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殷德顺, 陈文, 和成亮. 岩土应变硬化指数理论及其分数阶微积分理论基础[J]. 岩土工程学报, 2010, 32(5).
引用本文: 殷德顺, 陈文, 和成亮. 岩土应变硬化指数理论及其分数阶微积分理论基础[J]. 岩土工程学报, 2010, 32(5).
Theory of geotechnical strain hardening index and its rationale from fractional order calculus[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(5).
Citation: Theory of geotechnical strain hardening index and its rationale from fractional order calculus[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(5).

岩土应变硬化指数理论及其分数阶微积分理论基础

Theory of geotechnical strain hardening index and its rationale from fractional order calculus

  • 摘要: 应变硬化型岩土的三轴试验应力应变曲线能够表现出不同的弯曲程度,而应力应变曲线的弯曲程度是岩土应变硬化能力的体现,但已有的研究中还没有相应的参数来描述岩土的硬化能力。为了获得反映岩土应变硬化能力的参数,从而有助于了解岩土的塑性性能和指导土体的合理承载,根据Hollomon提出的描绘金属塑性拉伸变形的指数方程(经验公式),提出了岩土应变硬化指数理论。通过许多三轴试验,发现岩土应变硬化指数理论提出的岩土应力应变关系符合乘幂函数关系的假设能够被验证,岩土的应变硬化指数能够反映岩土的硬化能力。岩土的力学性质介于理想固体和理想流体之间,其应力应变关系既不遵守胡克定律,也不遵守牛顿黏性定律,而是遵守介于它们之间的某种关系。利用分数阶微积分理论给出了恒应变率加载情况下的土应力应变关系。关系式显示应力应变之间也呈乘幂函数关系,说明岩土分数阶应力应变关系能够为岩土应变硬化指数理论提供理论基础。

     

    Abstract: The curvature of stress-strain curves from triaxial tests on harden soil is a reflection of hardening ability, but there isn’t a parameter of hardening ability in geotechnical mechanics. In order to gain such a parameter that can help us to know plasticity and proper bearing capacity of soil, a theory of geotechnical strain hardening index (TAGSHI) in response to exponential equation (an empirical equation) which Hollomon established from experience in metal tensile deformation is developed. Based on a lot of triaxial tests, it is shown that the assumption in TAGSHI is right, which thinks that stress-strain relationship of soil is the power function in triaxial tests, and the strain hardening index may reflect geotechnical hardening ability. As we all know that geotechnical mechanical property should be intermediate between that of an ideal solid and an ideal fluid, so its stress-strain relation should neither follow the Hook’s law nor obey the Newton's law of viscosity, and it should be consistent with the fractional expression , ( ). The geotechnical stress-strain relation is derived by applying the theory of fractional order calculus operator under the condition of loading with constant strain rate. The analytic results show that the geotechnical stress-strain curves exhibit power relation, and it is consistent with the assumption in TAGSHI. This indicates that the fractional expression , ( ) can give a rationale for TAGSHI.

     

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