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Experimental characterization of Himalayan limestone

机译:喜马拉雅石灰石的实验表征

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In the present work, dynamic stress-strain response of Himalayan limestone is tested under high loading rates using 38 mm split Hopkinson pressure bar (SHPB) device. The physical and static mechanical properties of limestone are also determined. Petrological studies of limestone are carried out through X-ray diffraction (XRD) test and scanning electron microscope (SEM) test. In the SHPB tests, it is observed from the stress-strain response that the dynamic peak stress increases with increasing strain rate whereas the elastic modulus does not show any clear trend with increase in strain rate. Dynamic force equilibrium at the incident and transmission bar ends of the rock samples is attained in all tests till the failure of the rock samples. Dynamic increase factor (DIF) for the rock is determined at a particular strain rate by comparing the dynamic to static peak compressive stress and a correlation equation has been proposed herein.
机译:在目前的工作中,使用38 mm分裂霍普金森压棒(SHPB)装置的高装载速率测试喜马拉雅石灰石的动态应力 - 应变响应。还确定了石灰石的物理和静态力学性能。通过X射线衍射(XRD)试验和扫描电子显微镜(SEM)测试进行石灰石的岩石学研究。在SHPB测试中,从应力 - 应变响应观察到动态峰值应力增加随着应变率的增加而增加,而弹性模量没有显示出任何明显的趋势随着应变率的增加。在岩石样本的入射和传动杆端部处的动态力平衡在所有测试中获得直至岩石样品的失效。通过比较动态到静态峰值压缩应力和本文提出了相关方程,以特定的应变速率确定岩石的动态增加因子(DIF)。

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