Long‐term effects of revegetation on soil hydrological processes in vegetation‐stabilized desert ecosystems |
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| Authors: | Zhongbo Yu Haishen Lü Yonghua Zhu Sam Drake Chuan Liang |
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| Institution: | 1. State Key Laboratory of Hydrology‐Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, China;2. Department of Geoscience, University of Nevada, Las Vegas, NV 89154, USA;3. College of Science, Hohai University, Nanjing 210098, China;4. Office of Arid Lands Studies, University of Arizona, 1955 E. 6th Street, Tucson, AZ 85719, USA;5. College of Hydraulic and Hydroelectric Engineering, Sichuan University, Chengdu, Sichuan 610065, People's Republic of China |
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| Abstract: | Planting of sand‐binding vegetation in the Shapotou region on the southeastern edge of the Tengger Desert began in 1956. The revegetation programme successfully stabilized formerly mobile dunes in northern China, permitting the operation of the Baotou‐Lanzhou railway. Long‐term monitoring has shown that the revegetation programme produced various ecological changes, including the formation of biological soil crusts (BSCs). To gain insight into the role of BSCs in both past ecological change and current ecological evolution at the revegetation sites, we used field measurements and HYDRUS‐1D model simulations to investigate the effects of BSCs on soil hydrological processes at revegetated sites planted in 1956 and 1964 and at an unplanted mobile dune site. The results demonstrate that the formation of BSCs has altered patterns of soil water storage, increasing the moisture content near the surface (0–5 cm) while decreasing the moisture content in deeper layers (5–120 cm). Soil evaporation at BSC sites is elevated relative to unplanted sites during periods when canopy coverage is low. Rainfall infiltration was not affected by BSCs during the very dry period that was studied (30 April to 30 September 2005); during periods with higher rainfall intensity, differences in infiltration may be expected due to runoff at BSC sites. The simulated changes in soil moisture storage and hydrological processes are consistent with ongoing plant community succession at the revegetated sites, from deep‐rooted shrubs to more shallow‐rooted herbaceous species. Copyright © 2009 John Wiley & Sons, Ltd. |
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| Keywords: | sand dunes biological soil crusts soil water content soil hydrological processes Tengger Desert northern China |
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