Groundwater quality reflects substances that are dissolved or
suspended in the water. Suspended material is not transported far in most subsurface
materials, but it is usually filtered out. In general, groundwater flow is
very slow and depends on the permeability (water transmitting ability) 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
measured in feet (or meters) per day or feet (or meters) per year. In some
situations where flow is slow it is measured in inches (or centimeters) per year.
Groundwater usually contains higher concentrations of natural dissolved
materials than surface water. The materials dissolved in the water usually
reflect the composition and solubility of the earth materials (soil or rock) that the
groundwater is in contact with and time that it has been in the subsurface. A
number of the activities of man pose threats to water quality. Some of these
activities include:
Landfill solid waste disposal
Urban stormwater infiltration
The illustration on the above-right 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 (eg. 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).
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