Petrophysical properties of saprolites from the Oak Ridge Integrated Field Research Challenge site, Tennessee

Journal Article · Tue Jan 01 04:00:00 EST 2013 · Geophysics

DOI:https://doi.org/10.1190/geo2012-0176.1· OSTI ID:1059917

Revil, André ^[1]; Skold, Magnus ^[2]; Hubbard, Susan S. ^[3]; Wu, Yuxin ^[3]; Watson, David B. ^[4]; Karaoulis, Marios ^[2]

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1. Université de Savoie, ISTerre, Le Bourget du Lac, France; Colorado School of Mines, Department of Geophysics, Golden, Colorado, USA..; Colorado School of Mines
2. Colorado School of Mines, Department of Geophysics, Golden, Colorado, USA..
3. Lawrence Berkeley National Laboratory, Berkeley, California, USA..
4. Oak Ridge National Laboratory, Oak Ridge, Tennessee, USA..

At the Oak Ridge Integrated Field Research Challenge site, near Oak Ridge, Tennessee, the shallow saprolitic aquifer is contaminated by nitric acid, uranium, and metals originating from the former S3 settling ponds. To interpret low-frequency geophysical methods used to image contaminant plumes, we have characterized the petrophysical properties of three representative saprolite core samples. Their hydraulic conductivity ranges from [Formula: see text] to [Formula: see text] in agreement with field data. Complex conductivity measurements, in the frequency range of 1 mHz to 45 kHz, were performed with NaCl solutions with electrical conductivities in the range [Formula: see text] to [Formula: see text], a range representative of field conditions. The electrical conductivity data were well reproduced with a simple linear conductivity model between the saprolite conductivity and the pore water conductivity. The conductivity plots were used to estimate the formation factor (the cementation exponent was about [Formula: see text]) and the surface conductivity ([Formula: see text]). The magnitude of the surface conductivity depended on the degree of weathering and therefore on the amount of smectite and mixed layer (illite-smectite) clays present in the saprolite. The chargeability of the core samples was in the range of [Formula: see text] and is strongly dependent on the salinity. We also performed streaming potential measurements with the same pore fluid composition as that used for the complex conductivity measurements. We found an excess of movable electrical charges on the order of 100 to [Formula: see text] in agreement with previous investigations connecting the movable excess charge density to permeability. The zeta potential was in the range of [Formula: see text] to [Formula: see text] independent on the salinity. The electrical measurements were consistent with an average cation exchange capacity in the range of 1.4 to [Formula: see text] and a specific surface area on the order of 4000 to about 30,000 [Formula: see text].

• Research Organization: Colorado School of Mines, Golden, CO (United States)
• Sponsoring Organization: USDOE CI Office of Environment and Science (CI-40)
• DOE Contract Number: FG02-08ER64659
• OSTI ID: 1059917
• Report Number(s): 13
• Journal Information: Geophysics, Journal Name: Geophysics Journal Issue: 1 Vol. 78; ISSN 0016-8033
• Publisher: Society of Exploration Geophysicists
• Country of Publication: United States
• Language: English

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54 ENVIRONMENTAL SCIENCES