Changes in concentration of certain constituents of treated waste water during movement through the Magothy Aquifer, Bay Park, New York

Henry F. H. Ku; John Vecchioli; Stephen E. Ragone

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Changes in concentration of certain constituents of treated waste water during movement through the Magothy Aquifer, Bay Park, New York

Henry F. H. Ku·John Vecchioli·Stephen E. Ragone

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Abstract

Approximately 7 million gallons (27 million litres) of tertiary-treated sewage (reclaimed water) was injected by well into the Magothy aquifer and was subsequently pumped out. As the reclaimed water moved through the aquifer, concentrations of certain dissolved constituents decreased as follows: Total nitrogen, 7 percent; methylene blue active substances, 49 percent; chemical oxygen demand, 50 percent; and phosphate, more than 93 percent.

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Journal of Research of the U.S. Geological Survey Article

Source-reported bounding extent: 40.62567934338915° to 40.64704307144758° latitude; -73.69199752807617° to -73.6526870727539° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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Henry F. H. Ku, John Vecchioli, Stephen E. Ragone. 1975. Changes in concentration of certain constituents of treated waste water during movement through the Magothy Aquifer, Bay Park, New York. https://pubs.usgs.gov/publication/70232670

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