Groundwater recharge | Wikipedia audio article
Channel: wikipedia tts
Date: 02/12/2018

This is an audio version of the Wikipedia Article:
Groundwater recharge


00:00:34 1 Processes
00:02:25 1.1 Wetlands
00:03:39 1.2 Depression-focused recharge
00:04:27 1.2.1 Depression pressure
00:05:44 1.2.2 Pollution
00:06:08 2 Estimation methods
00:06:32 2.1 Physical
00:07:15 2.2 Chemical
00:07:35 2.3 Numerical models
00:08:10 3 Adverse factors
00:08:27 4 See also



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SUMMARY
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Groundwater recharge or deep drainage or deep percolation is a hydrologic process where water moves downward from surface water to groundwater. Recharge is the primary method through which water enters an aquifer.  This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table surface. Recharge occurs both naturally (through the water cycle) and through anthropogenic processes (i.e., "artificial groundwater recharge"), where rainwater and or reclaimed water is routed to the subsurface.