2022
DOI: 10.1016/j.agwat.2022.107887
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Impacts of a shallow saline water table on maize evapotranspiration and groundwater contribution using static water table lysimeters and the dual Kc water balance model SIMDualKc

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Cited by 14 publications
(1 citation statement)
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“…The isotopes tracers can extend our understanding of evaporation rates (Robertson and Gazis 2006), the extent of soil water recharge (Garvelmann et al 2012; Sprenger et al 2018), residence times of water along a soil profile (Gazis and Feng 2004), the infiltration and groundwater recharge (Song et al 2009; Zhu et al 2021), and root water uptake patterns (Ma and Song 2016; Rothfuss and Javaux 2017). Additionally, water balance simulation using Richards equation helps to analyze the mechanisms of water flow in soil (Liu et al 2022). In summary, the combined physical and isotopic techniques and water balance simulation have been proven useful in investigating vertical water movement in the unsaturated zone and identifying the recharge mechanism to groundwater.…”
Section: Introductionmentioning
confidence: 99%
“…The isotopes tracers can extend our understanding of evaporation rates (Robertson and Gazis 2006), the extent of soil water recharge (Garvelmann et al 2012; Sprenger et al 2018), residence times of water along a soil profile (Gazis and Feng 2004), the infiltration and groundwater recharge (Song et al 2009; Zhu et al 2021), and root water uptake patterns (Ma and Song 2016; Rothfuss and Javaux 2017). Additionally, water balance simulation using Richards equation helps to analyze the mechanisms of water flow in soil (Liu et al 2022). In summary, the combined physical and isotopic techniques and water balance simulation have been proven useful in investigating vertical water movement in the unsaturated zone and identifying the recharge mechanism to groundwater.…”
Section: Introductionmentioning
confidence: 99%