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The water quality is generally lower in the deeper parts of aquifers, resulting
in higher filtration costs for agricultural as well as rural uses. The
concentration of mineral salts in depleted aquifers can render the groundwater
useless for many water supply purposes. Federal drinking-water standards require
that total dissolved solids not exceed 500 parts per million. Agriculture also
has specific limits, although these vary based on the salinity tolerance of
different crops. In general, a salinity level of greater than 1,000 ppm renders
water useless for most irrigation applications (Leonard, 1986).
Andy Wingo
2001-12-10