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Partial sliding along a planar crack weakened by the presence of fluid

机译:沿平面裂缝的部分滑动由于流体的存在而减弱

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Partial sliding along a infinite planar crack that is locally weakened by the presence of fluid is analyzed. Under uniformly applied normal and shear loads the crack surface generates non-uniform frictional resistance that has a local minimum within a penny-shaped fluid-filled domain. After the applied shear load reaches the resistance minimum a circular sliding zone initiates and then spreads around as the applied shear load is gradually increased. The primary focus of this work is to analyze sliding evolution as a function of the applied loads and the induced fluid pressure. The growth of the sliding zone is studied based on the criterion that shear stress intensity factors are zero along the zone boundary. An analytical relation between the radius of the sliding zone and the applied shear load is determined. (C) 2003 Elsevier Ltd. All rights reserved.
机译:分析了沿着无限大平面裂缝的局部滑动,该裂缝由于流体的存在而局部减弱。在均匀施加法向和剪切载荷的情况下,裂纹表面会产生不均匀的摩擦阻力,该摩擦阻力在一分钱形的充满流体的区域内具有局部最小值。在施加的剪切载荷达到阻力最小值之后,一个圆形滑动区域开始,然后随着施加的剪切载荷逐渐增加而四处张开。这项工作的主要重点是分析作为施加载荷和感应流体压力的函数的滑动演化。基于剪切应力强度因子沿区域边界为零的准则研究滑动区域的增长。确定了滑动区域的半径与所施加的剪切载荷之间的解析关系。 (C)2003 Elsevier Ltd.保留所有权利。

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