ramosissima in all coppice dunes showed an increasing trend (Fig. 3 ).
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Seasonal dynamics and precipitation responses of water use strategies in Tamarix ramosissima in different developmental stages of coppice dunes in the Gurbantunggut Desert, northwest China.
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The water uptake from the 180–360 cm layer demonstrated a highly significant positive correlation with LOC, while that from the 360–500 cm layer was significantly positively correlated with iWUE.
The δD and δ 18 O values of soil water in all coppice dunes exhibited a decreasing trend with increasing depth, and below 60 cm the δ 18 O values became more negative before gradually stabilizing with further depth (Fig.
Variations in RWC, WSD, V a , V s , and V a / V s The average leaf RWC exhibited a clear trend in all coppice dunes according to the following order: growth stage of coppice dunes (81.54%) > stable stage of coppice dunes (80.84%) > initial stage of coppice dunes (79.56%) > declining stage of coppice dunes (72.49%) (Fig. 6 a).