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Soil water is the limitation factors in the semiarid region for vegetation growth. With the large scale “Grain for Green” implementation on the Loess Plateau of China, an amount of sloping cropland was converted to forestland, shrubland, and grassland. The spatial and temporal distribution of soil water was changed. However, the effect of revegetation on soil water movement is still unclear. In this study, we analyze the stable isotopes changes in precipitation and soil water in sloping cropland, forestland, shrubland, and grassland to trace the movement of moisture in soil. The results showed that δ18O in shallow layers (
Haocheng Ke; Peng Li; Zhanbin Li; Peng Shi; Jingming Hou. Soil Water Movement Changes Associated with Revegetation on the Loess Plateau of China. Water 2019, 11, 731 .
AMA StyleHaocheng Ke, Peng Li, Zhanbin Li, Peng Shi, Jingming Hou. Soil Water Movement Changes Associated with Revegetation on the Loess Plateau of China. Water. 2019; 11 (4):731.
Chicago/Turabian StyleHaocheng Ke; Peng Li; Zhanbin Li; Peng Shi; Jingming Hou. 2019. "Soil Water Movement Changes Associated with Revegetation on the Loess Plateau of China." Water 11, no. 4: 731.