2007
DOI: 10.1016/j.jhydrol.2006.07.020
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Plant water sources in the cold semiarid ecosystem of the upper Kherlen River catchment in Mongolia: A stable isotope approach

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Cited by 87 publications
(52 citation statements)
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“…1). Li et al (2007a) showed by the analysis of δ 18 O and δD (deuterium) signatures in precipitation, soil, and shoot water that forests of Siberian larch in northern Mongolia primarily depend on surface water from the current precipitation. Carbon assimilated at the end of the growing season is apparently used for wood formation in the following growing season, explaining the increase of tree-ring width with increasing precipitation in September and even October of the year prior to tree-ring formation.…”
Section: Discussionmentioning
confidence: 99%
“…1). Li et al (2007a) showed by the analysis of δ 18 O and δD (deuterium) signatures in precipitation, soil, and shoot water that forests of Siberian larch in northern Mongolia primarily depend on surface water from the current precipitation. Carbon assimilated at the end of the growing season is apparently used for wood formation in the following growing season, explaining the increase of tree-ring width with increasing precipitation in September and even October of the year prior to tree-ring formation.…”
Section: Discussionmentioning
confidence: 99%
“…soil water from varying depths, stream water, ground-water, etc.) (Asbjornsen et al 2007;Brunel et al 1995;Li et al 2007;Mensforth et al 1994). Furthermore, linear mixing models based on mass balance equations can determine the contributions of each potential water source to stem water (White et al 1985;Phillips and Gregg 2001).…”
Section: Introductionmentioning
confidence: 99%
“…If samples of all potential water sources can be obtained and the water within the plant's xylem sap is also extracted, it is possible to assess which sources of water are being used (Dawson et al 2002). In order to identify the most possible sources of water transpired by plants, stable hydrogen and/or oxygen isotopic compositions of stem water are compared with those of potential water sources (Brunel et al 1995;Asbjornsen et al 2007;Li et al 2007). As contributions of water from different water sources could account for the same stem water stable isotope values recorded in the plant, actual plant water sources may be misinterpreted based only on this direct inference approach (Asbjornsen et al 2007).…”
mentioning
confidence: 99%