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A new multi-scale modeling approach based on hygro-Cosserat theory for self-induced stress in hydrating cementitious mortars

机译:基于Hygro-Cosserat理论的水化水泥砂浆自生应力的多尺度建模新方法

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The present paper focuses on the modeling of internal stresses induced by the restrained autogenous shrinkage of hydrating cementitious matrix in cement-based mortars. At very early age (0-48 h), these self-induced stresses may be relatively high and even critical, especially for cementitious systems with low water-to-cement ratio, since the physico-chemical phenomena involved (hydration and self-desiccation) are particularly intense. To pursue the mentioned objective, an original multi-scale approach based on the application of hygro-Cosserat theory has been developed to model the self-induced stress variation in the cement paste surrounding the aggregates. In fact, the characteristic length scale parameter L_c in the Cosserat theory helps us to reduce the specimen size from macro-scale to micro-scale and even sub-micro-scale due to its explicit size effect features, which is not feasible in the classical theory, i.e. Cauchy-Bolzmann's theory. The self-shrinkage phenomenon at early age has been observed and modeled via the experiments and a freshly defined Cosserat Size effect number (CS) based upon the Representative Volume Element (RVE) concept. The proposed method is capable of treating the internal stress and could be followed by cracks appearance investigation in the cementitious matrix surrounding the sand inclusions, which should occur inside of the RVE of mortar subjected to self-desiccation shrinkage during the hydration process at early age. The occurrence of these micro-cracking networks are confirmed by Scanning Electronic Microscopy (SEM) observations at the interface cement paste/aggregate performed on different mortars at early age. By taking advantage of the time-dependent Finite Element Analysis (FEA), the numerical outcomes are well agreed with the experimental observations coming from SEM. It concludes that the inclusion creates high hygro-stress concentration around the grains: when the number of inclusions increases, this hygro-stress could lead to a micro-crack network through the matrix.
机译:本文重点研究了水泥基砂浆中水化水泥基体自发收缩受限引起的内应力建模。在很早的时候(0-48小时),这些自感应应力可能相对较高,甚至是至关重要的,特别是对于水灰比低的胶结体系,因为涉及物理化学现象(水合作用和自干燥) )特别强烈。为了实现上述目标,已经开发了一种基于应用Hygro-Cosserat理论的原始多尺度方法,以模拟集料周围水泥浆中自生应力变化。实际上,Cosserat理论中的特征长度尺度参数L_c可以帮助我们将样本大小从宏观尺度减小到微米尺度甚至亚微米尺度,这是因为它具有明显的尺寸效应特征,这在经典模型中是不可行的理论,即Cauchy-Bolzmann理论。通过实验以及基于“代表体积元素”(RVE)概念的最新定义的“科塞拉特尺寸效应数”(CS),已经观察到并模拟了早期的自收缩现象。所提出的方法能够处理内应力,并且可以在砂夹杂物周围的胶结基体中进行裂纹外观研究,裂纹应出现在砂浆的RVE内部,并在早期水化过程中受到自干燥收缩。这些微裂纹网络的出现是通过扫描电子显微镜(SEM)观察在早期在不同砂浆上进行的界面水泥浆/集料上的确认。利用时间相关的有限元分析(FEA),数值结果与SEM的实验结果非常吻合。结论是,夹杂物在晶粒周围产生了很高的湿应力集中度:当夹杂物数量增加时,这种湿应力可能导致通过基体的微裂纹网络。

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