Measuring the permeability of open-framework gravel.

Ground Water

Department of Earth and Environmental Sciences, Wright State University, Dayton, OH 45435, USA.

Published: November 2010

Open-framework gravel has permeability, k, above the measurement range of most laboratory constant-head permeameters because the head difference across the length of conventional permeameters is too small to be measured. Here we addressed the challenge of measuring the high k by using a 3 m long permeameter. The head difference over this length was of the order of 10(-2) to 10(-3) m, which we could measure to the nearest 10(-5) m. We collected data over the range of linear, laminar flow to nonlinear, laminar flow to verify that k was measured using data collected within the Darcian regime. We measured k between 4000 and 100,000 Darcies among experiments using different sediments.

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Source
http://dx.doi.org/10.1111/j.1745-6584.2010.00675.xDOI Listing

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