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Groundwater
quality describes the condition of groundwater relative to substances that are dissolved or suspended
in the water. Suspended material is not transported far in most
subsurface materials, but it is usually filtered (blocked by
pore-size or by adhesion to aquifer material) as the water
circulates through small openings in the soil or bedrock. In
general, groundwater flow is very slow and depends on the
permeability (water transmitting properties) of the subsurface
materials, as wells as the hydraulic gradient (slope of the
water-table or pressure gradient for artesian conditions). The
rate of groundwater flow is usually
The illustration above presents an example of how a source of groundwater contamination can pollute millions of gallons of groundwater in an underlying aquifer. The "industrial area" is presented as a typical source of contamination. In the illustration, the groundwater contaminants are volatile organic chemicals (e.g. trichloroethene or TCE) that are used as solvents or degreasers in various industrial processes. The degree of contamination is indicated by the concentration of total volatile organics by contours. Degree of contamination is also illustrated by varying colors in the aquifer. Those closest to the industrial area have the highest concentrations, while those at a distance or upgradient have lower concentrations. The downgradient water supply well is being impacted by the contamination from the industrial area and may have to be shut down until the aquifer is remediated (cleaned up).
The groundwater properties of
temperature and conductivity can be used to rapidly delineate bodies
of varying water quality. The quality of water in
wells and boreho |
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