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- W2181475720 abstract "The soil water characteristic curve was determined for two cracked soils of Saskatchewan, Canada. Using high quality undisturbed field samples, both soils indicated bimodal curves comprising of two air entry values. The fissure AEV (associated with drainage through cracks) and the matrix AEV (related to seepage through soil matrix) were found to be 10 kPa and 300 kPa for the expansive clay in Regina and 5 kPa and 100 kPa for the cemented sandstone at Avonlea. The appropriate parameter on the ordinate for presenting the curve is water content for expansive soils and degree of saturation for erodible soils." @default.
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- W2181475720 date "2013-01-17" @default.
- W2181475720 modified "2023-09-26" @default.
- W2181475720 title "Influence of cracks on soil water characteristic curve" @default.
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- W2181475720 doi "https://doi.org/10.1201/b14393-28" @default.
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