水物理化学效应下砂岩内变量蠕变本构模型研究
N INTERNAL VARIABLE CREEP CONSTITUTIVE MODEL OF SANDSTONE WITH HYDRO-PHYSICO-CHEMICAL EFFECTS
通过一系列砂岩单轴压缩蠕变试验,获得了干燥、饱水及经不同水化学溶液循环流动作用至水-岩反应平衡砂岩试件的蠕变特性。由于循环流动的水化学溶液对砂岩产生了润滑、软化或泥化等水物理作用以及物质扩散与运移等水化学作用,两者作用使得砂岩内部的组成及结构发生了变化,从而宏观上影响砂岩蠕变特性。内变量理论是一种采用材料内部结构变量(即内变量)描述材料性质的理论。基于试验数据,以不可恢复应变作为内变量,提出了水物理化学效应下砂岩的内变量蠕变本构模型。结果表明,基于不可恢复应变的内变量蠕变本构模型能够很好的反映复杂水物理化学作用下砂岩的蠕变行为。
he creep behavior of sandstones were studied by performing a series of uniaxial compression creep tests on dry, saturated sandstones, and the sandstones with hydro-physico-chemical effect subject to the circulating flow of different hydro-chemical solutions. The circulating flow of hydro-chemical solution had both hydro-physical effect and hydro-chemical effects on the sandstones, which changed the internal constituent and structure, therefore, the creep behavior of sandstones were changed. The internal variable theory is based on the internal structure variable, i.e., interbal variable. Based on the creep data, using irreversible strain as internal variable, the internal variable creep constitutive model of sandstone with hydro-physico-chemical effects was proposed. The fitting of test data into the model shows that the internal variable creep model is capable of describing the creep behavior of sandstones under complicated hydro-physico-chemical effects.
乔丽苹、王者超
水工材料
砂岩水物理化学作用不可恢复应变内变量蠕变本构模型
sandstonehydro-physico-chemical effectirreversible straininternal variablecreep constitutive model
乔丽苹,王者超.水物理化学效应下砂岩内变量蠕变本构模型研究[EB/OL].(2014-01-02)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/201401-68.点此复制
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