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- W2809107621 abstract "Elastic modulus of a soil can increase up to 20 times from the fully saturated to dry state. A recent study shows that such hardening can be empirically described by a power law. In light of recent experimental evidence, the author finds that the rate of hardening is highly controlled by soil water retention (SWR) mechanisms of capillarity and adsorption, in which a characteristic transition in modulus can be delineated between the two SWR mechanisms. A generalized elastic modulus function (EMF), based on the previous power law and a new function for adsorptive hardening, is proposed and assessed for nine natural soils from sandy to silty to clayey soils. It is demonstrated that the generalized EMF is far superior than the power law for its clear physical interpretation and close match to the experimental data. The analysis indicates that the transition zones between capillary and adsorption are different for SWR and EMF behavior. The affected range for adsorptive water content for EMF is ~2 times of the maximum adsorptive water content for SWR for almost all types of soils, indicating an earlier onset of mechanical effect due to the rapidly loss of capillary water during drying." @default.
- W2809107621 created "2018-06-29" @default.
- W2809107621 creator A5054598888 @default.
- W2809107621 date "2018-06-20" @default.
- W2809107621 modified "2023-10-18" @default.
- W2809107621 title "Generalized Elastic Modulus Equation for Unsaturated Soil" @default.
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- W2809107621 doi "https://doi.org/10.1061/9780784481677.002" @default.
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