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Investigation on mechanical parameters of water-rock interaction

机译:水-岩相互作用的力学参数研究

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The processes are very complex for the coupling of water-rock interaction, and the sensitivity of water for porous media material cracks should be focused for the research of fundamental mechanical properties of rocks. In the present research, the theories and measure technologies of conventional true and pseudo tri-axial tests are also analyzed.The mechanical parameters are obtained by true and pseudo tri-axial tests with/without water pressures. The idea that the tri-axial test is only suitable for the isotropic porous media materials is proposed, the sample of 50mm×50mm×100mmis proposed to conduct the tri-axial test to understand the anisotropic mechanical behaviors of porous media materials. The anisotropic Biot's coefficients and the damaged mechanical parameters under different stress states are obtained by considering the influences of unloading water pressure on porous media materials. The testing results show that variable trends of anisotropic Biot's coefficient in the different directions are not the same. A testing method of limit yield stress determination is suggested, the limit yield stress is equal to the deviatoric stress corresponding to the maximum water pressure between deviatoric stress and water pressure curve for the non-drainage test. The testing results also show the Skempton coefficient disparity is significant, and the mechanism of water pressure action is different under various injections and drainages. It is crucial for damage mechanics and civil engineering to study water-rock interaction.
机译:水-岩石相互作用的耦合过程非常复杂,应将水对多孔介质材料裂缝的敏感性用于研究岩石的基本力学性能。在本研究中,还分析了常规真三轴试验的理论和测量技术,通过在有/无水压下的真三轴试验获得了力学参数。提出了仅适用于各向同性多孔介质材料的三轴试验的思想,建议采用50mm×50mm×100mm的样品进行三轴试验,以了解多孔介质材料的各向异性力学行为。通过考虑卸荷水压对多孔介质材料的影响,获得了不同应力状态下的各向异性毕奥特系数和受损的力学参数。测试结果表明,各向异性比奥特系数在不同方向上的变化趋势不同。提出了极限屈服应力确定的测试方法,极限屈服应力等于不排水试验中偏应力与水压曲线之间的最大水压所对应的偏应力。测试结果还表明,Skempton系数差异显着,并且在各种注入和排水条件下水压作用的机理是不同的。研究水岩相互作用对破坏力学和土木工程至关重要。

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