Vicente Navarro , Gema Urraca , Gema De la Morena , Erik Tengblad , Laura Asensio
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引用次数: 0
Abstract
This work examines the thermodynamic consistency of the relationship between the strains caused by the rearrangement of the microstructure in an expansive soil and the coupled plastic strains caused by the resulting rearrangement of the macrostructure (strain coupling). Assuming a multi-dissipative process, it is found that, for the energy variation associated with the mass exchange between macro- and microstructure to be consistent with the macroscopic strain dissipation, the strain coupling is determined by the macro- and microstructural constitutive relations, without the need to introduce new and additional external functions to define the coupling. This results in a robust definition of the coupling function under isotropic conditions, with a structure independent of the adopted constitutive models, which consequently does not have to be adjusted heuristically depending on the type of material, the test or whether microstructural swelling or shrinkage occurs.
期刊介绍:
The aim of the Journal is to publish research results of the highest quality and of lasting importance on the subject of geomechanics, with the focus on applications to geological energy production and storage, and the interaction of soils and rocks with the natural and engineered environment. Special attention is given to concepts and developments of new energy geotechnologies that comprise intrinsic mechanisms protecting the environment against a potential engineering induced damage, hence warranting sustainable usage of energy resources.
The scope of the journal is broad, including fundamental concepts in geomechanics and mechanics of porous media, the experiments and analysis of novel phenomena and applications. Of special interest are issues resulting from coupling of particular physics, chemistry and biology of external forcings, as well as of pore fluid/gas and minerals to the solid mechanics of the medium skeleton and pore fluid mechanics. The multi-scale and inter-scale interactions between the phenomena and the behavior representations are also of particular interest. Contributions to general theoretical approach to these issues, but of potential reference to geomechanics in its context of energy and the environment are also most welcome.