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

The capillary fringe is the subsurface layer in which groundwater seeps up from a water table by capillary action to fill pores. Pores at the base of the capillary fringe are filled with water due to tension saturation. This saturated portion of the capillary fringe is less than the total capillary rise because of the presence of a mix in pore size. If the pore size is small and relatively uniform, it is possible that soils can be completely saturated with water for several feet above the water table. Alternately, when the pore size is large, the saturated portion will extend only a few inches above the water table. Capillary action supports a vadose zone above the saturated base, within which water content decreases with distance above the water table. In soils with a wide range in pore size, the unsaturated zone can be several times thicker than the saturated zone.

Some workers restrict their definition of the capillary fringe only to the tension-saturated base portion and exclude it wholly from the vadose zone. [1][2] This is more common among workers addressing solute transport and water flow. Others define the capillary fringe as including both the tension-saturated and unsaturated portions. [3][4] This is the preferred definition among workers dealing with the remediation of salt affected soils as well as those dealing with the vapor phase of soil processes and bioremediation. It is not uncommon to see the capillary fringe treated as a boundary condition separating the water table from the unsaturated zone, without defining it as a significant part of either. [5]

See also

References

  1. ↑ "Glossary of Hydrogeologic Terms". Ground-Water Remediation Technologies Analysis Center GWRTAC. Archived from the original on 2005-09-07. Retrieved 2019-01-12. ...saturated with water...held within pores...by capillary forces.
  2. ↑ "Origin, Occurrence and Movement of Ground Water". Groundwater Resources of British Columbia. Chapter 2: Origin, Occurrence, and Movement of Groundwater. Archived from the original on 2004-05-19. Retrieved 2019-01-12. ...thin saturated layer...
  3. ↑ "Introduction to Basic Ground-Water Flow". earthDRx. At the top of the capillary fringe, saturation by water is now limited to only the micropores
  4. ↑ "Definitions of Selected Ground-Water Terms - Revisions and Conceptual Refinements" (PDF). Geological Survey Water Supply Paper. US Department of Interior. 1988. Archived from the original (PDF) on 2015-09-25. Retrieved 2019-01-12. The capillary fringe is the zone immediately above the water table in which all or some of the interstices are filled with water...
  5. ↑ "Unsaturated Zone". Archived from the original on 2015-09-08. Retrieved 2019-01-12. The boundary between the unsaturated zone and the saturated zone....
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