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Spatiotemporal variations in soil water content (SWC) and soil water stable isotopic compositions (SWSIC; 2H/1H (δD) and 18O/16O (δ18O)) provide critical information on elucidating land surface processes across scales. Meanwhile, little is known about the spatiotemporal characteristics of SWSIC and its driving factors. Therefore, it's necessary to improve tracer techniques of SWSIC by interpreting their spatiotemporal variability patterns as well as the correlations with other factors such as texture, soil depth and vegetation. To this
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