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A Theory of Porous Media for Unsaturated Soils with Immobile Air

Machaček, Jan ; Fuentes, William ; Staubach, Patrick ; Zachert, Hauke ; Wichtmann, Torsten ; Triantafyllidis, Theodoros (2023)
A Theory of Porous Media for Unsaturated Soils with Immobile Air.
In: Computers and Geotechnics, 157
doi: 10.1016/j.compgeo.2023.105324
Artikel, Bibliographie

Kurzbeschreibung (Abstract)

The Theory of Porous Media (TPM) has served as a reliable theory to deduce governing equations for unsaturated soils. In most works, the unsaturated soil is considered as a three-phase medium composed of air, water and solid. This neglects effects caused by the presence of residual water and/or entrapped (immobile) air attached to the particles. In this work, a set of governing equations for unsaturated soils with residual water and entrapped air is deduced. A mass transfer mechanism between the free air and the entrapped air is considered. The present work focuses only on the entrapped air attached to the particles (immobile air), and therefore it is assumed to have the same intrinsic velocity as the solid. This assumption allows to keep the same number of independent kinematic variables as in conventional three-phase theories. The performance of the theory is examined in simulations of water retention curves subjected to suction cycles, as well as in the dynamic analysis of a centrifuge test on a dam subjected to earthquake loading.

Typ des Eintrags: Artikel
Erschienen: 2023
Autor(en): Machaček, Jan ; Fuentes, William ; Staubach, Patrick ; Zachert, Hauke ; Wichtmann, Torsten ; Triantafyllidis, Theodoros
Art des Eintrags: Bibliographie
Titel: A Theory of Porous Media for Unsaturated Soils with Immobile Air
Sprache: Englisch
Publikationsjahr: 21 Februar 2023
Verlag: Elsevier BV
Titel der Zeitschrift, Zeitung oder Schriftenreihe: Computers and Geotechnics
Jahrgang/Volume einer Zeitschrift: 157
DOI: 10.1016/j.compgeo.2023.105324
URL / URN: https://www.sciencedirect.com/science/article/pii/S0266352X2...
Kurzbeschreibung (Abstract):

The Theory of Porous Media (TPM) has served as a reliable theory to deduce governing equations for unsaturated soils. In most works, the unsaturated soil is considered as a three-phase medium composed of air, water and solid. This neglects effects caused by the presence of residual water and/or entrapped (immobile) air attached to the particles. In this work, a set of governing equations for unsaturated soils with residual water and entrapped air is deduced. A mass transfer mechanism between the free air and the entrapped air is considered. The present work focuses only on the entrapped air attached to the particles (immobile air), and therefore it is assumed to have the same intrinsic velocity as the solid. This assumption allows to keep the same number of independent kinematic variables as in conventional three-phase theories. The performance of the theory is examined in simulations of water retention curves subjected to suction cycles, as well as in the dynamic analysis of a centrifuge test on a dam subjected to earthquake loading.

Freie Schlagworte: Air entrapment, Multiphase fluid flow, Residual air, Soil water retention, Theory of porous media
Fachbereich(e)/-gebiet(e): 13 Fachbereich Bau- und Umweltingenieurwissenschaften
13 Fachbereich Bau- und Umweltingenieurwissenschaften > Institut für Geotechnik
Hinterlegungsdatum: 22 Feb 2023 09:50
Letzte Änderung: 22 Feb 2023 09:50
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