NITRATE CONTAMINATION OF A BEDROCK AQUIFER IN CENTRAL VERMONT
By analyzing nitrate levels in the groundwater from the bedrock wells over time, we delineated groups of wells with similar nitrate patterns. Groundwater flow directions calculated from static water levels indicate multiple flow domains in the bedrock aquifer that are controlled by brittle and ductile bedrock structures. Borehole camera surveys show that a single foliation-parallel zone contributes groundwater to each domestic well. In combination with EMI surveys, the configuration of flow domains can explain the distribution of well groups with different nitrate patterns. Herbicide patterns are similar to nitrate patterns for some wells.
Nitrogen and oxygen isotope data show that all wells fall in the soil nitrogen field on nitrate source discrimination diagrams. Combined CFC113 and Tritium/Helium groundwater dating techniques yielded ages ranging from 13-22 years. CFC11 and CFC12 ages could not be determined because of an excess local source(s) of these compounds. Three distinct fluorescent dyes were introduced at widely-spaced locations, but only one of these dyes reached a well during the study. We were able to fingerprint the groundwater from two wells by integrating major and trace element geochemical trends with physical parameters such as pH, Eh, DO, Temp., and Conductivity.