Beckwith, C. W. and Baird, A. J. and Heathwaite, A. L. (2003) Anisotropy and depth-related heterogeneity of hydraulic conductivity in a bog peat. I:laboratory measurements. Hydrological Processes, 17 (1). pp. 89-101. ISSN 0885-6087Full text not available from this repository.
Anisotropy and heterogeneity of hydraulic conductivity (K) are suspected of greatly affecting rates and patterns of ground-water seepage in peats. A new laboratory method, termed here the modified cube method, was used to measure horizontal and vertical hydraulic conductivity (Kh and Kv) of 400 samples of bog peat. The new method avoids many of the problems associated with existing field and laboratory methods, and is shown to give relatively precise measurements of K. In the majority of samples tested, Kh was much greater than Kv, indicating that the bog peat was strongly anisotropic. Log10Kh, log10Kv, and log10 (Kh/Kv) were found to vary significantly with depth, although none of the relationships was simple. We comment on the scale dependency of our measurements.
|Journal or Publication Title:||Hydrological Processes|
|Additional Information:||Anisotropy and depth-related heterogeneity of hydraulic conductivity in a bog peat. I: laboratory measurements 10.1002/hyp.1116|
|Uncontrolled Keywords:||bog peat ; hydraulic conductivity ; anisotropy ; heterogeneity ; modified cube method|
|Departments:||Faculty of Science and Technology > Lancaster Environment Centre|
|Deposited On:||13 Sep 2011 11:27|
|Last Modified:||27 Mar 2017 04:22|
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