The stress-strain of porous media is totally different from that of continuous solid materials. Terzaghi effective stress principle, as the cornerstone of soil mechanics, fits well for stress-strain of soils but fails to fit for cemented porous media. Many researchers are dedicated to propose a more comprehensive effective stress principle. By combining previous effective stress equations proposed by Skempton, Bishop, and Lade & de Boer, a more accurate and comprehensive effective stress constitutive equation is derived. A homogeneous coefficient ω, a stress concentration coefficient β, and a cemented coefficient λ for effective stress principle of all types of pore media are proposed. Appropriate experiments including three types of porous media, namely soils, rocks, and ceramics are designed. The strains of soils, rocks, and ceramics are tested in different confining pressure and fluid pressure. The results show that (a) the strain of soils is mostly caused by intergranular strain and λ is nearly 0, (b) the strain of ceramics is mainly caused by grains strain and λ is more close to 1 − φ, (c) the strain of rocks is combined with grains strain and intergranular strain and 0 < λ < 1 − φ. Three strain patterns of porous media are controlled by the cemented coefficient and the stress conditions. Demonstrated by theoretical derivation and experimental test, the new effective stress can be widely used to all types of porous media.
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