Exploratory drilling to locate new water‐supply wells on Cape Cod, Massachusetts encountered fuel‐related organic contaminants in a shallow unconfined aquifer. However, the plume could not be traced back to the water table and estimates of ground‐water velocities were not consistent with plausible contaminant releases, and thus the source of contamination was not located. In conjunction with an expanded hydrogeologic investigation, tritium and helium isotope analyses were performed to delineate ground‐water ages and flow rates. Vertical profiles of ground‐water age were used to determine recharge rates that range from 70 to 115 cm/yr. The age of water near the leading edge of the contaminant plume along with estimates of dispersion were used to estimate when the contaminant release occurred (1975 ± 3 years). Recharge estimates, the geometry of the aquifer, and contaminant data were used in a simple mass balance model to determine both the location of the contaminant source and the horizontal ground‐water velocity (ranging from 20 ± 12 m/y to 90 ± 20 m/y across the site). Concurrent site investigations revealed fuel floating on the water table within the area (± 250 m) determined by the model. The configuration of the water table and recharge estimates were used to estimate a horizontal hydraulic conductivity of 130 ± 30 m/d. The mean hydraulic conductivity from a subsequent 72 hr, 12 well pumping test was 100 m/d.
|Number of pages||9|
|Publication status||Published - Nov 1995|