The set of processes by which ground water is replenished is termed

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The term "recharge" refers to the various processes by which groundwater is replenished by precipitation, snowmelt, or other sources of water that infiltrate the soil and percolate down into the aquifer. Discharge refers to the opposite process, where groundwater is released back into the surface water or atmosphere. Saturation refers to the state where the soil, rock, or other materials are completely filled with water. Transpiration refers to the process where plants take up water from the soil and release it back into the atmosphere through their leaves.

The Set of Processes by Which Ground Water Is Replenished