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Monitoring of TDS and conductivity in groundwater in the seismically active region in NW Himalayas,India
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作者 Arvind Kumar Surinder Singh +3 位作者 Bikramjit Singh Bajwa sandeep mahajan Rajeev Kalia Sunil Dhar 《Earthquake Science》 CSCD 2010年第3期295-299,共5页
The earthquake precursors and earthquake prediction are the burning issue among the community of earth scientists and engineers. Studies of earthquake precursory phenomena since the last several decades have shown tha... The earthquake precursors and earthquake prediction are the burning issue among the community of earth scientists and engineers. Studies of earthquake precursory phenomena since the last several decades have shown that significant geophysical and geochemical changes may occur prior to intermediate and large earthquakes (Hartmann and Levy, 2005; Yang et al, 2005; Einarsson et al, 2008; Italiano et al, 2008; Kumar et al, 2009). Among the more intensely investigated geochemical phenomena there have been changes in the concentrations of dissolved ions and gases in groundwater as well as variations in the concentrations of crustal and mantle volatiles in ground gases. 展开更多
关键词 TDS (total dissolved solids) CONDUCTIVITY earthquake precursor NW Himalayas
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