Groundwater-recharge estimation in the Ordos Plateau, China: comparison of methods

Springer Science and Business Media LLC - Tập 19 - Trang 1563-1575 - 2011
Lihe Yin1, Guangcheng Hu2, Jinting Huang1, Dongguang Wen3, Jiaqiu Dong1, Xiaoyong Wang1, Hongbo Li1
1Xi’an Center of Geological Survey, China Geological Survey, Xi’an, China
2State Key Laboratory of Remote Sensing Science, Institute of Remote Sensing Applications, Chinese Academy of Sciences, Beijing, China
3China Geological Survey, Beijing, China

Tóm tắt

Groundwater recharge is a key factor in water-balance studies, especially in (semi-)arid areas. In this study, multiple methods were used to estimate groundwater recharge in the Ordos Plateau (China), including reference to water-table fluctuation, Darcy’s law and the water budget. The mean annual recharge rates found were: water-table-fluctuation method (46–109 mm/yr); saturated-zone Darcian method (17–54 mm/yr); and water-budget method (21–109 mm/yr). Generally, groundwater-recharge rates are higher in the eastern part of the plateau where the land surface is covered by permeable sand that is favorable for infiltration. Along with results from previous studies using the empirical method, the chloride-mass-balance method, the unsaturated-zone Darcian method and the hydrograph-separation method, groundwater recharge rates were compared. There is no one method that would consistently produce the largest or smallest estimate of annual recharge for all groundwater systems. The largest recharge estimates were usually determined using the unsaturated-zone Darcian method and the smallest estimates were usually determined using the chloride-mass-balance method. Comparison of multiple methods is found to be valuable for determining the range of plausible recharge rates and for highlighting the uncertainty of the estimates.

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