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Subcritical crack growth of edge and center cracks in façade rock panels subject to periodic surface temperature variations

机译:受表面温度周期性变化影响的立面岩石面板边缘和中心裂纹的亚临界裂纹扩展

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摘要

This paper examines subcritical cracking in a rock panel or slab containing either a pre-existing edge or a center crack perpendicular to the panel surface. The panel is subject to periodic surface temperature variation on one side of the panel while the other is kept at a constant temperature. The thermally induced stress intensity factors are determined using superposition technique by employing the fundamental point load solution for an edge crack or a center crack in a slab of finite thickness. Rock panel is modeled as a long elastic strip with either a free or a fully constrained lateral end condition. The temperature variations versus time at various depths of the rock panel appear roughly as a sinusoidal function. The lateral thermal stress for the free end case is larger than the constrained end case; whereas stress intensity factors for both edge and center cracks in the constrained end slab are 1000 times larger than that of free end case. Subcritical crack propagation in rock panels on façade is then estimated as a function of time. This subcritical crack propagation continues until a critical crack size is attained and the rock panel will fail under wind load. This new theoretical framework provides a new paradigm to examine the mechanisms of time-dependent cracking in rock panels on façade of buildings.
机译:本文研究了岩石面板或平板中的亚临界裂纹,该裂纹包含垂直于面板表面的预先存在的边缘或中心裂纹。面板在面板的一侧上经受周期性的表面温度变化,而另一侧保持在恒定温度下。使用叠加技术,通过对有限厚度平板中的边缘裂纹或中心裂纹采用基点载荷解,可以确定热诱导应力强度因子。岩石面板被建模为具有自由或完全约束的横向端部条件的长弹性条。在岩石面板的各个深度处,温度随时间的变化大致表现为正弦函数。自由端盒的横向热应力大于受约束端盒的热应力。而受约束端板中边缘和中心裂纹的应力强度因子是自由端情况的1000倍。然后,根据时间估算出外立面岩石面板中的亚临界裂纹扩展。这种亚临界裂纹的传播一直持续到达到临界裂纹尺寸,并且在风荷载作用下,岩石面板将失效。这个新的理论框架提供了一种新的范式,以检验建筑物立面上的岩板中随时间变化的开裂机理。

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  • 作者

    Chau, K.T.; Shao, Jian-Fu;

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  • 年度 2006
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  • 原文格式 PDF
  • 正文语种 en
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