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Determination of principal residual stresses’ directions by incremental strain method

机译:用增量应变法确定主要残余应力的方向

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The ring-core method is the semi-destructive experimental method used for evaluation of the homogeneous and non-homogeneous residual stresses, acting over depth of drilled core. By using incremental strain method (ISM) for the residual state of stress determination, this article describes procedure how unknown directions and magnitudes of principal residual stresses can be determined. Finite element method (FEM) is used for the numerical simulation of homogenous residual state of stress. Relieved strains on the top of the model ’ s core are measured by the three-element strain gauge, turned by the axis of strain gauge “ a ” from the direction of the principal stress sigma 1 about unknown angle α . Depth dependent magnitudes of relieved strains, their differences and set of known values of calibration coefficients K 1 and K 2 or relaxation functions A and B are used together for determination of the angle α and for re-calculation of principal stresses.
机译:环形岩心法是一种半破坏性实验方法,用于评估作用在钻芯深度上的均质和非均质残余应力。通过使用增量应变法(ISM)确定残余应力状态,本文介绍了如何确定未知方向和主要残余应力大小的过程。有限元方法(FEM)用于均质残余应力状态的数值模拟。通过三元素应变仪测量模型核心顶部的释放应变,并由应变仪“ a”的轴线从主应力sigma 1的方向绕未知角度α旋转。取决于深度的释放应变的大小,它们的差异以及校准系数K 1和K 2或松弛函数A和B的一组已知值一起用于确定角度α和重新计算主应力。

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