groundwater recession
groundwater recession
[′grau̇nd‚wȯd·ər ri′sesh·ən] (hydrology)
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Guangxi is in a traditional karst region, where natural depressions caused by groundwater recession and erosion are not uncommon.
The critical time is the time it takes the groundwater recession curve to reach a stable shape after the recharge period.
4 m deep) groundwater rise was approximately 100 mm, and occurred during the 2-month period of shallow groundwater recession.
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