2023
DOI: 10.1016/j.scitotenv.2023.164763
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Deep roots mitigate drought impacts on tropical trees despite limited quantitative contribution to transpiration

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Cited by 9 publications
(3 citation statements)
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“…Vegetation with shallow roots, such as cropland and grassland, exhibits high sensitivity to insufficient soil moisture in the upper layer, leading to a notably rapid response to flash droughts (Pendergrass et al 2020). Ecosystems generally exhibit extended response time with increasing rooting depth, which may be attributed to deeper-rooted vegetation having access to more abundant soil moisture to mitigate water stress (Kühnhammer et al 2023). Specifically, the augmented depth of vegetation roots enhances the efficient utilization of soil moisture resources by plants (Brunner et al 2015).…”
Section: Discussionmentioning
confidence: 99%
“…Vegetation with shallow roots, such as cropland and grassland, exhibits high sensitivity to insufficient soil moisture in the upper layer, leading to a notably rapid response to flash droughts (Pendergrass et al 2020). Ecosystems generally exhibit extended response time with increasing rooting depth, which may be attributed to deeper-rooted vegetation having access to more abundant soil moisture to mitigate water stress (Kühnhammer et al 2023). Specifically, the augmented depth of vegetation roots enhances the efficient utilization of soil moisture resources by plants (Brunner et al 2015).…”
Section: Discussionmentioning
confidence: 99%
“…12,37 If these steps are followed, new in-situ methods provide an enormous advantage and can provide insights into ecohydrological dynamics and processes on a (sub) daily basis. 42,43,59 5 CONCLUSION…”
Section: Cve Work Well-for Pure Water Samplesmentioning
confidence: 98%
“…39 Yet, it has been demonstrated that the analysed water mixing ratio in CRDS has a strong impact on obtained δ 2 H and δ 18 O values, 37,38,40 which has high relevance for studies, where the isotopic composition is measured directly (and is difficult to control) in the water vapour, such as soil evaporation, soil water vapour, atmospheric water vapour, plant transpiration or xylem water in the gas phase. 12,41,42 With the development and application of new water stable isotopologue measurement techniques, 2,8,10,12,43,44 which are based on the direct measurement of water vapour of different mixing ratios, the water mixing ratio-dependency of stable water isotopologues with CRDS is gaining relevance. The direct equilibration method to sample, for instance, soil water vapour is based on thermodynamic equilibrium and full water vapour saturation, which is controlled by the ambient temperature that typically varies considerably under natural conditions.…”
mentioning
confidence: 99%