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Electromagnetic Interference in Measurements of Radial Stress During Split Hopkinson Pressure Bar Experiments

机译:分裂霍普金森压力棒实验期间测量径向应力的电磁干扰

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摘要

Split Hopkinson pressure bar experiments on soils are often carried out using a rigid steel confining ring to provide plane strain conditions, and measurements of the circumferential strain in the ring can be used to infer the radial stress on the surface of the specimen. Previous experiments have shown evidence of irregular electromagnetic interference in measurements of radial stress, which obscures the signals and impedes analysis. The development of robust constitutive models for soils in blast and impact events relies on the accurate characterisation of this behaviour, and so it is necessary to isolate and remove the source of interference. This paper uses an induction coil to identify the source of the anomalous signals, which are found to be due to induced currents in the gauge lead wires from the movement of magnetised pressure bars (martensitic stainless steel, 440C). Comparative experiments on sand and rubber specimens are used to show that the deforming soil specimen does not make a significant contribution to this activity, and recommendations are made on reducing electromagnetic interference to provide reliable radial stress measurements.
机译:在土壤上进行的霍普金森分流式压力棒实验通常使用刚性钢约束环来进行,以提供平面应变条件,并且可以使用对环中周向应变的测量来推断样品表面的径向应力。先前的实验已经显示出在径向应力测量中出现不规则电磁干扰的证据,这会干扰信号并阻碍分析。针对爆炸和撞击事件中土壤的鲁棒本构模型的开发依赖于这种行为的准确表征,因此有必要隔离并消除干扰源。本文使用感应线圈来识别异常信号的来源,发现该异常信号是由于磁化压力棒(马氏体不锈钢,440C)的运动引起的表层导线中的感应电流所致。通过在沙子和橡胶样品上进行的对比实验表明,变形的土壤样品对此活动没有显着贡献,并建议减少电磁干扰以提供可靠的径向应力测量。

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