Dependences of the Omori and Gutenberg–Richter parameters

V. Smirnov, В Б Смирнов, A. Ponomarev, Андрей Викторович Пономарев, S. Stanchits, С А Станчиц, M. Potanina, М. Г. Потанина, A. Patonin, А.В. Патонин, G. Dresen, C. Narteau, P. Bernard, S. Stroganova, С. М. Строганова
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引用次数: 4

Abstract

Laboratory experiments on studying the aftershock regime are carried out with sandstone specimens under different axial loading and uniform compression and constant pore pressure. The aftershock sequences are modeled by the scenario of stepwise increasing axial loading of a specimen with strain control ensuring regular generation of aftershock sequences. The experiments are conducted on intact specimens and on the specimens with preliminarily formed shear macrofractures simulating natural faults. The experiments were conducted with multichannel recording of the acoustic emission (AE) signals which made it possible to locate the AE sources. Several types of the dependence of the acoustic activity relaxation parameters (parameters p and c of the modified Omori law and the Gutenberg–Richter b-value) on the level of acting stresses are revealed. The b-value decreases with the growth of axial stresses at all levels of uniform compression. In the case of fracture on the preexisting fault, the Omori relaxation parameter p increases with the growth of axial stresses whereas parameter c (the time delay before the onset of relaxation) decreases with the growth of axial stresses and increases with the rise of the level of uniform compression. In the case of a fracture of an undamaged specimen, parameter p remains unchanged as the axial stresses grow, whereas parameter c increases slightly. Parameter variations in the case of a complex stress state with both varying deviatoric (differential stresses) and spherical parts (effective pressure) of the stress tensor take on a unified form when expressed in terms of Coulomb stresses. It is hypothesized that the time delay of the aftershock activity relaxation is determined by the kinetics of fracture in accordance with the kinetic concept of strength in solids. This hypothesis is supported by exponential dependence of parameter c on stresses and on the effective strength of the medium revealed in the experiments. Under this hypothesis, the dependences of parameter c on the Coulomb stresses can be unified for different effective strength values with the use of Zhurkov’s formula for durability of materials. The obtained parameter estimates for the dependence of c on strength and stresses suggest that the c value is determined by the difference of the strength and the acting stresses, indicating how far the stress state of the medium is from the critical state corresponding to the ultimate strength.
Omori参数和Gutenberg-Richter参数的相关性
以不同轴向载荷、均压恒孔压条件下的砂岩试件为研究对象,进行了室内试验。余震序列是通过逐步增加试样的轴向载荷和应变控制来模拟的,以确保余震序列的规律产生。实验分别在完整试件和初步形成的模拟自然断裂的剪切大裂缝试件上进行。实验采用多声道声发射(AE)信号记录,使声发射源的定位成为可能。揭示了声活动弛豫参数(修正Omori定律参数p和c和Gutenberg-Richter b值)对作用应力水平的几种依赖类型。均匀压缩各水平下,b值随轴向应力的增大而减小。在已存在断层上发生断裂的情况下,Omori松弛参数p随轴向应力的增大而增大,而参数c(松弛发生前的时间延迟)随轴向应力的增大而减小,随均匀压缩水平的升高而增大。在未损伤试件断裂的情况下,参数p随轴向应力的增加而保持不变,而参数c则略有增加。在复杂应力状态下,当应力张量的偏态(微分应力)和球面(有效压力)都发生变化时,参数的变化以库仑应力表示为统一形式。根据固体中强度的动力学概念,假设余震活动松弛的时间延迟是由断裂动力学决定的。这一假设得到了参数c对应力和实验显示的介质有效强度的指数依赖性的支持。在此假设下,对于不同的有效强度值,参数c对库仑应力的依赖关系可以用材料耐久性的朱尔科夫公式统一。得到的c对强度和应力依赖关系的参数估计表明,c值由强度和作用应力之差决定,表明介质的应力状态离极限强度对应的临界状态有多远。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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