2013South-to-north Water Transfers and Water Science & TechnologyRequires access

Calculation of Groundwater Recharge during a Large Infiltration Test in the Hutuo River

Zengqi Zhang

Open publisher page 2 citations

Abstract

Water balance method was applied to calculate recharge from river water infiltration during a large infiltration test in the Hutuo River,and especially to calculate the infiltrating recharge in the water source area.The results showed that the amount of river infiltration water is 14 827 500m3 during the test,and groundwater recharge from river infiltration water is 13 828 900m3.The groundwater recharge coefficient from river infiltration is 93%.The amount of received water in the water source area is 7 425 300m3.Meanwhile,the maximum rising magnitude of groundwater level in the observation wells located in the water source area is 6.823m,indicating apparent groundwater recharge effects.

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What this paper is about

Water balance method was applied to calculate recharge from river water infiltration during a large infiltration test in the Hutuo River,and especially to calculate the infiltrating recharge in the water source area.The results showed that the amount of river infiltration water is 14 827 500m3 during the test,and groundwater recharge from river infiltration water is 13 828 900m3.The groundwater recharge coefficient from river infiltration is 93%.The amount of received water in the water source area is 7 425 300m3.Meanwhile,the maximum rising magnitude of groundwater level in the observation wells located in the water source area is 6.823m,indicating apparent groundwater recharge effects.

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Available abstract

Water balance method was applied to calculate recharge from river water infiltration during a large infiltration test in the Hutuo River,and especially to calculate the infiltrating recharge in the water source area.The results showed that the amount of river infiltration water is 14 827 500m3 during the test,and groundwater recharge from river infiltration water is 13 828 900m3.The groundwater recharge coefficient from river infiltration is 93%.The amount of received water in the water source area is 7 425 300m3.Meanwhile,the maximum rising magnitude of groundwater level in the observation wells located in the water source area is 6.823m,indicating apparent groundwater recharge effects.

Key concepts: Groundwater recharge, Infiltration (HVAC), Groundwater, Hydrology (agriculture), Depression-focused recharge, Environmental science, Water balance, Geology

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