National Library of Energy BETA

Sample records for abo sussex-shannon muddy

  1. WAVE-SEDIMENT INTERACTION ON A MUDDY SHELF A. Sheremet1

    E-Print Network [OSTI]

    Sheremet, Alexandru

    WAVE-SEDIMENT INTERACTION ON A MUDDY SHELF A. Sheremet1 , A. J. Mehta2 , and J. M. Kaihatu3-induced wave dissipation and 3- wave interactions on wave evolution over muddy environments. The model is used to simulate wave conditions typical for a muddy shallow shelf. Mud-induced long-wave dissipation introduces

  2. Cost estimate for muddy water palladium production facility at Mound

    SciTech Connect (OSTI)

    McAdams, R.K.

    1988-11-30

    An economic feasibility study was performed on the ''Muddy Water'' low-chlorine content palladium powder production process developed by Mound. The total capital investment and total operating costs (dollars per gram) were determined for production batch sizes of 1--10 kg in 1-kg increments. The report includes a brief description of the Muddy Water process, the process flow diagram, and material balances for the various production batch sizes. Two types of facilities were evaluated--one for production of new, ''virgin'' palladium powder, and one for recycling existing material. The total capital investment for virgin facilities ranged from $600,000 --$1.3 million for production batch sizes of 1--10 kg, respectively. The range for recycle facilities was $1--$2.3 million. The total operating cost for 100% acceptable powder production in the virgin facilities ranged from $23 per gram for a 1-kg production batch size to $8 per gram for a 10-kg batch size. Similarly for recycle facilities, the total operating cost ranged from $34 per gram to $5 per gram. The total operating cost versus product acceptability (ranging from 50%--100% acceptability) was also evaluated for both virgin and recycle facilities. Because production sizes studied vary widely and because scale-up factors are unknown for batch sizes greater than 1 kg, all costs are ''order-of-magnitude'' estimates. All costs reported are in 1987 dollars.

  3. Water Management: Clearing Cloudy and Muddy Water in Ponds and Lakes

    E-Print Network [OSTI]

    1 Water Management: Clearing Cloudy and Muddy Water in Ponds and Lakes T.L. Provin and J.L Pitt Professor and Soil Chemist, Program Specialist Texas A&M AgriLife Extension Service Soil, Water and Forage Testing Laboratory Department of Soil and Crop Sciences Cloudy or muddy water and ponds can

  4. Long waves in water over a visco-elastic muddy seabed

    E-Print Network [OSTI]

    Garnier, Erell-Isis

    2011-01-01

    The propagation of surface waves over a flat muddy seabed are studied. Mud is first considered as a Newtonian fluid. Water and mud equations are derived in order to obtain governing equation for surface and interface waves. ...

  5. ABO, D Blood Typing and Subtyping Using Plug-Based Microfluidics

    E-Print Network [OSTI]

    Ismagilov, Rustem F.

    ABO, D Blood Typing and Subtyping Using Plug-Based Microfluidics Timothy R. Kline, Matthew K-based microfluidic approach was used to perform multiple agglutination assays in parallel without cross-chip, a microfluidic device was designed to combine aqueous streams of antibody, buffer, and red blood cells (RBCs

  6. DFT study of the stability of oxygen vacancy in cubic ABO3 perovskites

    E-Print Network [OSTI]

    Li, Weixue

    /or Co at B sites of ABO3 perovskites are used as the cathode materials for solid oxide fuel cells (SOFC, incorporation and trans- port, which is related to oxygen conductivity and diffu- sivity in SOFC conditions and diffusion on LaMnO3 and 25 and 50 % Sr-doped LaMnO3 (LSM) cathode materials for SOFC [30­32]. They show

  7. Origin of the Diverse Behavior of Oxygen Vacancies in ABO3 Perovskites: A Symmetry Based Analysis

    SciTech Connect (OSTI)

    Yin, W. J.; Wei, S. H.; Al-Jassim, M. M.; Yan, Y. F.

    2012-05-15

    Using band symmetry analysis and density functional theory calculations, we reveal the origin of why oxygen vacancy (V{sub O}) energy levels are shallow in some ABO{sub 3} perovskites, such as SrTiO{sub 3}, but are deep in some others, such as LaAlO{sub 3}. We show that this diverse behavior can be explained by the symmetry of the perovskite structure and the location (A or B site) of the metal atoms with low d orbital energies, such as Ti and La atoms. When the conduction band minimum (CBM) is an antibonding {Gamma}12 state, which is usually associated with the metal atom with low d orbital energies at the A site (e.g., LaAlO{sub 3}), then the V{sub O} energy levels are deep inside the gap. Otherwise, if the CBM is the nonbonding {Gamma}25{prime} state, which is usually associated with metal atoms with low d orbital energies at the B site (e.g., SrTiO{sub 3}), then the V{sub O} energy levels are shallow and often above the CBM. The V{sub O} energy level is also deep for some uncommon ABO{sub 3} perovskite materials that possess a low s orbital, or large-size cations, and an antibonding {Gamma}{sub 1} state CBM, such as ZnTiO{sub 3}. Our results, therefore, provide guidelines for designing ABO{sub 3} perovskite materials with desired functional behaviors.

  8. Wet processing of palladium for use in the tritium facility at Westinghouse, Savannah River, SC. Preparation of palladium using the Mound Muddy Water process

    SciTech Connect (OSTI)

    Baldwin, D.P.; Zamzow, D.S.

    1998-11-10

    Palladium used at Savannah River for tritium storage is currently obtained from a commercial source. In order to better understand the processes involved in preparing this material, Savannah River is supporting investigations into the chemical reactions used to synthesize this material and into the conditions necessary to produce palladium powder that meets their specifications. This better understanding may help to guarantee a continued reliable source for this material in the future. As part of this evaluation, a work-for-others contract between Westinghouse Savannah River Company and the Ames Laboratory Metallurgy and Ceramics Program was initiated. During FY98, the process for producing palladium powder developed in 1986 by Dan Grove of Mound Applied Technologies (USDOE) was studied to understand the processing conditions that lead to changes in morphology in the final product. This report details the results of this study of the Mound Muddy Water process, along with the results of a round-robin analysis of well-characterized palladium samples that was performed by Savannah River and Ames Laboratory. The Mound Muddy Water process is comprised of three basic wet chemical processes, palladium dissolution, neutralization, and precipitation, with a number of filtration steps to remove unwanted impurity precipitates.

  9. Water waves over a muddy seabed

    E-Print Network [OSTI]

    Krotov, Mikhael

    2008-01-01

    A generalized viscoelastic model is used to describe the rheological properties of mud and is fitted to the available experimental data, so that its constitutive coefficients are just material properties independent of the ...

  10. ABO Wind AG | Open Energy Information

    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 Home Page on QA:QA J-E-1 SECTION JEnvironmental Jump to:EAand Dalton JumpProgram |RecentSulfonate as aEnergy1 Jump3-500AAONABIDAS

  11. ABO Wind Espana SA | Open Energy Information

    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 Home Page on QA:QA J-E-1 SECTION J APPENDIX E LIST OFAMERICA'S FUTURE.EnergyWoodenDate RecCompetitionCentury Solar IncWindEspana

  12. Muddy Boots, Y-12 and looking to the future

    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: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantityBonneville Power Administration wouldMass map shines light on77 PAGEMissionStressMove dataKiel ing ,Via electronic mailMAR

  13. Universitetsportfolj See also: users.abo.fi/mzevenho/portfolj

    E-Print Network [OSTI]

    Zevenhoven, Ron

    , INECSE EU/TEKES: ERANET- SCITOBICOM Company related: EKOKEM Fortum Säätiö 2x SAFEC (Foster Wheeler) POLKU

  14. Hydrodynamic flow in lower Cretaceous Muddy sandstone, Gas Draw Field, Powder River Basin, Wyoming 

    E-Print Network [OSTI]

    Lin, Joseph Tien-Chin

    1978-01-01

    potentiometric gradient of 32 ft/mi across the field yields a hydrodynamic oil column of 210 ft, whereas capillary-pressure differ- ences due to permeability changes can account for only 38 ft of oil column. The observed oil column over most of the field has a... height somewhat greater than 250 ft. The agreement between total calculated oil column of about 248 ft and the observed oil column demonstrates that the positive hydrodynamic gradient across the reservoir and the decrease in permeability updip...

  15. Y-12's historian receives 2013 Muddy Boot Award | National Nuclear

    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: Alternative Fuels Data Center Homesum_a_epg0_fpd_mmcf_m.xls" ,"Available from WebQuantityBonneville Power AdministrationRobust,Field-effectWorkingLos Alamos verifies largest single| National1958 nuclearDon2 By

  16. 38 Colorado School of Mines key To super CollAbo

    E-Print Network [OSTI]

    properties of these new silicon clathrates? Can they be used to build a better solar cell? The answer, once to the table. Lusk's solar cell work with REMRSEC on multiple-exciton generation (MEG) was successful. MEG of REMRSEC solar energy scientists and Center for Hydrate Research experts. Together they developed

  17. ABO Wind Biogas Sachsen Anhalt GmbH Co KG | Open Energy Information

    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 Home Page on QA:QA J-E-1 SECTION J APPENDIX ECoop IncIowa (UtilityMichigan)data bookresult9) JumpMultipleSprings Logo:

  18. Muddy Water? Variation in Reporting Receipt of Breast Cancer Radiation Therapy by Population-Based Tumor Registries

    SciTech Connect (OSTI)

    Walker, Gary V.; Giordano, Sharon H.; Williams, Melanie; Jiang, Jing; Niu, Jiangong; MacKinnon, Jill; Anderson, Patricia; Wohler, Brad; Sinclair, Amber H.; Boscoe, Francis P.; Schymura, Maria J.; Buchholz, Thomas A.; Smith, Benjamin D.

    2013-07-15

    Purpose: To evaluate, in the setting of breast cancer, the accuracy of registry radiation therapy (RT) coding compared with the gold standard of Medicare claims. Methods and Materials: Using Surveillance, Epidemiology, and End Results (SEER)–Medicare data, we identified 73,077 patients aged ?66 years diagnosed with breast cancer in the period 2001-2007. Underascertainment (1 - sensitivity), sensitivity, specificity, ?, and ?{sup 2} were calculated for RT receipt determined by registry data versus claims. Multivariate logistic regression characterized patient, treatment, and geographic factors associated with underascertainment of RT. Findings in the SEER–Medicare registries were compared with three non-SEER registries (Florida, New York, and Texas). Results: In the SEER–Medicare registries, 41.6% (n=30,386) of patients received RT according to registry coding, versus 49.3% (n=36,047) according to Medicare claims (P<.001). Underascertainment of RT was more likely if patients resided in a newer SEER registry (odds ratio [OR] 1.70, 95% confidence interval [CI] 1.60-1.80; P<.001), rural county (OR 1.34, 95% CI 1.21-1.48; P<.001), or if RT was delayed (OR 1.006/day, 95% CI 1.006-1.007; P<.001). Underascertainment of RT receipt in SEER registries was 18.7% (95% CI 18.6-18.8%), compared with 44.3% (95% CI 44.0-44.5%) in non-SEER registries. Conclusions: Population-based tumor registries are highly variable in ascertainment of RT receipt and should be augmented with other data sources when evaluating quality of breast cancer care. Future work should identify opportunities for the radiation oncology community to partner with registries to improve accuracy of treatment data.

  19. 1 av / of 4 Massverfring och separationsteknik

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. När har du gjort kursutvärderingen för denna kurs http://web.abo course evaluation for this course http://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm A) during

  20. 1 av / of 5 Massverfring och separationsteknik

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. När har du gjort kursutvärderingen för denna kurs http://web.abo course evaluation for this course http://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm A) during

  1. 1 av / of 3 Massverfring och separationsteknik

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. När har du gjort kursutvärderingen för denna kurs http://web.abo course evaluation for this course http://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm A) during

  2. Complexity Measures for Gene Assembly Tero Harju1

    E-Print Network [OSTI]

    Harju, Tero

    Turku, Finland email:harju@utu.fi 2 Department of Computer Science, °Abo Akademi University, Turku Center for Computer Science, FIN-20520 Turku, Finland email:lchang@abo.fi 3 Academy of Finland email

  3. Sodium Bose-Einstein condensates in an optical lattice K. Xu,* Y. Liu, J. R. Abo-Shaeer, T. Mukaiyama, J. K. Chin, D. E. Miller, and W. Ketterle

    E-Print Network [OSTI]

    Atoms, and Research Laboratory of Electronics, MIT, Cambridge, Massachusetts 02139, USA Kevin M. Jones-field theory 1­7 . Simply through varying the depth of the lattice potential, one changes the tunneling rate the recoil frequencies are lower and lasers are readily available to achieve trap depths of several tens

  4. Stocking and Management Recommendations for Texas Farm Ponds. 

    E-Print Network [OSTI]

    Anonymous,

    1983-01-01

    , ponds less than one acre receive different recommendations than larger ponds. The extent of water surface fluctuations, degree of expected fishing pressure and the muddiness of the water are a few of the traits which the pondowner needs to know... fluctuate considerably in surface area should be stocked on the basis of average annual low water surface area. Muddy Water Many Texas ponds have a tendency to stay muddy. This condition is caused by suspended soil particles in the water and should...

  5. Contents Lecture 1. Basic notions (AS) 2 Lecture 2. Sheaves: a ...

    E-Print Network [OSTI]

    2005-12-15

    This is the content of the rightly renowned. Quillen-Suslin ...... Before muddying the waters further with more definitions, let us have a concrete example which is ...

  6. p-Type transparent conducting oxides and methods for preparation

    DOE Patents [OSTI]

    Shahriari, Dean Y. (Evanston, IL); Barnabe, Antoine (Toulouse, FR); Mason, Thomas O. (Evanston, IL); Poeppelmeier, Kenneth R. (Evanston, IL)

    2011-05-31

    A facile, low temperature and low pressure method for the preparation of a wide range of phase pure ABO.sub.2 compositions.

  7. 1 av / of 4 Massverfring och separationsteknik

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. När har du gjort kursutvärderingen för denna kurs http://web.abo.fi/fak/tkf/vt/Swe/education_Evaluation_sw

  8. 1 av / of 5 Massverfring och separationsteknik

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. När har du gjort kursutvärderingen för denna kurs http://web.abo.fi/fak/tkf/vt/Swe/education_Evaluation_sw

  9. Accepted, subject to re-review, Journal of Hydraulic Engineering, ASCE, version of January 2006 Role of Ponded Turbidity Currents in Reservoir Trap Efficiency

    E-Print Network [OSTI]

    Parker, Gary

    by a hydraulic jump. If the interface of this muddy pond rises above any vent or overflow point at the damAccepted, subject to re-review, Journal of Hydraulic Engineering, ASCE, version of January 2006 1. The dam causes a sustained turbidity current to reflect and form a muddy pond bounded upstream

  10. Learning Chordal Markov Networks by Constraint Satisfaction

    E-Print Network [OSTI]

    Rintanen, Jussi

    Finland Tomi Janhunen Aalto University Finland Jussi Rintanen§ Aalto University Finland Henrik Nyman¶ °Abo Akademi University Finland Johan Pensar¶ °Abo Akademi University Finland Abstract We investigate]. This work was funded by the Academy of Finland, project 251170. Funded by ERC grant 239784. Also

  11. Synthesis and characterization of perovskite PbTiO3 nanoparticles with solution processability

    E-Print Network [OSTI]

    Lin, Zhiqun

    Synthesis and characterization of perovskite PbTiO3 nanoparticles with solution processability Jun with perovskite structure (ABO3), for example, lead titanate (PbTiO3), are the most studied ferroelectric oxides polarization direction. Ferroelectrics with perovskite structure (ABO3), such as barium titanate (BaTiO3

  12. _____ Caddisflies (except net spinners) _____ Mayflies

    E-Print Network [OSTI]

    Lawrence, Deborah

    , but tea-colored £ colored sheen (oily) £ foamy £ milky £ muddy £ black £ grey £ other __________ Stream beneath your feet in: £ no spots £ a few spots £ many spots Algae color: £ light green £ dark green

  13. CX-011619: Categorical Exclusion Determination

    Broader source: Energy.gov [DOE]

    Muddy Pass-Walden 69-kilovolt Transmission Line Danger Tree Management CX(s) Applied: B1.3 Date: 11/21/2013 Location(s): Colorado Offices(s): Western Area Power Administration-Rocky Mountain Region

  14. Lithology and cyclicity in the deposition of the Middle Ordovician McKee Sand member of the Tulip Creek Formation (Simpson Group) in the Tobosa Basin of Southeast New Mexico and West Texas 

    E-Print Network [OSTI]

    Bosco, Michael John

    1999-01-01

    in quads sand grain size and percentage of clay and carbonate composition accompanied by sharp breaks and repetition in facies delineate this cyclicity. The McKee Sand is largely composed of sandstones, muddy sandstones, and sandy mudstones. The sandstones...

  15. Depositional facies and environments of the lower Mineral Wells formation, Pennsylvanian Strawn group, north central Texas 

    E-Print Network [OSTI]

    Bradshaw, Susan Elizabeth

    1996-01-01

    , black mudstones with phosphate nodules, and limestones. The prodelta facies is largely nonfossiliferous and consists of massive mudstones, massive silty mudstones with occasional siltstone lenses, and horizontal planar-and lenticular-laminated muddy...

  16. Structural analysis of the perdido fold belt: timing, evolution, and structural style 

    E-Print Network [OSTI]

    Waller, Troy Dale, II

    2007-09-17

    the upper portion consist of fine grained and muddy siliciclastics which are typical of turbidite and other typical deep water deposits. 2-D, prestacked, depth-migrated seismic data (TGS Phase 45) was interpreted in conjunction with Hess Corporation...

  17. --No Title--

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

    ORNL's Smith, DOE's Brown winners of Muddy Boot Award On the left, DOE Oak Ridge Office Deputy Manager Robert Brown (left) and ORNL Deputy Director for Operations Jeff Smith...

  18. Paleontology and Geology of Indiana Department of Geological Sciences | P. David Polly 1

    E-Print Network [OSTI]

    Polly, David

    . Iowa Tracheophyta (vascular plants) Spores, New Albany Shale Sporing bodies, Dugger Fm. #12;Department (conifers) Walchia, Abo Fm. New Mexico (Permian) #12;Department of Geological Sciences | P. David Polly 5

  19. Processteknikens Vrme och Vrme och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    http://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm eller ska du snart göra det? Did you give your course evaluation för this course via the webpage http://web

  20. Processteknikens Vrme-och Vrme -och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. Hur du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 123. Ett värmeelement

  1. Processteknikens Vrme-och Vrme -och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. Hur du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 95. En

  2. Processteknikens Vrme-och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. Hur du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 59. Rökgas från en

  3. Processteknikens Vrme-och Vrme -och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. Hur du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 63. 1 mol av idealgas

  4. Processteknikens Vrme -och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    . Hur du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 131. I en

  5. Massverfring och separationsteknik Vrme -och strmningsteknik (MF-ST) 424302

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. När har du gjort kursutvärderingen för denna kurs http://web course evaluation for this course http://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm A) during

  6. Processteknikens Vrme-och Vrme -och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. Har du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 87. En viss process

  7. Processteknikens Vrme-och Vrme -och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. Hur du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 75. En viss volym gas

  8. Processteknikens Vrme-och Vrme -och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. Hur du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 79. En termosflaska är

  9. Processteknikens Vrme-och Vrme -och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. Hur du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 71. The Figure gives

  10. Processteknikens Vrme-och Vrme -och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. Hur du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 115. Vatten strömmar ut

  11. Processteknikens Vrme-och Vrme -och strmningsteknik grunder (PTG) 424101

    E-Print Network [OSTI]

    Zevenhoven, Ron

    many and in which year? b. Hur du gjort kursutvärderingen för denna kurs via websidan http://web://web.abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 91. Beräkna

  12. Fluid&ParticulateSystems 424514/2010

    E-Print Network [OSTI]

    Zevenhoven, Ron

    " Ron Zevenhoven ÅA Thermal and Flow Engineering ron.zevenhoven@abo.fi 9Fluid&ParticulateSystems 424514 Being often a low temperature process, better energy economy than, for example, distillation Fluid

  13. Nanoscale quantification of octahedral tilts in perovskite films

    E-Print Network [OSTI]

    Hwang, Jinwoo; Zhang, Jack; Son, Junwoo; Stemmer, Susanne

    2012-01-01

    tilts in ultrathin perovskite ?lms despite large unit cells,of octahedral tilts in perovskite films Jinwoo Hwang, a)BO 6 octahe- dra in perovskite unit cells (general formula

  14. Competing interactions in ferromagnetic/antiferromagnetic perovskite superlattices

    E-Print Network [OSTI]

    Takamura, Y.

    2010-01-01

    antiferromagnetic perovskite superlattices  Y.  TakamuraSr 0.3 MnO 3   (LSMO) perovskite oxide superlattices leads Specifically, the class of perovskite oxides  (ABO 3 ) has 

  15. Ab initio defect energetics of perovskite (001) surfaces for solid oxide fuel cells: A comparative study of LaMnO[subscript 3] versus SrTiO[subscript 3] and LaAlO[subscript 3

    E-Print Network [OSTI]

    Lee, Yueh-Lin

    In this paper, we perform a comparative study based on ab initio modeling for perovskite ABO[subscript 3] (001) surfaces and surface defect energetics in order to understand the influence of polarity and redox active Mn ...

  16. Hanson's Cement Plant 0.02 0 Lower Guadalupe River 0.03 0

    E-Print Network [OSTI]

    Hanson's Cement Plant 0.02 0 Lower Guadalupe River 0.03 0 Mills Creek 0.06 0 Lower Coyote Creek 0PabloCk SanFelipeCk LowerWalkerCk MuddyHollow LagunitasCk MillsCk SimasCk LowerCoyoteCk LowerGuadalupeR Hanson'sCement

  17. "Science affects the way we think together." L e w i s T h o m a s

    E-Print Network [OSTI]

    , and municipal water supplies. Far from being a simple cause and effect, the key agent is tradeoffs. The large CLARIFYING MUDDY WATER: PROBING THE LINKAGES TO MUNICIPAL WATER QUALITY I N S I D E Shutting Off the Spigot . . . . . . . . . . . . . . . . . . . . . . . . . 5 "Water, water everywhere, nor any drop to drink." --Samuel Taylor Coleridge PNWPacific Northwest

  18. CX-011721: Categorical Exclusion Determination

    Broader source: Energy.gov [DOE]

    Gore Pass-Muddy Pass 69 Kilovolt Transmission Line Danger Tree Management in Grand and Jackson Counties, Colorado CX(s) Applied: B1.3 Date: 12/31/2013 Location(s): Colorado, Colorado Offices(s): Western Area Power Administration-Rocky Mountain Region

  19. O r g a n of t he Un i ve r s it y of A l b e r t a M at he m at ic a l S c ie nce s S o c ie t y D e ce mb e r 4 2 0 0 5 2 Normal Vector

    E-Print Network [OSTI]

    Bowman,John C.

    Is Sometimes A One-way Road On A Tall Narrow Bridge Over A Shal- low Muddy River, On Whose South Bank Lies? Fuck you. #12;4 Normal Vector GOVER N MENT SMASHTHESTATE PO LICE BU R EAUCRA C Y TAXES LAWYERS

  20. Vol XXIV, Issue 7 In This Issue February 16, 2009

    E-Print Network [OSTI]

    Nikolaou, Michael

    Ethanol Blending Researchers Study Episodic Emissions' Impact on Airborne PM Report Forecasts of the Blend Wall' Heating up in Washington Report: By 2030, Ethanol Can Displace 60 Billion Gallons of Gasoline Underwriters Lab Muddies Waters on its E 15 Pump Position House Ag Committee Passes Bill

  1. The rigging material from Boscawen: setting the sails of a mid-eighteenth-century warship during the French and Indian War 

    E-Print Network [OSTI]

    Flanigan, Alan Thomas

    1999-01-01

    into the muddy bottom of Lake Champlain. In 1983 the accidental discovery of the sloop Boscawen led to its excavation during the next two simmers and a multidisciplinary study of the naval architecture, maritime history, and archaeology related to the vessel...

  2. A, Science Service Feature Released on receipt

    E-Print Network [OSTI]

    . This has hap9ened where the rain f e l l on a muddy surface, a f t e r which sand o r some other l i g h-drops," which i n some cases a r e the original p i t s and i n others a r e the casts of the material

  3. A Science Service Feature---Released upon receipt but intended f o r use

    E-Print Network [OSTI]

    e l l on a muddy surface, a f t e r vhich sand o r some other l i g h t material d r i f t e d over the original p i t s and in others are the casts of the material with which they were f i l l e d . !the shapes

  4. B8 Page 1 B8. Using CMS-Wave

    E-Print Network [OSTI]

    US Army Corps of Engineers

    B8 ­ Page 1 B8. Using CMS-Wave The most recent CMS-Wave code developed is Version 3.2. Several new capabilities and advanced features in this version include: · Full-plane wind-generation of waves · Automatic wave run-up calculation · Infra-gravity wave calculation · Nonlinear wave-wave interaction · Muddy

  5. Modification and recovery of the shoreface of Matagorda Peninsula, Texas, following the landfall of Hurricane Claudette: the role of antecedent geology on short-term shoreface morphodynamics 

    E-Print Network [OSTI]

    Majzlik, Edward James

    2006-08-16

    of the coast in this region. This clay surface also creates low accommodation space for the preservation of modern sediments. As a result, only a thin (1 m) layer of transgressive Holocene muddy sand extends throughout the lower shoreface. On 15 July, 2003...

  6. Day in the Life of the Hudson River 10/16/14 Data (Hudson River Salt Front RM 65.9)

    E-Print Network [OSTI]

    Lance, Veronica P.

    /commercial, 20% urban/residential Sampling Site: shoreline is sandy, muddy, rocky, small beach, bank altered°F Wind Speed 11:21 AM Beaufort #4 11-16 kt 13-18 inches wave height South Cloud Cover Mostly cloudy

  7. What does water look like? Marta Kryven

    E-Print Network [OSTI]

    Waterloo, University of

    is shallow and pure it is transparent. Deep water is a saturated blue-green colour [Pope and Fry 1997]. MuddyWhat does water look like? Marta Kryven William Cowan University of Waterloo (a) (b) (c) (d) (e) (f of water look like water? We conducted four psychophysical experiments to isolate perceptual qualities

  8. CX-008793: Categorical Exclusion Determination

    Broader source: Energy.gov [DOE]

    Gore Pass to Muddy Pass: Single Pole and Multiple Cross Arm Replacements Grand County, Wyoming CX(s) Applied: B1.3, B4.6 Date: 09/16/2011 Location(s): Wyoming Offices(s): Western Area Power Administration-Rocky Mountain Region

  9. Fluid&ParticulateSystems 424514/2010

    E-Print Network [OSTI]

    Zevenhoven, Ron

    Potential energy Including flows of Kinetic energy Internal energy Flow energy Thermal energy Electrical - Steady state (no time derivates) - Thermal energy is omitted since temperature is assumed to remain Ron Zevenhoven ÅA Thermal and Flow Engineering ron.zevenhoven@abo.fi 1Fluid&ParticulateSystems 424514

  10. Construction of Rational Surfaces in Projective Fourspace

    E-Print Network [OSTI]

    Abo, Hirotachi

    surface. #12;Double point formula · X:= smooth surface in P4 . · H:= its hyperplane class. · K:= its families of smooth nongeneral-type surfaces in P4 (1995) can be found in W. Decker and S] 0 1 [S] 0 12 5 [AR2, AS] +1 0 0 1 [AR1] #12;References [ADS] H. Abo, W. Decker, N. Sasakura

  11. A geometric construction of elliptic conic bundles in P4 by Kristian Ranestad

    E-Print Network [OSTI]

    Ranestad, Kristian

    to the memory of Nobuo Sasakura In the fall of 1996 Abo, Decker and Sasakura [ADS] discovered smooth elliptic characteristic of S is (OS) = 0. The double point formula for surfaces in P4 , cf. [H], yields the relation: (H2 (H2 )2 - H2 + 1, so H2 10. On the other hand eliminating H · K from the double point formula yields

  12. Effect of substituting of S for O: The sulfide perovskite BaZrS3 investigated with density functional theory

    E-Print Network [OSTI]

    Rappe, Andrew M.

    February 2009; revised manuscript received 16 April 2009; published 9 June 2009 We use first-principles to the rotation and expansion of the B-X6 octahedra. Such octahedral rotations often generate a low, respectively, these cations move in a concerted manner, so PbTiO3 t=1.02 is ferro- electric. Ferroelectric ABO3

  13. Population Structure of the Chenchu and Other South Indian Tribal Groups: Relationships between Genetic, Anthropometric, Dermatoglyphic, Geographic, and Linguistic Distances

    E-Print Network [OSTI]

    Sirajuddin, S. M.; Duggirala, R.; Crawford, Michael H.

    1994-10-01

    We describe the genetic structure and interrelationships of nine south Indian tribal groups (seven from Andhra Pradesh and two from the adjoining states of Tamil Nadu and Kerala) using seven polymorphic loci (ABO, MN, RH, PGM, ACP, PGD, and LDH). R...

  14. Dopant site selectivity in BaCe0.85M0.15O3-by extended x-ray absorption fine structure

    E-Print Network [OSTI]

    Haile, Sossina M.

    solid oxide fuel cells and in hydrogen sensors.1­3 Proton incorporation requires, as a first step compensating defects for dopant ions and which are later exchanged with protons under hydrogen atmospheres lead barium oxide evaporation at high temperatures, en- suring that the overall A:B mole ratio in the ABO3

  15. Introduction to Computational Fluid Dynamics 424512 E #2 -rz maj 2015 bo Akademi Univ -Chemical Engineering

    E-Print Network [OSTI]

    Zevenhoven, Ron

    .zevenhoven@abo.fi Introduction to Computational Fluid Dynamics 424512 E #2 - rz maj 2015 Åbo Akademi Univ - Chemical Engineering Dynamics 424512 E #2 - rz maj 2015 Åbo Akademi Univ - Chemical Engineering Thermal and Flow Engineering Introduction to Computational Fluid Dynamics 424512 E #2 - rz maj 2015 Åbo Akademi Univ - Chemical Engineering

  16. Introduction to Computational Fluid Dynamics 424512 E #5-rz maj 2015 bo Akademi Univ -Chemical Engineering

    E-Print Network [OSTI]

    Zevenhoven, Ron

    ://users.abo.fi/rzevenho/kursRZ.html#FPS Introduction to Computational Fluid Dynamics 424512 E #5- rz maj 2015 Åbo Akademi Univ - Chemical Engineering - Chemical Engineering Thermal and Flow Engineering - Biskopsgatan 8, 20500 Turku 3/70 Fluid flow around 2015 Åbo Akademi Univ - Chemical Engineering Thermal and Flow Engineering - Biskopsgatan 8, 20500 Turku

  17. Patterns for Representing FMEA in Formal Specification of Control Systems Ilya Lopatkin, Alexei Iliasov,

    E-Print Network [OSTI]

    Southampton, University of

    Patterns for Representing FMEA in Formal Specification of Control Systems Ilya Lopatkin, Alexei, Finland {Yuliya.Prokhorova, Elena.Troubitsyna}@abo.fi Abstract -- Failure Modes and Effects analysis (FMEA) is a widely used technique for inductive safety analysis. FMEA provides engineers with valuable information

  18. Thermal radiation Ron Zevenhoven

    E-Print Network [OSTI]

    Zevenhoven, Ron

    .00032, similarly for 2·T = 0.7·2500 = 1750 µmK4 this gives f0-2 = 0.03392. Thus for 0.4 - 0.7 µm, f1-2 = 0Thermal radiation revisited Ron Zevenhoven Åbo Akademi University Thermal and Flow Engineering Laboratory / Värme- och strömningsteknik tel. 3223 ; ron.zevenhoven@abo.fi Process Engineering

  19. LETTER doi:10.1038/nature12622 Perovskite oxides for visible-light-absorbing

    E-Print Network [OSTI]

    Rappe, Andrew M.

    LETTER doi:10.1038/nature12622 Perovskite oxides for visible-light-absorbing ferroelectric perovskites (with ABO3 composition) is due to the fundamental characteristics of the metal­ oxygen A­O and B cations enable the perovskite oxide to exhibitferroelectricity12 . Owing to a large difference

  20. BIOLOGICAL FRAMEWORKS FOR ENGINEERS Laboratory Experience #2

    E-Print Network [OSTI]

    Sniadecki, Nathan J.

    surfaces should be washed immediately and thoroughly if contaminated with blood or other body fluids. Hands is an eye hazard so wear safety glasses. 2. Remove the ABO Card from its packaging and place it on a clean, and clean the skin of the ring finger with rubbing alcohol. Continue to wear a glove on the other hand. 4

  1. BIOLOGICAL FRAMEWORKS FOR ENGINEERS Laboratory Experience #2

    E-Print Network [OSTI]

    Sniadecki, Nathan J.

    and thoroughly if contaminated with blood or other body fluids. Hands should be washed immediately after gloves the ABO Card from its packaging and place it on a clean surface of the lab bench. Dispose of the wrapping and run the card. 2. VOLUNTEER: wash one hand, dry it, and clean the skin of the ring finger with rubbing

  2. Charles Kerans Professional Summary January, 2011

    E-Print Network [OSTI]

    Yang, Zong-Liang

    control on carbonate seismic stratigraphy: a case study of the Kingdom Abo Sequence, West Texas, 2003 of Expertise A. Carbonate sequence stratigraphy B. Carbonate reservoir characterization C. Paleokarst analysis Andres/Grayburg Reservoir Characterization Research Laboratory. Sequence-and parasequence-scale analysis

  3. 12.11.2014bo Akademi Univ -Thermal and Flow Engineering Piispankatu 8, 20500 Turku 1/32 4. Refrigeration process comparison;

    E-Print Network [OSTI]

    Zevenhoven, Ron

    12.11.2014Åbo Akademi Univ - Thermal and Flow Engineering Piispankatu 8, 20500 Turku 1/32 4 Engineering Laboratory / Värme- och strömningsteknik tel. 3223 ; ron.zevenhoven@abo.fi Kylteknik ("KYL and Flow Engineering Piispankatu 8, 20500 Turku 2/32 4.1 Refrigeration process comparison #12;12.11.2014Åbo

  4. year, Career S report includes

    E-Print Network [OSTI]

    Plotkin, Joshua B.

    S information abo ust 2011. Info ecutive Masters bined. 58% o s industries, as /Robotics grew t or were contin Energ Res Gove Insur ment by Ind ufacturing Sub y Industry: M Tec Man Energy/Nat Resources/U 2 stry munications gn rgy/Natural sources/Utilitie ernment rance ustry bchart Manufacturing chnology 28

  5. Texas Rice, Volume VI, Number 8 

    E-Print Network [OSTI]

    2006-01-01

    Method for Rice Stink Bug ..........................6 Part 1: LCRA/SAWS Water Project ......................................8 State, National and International News ......................11 Rice Crop Update... the floodwater across the field and thus, there is potential for substantial ammonia volatilization losses of urea. In addition, the soil is not always dry when the preflood N fertilizer has to be applied, and urea applied to muddy soil aggravates ammonia...

  6. A Review of "'The Furie of the Ordnance' Artillery in the English Civil Wars" by Stephen Bull 

    E-Print Network [OSTI]

    Furgol, Edward M

    2010-01-01

    of battles rests on discrete incidents in a number of battles, chiefly Edgehill and Marston Moor. Unlike sieges, where the absence or presence of large caliber guns, mortars or munitions often determined the result, battlefield use of artillery cannot... be so objectively examined. For example, no one tal- lied the causes of death or wounds, and the expenditure of shot gives no idea of its effectiveness, since large amounts could be mitigated by muddy ground or poor gun crews. Nevertheless, Bull shows...

  7. Sr3PbNiO6: Trigonal Prismatic Lead in a Novel Inverse K4CdCl6-type Pseudo-One-Dimensional Oxide

    E-Print Network [OSTI]

    zur Loye, Hans-Conrad

    Sr3PbNiO6: Trigonal Prismatic Lead in a Novel Inverse K4CdCl6-type Pseudo-One-Dimensional Oxide example of lead in the 2H hexagonal perovskite-related family of oxides with the formula A3ABO6 Manuscript Received August 11, 1999 The new one-dimensional oxide Sr3PbNiO6 contains the first reported

  8. Massverfring och separationsteknik Vrme -och strmningsteknik (MF-ST) 424302

    E-Print Network [OSTI]

    Zevenhoven, Ron

    .abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm A) under den senaste vecka; B) några veckor sedan; C) några månader sedan; D) ett år eller längre sedan; E) inte ännu; F) kommer inte ihåg, skall därför ännu göra det (på nytt). When did you give your last week; B) a few weeks ago; C) several months ago ; D) a year or longer ago; E) not yet; F) don

  9. Towards 3D mapping of BO? octahedron rotations at perovskite thin film heterointerfaces, unit cell by unit cell

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    He, Qian; Ishikawa, Ryo; Lupini, Andrew R.; Qiao, Liang; Moon, Eun Ju; Ovchinnikov, Oleg S.; May, Steven J.; Biegalski, Michael D.; Borisevich, Albina Y.

    2015-07-15

    The rich functionalities in the ABO? perovskite oxides originate, at least in part, from the ability of the corner-connected BO? octahedral network to host a large variety of cations through distortions and rotations. Characterizing these rotations, which have significant impact on both fundamental aspects of materials behavior and possible applications, remains a major challenge. In this work, we have developed a unique method to investigate BO? rotation patterns in complex oxides ABO? with unit cell resolution at heterointerfaces, where novel properties often emerge. Our method involves column shape analysis in ABF-STEM images of the ABO? heterointerfaces taken in specific orientations.more »The rotating phase of BO? octahedra can be identified for all three spatial dimensions without the need of case-by-case simulation. In several common rotation systems, quantitative measurements of all three rotation angles are now possible. Using this method, we examined interfaces between perovskites with distinct tilt systems as well as interfaces between tilted and untilted perovskites, identifying an unusual coupling behavior at the CaTiO?/LSAT interface. We believe this unique method will significantly improve our knowledge of the complex oxide heterointerfaces.« less

  10. Towards 3D mapping of BO? octahedron rotations at perovskite heterointerfaces, unit cell by unit cell

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    He, Qian; Ishikawa, Ryo; Lupini, Andrew R.; Qiao, Liang; Moon, Eun Ju; Ovchinnikov, Oleg S.; May, Steven J.; Biegalski, Michael D.; Borisevich, Albina Y.

    2015-07-15

    The rich functionalities in the ABO? perovskite oxides originate at least partly from the ability of the corner-connected BO? octahedral network to host a large variety of cations through distortions and rotations. Characterizing these rotations, which significantly affect both fundamental aspects of materials behavior and possible applications, remains a major challenge. In this work, we have developed a unique method of investigating BO? rotation patterns in complex oxides ABO? with unit cell resolution at heterointerfaces, where novel properties often emerge. Our method involves column shape analysis in annular bright field - scanning transmission electron microscope images of the ABO? heterointerfacesmore »taken in specific orientations. The rotating phase of BO? octahedra can be identified for all three spatial dimensions without the need of case-by-case simulation. In several common rotation systems, it is now possible to quantitatively measure all three rotation angles. With this method, we examined interfaces between perovskites with distinct tilt systems as well as interfaces between tilted and untilted perovskites, identifying an unusual coupling behavior at the CaTiO?/LSAT interface. We believe this unique method will significantly improve our knowledge of the complex oxide heterointerfaces.« less

  11. Efficient Use of Water in the Garden and Landscape. 

    E-Print Network [OSTI]

    Parson, Jerry; Cotner, Sam; Roberts, Ronald

    1985-01-01

    , if not impossible, to protect them with mulch. Train vining plants away from the furrows even though it is not an easy task. Also, one gets muddy trying to work in a garden the day after furrow irrigation. In areas with salty water, salts accumulate near... Extension Service 8-1496 r-~ ",-P~& lIe!pbtg P~fJ& --------------- Efficient Use of Water in the Garden ? and Landscape Texas Agricultural Extension Service. The Texas A&M University System. College Station, Texas [Blank Page in Original Bulletin...

  12. Some Principles and Practices in the Irrigation of Texas Soils. 

    E-Print Network [OSTI]

    Bloodworth, Morris E.

    1959-01-01

    by muddy water, which is PERCENT SAND Figure 4. The percentages of sand (0.05 to 2.0 mm), silt (0.002 to 0.05 mm) and clay (below 0.002 mm) in the basic textural classes. Modified from USDA Handbook 18. To use the chart: (a) determine percentage compo..., water and plants. Good irrigation practices also must take into ac- t such important factors as soil fertility. amount and quality of water, adapted crops and varieties, land xration for irrigation, water distribution over the land, irrigation timing...

  13. Microalgae bioprospecting at NREL

    ScienceCinema (OSTI)

    None

    2013-05-29

    Prospecting for elusive fast-growing, oily microalgae is a soggy, muddy, rewarding job for NREL researcher Lee Elliott. Not only do algae grow in unlikely settings, but their ability to convert the light they receive into biomass has the potential to outperform that of land plants. Trees, grasses and shrubs typically are not very efficient in capturing and converting the sun's energy into biomass, but some algae are believed to be capable of much higher efficiencies, with some scientists thinking ideal strains may be able to approach the maximum theoretical photosynthetic efficiency under the right conditions.

  14. Isotopic dating of Lava Creek B tephra in terrace deposits along the Wind River, Wyoming--Implications for post 0. 6 Ma uplift of the Yellowstone hotspot

    SciTech Connect (OSTI)

    Izett, G.A.; Pierce, K.L.; Naeser, N.D. (U.S.G.S., Denver, CO (United States)); Jaworowski, C. (Univ. of Wyoming, Laramie, WY (United States). Dept. of Geology and Geophysics)

    1992-01-01

    Along the Wind River near Kinnear (Pavillon quadrangle), a meter-thick tephra layer occurs near the middle of a main-stem gravel deposit about 100 m above the river. On Muddy Ridge 25 km east of Kinnear, a Lava Creek B tephra layer occurs at the base of a terrace deposit about 100 m above Muddy Creek. Another Lava Creek B tephra site 67 km northwest and upstream from Kinnear occurs within main-stem gravels of a terrace deposit 145 m above the river. This upstream increase of 45 m of the tephra horizon raises the concern that the two tephra layers might not be of the same age. All three tephras contain the same assemblage of phenocrysts as that in the Lava Creek Tuff, Member B in Yellowstone National Park and the Lava Creek B volcanic ash bed of the Western U.S., and therefore they are arguably correlatives. The authors confirmed this petrographic correlation by isotopic dating of sanidine crystals recovered from cm-size pumice lapilli in the Kinnear tephra and from coarse-grained tephra at the Muddy Creek site. Laser total-fusion Ar-40-Ar-39 ages of sanidine from the two sites are coeval, 0.66[plus minus]0.01 Ma and 0.67[plus minus]0.01 Ma at Muddy Creek. Conventional K-Ar dating of sanidine from the tephra at the Cl453 site resulted in an age of 0.60[plus minus]0.02 Ma. Glass-mantled zircon crystals from the Cl453 site yielded a fission-track age of 0.67[plus minus]0.16 Ma. These isotopic ages are compatible with conventional K-Ar, Ar-40-Ar-39, and fission-track ages of the Lava Creek Tuff, Member B in Yellowstone National Park and other occurrences of Lava Creek B ash beds. The authors suggest that the terrace deposit that contains the Lava Creek B tephra rises from the Kinnear site northwest up the Wind River as a result of Quaternary uplift in the area of the Yellowstone hotspot.

  15. Microalgae bioprospecting at NREL

    SciTech Connect (OSTI)

    2011-01-01

    Prospecting for elusive fast-growing, oily microalgae is a soggy, muddy, rewarding job for NREL researcher Lee Elliott. Not only do algae grow in unlikely settings, but their ability to convert the light they receive into biomass has the potential to outperform that of land plants. Trees, grasses and shrubs typically are not very efficient in capturing and converting the sun's energy into biomass, but some algae are believed to be capable of much higher efficiencies, with some scientists thinking ideal strains may be able to approach the maximum theoretical photosynthetic efficiency under the right conditions.

  16. Fluid and particulate Vrme-och strmningsteknik systems (FPS) 424514

    E-Print Network [OSTI]

    Zevenhoven, Ron

    .abo.fi/fak/ktf/vt/Eng/education_Evaluation.htm or shall you soon do this? 006.A total volumetric flow of 52 litre/s (70°C, density = 977,7 kg/m3 , kinematic viscosity = 4,14×10-7 m2 /s) is pumped through 100 parallel tubes (length l = 4.7 m, diameter d the original ones (lnew = 4.7 m, dnew = 14.4 mm, knew = 0.05 mm). Calculate how the total volumetric flow

  17. Synthesis of Conducting Polymer-Metal Nanoparticle Hybrids Exploiting RAFT Polymerization

    E-Print Network [OSTI]

    Williams, Paul E.; Jones, Samuel T.; Walsh, Zarah; Appel, Eric A.; Abo-Hamed, Enass K.; Scherman, Oren A.

    2015-02-03

    Synthesis of Conducting Polymer-Metal Nanoparticle Hybrids Exploiting RAFT Polymerization Paul E. Williams†, Samuel T. Jones†, Zarah Walsh, Eric A. Appel, Enass K. Abo-Hamed, and Oren A. Scherman? Melville Laboratory for Polymer Synthesis, Department... ) Odoi, M. Y.; Hammer, N. I.; Sill, K.; Emrick, T.; Barnes, M. D. J. Am. Chem. Soc. 2006, 128, 3506–3507. (10) Milliron, D. J.; Alivisatos, A. P.; Pitois, C.; Edder, C.; Fréchet, J. M. J. Adv. Mater. 2003, 15, 58–61. (11) Milliron, D. J.; Gur, I...

  18. Protective coatings for metal alloys and methods incorporating the same

    DOE Patents [OSTI]

    Seabaugh, Matthew M.; Ibanez, Sergio; Swartz, Scott L.

    2015-06-09

    An electrochemical device having one or more solid oxide fuel cells (SOFCs), each of the SOFCs including a cathode, an anode, and an electrolyte layer positioned between the cathode and anode; and at least one additional component comprising a metallic substrate having an electronically conductive, chromium-free perovskite coating deposited directly thereon. The perovskite coating has the formula ABO.sub.3, wherein A is a lanthanide element or Y, and B is a mixture of two or more transition elements, with the A site undoped by any alkaline earth element, and the perovskite coating exhibits limited or no ionic transport of oxygen.

  19. RIVERTON DOME GAS EXPLORATION AND STIMULATION TECHNOLOGY DEMONSTRATION, WIND RIVER BASIN, WYOMING

    SciTech Connect (OSTI)

    Ronald C. Surdam; Zunsheng Jiao; Nicholas K. Boyd

    1999-11-01

    The new exploration technology for basin center gas accumulations developed by R.C. Surdam and Associates at the Institute for Energy Research, University of Wyoming, was applied to the Riverton Dome 3-D seismic area. Application of the technology resulted in the development of important new exploration leads in the Frontier, Muddy, and Nugget formations. The new leads are adjacent to a major north-south trending fault, which is downdip from the crest of the major structure in the area. In a blind test, the drilling results from six new Muddy test wells were accurately predicted. The initial production values, IP, for the six test wells ranged from < one mmcf/day to four mmcf/day. The three wells with the highest IP values (i.e., three to four mmcf/day) were drilled into an intense velocity anomaly (i.e., anomalously slow velocities). The well drilled at the end of the velocity anomaly had an IP value of one mmcf/day, and the two wells drilled outside of the velocity anomaly had IP values of < one mmcf/day and are presently shut in. Based on these test results, it is concluded that the new IER exploration strategy for detecting and delineating commercial, anomalously pressured gas accumulation is valid in the southwestern portions of the Wind River Basin, and can be utilized to significantly reduce exploration risk and to increase profitability of so-called basin center gas accumulations.

  20. Structure and ferroelectricity of nonstoichiometric (Na{sub 0.5}Bi{sub 0.5})TiO{sub 3}

    SciTech Connect (OSTI)

    Carter, Jared; Aksel, Elena; Iamsasri, Thanakorn; Forrester, Jennifer S.; Jones, Jacob L.; Chen, Jun

    2014-03-17

    Stoichiometric (Na{sub 0.5}Bi{sub 0.5})TiO{sub 3} (NBT) adopts the ABO{sub 3} perovskite structure with the A-site equally occupied by Na{sup +} and Bi{sup 3+} ions. However, non-stoichiometric compositions can be synthesized intentionally or unintentionally. To determine the effect of A-site nonstoichiometry on the crystal structure and ferroelectricity of NBT, the composition of (Na{sub 0.5?x}Bi{sub 0.5+x})TiO{sub 3+x} was varied using x?=??0.01, ?0.005, 0, 0.005, and 0.01. High resolution synchrotron x-ray diffraction and Rietveld refinement revealed that a shift in either direction from x = 0 results in a decrease in the spontaneous ferroelastic strain. Ferroelectric hysteresis and piezoelectric coefficients were found to be optimum in the stoichiometric composition.

  1. Static ferroelectric memory transistor having improved data retention

    DOE Patents [OSTI]

    Evans, Jr., Joseph T. (13609 Verbena Pl., N.E., Albuquerque, NM 87112); Warren, William L. (7716 Wm. Moyers Ave., NE., Albuquerque, NM 87112); Tuttle, Bruce A. (12808 Lillian Pl., NE., Albuquerque, NM 87112)

    1996-01-01

    An improved ferroelectric FET structure in which the ferroelectric layer is doped to reduce retention loss. A ferroelectric FET according to the present invention includes a semiconductor layer having first and second contacts thereon, the first and second contacts being separated from one another. The ferroelectric FET also includes a bottom electrode and a ferroelectric layer which is sandwiched between the semiconductor layer and the bottom electrode. The ferroelectric layer is constructed from a perovskite structure of the chemical composition ABO.sub.3 wherein the B site comprises first and second elements and a dopant element that has an oxidation state greater than +4 in sufficient concentration to impede shifts in the resistance measured between the first and second contacts with time. The ferroelectric FET structure preferably comprises Pb in the A-site. The first and second elements are preferably Zr and Ti, respectively. The preferred B-site dopants are Niobium, Tantalum, and Tungsten at concentrations between 1% and 8%.

  2. Ferroelectric capacitor with reduced imprint

    DOE Patents [OSTI]

    Evans, Jr., Joseph T. (13609 Verbena Pl., NE., Albuquerque, NM 87112); Warren, William L. (7716 Wm. Moyers Ave., NE., Albuquerque, NM 87122); Tuttle, Bruce A. (12808 Lillian Pl., NE., Albuquerque, NM 87122); Dimos, Duane B. (6105 Innsbrook Ct., NE., Albuquerque, NM 87111); Pike, Gordon E. (1609 Cedar Ridge, NE., Albuquerque, NM 87112)

    1997-01-01

    An improved ferroelectric capacitor exhibiting reduced imprint effects in comparison to prior art capacitors. A capacitor according to the present invention includes top and bottom electrodes and a ferroelectric layer sandwiched between the top and bottom electrodes, the ferroelectric layer comprising a perovskite structure of the chemical composition ABO.sub.3 wherein the B-site comprises first and second elements and a dopant element that has an oxidation state greater than +4. The concentration of the dopant is sufficient to reduce shifts in the coercive voltage of the capacitor with time. In the preferred embodiment of the present invention, the ferroelectric element comprises Pb in the A-site, and the first and second elements are Zr and Ti, respectively. The preferred dopant is chosen from the group consisting of Niobium, Tantalum, and Tungsten. In the preferred embodiment of the present invention, the dopant occupies between 1 and 8% of the B-sites.

  3. Do yield and quality of big bluestem and switchgrass feedstock decline over winter?

    SciTech Connect (OSTI)

    Jane M.F. Johnson; Garold L. Gresham

    2014-03-01

    Switchgrass (Panicum virgatum L.) and big bluestem (Andropogon gerdardii Vitman) are potential perennial bioenergy feedstocks. Feedstock storage limitations, labor constraints for harvest, and environmental benefits provided by perennials are rationales for developing localized perennial feedstock as an alternative or in conjunction with annual feedstocks (i.e., crop residues). Little information is available on yield, mineral, and thermochemical properties of native species as related to harvest time. The study’s objectives were to compare the feedstock quantity and quality between grasses harvested in the fall or the following spring. It was hypothesized that biomass yield may decline, but translocation and/or leaching of minerals from the feedstock would improve feedstock quality. Feedstock yield did not differ by crop, harvest time, or their interactions. Both grasses averaged 6.0 Mg ha-1 (fall) and 5.4 Mg ha-1 (spring) with similar high heating value (17.7 MJ kg-1). The K/(Ca + Mg) ratio, used as a quality indicator declined to below a 0.5 threshold, but energy yield (Megajoule per kilogram) decreased 13% by delaying harvest until spring. Only once during the four study-years were conditions ideal for early spring harvest, in contrast during another spring, very muddy conditions resulted in excessive soil contamination. Early spring harvest may be hampered by late snow, lodging, and muddy conditions that may delay or prevent harvest, and result in soil contamination of the feedstock. However, reducing slagging/fouling potential and the mass of mineral nutrients removed from the field without a dramatic loss in biomass or caloric content are reasons to delay harvest until spring.

  4. Data from selected Almond Formation outcrops -- Sweetwater County, Wyoming

    SciTech Connect (OSTI)

    Jackson, S.R.; Rawn-Schatzinger, V.

    1993-12-01

    The objectives of this research program are to: (1) determine the reservoir characteristics and production problems of shoreline barrier reservoirs; and (2) develop methods and methodologies to effectively characterize shoreline barrier reservoirs to predict flow patterns of injected and produced fluids. Two reservoirs were selected for detailed reservoir characterization studies -- Bell Creek field, Carter County, Montana, that produces from the Lower Cretaceous (Albian-Cenomanian) Muddy Formation, and Patrick Draw field, Sweetwater County, Wyoming that produces from the Upper Cretaceous (Campanian) Almond Formation of the Mesaverde Group. An important component of the research project was to use information from outcrop exposures of the producing formations to study the spatial variations of reservoir properties and the degree to which outcrop information can be used in the construction of reservoir models. A report similar to this one presents the Muddy Formation outcrop data and analyses performed in the course of this study (Rawn-Schatzinger, 1993). Two outcrop localities, RG and RH, previously described by Roehler (1988) provided good exposures of the Upper Almond shoreline barrier facies and were studied during 1990--1991. Core from core well No. 2 drilled approximately 0.3 miles downdip of outcrop RG was obtained for study. The results of the core study will be reported in a separate volume. Outcrops RH and RG, located about 2 miles apart were selected for detailed description and drilling of core plugs. One 257-ft-thick section was measured at outcrop RG, and three sections {approximately}145 ft thick located 490 and 655 feet apart were measured at the outcrop RH. Cross-sections of these described profiles were constructed to determine lateral facies continuity and changes. This report contains the data and analyses from the studied outcrops.

  5. [National Institute for Petroleum and Energy Research] quarterly technical report for April--June 30, 1993. Volume 2, Energy Production Research

    SciTech Connect (OSTI)

    Not Available

    1993-09-01

    Progress reports are presented for: chemical flooding--supporting research; gas displacement--supporting research; thermal recovery--supporting research; geoscience technology; resource assessment technology; and microbial technology. Chemical flooding includes; development of improved chemical flooding methods; development of improved alkaline flooding methods; mobility control and sweep improvement in chemical flooding; and surfactant-enhanced alkaline flooding field project. Gas displacement research covers: gas flooding performance prediction improvement; and mobility control, profile modification, and sweep improvement in gas flooding. Thermal recovery research includes: thermal processes for light oil recovery; thermal processes for heavy oil recovery; feasibility study of heavy oil recovery in the Midcontinent region: Oklahoma, Kansas, and Missouri; simulation analysis of steam-foam projects; and organization of UNITAR 6th International Conference on Heavy Crude and Tar Sands. Geoscience technology covers: three-phase relative permeability; and imaging techniques applied to the study of fluids in porous media. Resource assessment technology includes: reservoir assessment and characterization; TORIS research support; upgrade the BPO Crude Oil Analysis Data Base; compilation and analysis of outcrop data from the Muddy and Almond Formations; and horizontal well production from fractured reservoir. Microbial Technology covers: development of improved microbial flooding methods; and microbial-enhanced waterflooding field project.

  6. Monthly progress report for April 1993

    SciTech Connect (OSTI)

    Not Available

    1993-05-01

    Accomplishments for the month of April are described briefly for the following tasks: energy production research; fuels research; and supplemental government program. Energy production research includes: reservoir assessment and characterization; TORIS research support; development of improved microbial flooding methods; development of improved chemical flooding methods; development of improved alkaline flooding methods; mobility control and sweep improvement in chemical flooding; gas flood performance prediction improvement; mobility control, profile modification, and sweep improvement in gas flooding; three-phase relative permeability research; thermal processes for light oil recovery; thermal processes for heavy oil recovery; and imaging techniques applied to the study of fluids in porous media. Fuel research includes: development of analytical methodology for analysis of heavy crudes; and thermochemistry and thermophysical properties of organic nitrogen- and diheteratom-containing compounds. Supplemental government program includes: microbial-enhanced waterflooding field project; feasibility study of heavy oil recovery in the midcontinent region--Oklahoma, Kansas, and Missouri; surfactant-enhanced alkaline flooding field project; process- engineering property measurements on heavy petroleum components; development and application of petroleum production technologies; upgrade BPO crude oil data base; simulation analysis of steam-foam projects; DOE education initiative project; field application of foams for oil production symposium; technology transfer to independent producers; compilations and analysis of outcrop data from the Muddy and Almond Formations; implementation of oil and gas technology transfer initiative; and horizontal well production from fractured reservoirs.

  7. [National Institute for Petroleum and Energy Research], monthly progress report for March 1993

    SciTech Connect (OSTI)

    Not Available

    1993-04-01

    Accomplishments for the month of April are described briefly under tasks for: Energy Production Research; Fuels Research; and Supplemental Government Program. Energy Production Research includes: reservoir assessment and characterization; TORIS research support; development of improved microbial flooding methods; development of improved chemical flooding methods; development of improved alkaline flooding methods; mobility control and sweep improvement in chemical flooding; gas flood performance prediction improvement; mobility control, profile modification, and sweep improvement in gas flooding; three-phase relative permeability research; thermal processes for light oil recovery; thermal processes for heavy oil recovery; and imaging techniques applied to the study of fluids in porous media. Fuels Research includes: development of analytical methodology for analysis of heavy crudes; and thermochemistry and thermophysical properties of organic nigrogen- and diheteroatom-containing compounds. Supplemental Government Program includes: microbial-enhanced waterflooding field project; feasibility study of heavy oil recovery in the midcontinent region--Oklahoma, Kansas, and Missouri; surfactant- enhanced alkaline flooding field project; process- engineering property measurements on heavy petroleum components; development and application of petroleum production technologies; upgrade BPO crude oil data base; simulation analysis of steam-foam projects; DOE education initiative project; field application of foams of oil production symposium; technology transfer to independent producers; compilations and analysis of outcrop data from the Muddy and Almond formations; and horizontal well production from fractured reservoirs.

  8. National Institute for Petroleum and Energy Research monthly progress report, May 1993

    SciTech Connect (OSTI)

    Not Available

    1993-06-01

    Accomplishments for the month of May are described briefly under tasks for: Energy Production Research; Fuels Research; and Supplemental Government Program. Energy Production Research includes: reservoir assessment and characterization; TORIS research support; development of improved microbial flooding methods; development of improved chemical flooding methods; development of improved alkaline flooding methods; mobility control and sweep improvement in chemical flooding; gas flood performance prediction improvement; mobility control, profile modification, and sweep improvement in gas flooding; three-phase relative permeability research; thermal processes for light oil recovery; thermal processes for heavy oil recovery; and imaging techniques applied to the study of fluids in porous media. Fuels Research covers: development of analytical methodology for analysis of heavy crudes; and thermochemistry and thermophysical properties of organic nitrogen- and diheteratom-containing compounds. Supplemental Government Program covers: microbial-enhanced waterflooding field project; feasibility study of heavy oil recovery in the midcontinent region--Oklahoma, Kansas, and Missouri; surfactant-enhanced alkaline flooding field project; process-engineering property measurements on heavy petroleum components; development and application of petroleum production technologies; upgrade BPO crude oil data base; simulation analysis of steam-foam projects; DOE education initiative project; field application of foams for oil production symposium; technology transfer to independent producers; compilation and analysis of outcrop data from the Muddy and Almond formations; implementation of oil and gas technology transfer initiative; horizontal well production from fractured reservoirs; and chemical EOR workshop.

  9. Indirect fracture delineation in a carbonate reservoir: The Upper Jurassic Hanifa of Abqaiq field, Saudi Arabia

    SciTech Connect (OSTI)

    Bailey, D.L. (Saudi Aramco, Dhahran (Saudi Arabia))

    1991-03-01

    Abqaiq field is a northeast-trending anticline approximately 60 km long and 12 km wide and contains several reservoirs. The Hanifa Reservoir is approximately 100 m thick and consists of fine-grained, muddy limestone with subordinate dolomite and anhydrite. Since discovery of the Hanifa oil pool in 1947, pressure fluctuations have indicated communication with the overlying Arab-D Reservoir. Welltest permeability measurements are approximately 40 times higher than core permeability measurements of the Hanifa. This divergence of Hanifa permeability measurements combined with the indicated Arab-D communication suggests the presence of a natural fracture network. Direct observations of Hanifa cores reveal common, sub-vertical fractures with average apertures <200 microns. With limited core coverage and no oriented cores, a new technique was needed to delineate the areas affected by fractures. A technique combining indirect fracture indicators was devised for Abqaiq field and can be applied to other, similar fields. The actual flow system of the Abqaiq Hanifa is a complex interaction between matrix porosity/permeability and fracture permeability or enhanced permeability. Future development plans allow for low matrix permeability access to much of the Hanifa storage space and high fracture permeability both within the Hanifa and connecting to the Arab-D Reservoir.

  10. Tidally dominated depositional environment for the Mt. Simon Sandstone in central Illinois

    SciTech Connect (OSTI)

    Sargent, M.L.; Lasemi, Z. (Illinois State Geological Survey, Champaign, IL (United States))

    1993-03-01

    Several hundred feet of core from the upper part of the Mt. Simon in central Illinois have been examined macroscopically. Grain sizes and their systematics, bedding characteristics, sedimentary structures, and relationships among beds show that the upper Mt. Simon Sandstone is composed of a series of fining-upward cycles up to 10 m (30 feet) thick. A typical cycle consists, in ascending order, of a sandy subtidal facies, a mixed sand and mud intertidal-flat facies, and a muddy upper tidal-flat facies upward through the succession, the maximum and average grain size becomes progressively finer and the cycles thinner. The lower sandstone of each cycle contains beds that are massive to cross bedded and cross laminated; some beds show scoured reactivation surfaces. A few cycles contain a middle unit characterized by flaser and lenticular bedding and abundant mudcracks. Mudcracks also are common in the shale beds at the top of each cycle. Sedimentary structures such as reactivation surfaces, flaser and lenticular bedding, and mudcracks suggest that these cycles were deposited in peritidal environments. The presence of Skolithos in some cycles suggests very shallow marine conditions. The within-cycle upward fining is caused by regression or progradation that reflects a progressive decrease in current velocity from subtidal to intertidal parts of the tidal flat. Frequent flooding of the tidal flat resulted in repeated fining-upward cycles within the upper part of the Mt. Simon Sandstone.

  11. A study of conception rates resulting from natural and artificial breeding of dairy cattle in Texas 

    E-Print Network [OSTI]

    Burleson, Richard Earl

    1952-01-01

    48 8 i, OO'~34 5" "3d '+~M"' OXAVXC8 p@X~KOf3PX $7 DAM" 'Q@Vjl4 M 4~PA USZV8'~B!. (p?' boX'4 8?tx '5 4x' cod 8 t"' ~abo -'igGY o". u~icczoo ""0?438 N&x'8 xbo xa8&'2t of a&i M~$ 88"V. -'Clog 18 P~I88X'8 . vbGXi K @ O~P? COOCOIVOB 8'h ''C3. lg tb..., . '-p88 '~- yg &8 fe8tgooe ~, , 4W ~ ~:eieeg+e4~ C~ Bn@ BSXO (/) 'i5'Ci& htMggio ef 88~4K+@X XOX8BM~ig X%~8@&8 elf 7&ki. ?a @OX@ f~Q6 i. boy Qg Tio@ CCzl4 QXTCQ'. VQ2 bg tb(9 f: X'85 8QLKiLCB 8)16 GpNg Oig pSX" COOQ bog CC%06$VRQ Q Xbo fXfQ~ 58...

  12. Performance of the ATLAS Transition Radiation Tracker with Cosmic Rays and First High Energy Collisions at LHC

    E-Print Network [OSTI]

    Mashinistov, R; The ATLAS collaboration

    2010-01-01

    The ATLAS Transition Radiation Tracker (TRT) is the outermost of the three subsystems of the ATLAS Inner Detector at the Large Hadron Collider (LHC) at CERN. It consists of close to 300000 thin-wall drift tubes (straws) providing on average 30 two-dimensional space points with 130 ?m resolution for charged particle tracks with |?| < 2 and pT > 0.5 GeV. The TRT is immersed in a 2 T magnetic field generated by the central solenoid, significantly contributing together with the other two Inner Detector sub-systems to the particle momentum reconstruction. Along with continuous tracking, it provides particle identification capability through the detection of transition radiation X-ray photons generated by high velocity particles in the many polymer fibers or films that fill the spaces between the straws. As expected from the production of transition radiation (TR), the first collision results show the increase in the number of detected TR-photons for particles with a gamma-factor abo...

  13. NaIrO{sub 3}-A pentavalent post-perovskite

    SciTech Connect (OSTI)

    Bremholm, M.; Dutton, S.E.; Stephens, P.W.; Cava, R.J.

    2011-03-15

    Sodium iridium (V) oxide, NaIrO{sub 3,} was synthesized by a high pressure solid state method and recovered to ambient conditions. It is found to be isostructural with CaIrO{sub 3}, the much-studied structural analog of the high-pressure post-perovskite phase of MgSiO{sub 3}. Among the oxide post-perovskites, NaIrO{sub 3} is the first example with a pentavalent cation. The structure consists of layers of corner- and edge-sharing IrO{sub 6} octahedra separated by layers of NaO{sub 8} bicapped trigonal prisms. NaIrO{sub 3} shows no magnetic ordering and resistivity measurements show non-metallic behavior. The crystal structure, electrical and magnetic properties are discussed and compared to known post-perovskites and pentavalent perovskite metal oxides. -- Graphical abstract: Sodium iridium(V) oxide, NaIrO{sub 3}, synthesized by a high pressure solid state method and recovered to ambient conditions is found to crystallize as the post-perovskite structure and is the first example of a pentavalent ABO{sub 3} post-perovskite. Research highlights: {yields} NaIrO{sub 3} post-perovskite stabilized by pressure. {yields} First example of a pentavalent oxide post-perovskite. {yields} Non-metallic and non-magnetic behavior of NaIrO{sub 3}.

  14. New composition dependent cooling and heating curves for galaxy evolution simulations

    E-Print Network [OSTI]

    De Rijcke, Sven; Vandenbroucke, Bert; Jachowicz, Natalie; Decroos, Jeroen; Cloet-Osselaer, Annelies; Koleva, Mina

    2013-01-01

    In this paper, we present a new calculation of composition-dependent radiative cooling and heating curves of low-density gas, intended primarily for use in numerical simulations of galaxy formation and evolution. These curves depend on only five parameters: temperature, density, redshift, [Fe/H], and [Mg/Fe]. They are easily tabulated and can be efficiently interpolated during a simulation. The ionization equilibrium of 14 key elements is determined for temperatures between 10K and 10^9K and densities up to 100 amu/cm^3 taking into account collisional and radiative ionization, by the cosmic UV background and an interstellar radiation field, and by charge-transfer reactions. These elements, ranging from H to Ni, are the ones most abundantly produced and/or released by SNIa, SNII, and intermediate-mass stars. Self-shielding of the gas at high densities by neutral Hydrogen is taken into account in an approximate way by exponentially suppressing the H-ionizing part of the cosmic UV background for HI densities abo...

  15. Effect of cation ordering on oxygen vacancy diffusion pathways in double perovskites

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Uberuaga, Blas Pedro; Pilania, Ghanshyam

    2015-07-08

    Perovskite structured oxides (ABO3) are attractive for a number of technological applications, including as superionics because of the high oxygen conductivities they exhibit. Double perovskites (AA’BB’O6) provide even more flexibility for tailoring properties. Using accelerated molecular dynamics, we examine the role of cation ordering on oxygen vacancy mobility in one model double perovskite SrLaTiAlO6. We find that the mobility of the vacancy is very sensitive to the cation ordering, with a migration energy that varies from 0.6 to 2.7 eV. In the extreme cases, the mobility is both higher and lower than either of the two end member single perovskites.more »Further, the nature of oxygen vacancy diffusion, whether one-dimensional, two-dimensional, or three-dimensional, also varies with cation ordering. We correlate the dependence of oxygen mobility on cation structure to the distribution of Ti4+ cations, which provide unfavorable environments for the positively charged oxygen vacancy. The results demonstrate the potential of using tailored double perovskite structures to precisely control the behavior of oxygen vacancies in these materials.« less

  16. Air electrode composition for solid oxide fuel cell

    DOE Patents [OSTI]

    Kuo, Lewis (Monroeville, PA); Ruka, Roswell J. (Pittsburgh, PA); Singhal, Subhash C. (Murrysville, PA)

    1999-01-01

    An air electrode composition for a solid oxide fuel cell is disclosed. The air electrode material is based on lanthanum manganite having a perovskite-like crystal structure ABO.sub.3. The A-site of the air electrode composition comprises a mixed lanthanide in combination with rare earth and alkaline earth dopants. The B-site of the composition comprises Mn in combination with dopants such as Mg, Al, Cr and Ni. The mixed lanthanide comprises La, Ce, Pr and, optionally, Nd. The rare earth A-site dopants preferably comprise La, Nd or a combination thereof, while the alkaline earth A-site dopant preferably comprises Ca. The use of a mixed lanthanide substantially reduces raw material costs in comparison with compositions made from high purity lanthanum starting materials. The amount of the A-site and B-site dopants is controlled in order to provide an air electrode composition having a coefficient of thermal expansion which closely matches that of the other components of the solid oxide fuel cell.

  17. Air electrode composition for solid oxide fuel cell

    DOE Patents [OSTI]

    Kuo, L.; Ruka, R.J.; Singhal, S.C.

    1999-08-03

    An air electrode composition for a solid oxide fuel cell is disclosed. The air electrode material is based on lanthanum manganite having a perovskite-like crystal structure ABO{sub 3}. The A-site of the air electrode composition comprises a mixed lanthanide in combination with rare earth and alkaline earth dopants. The B-site of the composition comprises Mn in combination with dopants such as Mg, Al, Cr and Ni. The mixed lanthanide comprises La, Ce, Pr and, optionally, Nd. The rare earth A-site dopants preferably comprise La, Nd or a combination thereof, while the alkaline earth A-site dopant preferably comprises Ca. The use of a mixed lanthanide substantially reduces raw material costs in comparison with compositions made from high purity lanthanum starting materials. The amount of the A-site and B-site dopants is controlled in order to provide an air electrode composition having a coefficient of thermal expansion which closely matches that of the other components of the solid oxide fuel cell. 3 figs.

  18. Lanthanum manganite-based air electrode for solid oxide fuel cells

    DOE Patents [OSTI]

    Ruka, Roswell J. (Pittsburgh, PA); Kuo, Lewis (Monroeville, PA); Li, Baozhen (Essex Junction, VT)

    1999-01-01

    An air electrode material for a solid oxide fuel cell is disclosed. The electrode material is based on lanthanum manganite having a perovskite-like crystal structure ABO.sub.3. The A-site of the air electrode material preferably comprises La, Ca, Ce and at least one lanthanide selected from Sm, Gd, Dy, Er, Y and Nd. The B-site of the electrode material comprises Mn with substantially no dopants. The ratio of A:B is preferably slightly above 1. A preferred air electrode composition is of the formula La.sub.w Ca.sub.x Ln.sub.y Ce.sub.z MnO.sub.3, wherein Ln comprises at least one lanthanide selected from Sm, Gd, Dy, Er, Y and Nd, w is from about 0.55 to about 0.56, x is from about 0.255 to about 0.265, y is from about 0.175 to about 0.185, and z is from about 0.005 to about 0.02. The air electrode material possesses advantageous chemical and electrical properties as well as favorable thermal expansion and thermal cycle shrinkage characteristics.

  19. Lanthanum manganite-based air electrode for solid oxide fuel cells

    DOE Patents [OSTI]

    Ruka, R.J.; Kuo, L.; Li, B.

    1999-06-29

    An air electrode material for a solid oxide fuel cell is disclosed. The electrode material is based on lanthanum manganite having a perovskite-like crystal structure ABO[sub 3]. The A-site of the air electrode material preferably comprises La, Ca, Ce and at least one lanthanide selected from Sm, Gd, Dy, Er, Y and Nd. The B-site of the electrode material comprises Mn with substantially no dopants. The ratio of A:B is preferably slightly above 1. A preferred air electrode composition is of the formula La[sub w]Ca[sub x]Ln[sub y]Ce[sub z]MnO[sub 3], wherein Ln comprises at least one lanthanide selected from Sm, Gd, Dy, Er, Y and Nd, w is from about 0.55 to about 0.56, x is from about 0.255 to about 0.265, y is from about 0.175 to about 0.185, and z is from about 0.005 to about 0.02. The air electrode material possesses advantageous chemical and electrical properties as well as favorable thermal expansion and thermal cycle shrinkage characteristics. 10 figs.

  20. Higher Spin Currents in Wolf Space: Part III

    E-Print Network [OSTI]

    Ahn, Changhyun

    2015-01-01

    The large N=4 linear superconformal algebra (generated by four spin-1/2 currents, seven spin-1 currents, four spin-3/2 currents and one spin-2 current) found by Sevrin, Troost and Van Proeyen (and other groups) was realized in the N=4 superconformal coset SU(5)/SU(3) theory previously. The lowest 16 higher spin currents of spins (1, 3/2, 3/2, 2), (3/2, 2, 2, 5/2), (3/2, 2, 2, 5/2) and (2, 5/2, 5/2, 3) are obtained by starting with the operator product expansions (OPEs) between the four spin-3/2 currents from the above large N=4 linear superconformal algebra and the lowest higher spin-1 current which is the same as the one in the Wolf space coset SU(5)/[SU(3) x SU(2) x U(1)] theory. These OPEs determine the four higher spin-3/2 currents and the next six higher spin-2 currents are obtained from the OPEs between the above four spin-3/2 currents associated with the N=4 supersymmetry and these four higher spin-3/2 currents. The four higher spin-5/2 currents can be determined by calculating the OPEs between the abo...

  1. Insights into dynamic processes of cations in pyrochlores and other complex oxides

    DOE Public Access Gateway for Energy & Science Beta (PAGES Beta)

    Uberuaga, Blas Pedro; Perriot, Romain

    2015-08-26

    Complex oxides are critical components of many key technologies, from solid oxide fuel cells and superionics to inert matrix fuels and nuclear waste forms. In many cases, understanding mass transport is important for predicting performance and, thus, extensive effort has been devoted to understanding mass transport in these materials. However, most work has focused on the behavior of oxygen while cation transport has received relatively little attention, even though cation diffusion is responsible for many phenomena, including sintering, radiation damage evolution, and deformation processes. Here, we use accelerated molecular dynamics simulations to examine the kinetics of cation defects in onemore »class of complex oxides, A?B?O? pyrochlore. In some pyrochlore chemistries, B cation defects are kinetically unstable, transforming to A cation defects and antisites at rates faster than they can diffuse. When this occurs, transport of B cations occurs through defect processes on the A sublattice. Further, these A cation defects, either interstitials or vacancies, can interact with antisite disorder, reordering the material locally, though this process is much more efficient for interstitials than vacancies. Whether this behavior occurs in a given pyrochlore depends on the A and B chemistry. Pyrochlores with a smaller ratio of cation radii exhibit this complex behavior, while those with larger ratios exhibit direct migration of B interstitials. Similar behavior has been reported in other complex oxides such as spinels and perovskites, suggesting that this coupling of transport between the A and B cation sublattices, while not universal, occurs in many complex oxide.« less

  2. Recent carbonate sedimentation on Balearic platform: model for temperate-climate carbonate shelves

    SciTech Connect (OSTI)

    Fornos, J.; Rodriguez-Perea, A.; Massuti, C.; Pomar, L.; Acosta, J.; Herranz, P.; Sanz, J.L.

    1989-03-01

    Existing models for carbonate sedimentation on continental platforms are derived from the study of modern carbonate platforms in tropical climates. The Balearic platform in the western Mediterranean provides a new model for carbonate sedimentation in a temperature, semiarid climate. On most of the continental shelf around the Balearic Islands, modern sediments are exclusively bioclastic carbonates. Shoreline carbonate sediments are bioclastic sands and muds accumulating in beach-dune systems without significant tidal influence (there are no astronomical tides in the western Mediterranean ). From the upper shoreface to 35 m deep, the sandy bottom is extensively colonized by sea grass (Posidonia oceanica), the rhizomes and roots of which form a rigid entrapment that retains the sediment derived from calcareous organisms living within the sea grass and from calcareous epiphytes living on the stems and leaves. Archeological dating establishes a rate of vertical accretion in this zone of 10/sup 3/ Bubnoff units (1 Bubnoff unit = 1 mm/1000 years). Between depths of 40 and 60 m, carbonate sands are composed predominantly or red-algal fragments. Intensely bioturbated wave ripples occur in environments dominated by laminar red algae (Lithothamnium and Phymatolithon). Below depths of 60 m, coarse sediment produced by rhodolitic and ramose red algae is deposited in areas of tens to hundreds of meters in size. Biogenic buildups up to 2 m high occur in sandy areas as well as in deeper muddy areas. At the same depth in open-platform zones, the bottom topography is characterized by large hummocks several hundred meters across. From the horizontal distribution of facies, it is possible to construct the probable vertical sequence of lithofacies which would characterize carbonates accumulating on a temperate-climate carbonate shelf. Many of these lithofacies are recognized in upper Miocene limestones on the Balearic Islands.

  3. Sequence stratigraphic-based reservoir architecture in late Jurrassic outer-ramp carbonates, Hanifa Formation, Saudi Arabia

    SciTech Connect (OSTI)

    Markello, J.R.; Stockton, M.L. (Mobile E P Technical Center, Dallas, TX (United States)); McGuire, M.; Al'Shammery, M.J.; Al'Amoudi M.O. (Saudi Aramco, Dhahran (Saudi Arabia))

    1996-01-01

    The Hanifa Formation (135-160m tk; Kimmeridgian age), in our study area, comprises one 3rd-order, coarsening-upward, type 2 stratigraphic sequence. Sediments formed in outer ramp, ramp-margin and basinal environments defining a transition between the Rimthan Arch carbonate platform and adjacent Arabian intrashelf basin. Quantification of Hanifa reservoir architecture for simulation involved development of field-scale geologic models based on sequence stratigraphic principles. No seismic and biostratigraphic data were available. Sequence interpretations were based on regional facies and parasequence analysis from 32 cores and 142 gamma-ray/porosity logs. In the study area, the Hanifa Formation has basinward-thinning tabular geometry, and contains (1) a lower member of organic-rich muddy carbonates and (2) an upper reservoir member of thick, medium to coarse-grained skeletal packstones, skeletal peloidal grainstones, skeletal intraclast conglomerates, and stromatoporoid boundstones. The Hanifa reservoir consists of, from oldest to youngest: (1) a highstand systems tract: aggrading and prograding, sigmoidal-shaped parasequences and parasequence sets of grainstrines, conglomerates and boundstones, capped by a subaqueous, type 2 sequence boundary; (2) a shelf margin wedge: prograding to aggrading, sigmoidal to tabular-shaped parasequences and parasequence sets of skeletal packstones, grainstones and local boundstones showing maximum basinward progradation; and (3) a transgressive systems tract: backstepping tabular-shaped parasequences of grainstones capped by a drowning surface. All facies are interpreted to have formed in subtidal settings of water depths from 5 to 150m. No evidence was found for shoal-water bank, lagoonal or peritidal deposition or for subaerial exposure in any facies.

  4. Sequence stratigraphic-based reservoir architecture in late Jurrassic outer-ramp carbonates, Hanifa Formation, Saudi Arabia

    SciTech Connect (OSTI)

    Markello, J.R.; Stockton, M.L. [Mobile E & P Technical Center, Dallas, TX (United States); McGuire, M.; Al`Shammery, M.J.; Al`Amoudi M.O. [Saudi Aramco, Dhahran (Saudi Arabia)

    1996-12-31

    The Hanifa Formation (135-160m tk; Kimmeridgian age), in our study area, comprises one 3rd-order, coarsening-upward, type 2 stratigraphic sequence. Sediments formed in outer ramp, ramp-margin and basinal environments defining a transition between the Rimthan Arch carbonate platform and adjacent Arabian intrashelf basin. Quantification of Hanifa reservoir architecture for simulation involved development of field-scale geologic models based on sequence stratigraphic principles. No seismic and biostratigraphic data were available. Sequence interpretations were based on regional facies and parasequence analysis from 32 cores and 142 gamma-ray/porosity logs. In the study area, the Hanifa Formation has basinward-thinning tabular geometry, and contains (1) a lower member of organic-rich muddy carbonates and (2) an upper reservoir member of thick, medium to coarse-grained skeletal packstones, skeletal peloidal grainstones, skeletal intraclast conglomerates, and stromatoporoid boundstones. The Hanifa reservoir consists of, from oldest to youngest: (1) a highstand systems tract: aggrading and prograding, sigmoidal-shaped parasequences and parasequence sets of grainstrines, conglomerates and boundstones, capped by a subaqueous, type 2 sequence boundary; (2) a shelf margin wedge: prograding to aggrading, sigmoidal to tabular-shaped parasequences and parasequence sets of skeletal packstones, grainstones and local boundstones showing maximum basinward progradation; and (3) a transgressive systems tract: backstepping tabular-shaped parasequences of grainstones capped by a drowning surface. All facies are interpreted to have formed in subtidal settings of water depths from 5 to 150m. No evidence was found for shoal-water bank, lagoonal or peritidal deposition or for subaerial exposure in any facies.

  5. Northern Cheyenne Reservation Coal Bed Natural Resource Assessment and Analysis of Produced Water Disposal Options

    SciTech Connect (OSTI)

    Shaochang Wo; David A. Lopez; Jason Whiteman Sr.; Bruce A. Reynolds

    2004-07-01

    Coalbed methane (CBM) development in the Powder River Basin (PRB) is currently one of the most active gas plays in the United States. Monthly production in 2002 reached about 26 BCF in the Wyoming portion of the basin. Coalbed methane reserves for the Wyoming portion of the basin are approximately 25 trillion cubic feet (TCF). Although coal beds in the Powder River Basin extend well into Montana, including the area of the Northern Cheyenne Indian Reservation, the only CBM development in Montana is the CX Field, operated by the Fidelity Exploration, near the Wyoming border. The Northern Cheyenne Reservation is located on the northwest flank of the PRB in Montana with a total land of 445,000 acres. The Reservation consists of five districts, Lame Deer, Busby, Ashland, Birney, and Muddy Cluster and has a population of 4,470 according to the 2000 Census. The CBM resource represents a significant potential asset to the Northern Cheyenne Indian Tribe. Methane gas in coal beds is trapped by hydrodynamic pressure. Because the production of CBM involves the dewatering of coalbed to allow the release of methane gas from the coal matrix, the relatively large volume of the co-produced water and its potential environmental impacts are the primary concerns for the Tribe. Presented in this report is a study conducted by the Idaho National Engineering and Environmental Laboratory (INEEL) and the Montana Bureau of Mines and Geology (MBMG) in partnership with the Northern Cheyenne Tribe to assess the Tribe’s CBM resources and evaluate applicable water handling options. The project was supported by the U.S. Department of Energy (DOE) through the Native American Initiative of the National Petroleum Technology Office, under contract DEAC07- 99ID13727. Matching funds were granted by the MBMG in supporting the work of geologic study and mapping conducted at MBMG.

  6. Temporal and spatial variability of ooid sand shoals: Comparison of Mississippian of Kentucky and Quaternary of Bahamas

    SciTech Connect (OSTI)

    Boardman, M.R. (Miami Univ., Oxford, OH (USA))

    1989-08-01

    An examination of the lithology and topography of Andros Island, Bahamas, reveals it is a Pleistocene ooid sand shoal. A comparison with Joulters Cays (a modern ooid sand shoal directly to the north) shows that much of the original depositional topography is preserved through at least one cycle of sea level highstand and lowstand. Both the Pleistocene and the Holocene ooid sand bodies are a few kilometers to tens of kilometers wide. The total vertical relief of a single episode of Quaternary ooid sand deposition is more than 10 m and includes accumulation in tidal channels, shallow flat areas, and eolian dunes. Today, much of Andros Island is within 2 m of present sea level and is the site of a belt several kilometers wide consisting of muddy tidal flat sediments overlying an exposure surface. The site of ooid sand deposition and shoal complex formation is not continuous along shorelines, especially windward margins, but shifts abruptly along the margins of platforms as a result of minor fluctuations of sea level. Thus, it should be expected that ooid sand shoals (ancient and modern) should be in direct lateral and vertical contact with lagoons, tidal flats, and reefs. The Mississippian Slade Formation contains many of the features of Quaternary ooid sand accumulation: abrupt vertical and lateral gradations between oolitic grainstones, packstones, and lime mudstones, vertical relief of individual oolitic sedimentary packages up to 30 m (perhaps with eolian dunes) and numerous exposure surfaces of varying intensities. These characteristics suggest that this formation represents a time of rapid fluctuations of relative sea level and abrupt shifts in the sites of ooid sand shoal complexes.

  7. Stability of submerged slopes on the flanks of the Hawaiian Islands, a simplified approach

    SciTech Connect (OSTI)

    Lee, H.J.; Torresan, M.E.; McArthur, W.

    1994-12-31

    Undersea transmission lines and shoreline AC-DC conversion stations and near-shore transmission lines are being considered as part of a system for transporting energy between the Hawaiian Islands. These facilities will need to be designed so that they will not be damaged or destroyed by coastal or undersea landslides. Advanced site surveys and engineering design of these facilities will require detailed site specific analyses, including sediment sampling and laboratory testing of samples, in situ testing of sediment and rock, detailed charting of bathymetry, and two- or three-dimensional numerical analyses of the factors of safety of the slopes against failure from the various possible loading mechanisms. An intermediate approximate approach can be followed that involves gravity and piston cores, laboratory testing and the application of simplified models to determine a seismic angle of repose for actual sediment in the vicinity of the planned facility. An even simpler and more approximate approach involves predictions of angles of repose using classification of the sediment along a proposed route as either a coarse volcaniclastic sand, a calcareous ooze, or a muddy terrigenous sediment. The steepest slope that such a sediment can maintain is the static angle of repose. Sediment may be found on slopes as steep as these, but it must be considered metastable and liable to fail in the event of any disturbance, storm or earthquake. The seismic angle of repose likely governs most slopes on the Hawaiian Ridge. This declivity corresponds to the response of the slope to a continuing seismic environment. As a long history of earthquakes affects the slopes, they gradually flatten to this level. Slopes that exceed or roughly equal this value can be considered at risk to fail during future earthquakes. Seismic and static angles of repose for three sediment types are tabulated in this report.

  8. Stevens and earlier miocene turbidite sandstones, southern San Joaquin Valley, California

    SciTech Connect (OSTI)

    Webb, G.W.

    1981-03-01

    A thick marine turbidite succession, dominantly coarse sandstone, underlies the southern part of the San Joaquin Valley. Sands are pebbly to fine grained, commonly poorly sorted, quartzose to arkosic, and are interbedded with dark shales bearing deep-water foraminifers. Graded bedding is common and, with the depths of 2000 to 6000 ft (610 to 1830 m) implied by the fauna, is taken to indicate a turbidity-current origin for most of the sands. The upper, middle, and lower Miocene turbidite section was revealed by extensive coring at Paloma, and is similar to the more widespread and oil and gas productive upper Miocene Stevens sandstone. The central-basin Stevens was deposited as channel sands on deep-sea fans derived from several discrete troughs or canyons on the eastern and southeastern margin of the basin prior to their burial by prograding Santa Margarita sand. Sand channels and lobes in the Bakersfield arch area were controlled locally by compaction structures. The rising Paloma anticline deflected Stevens sands for a time and the very last sands were guided also by incipient folds on the outer Bakersfield arch. Coarse Stevens conglomerates and sands shed from the emergent Temblor Range were deflected by the Buena Vista Hills, Elk Hills, and other anticlinal shoals and were deposited in intervening gaps as thick oil-productive channel sands. They merge with sands from the east side in flowing axially into the distal northwestern basin. Facies recognized in the subsurface include a meander-channel facies developed in the prograded muddy slope area upstream from the massive braided-sand facies.

  9. A real two-phase submarine debris flow and tsunami

    SciTech Connect (OSTI)

    Pudasaini, Shiva P.; Miller, Stephen A. [Department of Geodynamics and Geophysics, Steinmann Institute, University of Bonn Nussallee 8, D-53115, Bonn (Germany)

    2012-09-26

    The general two-phase debris flow model proposed by Pudasaini is employed to study subaerial and submarine debris flows, and the tsunami generated by the debris impact at lakes and oceans. The model, which includes three fundamentally new and dominant physical aspects such as enhanced viscous stress, virtual mass, and generalized drag (in addition to buoyancy), constitutes the most generalized two-phase flow model to date. The advantage of this two-phase debris flow model over classical single-phase, or quasi-two-phase models, is that the initial mass can be divided into several parts by appropriately considering the solid volume fraction. These parts include a dry (landslide or rock slide), a fluid (water or muddy water; e.g., dams, rivers), and a general debris mixture material as needed in real flow simulations. This innovative formulation provides an opportunity, within a single framework, to simultaneously simulate the sliding debris (or landslide), the water lake or ocean, the debris impact at the lake or ocean, the tsunami generation and propagation, the mixing and separation between the solid and fluid phases, and the sediment transport and deposition process in the bathymetric surface. Applications of this model include (a) sediment transport on hill slopes, river streams, hydraulic channels (e.g., hydropower dams and plants); lakes, fjords, coastal lines, and aquatic ecology; and (b) submarine debris impact and the rupture of fiber optic, submarine cables and pipelines along the ocean floor, and damage to offshore drilling platforms. Numerical simulations reveal that the dynamics of debris impact induced tsunamis in mountain lakes or oceans are fundamentally different than the tsunami generated by pure rock avalanches and landslides. The analysis includes the generation, amplification and propagation of super tsunami waves and run-ups along coastlines, debris slide and deposition at the bottom floor, and debris shock waves. It is observed that the submarine debris speed can be faster than the tsunami speed. This information can be useful for early warning strategies in the coastal regions. These findings substantially increase our understanding of complex multi-phase systems and multi-physics and flows, and allows for the proper modeling of landslide and debris induced tsunami, the dynamics of turbidity currents and sediment transport, and the associated applications to hazard mitigation, geomorphology and sedimentology.

  10. Fergusonite-type CeNbO{sub 4+?}: Single crystal growth, symmetry revision and conductivity

    SciTech Connect (OSTI)

    Bayliss, Ryan D. [Department of Materials, Imperial College London, Prince Consort Road, London, SW7 2BP (United Kingdom); Pramana, Stevin S.; An, Tao; Wei, Fengxia; Kloc, Christian L. [School of Materials Science and Engineering, 50 Nanyang Avenue, Nanyang Technological University, 639798 (Singapore); White, Andrew J.P. [Chemical Crystallography Laboratory, Department of Chemistry, Imperial College London, Exhibition Road, London, SW7 2AZ (United Kingdom); Skinner, Stephen J. [Department of Materials, Imperial College London, Prince Consort Road, London, SW7 2BP (United Kingdom); White, Timothy J. [School of Materials Science and Engineering, 50 Nanyang Avenue, Nanyang Technological University, 639798 (Singapore); Baikie, Tom, E-mail: tbaikie@ntu.edu.sg [School of Materials Science and Engineering, 50 Nanyang Avenue, Nanyang Technological University, 639798 (Singapore)

    2013-08-15

    Large fergusonite-type (ABO{sub 4}, A=Ce, B=Nb) oxide crystals, a prototype electrolyte composition for solid oxide fuel cells (SOFC), were prepared for the first time in a floating zone mirror furnace under air or argon atmospheres. While CeNbO{sub 4} grown in air contained CeNbO{sub 4.08} as a minor impurity that compromised structural analysis, the argon atmosphere yielded a single phase crystal of monoclinic CeNbO{sub 4}, as confirmed by selected area electron diffraction, powder and single crystal X-ray diffraction. The structure was determined in the standard space group setting C12/c1 (No. 15), rather than the commonly adopted I12/a1. AC impedance spectroscopy conducted under argon found that stoichiometric CeNbO{sub 4} single crystals showed lower conductivity compared to CeNbO{sub 4+?} confirming interstitial oxygen can penetrate through fergusonite and is responsible for the higher conductivity associated with these oxides. - Graphical abstract: Large fergusonite-type CeNbO{sub 4} crystals were prepared for the first time in a floating zone mirror furnace. Crystal growth in an argon atmosphere yielded a single phase monoclinic CeNbO4, as confirmed by selected area electron diffraction, powder and single crystal X-ray diffraction. The structure was determined in the standard space group setting C12/c1 (No. 15), rather than the commonly adopted I12/a1. AC impedance spectroscopy found CeNbO{sub 4} single crystals showed lower conductivity compared to CeNbO{sub 4+?} confirming interstitial oxygen can penetrate through fergusonite and is responsible for the higher conductivity associated with these oxides. Highlights: • Preparation of single crystals of CeNbO{sub 4} using a floating zone mirror furnace. • Correction to the crystal symmetry of the monoclinic form of CeNbO{sub 4}. • Report the conductivity of a single crystal of CeNbO{sub 4}.

  11. The Bakken-An Unconventional Petroleum and Reservoir System

    SciTech Connect (OSTI)

    Frederick Sarg

    2011-12-31

    An integrated geologic and geophysical study of the Bakken Petroleum System, in the Williston basin of North Dakota and Montana indicates that: (1) dolomite is needed for good reservoir performance in the Middle Bakken; (2) regional and local fractures play a significant role in enhancing permeability and well production, and it is important to recognize both because local fractures will dominate in on-structure locations; and (3) the organic-rich Bakken shale serves as both a source and reservoir rock. The Middle Bakken Member of the Bakken Formation is the target for horizontal drilling. The mineralogy across all the Middle Bakken lithofacies is very similar and is dominated by dolomite, calcite, and quartz. This Member is comprised of six lithofacies: (A) muddy lime wackestone, (B) bioturbated, argillaceous, calcareous, very fine-grained siltstone/sandstone, (C) planar to symmetrically ripple to undulose laminated, shaly, very fine-grained siltstone/sandstone, (D) contorted to massive fine-grained sandstone, to low angle, planar cross-laminated sandstone with thin discontinuous shale laminations, (E) finely inter-laminated, bioturbated, dolomitic mudstone and dolomitic siltstone/sandstone to calcitic, whole fossil, dolomitic lime wackestone, and (F) bioturbated, shaly, dolomitic siltstone. Lithofacies B, C, D, and E can all be reservoirs, if quartz and dolomite-rich (facies D) or dolomitized (facies B, C, E). Porosity averages 4-8%, permeability averages 0.001-0.01 mD or less. Dolomitic facies porosity is intercrystalline and tends to be greater than 6%. Permeability may reach values of 0.15 mD or greater. This appears to be a determinant of high productive wells in Elm Coulee, Parshall, and Sanish fields. Lithofacies G is organic-rich, pyritic brown/black mudstone and comprises the Bakken shales. These shales are siliceous, which increases brittleness and enhances fracture potential. Mechanical properties of the Bakken reveal that the shales have similar effective stress as the Middle Bakken suggesting that the shale will not contain induced fractures, and will contribute hydrocarbons from interconnected micro-fractures. Organic-rich shale impedance increases with a reduction in porosity and an increase in kerogen stiffness during the burial maturation process. Maturation can be directly related to impedance, and should be seismically mappable. Fractures enhance permeability and production. Regional fractures form an orthogonal set with a dominant NE-SW trend parallel to Ï?1, and a less prominent NW-SE trend. Many horizontal wells are drilled perpendicular to the Ï?1 direction to intersect these fractures. Local structures formed by basement tectonics or salt dissolution generate both hinge parallel and hinge oblique fractures that may overprint and dominate the regional fracture signature. Horizontal microfractures formed by oil expulsion in the Bakken shales, and connected and opened by hydrofracturing provide permeability pathways for oil flow into wells that have been hydro-fractured in the Middle Bakken lithofacies. Results from the lithofacies, mineral, and fracture analyses of this study were used to construct a dual porosity Petrel geo-model for a portion of the Elm Coulee Field. In this field, dolomitization enhances reservoir porosity and permeability. First year cumulative production helps locate areas of high well productivity and in deriving fracture swarm distribution. A fracture model was developed based on high productivity well distribution, and regional fracture distribution, and was combined with favorable matrix properties to build a dual porosity geo-model.

  12. The Bakken - An Unconventional Petroleum and Reservoir System

    SciTech Connect (OSTI)

    Sarg, J.

    2011-12-31

    An integrated geologic and geophysical study of the Bakken Petroleum System, in the Williston basin of North Dakota and Montana indicates that: (1) dolomite is needed for good reservoir performance in the Middle Bakken; (2) regional and local fractures play a significant role in enhancing permeability and well production, and it is important to recognize both because local fractures will dominate in on-structure locations; and (3) the organic-rich Bakken shale serves as both a source and reservoir rock. The Middle Bakken Member of the Bakken Formation is the target for horizontal drilling. The mineralogy across all the Middle Bakken lithofacies is very similar and is dominated by dolomite, calcite, and quartz. This Member is comprised of six lithofacies: (A) muddy lime wackestone, (B) bioturbated, argillaceous, calcareous, very fine-grained siltstone/sandstone, (C) planar to symmetrically ripple to undulose laminated, shaly, very fine-grained siltstone/sandstone, (D) contorted to massive fine-grained sandstone, to low angle, planar cross-laminated sandstone with thin discontinuous shale laminations, (E) finely inter-laminated, bioturbated, dolomitic mudstone and dolomitic siltstone/sandstone to calcitic, whole fossil, dolomitic lime wackestone, and (F) bioturbated, shaly, dolomitic siltstone. Lithofacies B, C, D, and E can all be reservoirs, if quartz and dolomite-rich (facies D) or dolomitized (facies B, C, E). Porosity averages 4-8%, permeability averages 0.001-0.01 mD or less. Dolomitic facies porosity is intercrystalline and tends to be greater than 6%. Permeability may reach values of 0.15 mD or greater. This appears to be a determinant of high productive wells in Elm Coulee, Parshall, and Sanish fields. Lithofacies G is organic-rich, pyritic brown/black mudstone and comprises the Bakken shales. These shales are siliceous, which increases brittleness and enhances fracture potential. Mechanical properties of the Bakken reveal that the shales have similar effective stress as the Middle Bakken suggesting that the shale will not contain induced fractures, and will contribute hydrocarbons from interconnected micro-fractures. Organic-rich shale impedance increases with a reduction in porosity and an increase in kerogen stiffness during the burial maturation process. Maturation can be directly related to impedance, and should be seismically mappable. Fractures enhance permeability and production. Regional fractures form an orthogonal set with a dominant NE-SW trend, and a less prominent NW-SE trend. Many horizontal 1 direction to intersect these fractures. Local structures formed by basement tectonics or salt dissolution generate both hinge parallel and hinge oblique fractures that may overprint and dominate the regional fracture signature. Horizontal microfractures formed by oil expulsion in the Bakken shales, and connected and opened by hydrofracturing provide permeability pathways for oil flow into wells that have been hydro-fractured in the Middle Bakken lithofacies. Results from the lithofacies, mineral, and fracture analyses of this study were used to construct a dual porosity Petrel geo-model for a portion of the Elm Coulee Field. In this field, dolomitization enhances reservoir porosity and permeability. First year cumulative production helps locate areas of high well productivity and in deriving fracture swarm distribution. A fracture model was developed based on high productivity well distribution, and regional fracture distribution, and was combined with favorable matrix properties to build a dual porosity geo-model.

  13. Scale-Up of Palladium Powder Production Process for Use in the Tritium Facility at Westinghouse, Savannah River, SC/Summary of FY99-FY01 Results for the Preparation of Palladium Using the Sandia/LANL Process

    SciTech Connect (OSTI)

    David P. Baldwin; Daniel S. Zamzow; R. Dennis Vigil; Jesse T. Pikturna

    2001-08-24

    Palladium used at Savannah River (SR) for process tritium storage is currently obtained from a commercial source. In order to understand the processes involved in preparing this material, SR is supporting investigations into the chemical reactions used to synthesize this material. The material specifications are shown in Table 1. An improved understanding of the chemical processes should help to guarantee a continued reliable source of Pd in the future. As part of this evaluation, a work-for-others contract between Westinghouse Savannah River Company and Ames Laboratory (AL) was initiated. During FY98, the process for producing Pd powder developed in 1986 by Dan Grove of Mound Applied Technologies, USDOE (the Mound muddy water process) was studied to understand the processing conditions that lead to changes in morphology in the final product. During FY99 and FY00, the process for producing Pd powder that has been used previously at Sandia and Los Alamos National Laboratories (the Sandia/LANL process) was studied to understand the processing conditions that lead to changes in the morphology of the final Pd product. During FY01, scale-up of the process to batch sizes greater than 600 grams of Pd using a 20-gallon Pfaudler reactor was conducted by the Iowa State University (ISU) Chemical Engineering Department. This report summarizes the results of FY99-FY01 Pd processing work done at AL and ISU using the Sandia/LANL process. In the Sandia/LANL process, Pd is dissolved in a mixture of nitric and hydrochloric acids. A number of chemical processing steps are performed to yield an intermediate species, diamminedichloropalladium (Pd(NH{sub 3}){sub 2}Cl{sub 2}, or DADC-Pd), which is isolated. In the final step of the process, the Pd(NH{sub 3}){sub 2}Cl{sub 2} intermediate is subsequently redissolved, and Pd is precipitated by the addition of a reducing agent (RA) mixture of formic acid and sodium formate. It is at this point that the morphology of the Pd product is determined. During FY99 and FY00, a study of how the characteristics of the Pd are affected by changes in processing conditions including the RA/Pd molar ratio, Pd concentration, mole fraction of formic acid (mf-FA) in the RA solution, reaction temperature, and mixing was performed. These parameters all had significant effects on the resulting values of the tap density (TD), BET surface area (SA), and Microtrac particle size (PS) distribution for the Pd samples. These effects were statistically modeled and fit in order to determine ranges of predicted experimental conditions that resulted in material that meets the requirements for the Pd powder to be used at SR. Although not statistically modeled, the method and rate of addition of the RA and the method and duration of stirring were shown to be significant factors affecting the product morphology. Instead of producing an additional statistical fit and due to the likely changes anticipated during scale-up of this processing procedure, these latter conditions were incorporated into a reproducible practical method of synthesis. Palladium powder that met the SR specifications for TD, BET SA, and Microtrac PS was reliably produced at batch sizes ranging from 25-100 grams. In FY01, scale-up of the Sandia/LANL process was investigated by the ISU Chemical Engineering Department for the production of 600-gram batches of Pd. Palladium that meets the SR specifications for TD, BET SA, and Microtrac PS has been produced using the Pfaudler reactor, and additional processing batches will be done during the remainder of FY01 to investigate the range of conditions that can be used to produce Pd powder within specifications. Palladium product samples were analyzed at AL and SR to determine TD and at SR to determine BET SA, Microtrac PS distribution, and Pd nodule size and morphology by scanning electron microscopy (SEM).