- groundwater [groundwôt΄ər]n.
* * *ground water also ground·wa·ter (groundʹwô'tər, -wŏt'ər) n.Water beneath the earth's surface, often between saturated soil and rock, that supplies wells and springs.
* * *or subsurface waterWater that occurs below the surface of the Earth, where it occupies spaces in soils or geologic strata.Most groundwater comes from precipitation, which gradually percolates into the Earth. Typically, 10–20% of precipitation eventually enters aquifers. Most groundwater is free of pathogenic organisms, and purification for domestic or industrial use is not necessary. Furthermore, groundwater supplies are not seriously affected by short droughts and are available in many areas that do not have dependable surface water supplies.
* * *water that occurs below the surface of the Earth, where it occupies all or part of the void spaces in soils or geologic strata. It is also called subsurface water to distinguish it from surface water which is found in large bodies like the oceans or lakes, or which flows overland in streams. Both surface and subsurface water are related through the hydrologic cycle (the continuous circulation of water in the Earth-atmosphere system).A brief treatment of groundwater follows. For full treatment, see hydrosphere: Groundwaters (hydrosphere).Most groundwater comes from precipitation. Precipitation infiltrates below the ground surface into the soil zone. When the soil zone becomes saturated, water percolates downward. A zone of saturation occurs where all the interstices are filled with water. There is also a zone of aeration (vadose zone) where the interstices are occupied partially by water and partially by air. Groundwater continues to descend until, at some depth, it merges into a zone of dense rock. Water is contained in the pores of such rocks, but the pores are not connected and water will not migrate. The process of precipitation replenishing the groundwater supply is known as recharge. In general, recharge occurs only during the rainy season in tropical climates or during winter in temperate climates. Typically, 10 to 20 percent of the precipitation that falls to the Earth enters water-bearing strata (aquifers (aquifer)).Groundwater is constantly in motion. Compared to surface water, it moves very slowly, the actual rate dependent on the transmissivity and storage capacity of the aquifer. Natural outflows of groundwater take place through springs and riverbeds when the groundwater pressure is higher than atmospheric pressure in the vicinity of the ground surface. Internal circulation is not easily determined, but near the water table the average cycling time of water may be a year or less, while in deep aquifers it may be as long as thousands of years.Groundwater plays a vital role in the development of arid and semiarid zones, sometimes supporting vast agricultural and industrial enterprises that could not otherwise exist. It is particularly fortunate that aquifers antedating the formation of deserts remain unaffected by increases in aridity with the passage of time. Withdrawal, however, will deplete even the largest of groundwater basins so that development based on the existence of aquifers can be only temporary at best.A vast amount of groundwater is distributed throughout the world, and a large number of groundwater reservoirs are still underdeveloped or uninvestigated. The most frequently investigated or exploited groundwater reservoirs are of the unconsolidated clastic (mainly sand and gravel) or carbonate hardrock type found in alluvial valleys and coastal plains under temperate or arid conditions.Though some groundwater dissolves substances from rocks and may contain traces of old seawater, most groundwater is free of pathogenic organisms, and purification for domestic or industrial use is not necessary. Furthermore, groundwater supplies are not seriously affected by short droughts and are available in many areas that do not have dependable surface water supplies.
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Look at other dictionaries:
groundwater — water in the ground, also ground water, 1890, from GROUND (Cf. ground) (n.) + WATER (Cf. water). Attested from mid 15c. in sense water at the bottom of a stream … Etymology dictionary
groundwater — ► NOUN ▪ water held underground in the soil or in pores and crevices in rock … English terms dictionary
groundwater — [groundwôt΄ər] n. water found underground in porous rock strata and soils, as in a spring: also written ground water … English World dictionary
Groundwater — Shipot, a common source of drinking water in a Ukrainian village. Groundwater is water located beneath the ground surface in soil pore spaces and in the fractures of rock formations. A unit of rock or an unconsolidated deposit is called an… … Wikipedia
Groundwater — This interesting name with variant spellings, Groundwator and Grundwater, is of locational origin from a place so called in Orphir, Orkney Islands, Scotland. The placename derives from the Old English pre 7th Century grand ground, plus waeter… … Surnames reference
groundwater — [[t]gra͟ʊndwɔːtə(r)[/t]] N UNCOUNT Groundwater is water that is found under the ground. Groundwater has usually passed down through the soil and become trapped by rocks. The groundwater is only feet beneath the city streets … English dictionary
groundwater — ground|wa|ter [ˈgraundˌwo:tə US ˌwo:tər, ˌwa: ] n [U] water that is below the ground ▪ There are fears that groundwater might become contaminated … Dictionary of contemporary English
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groundwater — gruntinis vanduo statusas T sritis ekologija ir aplinkotyra apibrėžtis Gravitacinis požeminis vanduo, susikaupęs pirmajame vandeningame sluoksnyje virš pirmosios nuo žemės paviršiaus vandensparos. Turi laisvą (nespūdinį) paviršių, kurį slegia… … Ekologijos terminų aiškinamasis žodynas
groundwater — noun Date: circa 1889 water within the earth especially that supplies wells and springs … New Collegiate Dictionary