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Determination of Dynamic-Compressibility Parameters and of Shear Strength for a Ground Medium by the Striker-Penetration Method

机译:用Striker-穿透法确定地面介质的动态可压缩性参数和抗剪强度

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Study of the behavior of soft ground media within a wide range of pressures remains one of the problems of current interest in mechanics of a deformable solid. Traditionally, the determination of the deformation and strength properties of ground media is carried out experimentally with simultaneous measurements of the stress-strain-tensor components as functions of time. Field experimental studies of explosion waves in sandy grounds with disturbed and undisturbed structures at pressures below 100 atm were performed, e.g., in [1]. In dynamic tests [2] of ground samples in an elastic yoke supplied with tensile sensors, pressures attain on the order of 1000 atm. These experiments yield us valuable information on the compression and shear strengths of ground media. However, performing these experiments meets significant technical difficulties. In plane-wave experiments [2, 3], pressures of 104 atm had been attained but only compressibility (Hugoniot adiabat) of the ground medium was determined. Thus, efficient methods for studying the elastoplastic properties of ground media in a wide range of pressures have been absent up to now.
机译:研究软土介质在较大压力范围内的行为仍然是可变形固体力学中当前关注的问题之一。传统上,地面介质的变形和强度特性的确定是通过对应力-应变-张量分量随时间的变化进行同步测量而进行的。例如,在[1]中,在压力低于100atm的具有扰动和无扰动结构的沙质地面上,进行了爆炸波的现场实验研究。在带有张力传感器的弹性叉架中的地面样品的动态测试[2]中,压力达到1000 atm的数量级。这些实验为我们提供了有关地面介质抗压强度和抗剪强度的有价值的信息。但是,进行这些实验遇到了重大的技术难题。在平面波实验中[2,3],已达到104个大气压的压力,但仅确定了地面介质的可压缩性(Hugoniot绝热材料)。因此,到目前为止,还没有有效的方法来研究大范围压力下地面介质的弹塑性特性。

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