Groundwater is tightly held by surface tension to mineral grains or other soil particles in the

Name: Groundwater is tightly held by surface tension to mineral grains or other soil particles in the
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The capillary fringe is the subsurface layer where groundwater is pulled upward from the water table by capillary action into the pores of soil or rock. This action is due to the surface tension between the water and soil particles, causing the water to adhere to them.

Groundwater Is Tightly Held by Surface Tension to Mineral Grains