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ESTIMATING TRANSMISSIVITY AND HYDRAULIC CONDUCTIVITY OF CHICOT AQUIFER FROM SPECIFIC CAPACITY DATA1

 

作者: G. N. Rao,   J. N. Beck,   H. E. Murray,   D. J. Nyman,  

 

期刊: JAWRA Journal of the American Water Resources Association  (WILEY Available online 1991)
卷期: Volume 27, issue 1  

页码: 47-58

 

ISSN:1093-474X

 

年代: 1991

 

DOI:10.1111/j.1752-1688.1991.tb03112.x

 

出版商: Blackwell Publishing Ltd

 

关键词: ground water;aquifer;transmissivity;hydraulic conductivity;specific capacity

 

数据来源: WILEY

 

摘要:

ABSTRACT:Specific capacity data obtained from Well Construction reports which are available from USGS offices, can provide useful estimates of tranamissivity (T), and hydraulic conductivity (K), of an aquifer. The Chicot Aquifer in Louisiana is one of the largest sources of fresh ground water in North America. Hydrologic data collected for the Chicot Aquifer indicate that specific capacity tests can be used in estimating local and regional values for T and K, if the Cooper‐Jacob equation for transient flow is used with proper corrections for well loss and partial penetration. Where full scale pumping test data are scarce, specific capacity test data that are adequately distributed spatially can be used to map changes in T and K values and can be summarized statistically to indicate applicable regional values. A computer program called “TGUESS” which is available from International Ground Water Modeling Center, Holcomb Research Institute, was used in this study. The contour maps for T and K values are prepared for different well depth intervals to avoid wide variation of v

 

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