| ground water |
The portion of the subsurface water which is in the zone of saturation where nearly all openings particles are filled with water. The between soil n in the ground is top of the zone of saturation called the water-table.
출처: www.lehigh.edu/~kaf3/books/reporting/glossary.html
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| ground water |
the capacity of a rock to transmit water under pressure. The coefficient of transmissibility is the rate of flow of water, at the prevailing water temperature, in gallons per day, through a vertical strip of the aquifer one foot wide, extending the full saturated height of the aquifer under a hydraulic gradient of 100-percent. A hydraulic gradient of 100-percent means a one foot drop in head in one foot of flow distance.
출처: www.texaswater.org/water/facts/glossary/glossary7....
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| ground water |
Water found below the surface of the land, usually in porous rock formations. Ground water is the source of water found in wells and springs and is used frequently for drinking.
출처: www.botany.uwc.ac.za/inforeep/glossary1.htm
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| ground water |
That portion of water below the surface of the ground at a pressure equal to or greater then atmospheric (= watertable)
출처: www.irrig8right.com.au/Glossary/Glossary.htm
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| ground water |
Ground water is the water found underground in the spaces between particles of rock and soil.
출처: www.uldrinkwell.com/drinkwell/glossary.html
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