U.S. Geological Survey Toxic Substances Hydrology Program--Proceedings
of the Technical Meeting, Colorado Springs, Colorado, September 20-24, 1993,
Water-Resources Investigations Report 94-4015
Observational, Experimental and Inferred Evidence for Solute
Diffusion in Fractured Granite Aquifers: Examples from the Mirror Lake Watershed,
Grafton County, New Hampshire
by
Warren W. Wood (U.S. Geological Survey, Reston, Va.), Allen M.
Shapiro (U.S. Geological Survey, Reston, Va.), Paul A. Hsieh (U.S. Geological
Survey, Menlo Park, Ca.), and Terry B. Councell (U.S. Geological Survey,
Reston, Va.)
Abstract
The role of solute diffusion between ground water and granite
in the Mirror Lake drainage area was evaluated by direct observation,
experiment, and inference. The outcrops display ubiquitous Liesegang
bands associated with fractures that clearly indicate the activity
of diffusion in this system in the past. Laboratory experiments
determined that the effective diffusion coefficient for 137Cs
was approximately 6 x 10-13 m2/s in granite from Mirror
Lake. The 137Cs penetrated to a depth of approximately 7 mm
in 101 days, demonstrating the potential for rapid diffusion in this
system. Porosities of 32 granite samples averaged of 1.46
percent with a range of 1.07 to 2.32 percent. Measurements of
carbon-isotope of ground water in the fractures suggest that
calcite, identified in the granite, is dissolving and the bicarbonate
generated is diffusing to the fractures; that is, a significant
amount of the dissolved solids in the water in the fractures
are derived from diffusion of weathering products from the rock
matrix. These observations taken together are consistent with
the interpretation that diffusion is a major process
controlling solutes in this fractured granite aquifer.
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