Abstract
The presence of technological subsurface heat sources in permafrost regions leads to the melting process. It significantly decreases the strength of the geological massif and may lead to the subsidence of the day surface. In this chapter, we investigated the capabilities of the seismic survey for monitoring of this process. To describe the dynamic behavior of thawed zones, the model of the porous fluid-filled medium was used. Its numerical solution in two-dimensional case was obtained with the grid-characteristic method on rectangular grids. It allows to set physically correct contact conditions between elastic and porous media. To increase the simulation precision, the compact scheme for one-dimensional case was proposed and successfully tested. It is based on the extension of the original system with differential consequences. This approach provided the third order of the accuracy on the three-point spatial stencil. Based on a set of computer experiments, the seismic response was analyzed quantitatively and qualitatively.
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This work was supported by the Russian Science Foundation, grant no. 16-11-00100.
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Golubev, V.I., Vasyukov, A.V., Churyakov, M. (2021). Modeling Wave Responses from Thawed Permafrost Zones. In: Favorskaya, M.N., Favorskaya, A.V., Petrov, I.B., Jain, L.C. (eds) Smart Modelling For Engineering Systems. Smart Innovation, Systems and Technologies, vol 214. Springer, Singapore. https://doi.org/10.1007/978-981-33-4709-0_12
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