Phreatic - Wikipedia, the free encyclopedia
The term phreatic is used in Earth sciences to refer to matters relating to ground water below the static water table (the word originates from the Greek phrear , phreat- meaning "well" or "spri...
en.wikipedia.org/wiki/Phreatic
Phreatic zone - Wikipedia, the free encyclopedia
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 may fluctuate ...
en.wikipedia.org/wiki/Phreatic_zone
The saturated zone encompasses the area below ground in which all interconnected openings within the geologic medium are completely filled with water. Many hydrogeologists separate this zone into two subzones: the phreatic zone and the capillary fringe.
www.bookrags.com/research/saturated-zone-woes-02/ www.bookrags.com/research/saturated-zone-woes-02/
phreatic zone were logged and recorded continuously at the depth of 50 cm from the water table .... soil water from the vadose zone and the upper phreatic ...
www.springerlink.com/index/M3KJ4AND0Q8Y4WPC.pdf
The water-table is the surface that divides the zone that is permanently saturated with water (the phreatic zone) from the zone above in which the pore spaces are not completely filled with water (the vadose zone).
science.jrank.org/pages/48261/water-table.html
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phreaticzone.thedeepstop.com/ phreaticzone.thedeepstop.com/
samples from the phreatic zone in the Ganga alluvium has revealed that the quality of ground water fluctuates considerably with time. ...
iahs.info/redbooks/a150/150016.pdf
David Burney (PI) ; William Jungers (Co-PI) ... Fordham University, NY 10458 7188174650 ... Start Date/Expiration Date...
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. n. Referring to fast moving water in the top of the phreatic zone or in the zone liable to be subject to flood part of the time. cf. nothephreatic.
wasg.iinet.net.au/glossary.html
This record provided courtesy of AGI/GeoRef. ... Email this article to a friend ... Similar articles in this journal...
jsedres.sepmonline.org/cgi/content/abstract/49/2/670