首页> 外文期刊>Journal of thermal stresses >REFLECTION AND DIFFRACTION OF PLANE TEMPERATURE-STEP WAVES IN ORTHOTROPIC THERMOELASTIC SOLIDS
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REFLECTION AND DIFFRACTION OF PLANE TEMPERATURE-STEP WAVES IN ORTHOTROPIC THERMOELASTIC SOLIDS

机译:正交各向异性热塑性弹性体中平面温度-阶跃波的反射和衍射

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摘要

For either Fourier model or model with one or two relaxation times, a plane temperature-step (shock) wave can travel without attenuation at constant speeds in orthotropic solids. For travel not in a principal plane, the temperature step generates for all traction components plane step-stress waves that travel with the same speed. For travel in a principal plane, some traction signals uncouple and travel as rotational (perhaps non-shock) waves. Reflection of a temperature-step wave at a traction-free surface, and its diffraction by a crack, are studied for the Fourier model version of this case. Surface temperature changes, and temperature decreases ahead of the crack edge, but increases behind it. For a crack initially closed by compression the incident wave must generate tension, but it need not exceed the pre-stress in magnitude to produce opening.
机译:对于傅立叶模型或具有一或两个弛豫时间的模型,平面温度阶跃(冲击)波可以在正交各向异性固体中以恒定速度传播而不会衰减。对于不在主平面中的行进,温度阶跃会为所有牵引分量生成以相同速度行进的平面阶跃应力波。对于在主平面上行驶,一些牵引信号会解耦并以旋转(也许非冲击)波的形式行驶。对于这种情况的傅里叶模型,研究了温度阶跃波在无牵引力的表面的反射及其在裂缝中的衍射。表面温度发生变化,并且温度在裂纹边缘之前降低,但在裂纹边缘之后升高。对于最初通过压缩而闭合的裂纹,入射波必须产生拉力,但是它不必超过预应力的大小即可产生开裂。

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