2019
DOI: 10.1016/j.jhydrol.2019.01.077
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Seasonal-to-diurnal scale isotopic signatures of tidally-influenced submarine groundwater discharge to the Bay of Bengal: Control of hydrological cycle on tropical oceans

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Cited by 19 publications
(2 citation statements)
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“…Groundwater is rich in these isotopes relative to seawater (Burnett et al, 2006). In addition, their different half-lives allow tracing processes that occur at different time scales and provide information on groundwater fluxes (Michael et al, 2011;Kiro et al, 2013;Rodellas et al, 2017;Tamborski et al, 2017;Debnath et al, 2019;Yi et al, 2019, Diego-Feliu et al, 2021. Given that 222 Rn is an inert gas and thus not influenced by the physicochemistry of coastal groundwater (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…Groundwater is rich in these isotopes relative to seawater (Burnett et al, 2006). In addition, their different half-lives allow tracing processes that occur at different time scales and provide information on groundwater fluxes (Michael et al, 2011;Kiro et al, 2013;Rodellas et al, 2017;Tamborski et al, 2017;Debnath et al, 2019;Yi et al, 2019, Diego-Feliu et al, 2021. Given that 222 Rn is an inert gas and thus not influenced by the physicochemistry of coastal groundwater (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…Groundwater, as an active component of the global hydrological cycle, is extensively distributed within pore spaces and fractures of crustal lithospheres (Aeschbach‐Hertig & Gleeson, 2012; J. Han et al., 2017; H. Dai et al., 2019; De Graaf et al., 2019; Debnath et al., 2019; Gleeson et al., 2020; Ferreira et al., 2021). An accurate representation of groundwater distribution within subsurface environment is therefore crucial for addressing the problems that emerge at geoscience‐, energy‐, and environmental‐related contents, including land subsidence (Miller & Shirzaei, 2015; H. Dai, Ye, et al., 2017; Ha et al., 2020; Zhu et al., 2020), contaminant transports (Z. Dai et al., 2009; Ghanbarian et al., 2015; Cao et al., 2021; X. Zhang, Ma, Yin, et al., 2021), nuclear waste disposal (Viswanathan et al., 1998; Juhlin & Stephens, 2006; Wolfsberg et al., 2017; X. Zhang, Ma, Dai, et al., 2021), water inrush in tunnel and mine excavations (Dong et al., 2020; Ma et al., 2017; Qin et al., 2019), methane migration (Barth‐Naftilan et al., 2018; M. R. Soltanian et al., 2018; Pape et al., 2020; Ershadnia, Wallace, Hosseini, et al., 2021; Stanish et al., 2021; Wen et al., 2021), geological carbon storage (Castelletto et al., 2013; Z. Dai et al., 2014; Ershadnia, Wallace, Hajirezaie, et al., 2021; Fu et al., 2017; Njiekak et al., 2013), and groundwater and surface water interactions (Brunner et al., 2017; Jia et al., 2021; Wallace & Soltanian, 2021a, 2021b; Xin et al., 2022).…”
Section: Introductionmentioning
confidence: 99%