Summary
We investigate the influence of temperature on the retention curve of soils. This curve represents the constitutive relation between water content w and suction s, for a given temperature T and a given void ratio e. We present a model based on the differential of suction as a function of T, w and e. When adjusted for a retention curve obtained at a given temperature, this model enables to predict this curve for any temperature. In parallel, we carried out experiments on a clayey silty sand by using a pressure cell immersed in a thermostatic bath. The model was validated by several tests on the clayey silty sand at 20 and 60˚ C. The application of the model to data found in the literature confirms its predictive power for a wide range of porous materials. These results allow us to plot the retention surface, from experimental tests obtained at a given temperature and from modelling. It can be considered as a generalization of the classical retention curve. Finally, we discuss the influence of the void ratio variation during experiments on the curve predicted by the model.
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© 2007 Springer-Verlag
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Salager, S., Youssoufi, M.S.E., Saix, C. (2007). Influence of Temperature on the Water Retention Curve of Soils. Modelling and Experiments. In: Schanz, T. (eds) Experimental Unsaturated Soil Mechanics. Springer Proceedings in Physics, vol 112. Springer, Berlin, Heidelberg. https://doi.org/10.1007/3-540-69873-6_24
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DOI: https://doi.org/10.1007/3-540-69873-6_24
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-540-69872-2
Online ISBN: 978-3-540-69873-9
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