The phreatic zone, or zone of saturation, is the area in an aquifer, below the
water table, in which relatively all pores and fractures are saturated with water.
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The pores and fractures in soil and rocks are saturated with water. The zone of
saturation is less corrosive than the unsaturated zone above the water table.
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By definition, the zone of saturation is saturated with water. Also see WATER
TABLE. Where raw wastewater is exfiltrating from a sewer pipe, the area of soil
Zone of Saturation: Region in the ground in which pore spaces are filled with
water. Water table: The interface between the zone of saturation and the zone of
Aug 5, 1991 ... A significant zone of saturation is a hydrogeologic unit in the zone of saturation
that possesses certain hydraulic properties that allow it to ...
Jul 21, 2016 ... The zone of aeration and zone of saturation are two sub-earthen zones that are
associated with the storage and replenishment of groundwater.
Dec 14, 2015 ... The “Zone of Saturation” is an area of land under the water table where all of the
pore spaces in the soil are filled with water. It occurs naturally ...
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Aug 1, 2016 ... Difference Between Zone of Aeration and Zone of Saturation.