Phreatic zone

The phreatic zone, or zone of saturation, is the part of an aquifer, below the water table, in which relatively all pores and fractures are saturated with water. Above the water table is the vadose zone.

Cross-section of a hillslope depicting the vadose zone, capillary fringe, water table, and saturated zone

The phreatic zone size, color, and depth may fluctuate with changes of season, and during wet and dry periods.[1][2] Depending on the characteristics of soil particles, their packing and porosity, the boundary of a saturated zone can be stable or instable, exhibiting fingering patterns known as Saffman–Taylor instability. Predicting the onset of stable vs. unstable drainage fronts is of some importance in modelling phreatic zone boundaries.[3]

See also
  • Phreatic – Term used in several scientific disciplines
  • Epiphreatic zone – The zone between the vadose zone above and phreatic zone below
  • Capillary fringe – The subsurface layer in which groundwater seeps up from a water table by capillary action
  • Infiltration (hydrology)
  • Phreatophyte – A deep-rooted plant that obtains a significant portion of the water that it needs from the phreatic zone
  • Vadose zone – unsaturated aquifer above the water table
  • Index: Aquifer articles

References
  1. "Phreatic Zone". TheFreeDictionary.com. Retrieved 7 June 2012.
  2. "Phreatic Zone". Encyclopædia Britannica. Retrieved 7 June 2012.
  3. Dynamics of Drainage and Viscous Fingering in Transport in Porous Media
    Note that zones "behind" the drainage front are areas on the 'dry' (low-viscosity) (typically above / beyond the 'wet' zone).


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