Hubbell, Joel M. (Idaho Falls, ID); Sisson, James B. (Idaho Falls, ID)

2001-01-01T23:59:59.000Z

474

2010 19th World Congress of Soil Science, Soil Solutions for a Changing World  

E-Print Network [OSTI]

underestimated in parts of northwestern and central Russia (Boyd et al., 2009). Soil contaminated from smelter concentrations. Native plants like berries and mushrooms growing 3000 km2 around the smelter complex contain

Sparks, Donald L.

475

Selenium in Oklahoma ground water and soil  

SciTech Connect (OSTI)

Selenium with a consumption of 2 liters per day (5). The objectives of this study are: (1) to determine the concentrations of Se in Oklahoma ground water and soil samples. (2) to map the geographical distribution of Se species in Oklahoma. (3) to relate groundwater depth, pH and geology with concentration of Se.

Atalay, A.; Vir Maggon, D.

1991-03-30T23:59:59.000Z

476

Healthy soils for food system resiliency  

E-Print Network [OSTI]

, air, and point sources like lead paint chips. This duality, emphasized in urban areas where more sources of pollution exist, means that urban gardeners must know their soils to participate effectively in sustainability. Gardeners must investigate... of mining and metallurgy ----------------------------------------------------------------------------- 37 3.2. History of waste management --------------------------------------------------------------------------------- 38 3.3. History of industrial...

Jackson, Trisha L.

2011-08-31T23:59:59.000Z

477

ASSESSMENT OF ABORIGINAL SMALLHOLDER SOILS FOR  

E-Print Network [OSTI]

potential and tree health Chemical property pH a,e Totallimiting pH and Ca levels, which may have been causing treepH can cause stunting or death Deficiency inhibits soil build-up of N; suboptimal productivity Deficiency increases immature stage of tree,

Kurt A. Schwabe

2006-01-01T23:59:59.000Z

478

Soil Conditions Favoring Micronutrient Deficiencies and  

E-Print Network [OSTI]

; high free iron High pH; wet areas; burned peats; cool weather High pH Sands; high pH; eroded; cool availability: 4. Soil exchange capacity / leachability Retention vs. loss 5. Ion Interaction Competition deficiencies: B Cl Mo Mn Fe Zn Cu Ni Sands; low organic matter; dry weather Far from oceans; no use Acid sands

Balser, Teri C.

479

Actinide Thermodynamics at Elevated Temperatures  

SciTech Connect (OSTI)

The postclosure chemical environment in the proposed Yucca Mountain repository is expected to experience elevated temperatures. Predicting migration of actinides is possible if sufficient, reliable thermodynamic data on hydrolysis and complexation are available for these temperatures. Data are scarce and scattered for 25 degrees C, and nonexistent for elevated temperatures. This collaborative project between LBNL and PNNL collects thermodynamic data at elevated temperatures on actinide complexes with inorganic ligands that may be present in Yucca Mountain. The ligands include hydroxide, fluoride, sulfate, phosphate and carbonate. Thermodynamic parameters of complexation, including stability constants, enthalpy, entropy and heat capacity of complexation, are measured with a variety of techniques including solvent extraction, potentiometry, spectrophotometry and calorimetry

Friese, Judah I.; Rao, Linfeng; Xia, Yuanxian; Bachelor, Paula P.; Tian, Guoxin

2007-11-16T23:59:59.000Z

480

Humidity, Temperature, and Voltage (Presentation)  

SciTech Connect (OSTI)

An update is given on the work of the PV Quality Assurance Task Force; Group 3: studying the effects of humidity, temperature, and voltage bias.

Wohlgemuth, J.

2012-03-01T23:59:59.000Z

Note: This page contains sample records for the topic "2-meter soil temperature" from the National Library of EnergyBeta (NLEBeta).
While these samples are representative of the content of NLEBeta,
they are not comprehensive nor are they the most current set.
We encourage you to perform a real-time search of NLEBeta
to obtain the most current and comprehensive results.


481

High Temperature Processing Symposium 2014  

E-Print Network [OSTI]

} High temperature recycling operations } Materials sustainability } New furnace technology (including solar) We look forward to seeing you in February 2014. Dr M Akbar Rhamdhani (Chairman HTPS 2014) Prof

Liley, David

482

Low Temperature Material Bonding Technique  

DOE Patents [OSTI]

A method of performing a lower temperature bonding technique to bond together two mating pieces of glass includes applying a sodium silicate aqueous solution between the two pieces.

Ramsey, J. Michael (Knoxville, TN); Foote, Robert S. (Oak Ridge, TN)

2000-10-10T23:59:59.000Z

483

Low temperature material bonding technique  

DOE Patents [OSTI]

A method of performing a lower temperature bonding technique to bond together two mating pieces of glass includes applying a sodium silicate aqueous solution between the two pieces.

Ramsey, J. Michael (Knoxville, TN); Foote, Robert S. (Oak Ridge, TN)

2002-02-12T23:59:59.000Z

484

Dual-energy synchrotron X ray measurements of rapid soil density and water content changes in swelling soils  

E-Print Network [OSTI]

Dual-energy synchrotron X ray measurements of rapid soil density and water content changes content and bulk density. A number of studies have used dual-energy gamma rays to investigate soil in moisture content and soil swelling shortly after infiltration is initiated. In this paper, we use the dual-energy

Walter, M.Todd

485

Soil compaction is a manageable factor that can lim-it grain or silage yield on many Virginia soils. Corn  

E-Print Network [OSTI]

Soil compaction is a manageable factor that can lim- it grain or silage yield on many Virginia soils. Corn plants growing on compacted areas are often stunted and have slower root penetration rates grown in these areas. Compaction is created when soil particles are pressed together, reducing the pore

Liskiewicz, Maciej

486

TSNo s02-staats173645-P Alum Amendment Effects on Soil Phosphorus Stabilization in Poultry Litter Amended Sandy Soils.  

E-Print Network [OSTI]

TSNo s02-staats173645-P Title Alum Amendment Effects on Soil Phosphorus Stabilization in Poultry Litter Amended Sandy Soils. abstract Increased poultry production has contributed to excess nutrient (i.e., phosphorus (P)) problems in Atlantic Coastal Plain soils due to land application of poultry litter and manure

Sparks, Donald L.

487

Mineralogical and chemical characterization of lunar highland soils: Insights into the space weathering of soils on airless bodies  

E-Print Network [OSTI]

Mineralogical and chemical characterization of lunar highland soils: Insights into the space soils, with respect to their mineralogical and chemical makeup. It is these lunar soils that are being, A. Patchen, D.-H. S. Taylor, R. V. Morris, L. P. Keller, and D. S. McKay (2010), Mineralogical

Perfect, Ed

488

Soil solution chemistry of sewage-sludge incinerator ash and phosphate fertilizer amended soil  

SciTech Connect (OSTI)

The chemical composition of the soil provides useful information on the feasibility of amending agricultural land with municipal and industrial waste, because the soil solution is the medium for most soil chemical reactions, the mobile phase in soils, and the medium for mineral adsorption by plant roots. The soil solutions studies in this research were from plots in a 4-yr field experiment conducted to evaluate the effects of the trace metals and P in sewage-sludge incinerator ash. Treatments compared ash with equivalent P rates from triple-superphosphate fertilizer and a control receiving no P application. Ash and phosphate fertilizer were applied annually at rates of 35, 70, and 140 kg citrate-soluble P ha{sup -1}. Cumulative ash applications during 4 yr amounted to 3.6, 7.2, and 14.4 Mg ash ha{sup -1}. Soil solutions were obtained by centrifugation-immiscible liquid displacement using a fluorocarbon displacing agent. Following chemical analysis, a chemical speciation model was used to determine possible solubility-controlling minerals for trace metals and P, and correlations between solution composition and plant uptake were analyzed. 37 refs., 5 tabs.

Bierman, P.M.; Rosen, C.J.; Bloom, P.R.; Nater, E.A. [Univ. of Minnesota, St. Paul, MN (United States)

1995-03-01T23:59:59.000Z

489

Experiment Hazard Class 3 - High Temperatures  

Broader source: All U.S. Department of Energy (DOE) Office Webpages (Extended Search)

Operation * APS Base Low Temperatures * Cryogenic Systems High Temperatures * Electric Furnace * Optical Furnace * Other High Temperature Lasers * Laser, Class 2 * Laser,...

490

Apparatus for treatment of soils contaminated with organic pollutants  

DOE Patents [OSTI]

An apparatus for treating soil contaminated by organic compounds wherein an ozone containing gas is treated with acid to increase the stability of the ozone in the soil environment and the treated ozone applied to the contaminated soil in a manner adapted to decompose the organic compounds; one embodiment of the apparatus comprises a means to supply ozone as a gas-ozone mixture, a stability means to treat ozone obtained from the supply and distribution means to apply the stabilized gas-ozone to soil. The soil may be treated in situ or may be removed for treatment and refilled.

Wickramanayake, Godage B. (Columbus, OH)

1993-01-01T23:59:59.000Z

491

A laboratory investigation of vibratory compaction of dry soils  

E-Print Network [OSTI]

. Standard Compaction Curve for Soil 3 (CL) 48 49 50 53 54 56 25 Effect of Frequency Variation on the Time Required to Achieve I/2 inch (12. 7 mm) of Settlement 57 26. Foot Size Effects on Compaction of Various Soils 59 27. Effect of Frequency... on the Compaction of Soil 1 (SP) Using Two Different Feet 63 28. Effect of Frequency on the Compaction of Soil 1 (SP) Using the Semi-Circular Foot with Various Static Weights 64 29. Effect of Frequency on the Compaction of Soil 1 (SP) Using the 5 Inch Diameter...

Webster, Cecil Ray

1984-01-01T23:59:59.000Z

492

Subsurface Temperature, Moisture, Thermal Conductivity and Heat Flux, Barrow, Area A, B, C, D  

DOE Data Explorer [Office of Scientific and Technical Information (OSTI)]

Subsurface temperature data are being collected along a transect from the center of the polygon through the trough (and to the center of the adjacent polygon for Area D). Each transect has five 1.5m vertical array thermistor probes with 16 thermistors each. This dataset also includes soil pits that have been instrumented for temperature, water content, thermal conductivity, and heat flux at the permafrost table. Area C has a shallow borehole of 2.5 meters depth is instrumented in the center of the polygon.

Cable, William; Romanovsky, Vladimir

493

Subsurface Temperature, Moisture, Thermal Conductivity and Heat Flux, Barrow, Area A, B, C, D  

SciTech Connect (OSTI)

Subsurface temperature data are being collected along a transect from the center of the polygon through the trough (and to the center of the adjacent polygon for Area D). Each transect has five 1.5m vertical array thermistor probes with 16 thermistors each. This dataset also includes soil pits that have been instrumented for temperature, water content, thermal conductivity, and heat flux at the permafrost table. Area C has a shallow borehole of 2.5 meters depth is instrumented in the center of the polygon.

Cable, William; Romanovsky, Vladimir

2014-03-31T23:59:59.000Z

494

Low temperature irradiation tests on  

E-Print Network [OSTI]

Sample cool down by He gas loop 10K ­ 20K Fast neutron flux Measured by Ni activation in 2010 1.4xK #12;reactor Cryogenics #12;Al-Cu-Mg He gas temperature near sample 12K Resistance changesLow temperature irradiation tests on stabilizer materials using reactor neutrons at KUR Makoto

McDonald, Kirk

495

Detecting temperature fluctuations at equilibrium  

E-Print Network [OSTI]

Gibbs and Boltzmann definitions of temperature agree only in the macroscopic limit. The ambiguity in identifying the equilibrium temperature of a finite sized `small' system exchanging energy with a bath is usually understood as a limitation of conventional statistical mechanics. We interpret this ambiguity as resulting from a stochastically fluctuating temperature coupled with the phase space variables giving rise to a broad temperature distribution. With this ansatz, we develop the equilibrium statistics and dynamics of small systems. Numerical evidence using an analytically tractable model shows that the effects of temperature fluctuations can be detected in equilibrium and dynamical properties of the phase space of the small system. Our theory generalizes statistical mechanics to small systems relevant to biophysics and nanotechnology.

Dixit, Purushottam D

2015-01-01T23:59:59.000Z

496

Flow Partitioning in Fully Saturated Soil Aggregates  

SciTech Connect (OSTI)

Microbes play an important role in facilitating organic matter decomposition in soils, which is a major component of the global carbon cycle. Microbial dynamics are intimately coupled to environmental transport processes, which control access to labile organic matter and other nutrients that are needed for the growth and maintenance of microorganisms. Transport of soluble nutrients in the soil system is arguably most strongly impacted by preferential flow pathways in the soil. Since the physical structure of soils can be characterized as being formed from constituent micro aggregates which contain internal porosity, one pressing question is the partitioning of the flow among the “inter-aggregate” and “intra-aggregate” pores and how this may impact overall solute transport within heterogeneous soil structures. The answer to this question is particularly important in evaluating assumptions to be used in developing upscaled simulations based on highly-resolved mechanistic models. We constructed a number of diverse multi-aggregate structures with different packing ratios by stacking micro-aggregates containing internal pores and varying the size and shape of inter-aggregate pore spacing between them. We then performed pore-scale flow simulations using computational fluid dynamics methods to determine the flow patterns in these aggregate-of-aggregates structures and computed the partitioning of the flow through intra- and inter-aggregate pores as a function of the spacing between the aggregates. The results of these numerical experiments demonstrate that soluble nutrients are largely transported via flows through inter-aggregate pores. Although this result is consistent with intuition, we have also been able to quantify the relative flow capacity of the two domains under various conditions. For example, in our simulations, the flow capacity through the aggregates (intra-aggregate flow) was less than 2% of the total flow when the spacing between the aggregates was larger than 18 micron. Inter-aggregate pores continued to be the dominant flow pathways even at much smaller spacing; intra-aggregate flow was less than 10% of the total flow when the inter- and intra-aggregate pore sizes were comparable. Such studies are making it possible to identify which model upscaling assumptions are realistic and what computational methods are required for detailed numerical investigation of microbial carbon cycling dynamics in soil systems.

Yang, Xiaofan; Richmond, Marshall C.; Scheibe, Timothy D.; Perkins, William A.; Resat, Haluk

2014-03-30T23:59:59.000Z

497

Effect of Gas Turbine Exhaust Temperature, Stack Temperature and Ambient Temperature on Overall Efficiency of Combine Cycle Power Plant  

E-Print Network [OSTI]

Abstract—The gas turbine exhaust temperature, stack temperature and ambient temperature play a very important role during the predication of the performance of combine cycle power plant. This paper covers parametric analysis of effects of gas turbine exhaust temperature, stack temperature and ambient temperature on the overall efficiency of combine cycle power plant keeping the gas turbine efficiency as well as steam turbine efficiency constant. The results shows that out of three variables i.e. turbine exhaust temperature, stack temperature and ambient temperature, the most dominating factor of increasing the overall efficiency of the combine cycle power plant is the stack temperature.

unknown authors

498

Shock temperature measurements in ammonia  

SciTech Connect (OSTI)

Our first shock temperature measurements on a cryogenic target are reported for NH/sub 3/. A new fast optical pyrometer and a cryogenic specimen holder for liquid NH/sub 3/ were developed to measure shock temperatures of 4400 and 3600 K at pressures of 61 and 48 GPa. These conditions correspond to those in the ice layers in Uranus and Neptune. The shock temperature data are in reasonable agreement with an equation of state based on an intermolecular potential derived from NH/sub 3/ Hugoniot data.

Radousky, H.B.; Mitchell, A.C.; Nellis, W.J.; Ross, M.

1985-07-01T23:59:59.000Z

499

A Dynamical Approach to Temperature  

E-Print Network [OSTI]

We present a new dynamical approach for measuring the temperature of a Hamiltonian dynamical system in the micro canonical ensemble of thermodynamics. We show that under the hypothesis of ergodicity the temperature can be computed as a time-average of the functional, div(grad H/|grad H|^2), on the energy-surface. Our method not only yields an efficient computational approach for determining the temperature it also provides an intrinsic link between dynamical systems theory and the statistical mechanics of Hamiltonian systems.

Hans Henrik Rugh

1997-01-30T23:59:59.000Z

500

Method for measuring surface temperature  

SciTech Connect (OSTI)

The present invention relates to a method for measuring a surface temperature using is a fluorescent temperature sensor or optical thermometer. The sensor includes a solution of 1,3-bis(1-pyrenyl)propane within a 1-butyl-1-1-methyl pyrrolidinium bis(trifluoromethylsulfonyl)imide ionic liquid solvent. The 1,3-bis(1-pyrenyl)propane remains unassociated when in the ground state while in solution. When subjected to UV light, an excited state is produced that exists in equilibrium with an excimer. The position of the equilibrium between the two excited states is temperature dependent.

Baker, Gary A. (Los Alamos, NM); Baker, Sheila N. (Los Alamos, NM); McCleskey, T. Mark (Los Alamos, NM)

2009-07-28T23:59:59.000Z