Researchers from North Carolina State University have developed a new
way to determine the rate at which nitrate pollution will make its way
from groundwater into streams. The work has implications for predicting
long-term pollution in groundwater-fed streams.
Nitrate pollution,
primarily from fertilizer runoff, is one of the major freshwater
contaminants in the United States. Additionally, the pollution persists
in aquifers – and thus in groundwater – which feed into streams over a
period of years or decades.
Measuring the rate of movement, or
flux, of nitrate from groundwater into streams is critical to
understanding how this pollutant moves through the environment and to
assessing the effectiveness of water quality management. However,
nitrate flux has traditionally been difficult to measure and since there
is no standard method for doing so, it is rarely measured.
David
Genereux, professor of hydrogeology at NC State, along with Troy
Gilmore, former NC State Ph.D. student, current faculty member at the
University of Nebraska and first author of a paper describing the
research, wanted to see if there was a reliable way to measure the flux.
They developed a new form of aquifer analysis that uses field sampling
results to estimate the rate at which nitrate contamination will be
flushed from an aquifer into streams in the coming decades.
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