Recharge pathways and rates for a sand aquifer beneath a loess-mantled landscape in western Tennessee, U.S.A.

Author:

Larsen Daniel,Bursi John,Waldron Brian,Schoefernacker Scott,Eason James

Funder

University of Memphis Ground Water Institute

U.S. Geological Survey Water Resources Research Center

Presbytery of the Mid-South Pinecrest Camp

Publisher

Elsevier BV

Subject

Earth and Planetary Sciences (miscellaneous),Water Science and Technology

Reference90 articles.

1. The ASCE standardized reference evapotranspiration equation;Allen;ASCE Am. Soc. Civil Eng.,2005

2. The use of environmental chloride and tritium to estimate total recharge to an unconfined aquifer;Allison;Aust. J. Soil Res.,1978

3. The use of natural tracers as indicators of soil-water movement in a temperate semi-arid region;Allison;J. Hydrol.,1983

4. Ground-water flow analysis of the Mississippi Embayment aquifer system, South-Central United States;Arthur,1998

5. Hydrology of the Jackson, Tennessee, area and delineation of areas contributing ground water to the Jackson well fields;Bailey,1993

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