Delineation of groundwater Potential and recharge zone using electrical resistivity method around veeranam tank, Tamil Nadu, India (Record no. 8525)

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000 -LEADER
fixed length control field a
003 - CONTROL NUMBER IDENTIFIER
control field OSt
005 - DATE AND TIME OF LATEST TRANSACTION
control field 20190315145012.0
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 190315b xxu||||| |||| 00| 0 eng d
040 ## - CATALOGING SOURCE
Original cataloging agency AIKTC-KRRC
Transcribing agency AIKTC-KRRC
100 ## - MAIN ENTRY--PERSONAL NAME
9 (RLIN) 8055
Author Sathiyamoorthy, Mahenthiran
245 ## - TITLE STATEMENT
Title Delineation of groundwater Potential and recharge zone using electrical resistivity method around veeranam tank, Tamil Nadu, India
250 ## - EDITION STATEMENT
Volume, Issue number Vol. 99(4), December
260 ## - PUBLICATION, DISTRIBUTION, ETC.
Place of publication, distribution, etc. Kolkata
Name of publisher, distributor, etc. Springer
Year 2018
300 ## - PHYSICAL DESCRIPTION
Pagination 637-645p.
520 ## - SUMMARY, ETC.
Summary, etc. Veeranam tank is one of the largest tank in Tamil Nadu, India which plays a vital role in groundwater recharge to the surrounding aquifer. Electrical resistivity survey were carried out in ten locations around the Veeranam tank. The resistivity, thickness of subsurface formations, longitudinal conductance (S), transverse resistance (R), average longitudinal resistivity (ST), average transverse resistivity (RT) and anisotropy (λ) were used to characterize the lithological formations and also groundwater potential and recharge zones were delineated. The four major zones clay, clayey sand, saline sand and sandstone were identified as a result of primary geo-electrical parameters which includes resistivity and thickness of the formations. The sandstone formation is identified as good water bearing formation and this formation possess low longitudinal conductance, high transverse resistance, and low anisotropy values. The clay and saline formation possess high longitudinal conductance, low transverse resistance and high anisotropy values and these formations are identified as moderate groundwater water bearing formations. High longitudinal conductance is observed in eastern region of the study area due to intrusion of saline water. Sandstone formation of low longitudinal conductance is associated with high percolation rate and groundwater potential is also good in this formation. High transverse resistance zones are associated with high infiltration rate and high transmissivity whereas groundwater potential is good in these zones. VES 2 and VES 3 stations comprises of sandstone formation as second layer and Veeranam tank water infiltrated into these zones due to high infiltration rate of these formations. The resistivity value is decreased in VES 10 station due to intrusion of sea water. The true resistivity near the Veeranam tank is high and decreases towards east which clearly indicates that groundwater recharge is the major process that occurs nearby the downstream shore of tank and intrusion of saline water in the eastern part of the study area. Thus good interaction between exists between Veeranam tank and its downstream zones and interaction decreases as the distance increases from the tank.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
9 (RLIN) 4621
Topical term or geographic name entry element Civil Engineering
700 ## - ADDED ENTRY--PERSONAL NAME
9 (RLIN) 8056
Co-Author Ganesan, Madhavi
773 0# - HOST ITEM ENTRY
International Standard Serial Number 2250-2149
Title Journal of the institution of engineers (India) Series A
Place, publisher, and date of publication Dordrecht Springer
856 ## - ELECTRONIC LOCATION AND ACCESS
URL https://link.springer.com/article/10.1007/s40030-018-0318-3
Link text Click here
942 ## - ADDED ENTRY ELEMENTS (KOHA)
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    Dewey Decimal Classification     School of Engineering & Technology School of Engineering & Technology Archieval Section 29/03/2019   2018207 10/06/2019 29/03/2019 Articles Abstract Database
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