2016
DOI: 10.18520/cs/v111/i3/524-534
|View full text |Cite
|
Sign up to set email alerts
|

Estimation of Aquifer Parameters from Surfacial Resistivity Measurement in a Granitic Area in Tamil Nadu

Abstract: This article aims to establish an empirical relationship among geoelectrical properties of aquifer and hydrogeological parameters to estimate its hydraulic properties, and reduce the processes of pumping test, which are costly and time consuming. A total of 19 Vertical Electrical Sounding (VES) data were collected using Schlumberger configuration in a granitic terrain in Tamil

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
1
0

Year Published

2017
2017
2021
2021

Publication Types

Select...
3
2

Relationship

0
5

Authors

Journals

citations
Cited by 6 publications
(1 citation statement)
references
References 14 publications
0
1
0
Order By: Relevance
“…T values vary from 15 to 200 m 2 /day, whereas S values from 0.0000225 to 0.00095. Aquifer transmissivity is proportional to hydraulic conductivity (K), which is best defined as an exponential function of aquifer resistivity (Mondal et al 2016a). Therefore, the calculated T values were directly used to prepare transmissivity map of the study area.…”
Section: Data Collectionmentioning
confidence: 99%
“…T values vary from 15 to 200 m 2 /day, whereas S values from 0.0000225 to 0.00095. Aquifer transmissivity is proportional to hydraulic conductivity (K), which is best defined as an exponential function of aquifer resistivity (Mondal et al 2016a). Therefore, the calculated T values were directly used to prepare transmissivity map of the study area.…”
Section: Data Collectionmentioning
confidence: 99%