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Groundwater recharge, or deep drainage, is the process in which water percolates from the surface down into the groundwater supplies. Recharge does occur naturally, but it can also be achieved through anthropogenic methods, called artificial recharge. In artificial recharge, surface water is rerouted to the subsurface. This is normally done by creating "dug-wells", which are very wide wells that are used to allow water to percolate into the ground at a much faster pace. This is commonly performed in areas with depleted groundwater levels, such as India.
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Groundwater is difficult to clean because, the water is dispersed throughout large areas of rock, and also because the pollutants can cling to the materials that make up the aquifer.
Groundwater is difficult to clean because, the water is dispersed throughout large areas of rock, and also because the pollutants can cling to the materials that make up the aquifer.
Some ground water will return to the surface, especially during flooding. At times, areas near bodies of water will have returning ground water in spots.
Groundwater recharge has begun in some areas
Yes, but run-offs (like from oceans and rivers) help too.Answer:Ultimately all water is from precipitation but it can reach the groundwater through several routes.First off groundwater systems have recharge areas (where the water enters) and discharge areas (where the water comes out). Generally the recharge areas are higher than the discharge areas. This is fortunate as water from the sea (the lowest level of water) returning to the groundwater would make it salty and unfit for agriculture or drinking.Recharge areas can be:* Where the rain or snow falls on porous ground * The bottoms of lakes or rivers * The base of glaciers Groundwater can also be perched (essentially in a pocket of impervious soil or rock where the water is essentially trapped) or in an aquider which has a very low permeability (the flow is very slow). In some areas this water may have been there for several thousand years and laid down in the last glaciation (ice age).
Groundwater recharge, or deep drainage, is the process in which water percolates from the surface down into the groundwater supplies. Recharge does occur naturally, but it can also be achieved through anthropogenic methods, called artificial recharge. In artificial recharge, surface water is rerouted to the subsurface. This is normally done by creating "dug-wells", which are very wide wells that are used to allow water to percolate into the ground at a much faster pace. This is commonly performed in areas with depleted groundwater levels, such as India.
the rate of natural groundwater recharge decreases as urban areas develop because human clear natural environments such as trees, and replace them with material such as concrete. In order for groundwater to recharge the water has to be able to permeate the soil and sink downwards to aquifers. So by replacing permeable material such as soil with material such as concrete the water can not permeate the soil and travel down to aquifers.
Peter Meyboom has written: 'Patterns of groundwater flow in seven discharge areas in Saskatchewan and Manitoba' -- subject(s): Groundwater
Thomas E. Reilly has written: 'Factors affecting areas contributing recharge to wells in shallow aquifers' -- subject(s): Groundwater flow, Aquifers 'Guidelines for evaluating ground-water flow models' -- subject(s): Computer simulation, Groundwater flow
groundwater is used faster than it is replaced
Groundwater erosion occurs most often in areas with an abundance of limestone and rainfall. This erosion can create large cavities and caves.
rural
geothermal energy
J. F Ruhl has written: 'Simulation of ground-water flow and delineation of areas contributing recharge within the Mt. Simon-Hinckley Aquifer to well fields in the Priarie Island Indian Community, Minnesota' -- subject(s): Mathematical models, Groundwater flow 'Simulation of ground-water flow and delineation of areas contributing recharge within the Mt. Simon-Hinckley aquifer to well fields in the Prairie Island Indian Community, Minnesota' -- subject(s): Artificial groundwater recharge, Computer simulation, Groundwater flow 'Nitrate and pesticides in surficial aquifers and trophic state and phosophorus sources for selected lakes, eastern Otter Tail County, west-central Minnesota, 1993-96' -- subject(s): Environmental aspects, Environmental aspects of Nitrates, Environmental aspects of Pesticides, Groundwater, Nitrates, Pesticides, Quality, Water quality management 'Quantity and quality of seepage from two earthen basins used to store livestock waste in southern Minnesota during the first year of operation, 1997-98' -- subject(s): Animal waste, Environmental aspects, Environmental aspects of Animal waste, Groundwater, Pollution, Seepage 'Hydraulic properties of the Prairie du Chien-Jordan aquifer, Shakopee Mdewakanton Sioux Community, southeastern Minnesota, 1997' -- subject(s): Hydrogeology, Water-supply, Aquifers 'Estimates of recharge to unconfined aquifers and leakage to confined aquifers in the seven-county metropolitan area of Minneapolis-St. Paul, Minnesota' -- subject(s): Artificial groundwater recharge, Hydrogeology, Water table 'Water resources of the White Earth Indian Reservation, northwestern Minnesota' -- subject(s): Hydrology, Groundwater, Groundwater flow
groundwater