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基于修正系数的岩石本构关系研究

Discussion of constitutive relation of rocks based on correction factor

  • 摘要: 为对具有原始微元破坏的工程岩石建立更切合实际的本构关系,通过引入修正系数得到原始损伤部分与岩石整体部分的关系,并基于Weibull随机分布和损伤力学理论,在微元破坏符合摩尔-库仑准则的条件下,采用理论推导与试验验证相结合的方法,建立了基于修正系数的岩石损伤本构关系,并以红砂岩常规力学特性试验验证其合理性。结果表明:通过该本构关系获得的理论曲线与试验曲线较为吻合,能够较好的反映岩石变形破坏阶段的特征;受荷过程中,岩石以原始损伤为基准进一步损伤,最终完全破坏;模型参数m和F0的变化均对岩石损伤关系有一定影响,随着F0变化,弹性阶段、峰值应力和相应应变以及最终达到完全破坏时的应变都呈现一致性变化,影响岩石脆延性;随着m变化,弹性阶段及峰值点有所变化但不明显,峰值应力、峰后损伤程度影响较大;随着修正系数γ变化,峰前峰后同一应变对应的应力均发生变化,但γ的取值对理论曲线的发展趋势及峰值点的大小和位置没有影响。

     

    Abstract: In order to establish a more realistic constitutive relation to the engineering rocks with original micro-failure,the relationship between the original damage part and the whole part of the rock was obtained by introducing the correction coefficient. Based on the Weibull random distribution and damage mechanics theory, and under the condition of Coulomb criterion, the combination of theoretical derivation and experimental verification were used to establish the damage constitutive relation of rock based on the correction coefficient. The rationality of the red sandstone was verified by the conventional mechanical properties test. The results show that the theoretical curve obtained by the model is in good consistent with the experimental curve, which can better reflect the characteristics of various rock deformation and failure stages. In the process of loading, the rock is further damaged on the basis of original damage, and ultimately completely failed; The changes of the model parameters m and F0 have an effect on the rock damage model. With the change of F0 , the elastic phase, the peak stress and the corresponding strain, and the strain just reaching the complete failure show a consistent change, affecting the brittleness and ductilityof the rock.As the change of m, the elastic phase and the peak point change but are not obvious, the peak stress and post-peak damage degree have a greater influence. With the change of correction coefficient , the stress corresponding to the same strain changes before and after the peak changes. However, the value of γ has no effect on the development trend of the theoretical curve, nor does it change the size and position of the peak point.

     

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