1D geoelectrical resistivity survey for groundwater studies in coastal area: A case study from Pearl city, Tamil Nadu
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- 作者：S. Selvam
- 关键词：VES ; Schlumberger electrode ; WINSEV ; Sandy Shell limestone ; Water ; bearing formation ; Tamil Nadu
- 刊名：Journal of the Geological Society of India
- 出版年：2016
- 出版时间：February 2016
- 年：2016
- 卷：87
- 期：2
- 页码：169-178
- 全文大小：1,869 KB
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1. Department of Geology, V.O. Chidambaram College, Tuticorin, 628 008, India - 刊物类别：Earth and Environmental Science
- 刊物主题：Geology
Geosciences
Geography
Mineralogy - 出版者：Springer India, co-published with Geological Society of India
- ISSN：0974-6889
文摘
Geoelectrical resistivity method involving vertical electrical sounding (VES) was carried out in a sedimentary environment to determine the suitability of the method for sub-surface groundwater investigations. The EC and TDS hydrochemical data in the study area clearly showed the influence of seawater intrusion. The abundance of the major cations and anions are in the following order, Na+ > Ca2+ > Mg 2+ > K+ = Cl- > HCO3 - > SO4 2- > CO3 > NO3 > PO4. Results suggest that the groundwater in this study area is very hard and alkaline in nature. As indicated by Piper trilinear diagram, NaCl and Ca2+ - Mg2+–Cl- - SO4 2- facies are the dominant hydrochemical facies in the groundwater of Pearl city. The VES method by Schlamberger electrode array was applied in 12 locations, which is expected to represent the whole area. The resistivity meter (aquameter CRM 5OO) was used to collect the VES data by employing a Schlumberger electrode configuration, with half current electrode spacing (AB/2) ranging from 2 to 180 m and the potential electrode (MN) from 1 to 50 m. The resistivity data is then interpreted by WINSEV 1-D inversion program geoelectric software to entirely describe the aquifer system as well as the occurrence of groundwater. The outputs of sub-surface layers with resistivities and thickness presented in contour maps and 2-D views by using SURFER software were created. Accordingly, three zones with different resistivity values were detected, corresponding to three different formations: (1) a transition zone of sandy soil (aeolian deposits) thick formation, (2) strata’s saturated with fresh groundwater in the east disturbed by the presence of sandy shell limestone horizons, (3) a water-bearing formation in the west containing low saltwater horizons. The bedrock is encountered at an average depth of 95m. This study indicates that the groundwater reservoirs are mainly confined to the alluvial aquifer.