Abstract
The hydrogen isotope (deuterium-\( \delta D \)) composition at natural abundance levels of xylem water, soil water, groundwater, river water, and rainwater was used to evaluate whether adult plant species use groundwater and to detect seasonal shifts (dry/wet season) in water sources for plants growing in a semi-arid coal-mining area (located at the frontier of the Mu Us Desert). A direct inference approach and the IsoSource mixing model were used to estimate the contributions of different sources to the plant xylem water. The results showed that (1) the \( \delta D \) values of rainfall fluctuated considerably, while those of groundwater were generally constant during the experimental period; (2) the \( \delta D \) patterns in plant xylem water suggest that groundwater was a significant source of water for transpiration in the dry season, while all five selected species reduced dependence on groundwater sources in the wet season; and (3) soil water from the deep layer (50–100 cm) was used largely by adult species possibly because of interspecific competition. These results indicated that coal mining would significantly affect plant growth by reducing the water supply if it leads to a water table decrease. Therefore, it is necessary to protect groundwater resources during the coal mining operations in the region.
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Acknowledgments
The study was funded by National Natural Science Foundation of China (51239009), the CAS Action-plan for Western Development (KZCX2-XB3-13—the 3rd), and the “Western Light” Project of the Chinese Academy of Sciences (2007YB02). Great appreciation goes to the farmers in Shenmu County for their active participation in field sampling, and Dr. Ke Yuan (Chinese Academy of Forestry) for her help in measuring the \( \delta D \) values. Thanks also go to Dr. David Warrington from UK for his great help to the revised manuscript.
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This manuscript was edited by Dr. Paul Kretchmer who is a native-English speaker and soil scientist.
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Li, W., Yan, M., Qingfeng, Z. et al. Groundwater use by plants in a semi-arid coal-mining area at the Mu Us Desert frontier. Environ Earth Sci 69, 1015–1024 (2013). https://doi.org/10.1007/s12665-012-2023-2
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DOI: https://doi.org/10.1007/s12665-012-2023-2