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Published online 20 November 2007
Published in Vadose Zone J 6:906-912 (2007)
DOI: 10.2136/vzj2006.0175
© 2007 Soil Science Society of America
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Standardization of Borehole Data to Support Vadose Zone Flow and Transport Modeling

G. V. Lasta,*, C. J. Murraya, D. A. Bushb, E. C. Sullivana, M. L. Rockholda, R. D. Mackleya and B. N. Bjornstada

a Environmental Technology Division, Pacific Northwest National Lab., P.O. Box 999, Richland, WA 99352
b Geologic Consulting, Stevensville, MT 59870

Figure 1
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  		FIG. 1. Location of the Hanford Site and geologic elements of the Pasco Basin in eastern Washington (from Cannon et al., 2005).

 

Figure 2
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  		FIG. 2. Site-specific lithofacies and hydrofacies construction (after Bush et al., 2005).

 

Figure 3
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  		FIG. 3. Outcrop studies (such as this one at Pit 30, near the center of the Hanford Site) provide information on inter- and intrafacies heterogeneity, including the lateral continuity of lithofacies, and lithofacies associations within and between sedimentary packages.

 

Figure 4
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  		FIG. 4. Example of three-dimensional geostatistical models representing site-specific lithofacies models. (A) Lithofacies simulation with maximum sandy gravel facies; (B) simulation with maximum silty sand facies; and (C) most probable lithofacies, based on mode of 100 simulations. (sG, sandy gravel; gS, gravelly sand; cS, coarse sand; fS, fine sand; mS, silty sand.)

 




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