HYDROGEOLOGIC STUDIES TO ADDRESS CHANGING WATER LEVELS AT THE WIPP SITE
Three hypotheses involving human activities were developed to explain the water-level changes: 1) potash processing effluent discharged onto a tailings pile upgradient of the WIPP site may be leaking into the Culebra through poorly plugged boreholes beneath the tailings pile or through subsidence fractures; 2) water from overlying units may be leaking into the Culebra through poorly plugged potash exploration holes; and 3) brine injected into deeper formations for secondary oil recovery or salt-water disposal may be leaking into the Culebra, either through casing failures in the injection well(s) or through nearby poorly plugged boreholes.
Both field and modeling activities were initiated to address these hypotheses. New wells were installed downgradient of the potash tailings pile and in other areas where data were lacking. Bureau of Land Management and New Mexico Oil Conservation Division databases were searched to: 1) identify exploration holes and wells that may have been inadequately plugged, and 2) obtain information on injection wells, their target horizons, and injection rates. Records from the New Mexico Office of the State Engineer show how much water is pumped for potash refining.
Modeling studies show that some combination of leakage from the tailings pile and leakage through boreholes in other locations is required to match the observed spatial distribution of water-level changes. None of the scenarios considered suggest any threat to WIPPs compliance with regulations.