Chapter
Apr 26, 2012
Meso-Scale Heterogeneity Effects on Excess Pore Water Pressure Dissipation
Publication: GeoFlorida 2010: Advances in Analysis, Modeling & Design
Abstract
Soil properties such as void ratio, hydraulic conductivity and volume compressibility, which determine consolidation process, are usually spatially varying in natural soils. Such spatial variability of consolidation-related soil properties promotes the specific patterns of the excessive pore water pressure dissipation during consolidation process with respect to the heterogeneity configuration, which is not the same as the typical ones shown at homogeneous soils. This study highlights specific characteristics of consolidation at heterogeneous soils explored by numerical simulations.
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GeoFlorida 2010: Advances in Analysis, Modeling & Design
Pages: 656 - 663
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© 2010 American Society of Civil Engineers.
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Published online: Apr 26, 2012
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School of Civil and Environmental Engineering, Kookmin University, Seoul, Korea. E-mail: [email protected]
School of Civil and Environmental Engineering, Kookmin University, Seoul, Korea. E-mail: [email protected]
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