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Experimental Investigation of the spatial-temporal localization of deformation and damage in sylvinite specimens under uniaxial tension

机译:单轴拉伸下银云母试样变形和损伤的时空局部化实验研究

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A good deal of experimental and theoretical data gained from studying the behavior of salt rocks under compressive loads can serve as a basis for computation of the stress-strain state of the mine field elements. However, the specific features of the deformation behavior of rock salts under the action of tensile stresses are still not clearly understood. With reference to geomechanics the emphasis has been placed mainly on studying the strength properties of the salt rocks under tensile loads. The significance and necessity of exploring the process of strain and damage localization in salt rocks under tension is related to a possibility of transition of the shear crack growth mode in the field of compressive stresses to a mode of rapidly growing tensile cracks due to the appearance of tensile stresses. With this scenario, there always exists probability of failure of the working, in addition to the formation and growth of quasi-vertical cracks in the waterproof stratum. In mining of water -soluble minerals these processes can lead to disastrous effects. This paper is concerned with experimental studying the spatial-temporal localization of the deformation and damage processes in sylvinite under quasi-static tension based on the method of acoustic emission and construction of deformation fields on the specimen surface. A series of quasi-static tensile tests were carried out using the original device for specimen fixture. The loading rate varied in the range from 0.025 mm/min до 0.1 mm/min. During experiments the acoustic emission signals were recorded with the Amsy-5 system (Vallen, Germany) over two frequency ranges of 50-400 kHz and 350-2000 kHz. The construction of the deformation and displacement fields on the specimen surfaces was accomplished through the use of the optical system Strain Master (Germany). A comparative analysis of the constructed deformation fields and the results of acoustic emission allowed us to define special features of the localized deformation and damage. Research was supported by the Russian Foundation of Basic Research (grant № 10-05-96065-р_урал_а, 11-05-96005-р_урал_а, 12-05-00253-a), program of RAS Presidium № 09-П-1-1010.
机译:通过研究盐岩在压缩载荷下的行为而获得的大量实验和理论数据,可作为计算矿场单元应力应变状态的基础。但是,尚不清楚岩石盐在拉伸应力作用下的变形行为的具体特征。关于地质力学,重点主要放在研究盐岩在拉伸载荷下的强度特性。探索在拉伸作用下盐岩中应变和损伤局部化过程的意义和必要性与由于压应力的出现而使压裂领域中的剪切裂纹扩展模式转变为快速扩展的拉伸裂纹模式的可能性有关。拉应力。在这种情况下,除了在防水层中形成和增加准垂直裂缝外,总是存在工作失败的可能性。在水溶性矿物的开采中,这些过程可能导致灾难性的后果。本文基于声发射法和试样表面形变场的构造方法,对准静态拉力作用下,银云母的形变和损伤过程的时空局部化进行了实验研究。使用用于样品固定的原始设备进行了一系列的准静态拉伸测试。加载速率在0.025毫米/分钟至0.1毫米/分钟的范围内变化。在实验过程中,使用Amsy-5系统(德国瓦伦)在50-400 kHz和350-2000 kHz的两个频率范围内记录了声发射信号。通过使用光学系统Strain Master(德国)完成了样品表面变形和位移场的构建。通过对构造变形场和声发射结果的比较分析,我们可以定义局部变形和损伤的特殊特征。俄罗斯基础研究基金会(拨款№10-05-96065-р_урал_а,11-05-96005-р_урал_а,12-05-00253-a),RAS主席团№09-П-1-1010计划支持了该研究。 。

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