Groundwater Recharge: Revision history

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3 February 2024

  • curprev 09:4009:40, 3 February 2024‎ Ai talk contribs‎ 4,105 bytes +4,105‎ Created page with "==Introduction== Groundwater recharge, also known as deep drainage or deep percolation, is a hydrologic process where water moves downward from surface water to groundwater. This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table surface. Groundwater recharge is an important process for sustainable groundwater management, as the volume-rate abstracted from an aquifer in the long term should be l..."
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