Abstract
Coulomb failure stress changes (ΔCFS) are used in the study of reservoir-induced seismicity (RIS) generation. The threshold value of ΔCFS that can trigger earthquakes is an important issue that deserves thorough research. The M s6.1 earthquake in the Xinfengjiang Reservoir in 1962 is well acknowledged as the largest reservoir-induced earthquake in China. Therefore, it is a logical site for quantitative calculation of ΔCFS induced by the filling of the reservoir and for investigating the magnitude of ΔCFS that can trigger reservoir seismic activities. To better understand the RIS mechanism, a three-dimensional poroelastic finite element model of the Xinfengjiang Reservoir is proposed here, taking into consideration of the precise topography and dynamic water level. We calculate the instant changes of stress and pore pressure induced by water load, and the time variation of effective stresses due to pore water diffusion. The ΔCFS on the seismogenesis faults and the accumulation of strain energy in the reservoir region are also calculated. Primary results suggest that the reservoir impoundment increases both pore pressure and ΔCFS on the fault at the focal depth. The diffusion of pore pressure was likely the main factor that triggered the main earthquake, whereas the elastic stress owing to water load was relatively small. The magnitude of ΔCFS on seismogenesis fault can reach approximately 10 kPa, and the ΔCFS values at the hypocenter can be about 0.7–3.0 kPa, depending on the fault diffusion coefficient. The calculated maximum vertical subsidence caused by the water load in the Xinfengjiang Reservoir is 17.5 mm, which is in good agreement with the observed value of 15 mm. The accumulated strain energy owing to water load was only about 7.3×1011 J, even less than 1% of the seismic wave energy released by the earthquake. The reservoir impoundment was the only factor that triggered the earthquake.
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References
Carder D S. Seismic investigations in the Boulder Dam area 1940–1944 and the influence of reservoir loading on local earthquake activity. Bull Seismol Soc Amer, 1945, 35: 175–192
Yu P Q, Kong F J. Discussion the reservoir seismic geological conditions. Crustal Deform Earthq, 1983, 3: 71–81
Xia Q F. The basic parameters of the typical reservoir-induced earthquake cases in the World (in Chinese). Chin J Geol Hazard Control, 1992, 3: 95–100
Liu Y Z, Ma J, Jiang T, et al. Analysis of effect of reservoir water seepage and loading on theoccurrence of earthquakes. Seismol Geol, 2010, 32: 570–585
Guang Y H. The relations between the key element of reservoir and reservoir earthquake. South Chin J Seismol, 1988, 8: 79–85
Li Z W. The relation between the reservoir induced earthquakes and geologic structures. Seismol Geol, 1981, 3: 61–69
Terzaghi K. Die Berechnung der Durchlassigkritsziffer des Tones aus dem Verlauf Der Hydrodynamicschen Spannugsers Cheinungen. Sbe Akad Wiss Wien, 1923, 132: 105–132
Yi L X, Wang G C, Li L F. Hydrogeological structure and reservoir induced seismicity. Hydrogeol Engineering Geol, 2004, 2: 29–32
Yi L X, Che Y T, Wang G C. Retrospection and prospect of the research on reservoir induced seismicity. South Chin J Seismol, 2003, 23: 28–37
Hu Y L, Chen X C. Discussion on the reservoir-induced earthquakes in China and some problems related to their origin. Seismol Geol, 1979, 1: 45–57
Du Y L, Wang H T, Yuan L W. Analysis and research of China’s reservoir induced seismicity. Earthquake, 2008, 28: 39–51
Ding Y Z, Pan J X, Xiao A Y, et al. Tectonic environment of reservoir induced earthquake in Xinfengjiang reservoir area. Seismol Geol, 1983, 5: 63–74
Ding Y Z. The reservoir-induced earthquakes in China. South Chin J Seismology, 1989, 9: 64–72
Xu Y J. On the Earthquakes induced by impounding reservoir. Chin J Rock Mech Eng, 1984, 3: 66–74
Bell M L, Nur A. Strength changes due to reservior-induced pore pressure and stresses and application to Lake Oroville. J Geophys Res, 1978, 83: 4469–4483
Talwani P, Acree S. Pore press diffusion and the mechanism of reservoir-induced seismicity. Pure Appl Geophys, 1984, 122: 947–965
Talwani P. On the nature of reservoir-induced seismicity. Pure Appl Geophys, 1997, 150: 473–492
Roeloffs E A. Fault stability changes induced beneath a reservoir with cyclic variations in water level. J Geophys Res, 1988, 93: 2107–2124
Simpson D W, Gharib A A, Kebeasy R M. Induced seismicity and changes in water level at Aswan reservoir. Gerlands Beitr Geophys, 1990, 99: 191–201
Gough D I, Gough W L. Stress and deflection in the lithosphere near Lake Kariba. Geophys J Roy Astron Soc, 1970, 21: 70–101
Chen Y. Is the Wenchuan Earthquake induced by Zipingpu reservoir? Sci China Ser D-Earth Sci, 2009, 52: 431–433
Ma W T, Xu C M, Zhang X D, et al. Study on the relationship between the reservoir-induced seismicity at Zipingpu reservoir and the Ms 8.0 Wenchuan earthquake. Seismol Geol, 2011, 33: 175–190
Lei X L, Ma S L, Wen X Z, et al. Integrated analysis of stress and regional seismicity by surface loading—A case study of Zipingpu reservoir. Seismol Geol, 2008, 30: 1046–1064
Lei X. Possible roles of the Zipingpu Reservoir in triggering the 2008 Wenchuan earthquake. J Asian Earth Sci, 2010, 40: 844–854
Ge S M, Liu M, Lu N, et al. Did the Zipingpu Reservoir trigger the 2008 Wenchuan earthquake? Geophys Res Lett, 2009, 36: 1–5
Zhang B, Shi Y L. A discussion on the influences of Zipingpu reservoir on the stability of faults in the neighborhood. J Grad School Chin Acad Sci, 2010, 27: 755–762
Zhou B, Xue S F, Deng Z H, et al. Relationship between the evolution of reservoir-induced seisimicity in space-time and the process of reservoir water body loading-unloading and water infiltration-a case study of Zipingpu reservoir. Chin J Geophys, 2010, 53: 2651–2670
Gahalaut K, Gahalaut V K. Effect of the Zipingpu reservoir impoundment on the occurrence of the 2008 Wenchuan earthquake and local seismicity. Geophys J Int, 2010, 183: 277–285
Zhu B J, Cheng H H, Liu C, et al. Porosity and permeability evolution and evaluation in ani-sotropic porosity multiscale-multiphase-multicomponent structure. Chin Sci Bull, 2011, 56: 1–6
Zhu B J, Liu C, Shi Y L, et al, Apllication of flow driven pore-network crack model to Zipingpi reservoir and Longmenshan slip. Sci China Ser E-Physic Sci, 2011, 54: 1–9
Shen C G, Chen H Q, Zhang C H, et al. The influence of Xinfengjiang reservoir-induced earthquake to the dams. Sci China Ser A, 1974, 2: 184–205
Wang M Y, Yang C Y, Hu Y L, et al. The study on the mechanisms of Xinfengjiang reservoir-induced earthquake. Sci China Ser A, 1976, 1: 85–97
Ding Y Z. The Reservoir-Induced Earthquake. Beijing: Seismological Press, 1989. 10–60
Shen L Y, Chang B Q, Wu M B. Application of the stress-pore pressure coupled theory of porous medium to the research of inducing earthquakes at Xinfengjiang Reservoir. Earthq Res Chin, 1992, 8: 36–43
Wei B L. Focal stress field and tectonic stress field of the Xinfengjiang reservoir induced earthquakes. Seismol Geol, 1981, 3: 75–79
Chen Y M. Research on the focal mechanism of Xinfengjiang reservoir earthquake and its small earthquake. South Chin J Seismol, 1982, 2: 64–71
Gong H Q. The causes of the Xinfengjiang Reservoir-induced earthquake. South Chin J Seismol, 1982, 2: 72–78
Chen L, Talwani P. Reservoir-induced seismicity in China. Pure Appl Geophys, 1998, 153: 133–149
Herbert F W. Theory of Linear Poroelasticity with Applications to Geomechanics and Hydrogeology. Princeton: Princeton University Press, 2000. 4–10
Biot M A. General theory of three-dimensional consolidation. J Appl Phys, 1941, 12: 155–164
Biot M A. General solutions of the equations of elasticity and consolidation for a Porous Material. J Appl Mech, 1956, 78: 91–96
Rice J R, Cleary M P. Some basic stress diffusion solutions for fluid-saturated elastic porous media with compressible constituents. Rev Geophys Space Phys, 1976, 14: 227–241
Patrick A D, Franklin W S. Physcical and Chemical Hydrogeology. New York: John Wiley & Sons Inc, 1998. 159–180
Shi Y L, Cao J L. Some aspects in static stress change calculation—Case study on Wenchuan earthquak. Chin J Geophys, 2010, 53: 102–110
Li A R, Zhang F F, Zhang K. Discussion on the prediction of reservoir-induced earthquake from enviro nmental conditions of Xinfengjiang reservoir earthquake. South Chin J Seismol, 1992, 12: 88–94
Gong G Y, Xie Y D. Review of laboratory investigation of rock permeability. Chin J Rock Mech Eng, 1989, 3: 219–227
Gong G Y, Xie Y D. Research on the diffusion of pore fluid and in-situ hydraulic diffusivity in the epicentral region of Xinfengjiang reservoir earthquake. Acta Seismol Sin, 1991, 13: 364–371
Xie Y D. Analyzing the hydraulic diffusion and reservoir induced seismicity in Xinfengjiang reservoir area. Plateau Earthq Res, 1996, 8: 27–35
Li S Y, He T M, Yin X J. Introduction to Fracture Mechanics of Rock (in Chinese). Hefei: China Science and Technology University Press, 2010. 2–20
King G C P, Stein R S, Lin J P. Static stress changes and the trgering of earthquake. Bull Seismol Soc Amer, 1994, 84: 935–953
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Cheng, H., Zhang, H., Zhu, B. et al. Finite element investigation of the poroelastic effect on the Xinfengjiang Reservoir-triggered earthquake. Sci. China Earth Sci. 55, 1942–1952 (2012). https://doi.org/10.1007/s11430-012-4470-8
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DOI: https://doi.org/10.1007/s11430-012-4470-8