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Title Comparing geophysical measurements to theoretical estimates for soil mixtures at low pressures
Creator/Author Wildenschild, D ; Berge, P A ; Berryman, K G ; Bonner, B P ; Roberts, J J
Publication Date1999 Jan 15
OSTI IdentifierOSTI ID: 8169
Report Number(s)UCRL-JC-132893; EW45100000
DOE Contract NumberW-7405-ENG-48
Other Number(s)Other: EW45100000; TRN: AH200117%%122
Resource TypeConference
Resource RelationConference: Environmental and Engineering Geophysical Society Symposium on the Application of Geophysics to Engineering and Environmental Problems, Oakland, CA (US), 03/14/1999--03/18/1999; Other Information: PBD: 15 Jan 1999
Research OrgLawrence Livermore National Lab., CA (US)
Sponsoring OrgUSDOE Office of Environmental Management (EM) (US)
Subject01 COAL, LIGNITE, AND PEAT; 58 GEOSCIENCES; ALGORITHMS; GEOPHYSICS; MICROSTRUCTURE; MIXTURES; PEAT; QUARTZ; REFINING; SAND; SOILS; VELOCITY
Description/AbstractThe authors obtained good estimates of measured velocities of sand-peat samples at low pressures by using a theoretical method, the self-consistent theory of Berryman (1980), using sand and porous peat to represent the microstructure of the mixture. They were unable to obtain useful estimates with several other theoretical approaches, because the properties of the quartz, air and peat components of the samples vary over several orders of magnitude. Methods that are useful for consolidated rock cannot be applied directly to unconsolidated materials. Instead, careful consideration of microstructure is necessary to adapt the methods successfully. Future work includes comparison of the measured velocity values to additional theoretical estimates, investigation of Vp/Vs ratios and wave amplitudes, as well as modeling of dry and saturated sand-clay mixtures (e.g., Bonner et al., 1997, 1998). The results suggest that field data can be interpreted by comparing laboratory measurements of soil velocities to theoretical estimates of velocities in order to establish a systematic method for predicting velocities for a full range of sand-organic material mixtures at various pressures. Once the theoretical relationship is obtained, it can be used to estimate the soil composition at various depths from field measurements of seismic velocities. Additional refining of the method for relating velocities to soil characteristics is useful for development inversion algorithms.
Country of PublicationUnited States
LanguageEnglish
FormatMedium: ED; Size: 971 Kilobytes pages
System Entry Date2008 Feb 04
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