In recent years, Mill Lane, a production well field located on the North Fork of Long Island, has been adversely affected by increasing chloride contamination. Geophysical surveys completed at the site indicate that a chloride plume is emanating from a recharge basin in close proximity to the well field. Road-salt runoff, entering the aquifer from the recharge basin, may be the source of measured increases in chloride concentrations at the well field. Potential factors influencing plume migration include quantity of salinity and volume of road-salt runoff, rate of recharge from precipitation [ in the context of a changing climate], aquifer transmissivity, proximity to the well field capture zone, and intensity and duration of pumping.
The USGS in cooperation with the Suffolk County Water Authority recently installed a real-time monitoring station within the recharge basin. This continuous-recording station measures water elevation, water temperature, and salinity (calculated from specific conductance) every fifteen minutes. Collected data are transmitted by satellite telemetry to the USGS National Water Information System Web Interface (NWISWeb) at http://waterdata.usgs.gov/ny/nwis every hour, where it is available for public dissemination.
The objective of this monitoring is to accurately assess the correlation between road-salt runoff and seasonal recharge basin salinity concentrations. This information may help delineate a point source of aquifer contamination and empower water managers with the data required to evaluate the potential for future chloride contamination at the well field.
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