2019
DOI: 10.1016/j.gexplo.2018.09.013
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Hydrochemistry in integration with stable isotopes (δ18O and δD) to assess seawater intrusion in coastal aquifers of Kachchh district, Gujarat, India

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Cited by 89 publications
(30 citation statements)
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“…δ 18 O isotopic dissimilarity and allocation in groundwater samples of this area signifies that the quality of groundwater within this region is highly diverse as well as intricate due to influence of SWI, inherent sediment salinity, over-exploitation, and pollution. Stable isotopic study was conducted to assess SWI in coastal aquifers of Kachchh district [107]. According to the hydrochemical study, majority of the samples indicated NaCl type of facies.…”
Section: Seawater Intrusion In Gujaratmentioning
confidence: 99%
“…δ 18 O isotopic dissimilarity and allocation in groundwater samples of this area signifies that the quality of groundwater within this region is highly diverse as well as intricate due to influence of SWI, inherent sediment salinity, over-exploitation, and pollution. Stable isotopic study was conducted to assess SWI in coastal aquifers of Kachchh district [107]. According to the hydrochemical study, majority of the samples indicated NaCl type of facies.…”
Section: Seawater Intrusion In Gujaratmentioning
confidence: 99%
“…Studies on surface and groundwater monitoring with respect to WQI has been done by various [17][18][19] Water chemistry is constrained by various hidden factors related to natural and anthropogenic in uences that are hard to comprehend and decipher signi cant data using simple techniques [20,21]. Therefore, in addition to the WQI and hydro geochemical analysis, the multivariate statistical approaches were used to understand complex information grids of water quality for e cient management and identi cation of effective solutions to pollution problems [22][23].…”
Section: Introductionmentioning
confidence: 99%
“…So, the studies of the identification origin of groundwater are of great importance in hydrology and hydrogeology (Nair et al 2015;Seddique et al 2019) With the ever-increasing industrial development and increasing population, it becomes necessary to use advanced techniques alongside classical investigations to develop and use water resources efficiently and sustainably. Isotope hydrology is at the top of these techniques, and stable isotopes of oxygen-18 (δ 18 O) and hydrogen (δ 2 H) are frequently used to identify the origins of groundwater (Jayathunga et al 2020;Maurya et al 2019). The δ 18 O and δ 2 H, among the environmental isotopes, are good tracers as they are natural water components.…”
Section: Introductionmentioning
confidence: 99%