4.5 Article

Revisiting the Fundamental Concepts of Soil Mechanics Using the General Effective Stress Concept for Saturated Geomaterials

Journal

INTERNATIONAL JOURNAL OF GEOMECHANICS
Volume 23, Issue 1, Pages -

Publisher

ASCE-AMER SOC CIVIL ENGINEERS
DOI: 10.1061/(ASCE)GM.1943-5622.0002617

Keywords

General effective stress; Archimedes' principle; Submerged unit weight; Seepage force; Critical hydraulic gradient

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This paper defines four fundamental concepts for saturated geomaterials under normal and high pressures using the general effective stress (GES) concept. The four concepts include buoyant force, submerged unit weight, seepage force, and critical hydraulic gradients. By comparing four typical GES expressions and their impacts on the definition of the four concepts, the results suggest their profound significance for geotechnical applications and the need for further validation.
This paper presents a work to define four fundamental concepts, namely, buoyant force, submerged unit weight, seepage force, and critical hydraulic gradients, for saturated geomaterials including soils, rocks, and concrete under normal and high pressures using the general effective stress (GES) concept along with Terzaghi's effective stress. In particular, four typical GES expressions are used for this purpose, and their impacts on the definition of the four concepts are compared based on available experimental evidence in the literature. The results suggest that (1) Terzaghi's effective stress can be physically validated in the context of Archimedes' principle for soils under normal conditions; (2) the generalized buoyant force on the unit volume of saturated geomaterials is the product of the unit weight of pore fluid and the GES coefficient tensor; and (3) the generalized seepage force theoretically acts in the direction of pore fluid flow only when the GES coefficient tensor is proportional to the permeability coefficient tensor. These four fundamental concepts have a profound significance for geotechnical applications with GES and thus merit further validation with adequate laboratory and in situ observations.

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