Variations in water use strategies of <i>Tamarix ramosissima</i> at coppice dunes along a precipitation gradient in desert regions of northwest China.

As soil depth increased, there was an increasing trend in SWC across all sites.

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Specifically, the average δD and δ 18 O values of soil water in each layer exhibited a decreasing trend from the shallow to deep layer in arid and hyper-arid areas, with the highest values observed at 0−20 cm.

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