Abstract
Soil covers are widely used in mine waste and landfill applications to protect the environment. The finite-element based model was used to simulate the vertical flow of water through unsaturated cover soils. A hysteretic model for two-phase permeability-saturation-pressure (k-S-p) relations is implemented in unsaturated flow model to predict temporal and spatial fluid distributions in a soil cover. A representation of hysteretic soil hydraulic properties is based on a combination of van Genutchen’s equation and statistical model for relative permeability. Predictions ofk-S-p relations along major flow paths are presented for fine sand, silt, and coarse sand. Employing hysteretic and nonhysteretic relationships, this study also presents a comparison of saturation profiles in four different cover soils: fine sand, silt, and coarse sand as single covers and multi-layered soils. A number of simulations were performed to analyze the saturation profile in the cover soils subject to downward drainage due to gravity and infiltration under various conditions of at the top and bottom. The numerical results indicate that simulation of water flow involving saturation path reversals may produce significant differences between hysteretic and nonhysteretic results. Considerations should be given to effects of hysteresis in hydraulic properties to accurately predict fluid distributions in a cover soil.
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References
Assouline, S., 2001, A model for soil relative hydraulic conductivity based on the water retention characteristic curve, Water Resources Res., 37, 265–271.
Charbeneau, R.J., 2000, Groundwater Hydraulics and Pollutant Transport, Prentice Hall, Upper Saddle River, NJ, 593 p.
Choo, L.-P. and Yanful, E.K., 2000, Water flow through cover soils using modeling and experimental methods, J. of Geotech and Geoenviron Eng., 324–334.
Guarnaccia, J., Pinder, G., and Fishman, M., 1997, NAPL: Simulator Documentation, National Risk Management Research Laboratory, Ada, OK, 221 p.
Lenhard, R.J., Parker, J.C., and Kaluarachchi, J.J., 1991, Comparing simulated and experimental hysteretic two-phase transient fluid flow phenomena, Water Resources Res. 27, 2113–2124.
Mualem, Y., 1976, A new model for predicting the hydraulic conductivity of unsaturated porous media, Water Resources Res., 12, 513–522.
Mualem, Y., 1978, A new model for predicting the hydraulic conductivity of unsaturated porous media, Water Resources Res., 14, 325–334.
Parker, J.C. and Lenhard, R.J., 1987, A model for hysteretic constitutive relations governing multiphase flow: 1 saturation-pressure relations, Water Resources Res., 23, 2187–2196.
van Genutchen, M. Th., 1980, A closed-form equation for predicting the hydraulic conductivity of unsaturated soils, Soil Sci. Soc. Am. J., 892–898.
Yang, M. and Yanful, E.K., 2002, Water balance during evaporation and drainage in cover soils under different water table conditions. Adv. in Water Resourses, 24, 505–521.
Yanful, E.K., Mousavi, S.M., and Yang, M., 2003, Modeling and measurement of evaporation in moisture-retaining soil covers. Adv. in Environ Res., 7, 783–801.
Yanful, E.K., Mousavi, S.M., and De Souza, L.-P., 2006, A numerical study of soil cover performance. J. Environ. Management, 81, 72–92.
Vogel, T., van Genuchten M. Th., and Cislerova, M., 2000, Effect of the shape of the soil hydraulic functions near saturation on variably-saturated predictions, Adv. in Water Resourses, 24, 505–521.
Vogel, T., van Genuchten, M. Th., and Cislerova, M., 2001, Effects of the shape of the soil hydraulic functions near saturation on variably-saturated flow predictions, Adv. in Water Resources, 24, 133–144.
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Lee, K.S. Effects of hysteresis ink-S-p relationships on the performance of minewaste soil covers. Geosci J 11, 241–247 (2007). https://doi.org/10.1007/BF02913937
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DOI: https://doi.org/10.1007/BF02913937