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Correlation of Reservoir and Earthquake by Multi Temporal-Spatial Scale Flow Driven Pore-Network Crack Model in Parallel CPU and GPU Platform

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Part of the book series: Lecture Notes in Earth System Sciences ((LNESS))

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Abstract

Coulomb failure assumptions. Jaeger and Cook (Fundamentals of rock mechanics. Methuen, New York, 1969) is used to evaluate the earthquake trigger, and pore pressure (Biot, J Appl Phys 12:155, 1941; 26:182, 1955; 78:91, 1956; J Geophys Res 78:4924, 1973) parts reflect the effect of reservoir which closed to the earthquake slip. Fluid flow driven pore-network crack model (Zhu and Shi, Theor Appl Fract Mech 53:9, 2010) is use to study the reservoir and earthquake. Based on the parallel CPU computation and GPU visualization technology, the relationship between the water-drainage sluice process of the Zipingpu reservoir, stress triggers and shadows of 2008 Wenchuan \(\text{ M}_{\mathrm{s}}\) 8.0 earthquake and porosity variability of Longmenshan slip zone have been analyzed and the flow-solid coupled facture mechanism of Longmenshan coseismic fault slip is obtained.

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Correspondence to B. J. Zhu .

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Zhu, B., Liu, C., Shi, Y., Yuen, D. (2013). Correlation of Reservoir and Earthquake by Multi Temporal-Spatial Scale Flow Driven Pore-Network Crack Model in Parallel CPU and GPU Platform. In: Yuen, D., Wang, L., Chi, X., Johnsson, L., Ge, W., Shi, Y. (eds) GPU Solutions to Multi-scale Problems in Science and Engineering. Lecture Notes in Earth System Sciences. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-16405-7_19

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