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Studies of Specific Energy Fracture of Ice Using Method Test Samples on Uniaxial Compression

机译:使用方法测试样品对单轴压缩的特定能量骨折的研究

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The most well-known method of determining specific energy fracture of ice is the falling hard spheres method (Drop Ball Test -DBT), when the value of this magnitude is calculated as the ratio of the spent on fracture of ice energy of sphere after it struck on to ice surface to volume of the fractured ice in a sphere imprint in the ice. Earlier studies have shown that the ice crumbling layer by layer in such experiments, and specific energy fracture of ice is fairly stable, with the expressed the temperature dependence of ice only and not dependent on mass and velocity of indenter. But localization processes fracture the ice in the array is different from development fracture in the edge of ice field limited thickness, when ice sheet dissected by the vertical radial cracks and splitting by horizontal cracks on the trapezoidal and wedge-shaped blocks, which not separated from ice cover array in the distance from the contact zone. In this study adopted a form of ice samples trapezoidal beams such as in nature, as well as the scheme of deformation and fracture of samples like the fracture of the edges of these blocks in contact with the surface of penetration into the ice cover of the leg of structure. The objective of the laboratory experiments is the approbation of the testing method axial compression samples of ice trapezoidal and wedge-shaped to determine the specific energy of mechanical fracture of ice.
机译:确定冰的比能量骨折的最公知的方法是降硬球方法(落球试验-DBT),当该幅值的值作为的比率被计算的花费在后球的冰能量的断裂撞击到冰表面到裂缝冰的体积在冰球形印记。早先的研究已经表明,通过冰在此类实验层,和冰的比能量断裂破碎层是相当稳定的,与表达的冰的温度依赖性,并且不依赖于质量和压头的速度。但本地化流程断裂阵列中的冰是在冰场有限厚度的边缘,当冰片由垂直径向裂纹和分离由在梯形和楔形块横向裂缝,其不从分离解剖从开发断裂不同冰覆盖阵列中从接触区的距离。在这项研究中采用的冰样本的形式在本质上是梯形梁等,以及变形的样品的像这些块中的与渗透的表面接触的边缘的断裂插入腿部的冰覆盖的方案和断裂的结构。实验室实验的目的是冰梯形的楔形,以确定冰的机械断裂的比能量的测试方法的轴向压缩样本的认可。

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