Abstract
Regularities in the excitation and relaxation of rock failure were revealed in a series of laboratory experiments. Similar regularities are found also in natural conditions. A physical idea and its mathematical description are suggested for explaining the obtained experimental data. The aim of the experiments was to understand the character of excitation of the failure, triggered by the external impact, and its relaxation after the cessation of the pressure, depending on the intensity of the acting stresses. Different rates of increase in the initiating strains result in different acoustic responses that reflect the development of failure. At the higher rates of deformation, the observed process was similar to the aftershock sequences, and at the lower, to the seismic swarms. The character and parameters of the acoustic response change with the increase in the acting strains. The patterns of the changes exhibit several regularities. In case of the swarm-like activity, the time of maximum activity (and, correspondingly, the beginning in its decay) increases with the increase in acting strains. In case of the aftershock-like activity, the level of applied strains determines the parameters of the Omori’s law. The delay in the power-law’s decrease in activity increases with the growth of the load (similar to the increasing time until the beginning of the decay in the swarm-like activity). Similar regularities are defined in natural conditions in the experiments on the rock’s failure induced by water infusion into a borehole (Soultz-sous-Forêts, France). A hypothesis of competitive excitation and relaxation is suggested for explaining the observed experimental data. Mathematical modeling has confirmed the validity of this hypothesis.
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Original Russian Text © V.B. Smirnov, A.V. Ponomarev, P. Benard, A.V. Patonin, 2010, published in Fizika Zemli, 2010, No. 2, pp. 17–49.
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Smirnov, V.B., Ponomarev, A.V., Benard, P. et al. Regularities in transient modes in the seismic process according to the laboratory and natural modeling. Izv., Phys. Solid Earth 46, 104–135 (2010). https://doi.org/10.1134/S1069351310020023
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DOI: https://doi.org/10.1134/S1069351310020023