Quantification of ground-water flow in fractured rock, Oak Ridge, Tennessee

Ground Water

Volumn 35, Issue 3, 1997, Pages 478-482

  Moore, Gerald K ^a  

^a Tennessee Division of Forestry   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

AQUIFERS; DATA REDUCTION; DISCHARGE (FLUID MECHANICS); FRACTURE; HYDROGRAPHIC SURVEYS; RECHARGING (UNDERGROUND WATERS); ROCKS; STREAM FLOW; WATER WELL PUMPS;

GROUNDWATER DISCHARGES;

GROUNDWATER FLOW;

GASTROPODA; QUERCUS;

EID: 0031149770     PISSN: 0017467X     EISSN: None     Source Type: Journal    
DOI: 10.1111/j.1745-6584.1997.tb00108.x     Document Type: Article

References (19)

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2. Bouwer, H. and R. C. Rice. 1976. A slug test for determining hydraulic conductivity of unconfined aquifers with completely or partially penetrating wells. Water Resour. Res. v. 12, no. 3, pp. 423-428.
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12. Moore, G. K. 1992. Supplement to a hydrologic framework for the Oak Ridge Reservation, Oak Ridge, Tennessee, With a Summary of ground-water modeling by L. E. Toran. Oak Ridge National Laboratory, Oak Ridge, TN. ORNL/TM-12191.
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14. Rorabaugh, M. I. 1960. Use of water levels in estimating aquifer constants. In: Intern. Assoc. of Scientific Hydrology Proceedings, General Assembly of Helsinki. Pub. no. 52, pp. 314-323.
15. Shevenell, L. A., G. K. Moore, and R. B. Dreier. 1994. Contaminant spread and flushing in fractured rocks near Oak Ridge, Tennessee. Ground Water Monitoring and Remediation, v. 14, no. 2, pp. 120-129.
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