Date of Creation: 1983
The ultimate source of natural potable water is rain, rarely used
today as a direct source except where rain is collected into cisterns and
serves as the only available water supply. When rain falls, it runs off into
streams or soaks into the ground, percolating through porous strata until it
reaches an impervious stratum and collects, forming groundwater. Groundwater is
the source of wells and of springs that feed streams, rivers, and lakes.
Surface waters contain larger quantities of bacteria than groundwaters, but
groundwater has higher concentrations of dissolved chemicals.
Early
peoples had no need of engineering works to supply their water. Hunters and
nomads camped near natural sources of fresh water. After community life
developed, supplying water became important for inhabitants of a city and the
surrounding farms. The first people to consider sanitation of their water
supply were the ancient Romans, who constructed a vast system of aqueducts to
bring the clean waters of the Apennine Mountains into the city and built
settling basins with filters along these mains to ensure the clarity of the
water.
The invention of the force pump in England in the 16th century
extended the possibilities of development of water-supply systems. The first
municipal pumping station in the U.S. was erected about 1760 to supply water to
the town of Bethlehem, Pennsylvania. By 1800, 16 U.S. cities had water-supply
systems, and since that time almost every city and town in the country has been
provided with municipal waterworks, most of them publicly owned and
operated.
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