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Delineation of groundwater-bearing fracture zones in a hard rock area integrating very low frequency electromagnetic and resistivity data

Delineation of groundwater-bearing fracture zones in a hard rock area integrating very low frequency electromagnetic and resistivity data
Delineation of groundwater-bearing fracture zones in a hard rock area integrating very low frequency electromagnetic and resistivity data
Integrated electrical and electromagnetic surveys were carried out in hard rock areas of Purulia district (West Bengal), India, for delineation of groundwater-bearing zones that would be suitable for construction of deep tube-wells for large amounts of water. Groundwater movement that occurs through fractures in hard rocks is suitable to be delineated by very low frequency (VLF) electromagnetic surveys. A detailed survey of the area was done using a VLF-WADI instrument and appropriate locations were selected for further study using Schlumberger resistivity sounding. Hence, the entire area was surveyed in a relatively short time by the combined use of resistivity and electromagnetic surveys. Areas showing VLF anomalies may or may not be appropriate for drilling tube-wells. In the northern part of the area, fracture zones are shallow, as exhibited by the small magnitude of VLF anomalies and by shallow conducting structures interpreted from the resistivity data. A VLF survey and subsequent resistivity sounding at suitable locations suggest the existence of deep groundwater sources in the southern part of the area. VLF anomalies have shown larger magnitudes in the southern part of the area than those in the northern part of the area. Self-potential and resistivity profiling data also showed correlation with results obtained using VLF and resistivity sounding. A typical variation in self-potential (SP) anomaly, i.e. positive SP anomaly for low resistivity, was observed near the locations found suitable and could be interpreted as the result of potential developed due to streaming of fluid within the fractured rocks.
Groundwater exploration, Hard rock areas, Integrated interpretation, VLF electromagnetic method, Resistivity method, Self-potential
0926-9851
155-166
Sharma, S.P.
a9b45063-287a-46ee-8289-c40a514dab5f
Baranwal, V.C.
db5192cf-b2b5-4eef-aadf-4720b5a8d8ca
Sharma, S.P.
a9b45063-287a-46ee-8289-c40a514dab5f
Baranwal, V.C.
db5192cf-b2b5-4eef-aadf-4720b5a8d8ca

Sharma, S.P. and Baranwal, V.C. (2006) Delineation of groundwater-bearing fracture zones in a hard rock area integrating very low frequency electromagnetic and resistivity data. Journal of Applied Geophysics, 57 (2), 155-166. (doi:10.1016/j.jappgeo.2004.10.003).

Record type: Article

Abstract

Integrated electrical and electromagnetic surveys were carried out in hard rock areas of Purulia district (West Bengal), India, for delineation of groundwater-bearing zones that would be suitable for construction of deep tube-wells for large amounts of water. Groundwater movement that occurs through fractures in hard rocks is suitable to be delineated by very low frequency (VLF) electromagnetic surveys. A detailed survey of the area was done using a VLF-WADI instrument and appropriate locations were selected for further study using Schlumberger resistivity sounding. Hence, the entire area was surveyed in a relatively short time by the combined use of resistivity and electromagnetic surveys. Areas showing VLF anomalies may or may not be appropriate for drilling tube-wells. In the northern part of the area, fracture zones are shallow, as exhibited by the small magnitude of VLF anomalies and by shallow conducting structures interpreted from the resistivity data. A VLF survey and subsequent resistivity sounding at suitable locations suggest the existence of deep groundwater sources in the southern part of the area. VLF anomalies have shown larger magnitudes in the southern part of the area than those in the northern part of the area. Self-potential and resistivity profiling data also showed correlation with results obtained using VLF and resistivity sounding. A typical variation in self-potential (SP) anomaly, i.e. positive SP anomaly for low resistivity, was observed near the locations found suitable and could be interpreted as the result of potential developed due to streaming of fluid within the fractured rocks.

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More information

Published date: February 2006
Keywords: Groundwater exploration, Hard rock areas, Integrated interpretation, VLF electromagnetic method, Resistivity method, Self-potential

Identifiers

Local EPrints ID: 48879
URI: http://eprints.soton.ac.uk/id/eprint/48879
ISSN: 0926-9851
PURE UUID: 43130a42-852d-4c89-aeb6-f54f94f8974d

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Date deposited: 16 Oct 2007
Last modified: 15 Mar 2024 09:51

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Contributors

Author: S.P. Sharma
Author: V.C. Baranwal

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