2007
DOI: 10.1016/j.jhydrol.2007.05.024
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Seasonal water use patterns of Juniperus ashei on the Edwards Plateau, Texas, based on stable isotopes in water

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Cited by 143 publications
(92 citation statements)
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“…Therefore, comparison of the isotopic composition in the plants and possible sources of water can be used to infer the depth of water uptake (Brunel et al, 1995). The proportion of varying potential water sources accessed by plants was preliminarily determined using stable isotope analysis in conjunction with two-or three-compartment linear mixing models (Snyder and Williams, 2000;Darrouzet-Nardi et al, 2006;McCole and Stern, 2007). However, the linear mixing models were unable to provide a unique solution when the number of sources exceeded three.…”
mentioning
confidence: 99%
“…Therefore, comparison of the isotopic composition in the plants and possible sources of water can be used to infer the depth of water uptake (Brunel et al, 1995). The proportion of varying potential water sources accessed by plants was preliminarily determined using stable isotope analysis in conjunction with two-or three-compartment linear mixing models (Snyder and Williams, 2000;Darrouzet-Nardi et al, 2006;McCole and Stern, 2007). However, the linear mixing models were unable to provide a unique solution when the number of sources exceeded three.…”
mentioning
confidence: 99%
“…The findings of this study complement those of other recent work examining the ecohydrology of karst shrublands in Central Texas. These include large-scale rainfall simulation experiments (Wilcox et al, 2008), tracer studies (Taucer et al, 2005;Dasgupta et al, 2006), and small-catchment experiments , as well as studies focusing on soil-landform relationships (Wilcox et al, 2007), interception , rooting depth (Jackson et al, 1999), and seasonal water use (McCole and Stern, 2007). In addition, the findings of this study provide particular insights into (1) the importance of canopy interception during runoff-producing events; (2) the nature and relative magnitude of rapid recharge; and (3) the interplay between recharge and surface runoff.…”
Section: Discussionmentioning
confidence: 99%
“…Moreover, comparison between the stable isotope composition of soil water, surface water, xylem water, and groundwater can confirm the vegetation reliance on the groundwater resource [58][59][60], particularly in semi-arid regions in which groundwater originated from snowmelt or winter precipitation and therefore has a distinctive isotopic composition [61]. Stable water isotopes have been used in a variety of studies and applications related to GDEs: to examine springs in the boreal regions [62], to examine the water uptake patterns in woody riparian GDEs of the southwestern United States [63], and to determine the seasonal water sources of woody GDEs and their connection to soil water content [64].…”
Section: Ground-based Methods Useful In Identifying Groundwater Depenmentioning
confidence: 99%