Tiny sediment grains are covered with a very fine-grained, complex mixture of minerals in an open fabric that results in a large surface area in contact with water between the grains. Scientists at the U.S. Geological Survey (USGS) are studying this microscopic layer and finding that the mineral composition of these coatings on sediment grains in the unsaturated zone (i.e., between land surface and the water table) can have a substantial effect on the retention of nitrate and sulfate.
Their findings are
particularly important for evaluating the long-term effects of agriculture on
water quality, as the storage of these common components of fertilizer in the
unsaturated zone can affect the quality of shallow ground water for many years
after fertilizer application ceases.
Nitrate and sulfate are
important plant nutrients. Farmers and soil scientists routinely monitor the
nutrient content of the soil in farm fields so that fertilizer application can
be managed to maintain profitability and to minimize runoff or infiltration.
Loss of excess nutrients can elevate levels in streams and shallow ground water.
Understanding the mechanisms of nutrient storage in the unsaturated zone is
critical to protecting ground water resources.
Timothy Reilly, the lead
author of the study, states, “The unsaturated zone is potentially a large
reservoir for anions (negatively charged ions) like nitrate and sulfate. The
increased residence time indicated by these findings suggests that models in
areas with similar mineral characteristics, which neglect or minimize storage,
will not accurately predict nutrient transport to the water table.”
In the study,
unsaturated-zone sediments and the chemistry of shallow ground water underlying
a small (about 3 square miles) watershed in southern New Jersey were studied to
identify mechanisms responsible for nutrient storage. Lower unsaturated zone
sediments and shallow ground water samples were collected at 11 locations, and
concentrations of nitrate and sulfate were determined. Nutrient storage in the
very fine-grained mineral coatings on the sediment grains was attributed to a
complex combination of chemical and physical storage mechanisms.
Results from the study,
supported by the US Geological Survey Toxic Substances Hydrology Program, were
published in a recent issue of the Vadose Zone Journal, and these findings are
particularly important for evaluating the long-term effects of agricultural
land use on ground water quality.