2021
DOI: 10.1016/j.agrformet.2021.108321
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Isotopic partitioning of evapotranspiration in a mesic grassland during two wetting–drying episodes

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Cited by 6 publications
(11 citation statements)
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“…(2) the 18 O is more sensitive than 2 H to the equilibrium fractionation (Sun et al, 2021;Wei et al, 2015). The dual-isotope plot of leaf, soil, xylem, and vapour water are shown in Figure 2.…”
Section: Isotope Measurementsmentioning
confidence: 99%
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“…(2) the 18 O is more sensitive than 2 H to the equilibrium fractionation (Sun et al, 2021;Wei et al, 2015). The dual-isotope plot of leaf, soil, xylem, and vapour water are shown in Figure 2.…”
Section: Isotope Measurementsmentioning
confidence: 99%
“…The SS assume δ T is equal to the isotope composition of xylem water. This assumption works well for shorter timescales at the mid-noon period; however, many researchers raise concerns about the reliability of this hypothesis at other time periods of the day (Dubbert et al, 2014;Dubbert & Werner, 2019;Lai et al, 2006;Lee et al, 2007;Sun et al, 2021;Welp et al, 2008). Alternately, the non-steady-state (NSS) assumption has been developed and applied in past decades, which determines δ T by parameterizing the diurnal change of xylem water or source water isotope composition (Dubbert & Werner, 2019;Quade et al, 2019).…”
Section: Introductionmentioning
confidence: 99%
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