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USGS · ofr821016

Vertical movement of ground water under the Merrill Field landfill, Anchorage, Alaska

Gordon L. Nelson·L.L. Dearborn
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Abstract

Shallow groundwater under the Merrill Field sanitary landfill at Anchorage is polluted by leachate. Wells, including three Municipal-supply wells, obtain water from two confined aquifers 100-300 feet beneath the landfill area. Aquifer-test data and information on subsurface geology, ground-water levels, and properties of materials were used to estimate vertical gradients and vertical permeabilities under the landfill. The authors ' best estimates ' of vertical permeabilities of two confining units are 1 x 10 super -2 foot per day and 2 x 10 super -4 foot per day. Theoretical travel-time calculations indicate that minor amounts of pollutants may reach the upper confined aquifer after many tens of years, but that water of the composition of the leachate probably would not reach the aquifer for more than three centuries. The range of error in the theoretical travel-time calculations is likely to be plus or minus a factor of two or three. (USGS)

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Gordon L. Nelson, L.L. Dearborn. 1982. Vertical movement of ground water under the Merrill Field landfill, Anchorage, Alaska. https://doi.org/10.3133/ofr821016

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