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| Unsaturated-Zone Hydrochemistry | ||
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A thorough understanding of hydrochemical processes in the unsaturated zone is important in characterizing the potential and time for water to infiltrate from the surface to the water table at Yucca Mountain. Several milliliters of water contained in the pores of the volcanic rocks (pore water) at Yucca Mountain were extracted from volcanic samples at Yucca Mountain and analyzed:
Methods of extracting pore water from rock samples |
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Ultracentrifuge Method: Approximately 150 to 200 grams of core rubble is loaded into three titanium cups which are attached to a rotor and spun for 6 hours at 15,000 revolutions per minute. Depending on the moisture content of the rock, 0.5 to 3 millilters of pore water were extracted. |
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Uniaxial Compression Method: Approximately 400 to 900 grams of core or rubble are loaded into the compression cell. Pressure is applied with progressive loading of the samples to a stress level of 827 megapascals to extract the pore water. |
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Yang, I.C., Turner, A.K., Sayre, T.M, and Montazer, Parvis, 1988, Triaxial-compression extraction of pore water from unsaturated tuff, Yucca Mountain, Nevada: U.S. Geological Survey Water-Resources Investigations Report 88-4189, 68 p. Mower, T.E., Higgins, J.D., Yang, I.C., and Peters, C.A., 1994, Pore-water extraction from unsaturated tuff by triaxial and one-dimensional compression methods, Nevada Test Site: U.S. Geological Survey Water-Resources Investigations Report 93-4144, |
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