1. See also

2. References

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.

The phreatic zone defines the lower edge of the vadose zone.

The phreatic zone size, color, and depth may fluctuate with changes of season, and during wet and dry periods.^[1][2]

See also

• {{annotated link|Phreatic}}
• {{annotated link|Epiphreatic zone}}
• {{annotated link|Capillary fringe}}
• {{annotated link|Infiltration (hydrology)}}
• {{annotated link|Phreatophyte}}
• {{annotated link|Vadose zone}}
• Index: Aquifer articles

References

• Gerald Martin Smith
• Gerald Mauroka Baker
• Gerald McCallum
• Gerald McClearn
• Gerald McKee (basketball)
• Gerald McKellar (disambiguation)
• Gerald McKellar (rugby union)
• Gerald McKenny
• Gerald McLellan
• Gerald McNamee
• Gerald Meerschaert
• Gerald M. Glaskin
• Gerald Michael Browne
• Gerald Michael Butts
• Gerald Miller
• Gerald Miller (disambiguation)
• Gerald Moore (journalist)
• Gerald Mordaunt
• Gerald Mordaunt Broome Salmon
• Gerald Nachman
• Gerald Nachman (journalist)
• Gerald Nailor, Sr.
• Gerald Nash
• Gerald Neugebauer
• Gerald N. Felando