Development of a Model of a GPR Section of a Frozen Rock Mass with a Crack

K. Sokolov, R. A. Dyagileva, P. Popkov
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Abstract

Summary The results of research on the development of a wave field model obtained during the study of frozen rock mass with crack by GPR are presented. The presence of cracks significantly affects the physical and mechanical properties of rocks, which must be taken into account when planning mining operations and the construction of mining facilities. To establish the peculiarities of manifestation of cracks in the GPR data studied materials of long-term fieldwork in developing areas of alluvial diamond deposits ("Almazy Anabara"), the basic building blocks of GPR and presented in single formula. This formula implemented in program in CKM Matlab, and the results of its performance are compared with simulation results in the system of gprMax. The comparison of the obtained results showed the identity of structure of the GPR wave fields. The correlation coefficient between the obtained matrices, without taking into account the low-amplitude values of multiple re-reflections was 0.91. The conducted studies confirmed the possibility of mathematical description of GPR wave field obtained by probing an array of frozen rocks with crack. The high correlation coefficient showed the adequacy of the developed model of radargram which will be finalized taking into account the radiation patterns of existing GPR.
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含裂隙冻结岩体探地雷达剖面模型的建立
摘要介绍了探地雷达在研究含裂纹冻结岩体过程中所获得的波场模型的发展研究结果。裂缝的存在严重影响岩石的物理力学性质,在规划采矿作业和建设采矿设施时必须考虑到这一点。为了建立探地雷达数据中裂缝表现的特殊性,研究了冲积型金刚石矿床(“Almazy Anabara”)开发地区长期野外工作资料,将探地雷达的基本组成部分用单一公式表示出来。该公式在CKM Matlab中编程实现,并与gprMax系统中的仿真结果进行了比较。所得结果的比较表明了探地雷达波场结构的同一性。在不考虑多次重反射低幅值的情况下,得到的矩阵之间的相关系数为0.91。所进行的研究证实了用数学方法描述探地雷达探测阵列含裂纹冻结岩石波场的可能性。高相关系数表明所开发的雷达图模型的充分性,该模型将考虑到现有探地雷达的辐射分布而最终确定。
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