Abstract
We observed abnormal changes of the water temperature in Yushu (YSWT) well, China, most of which were followed by earthquakes. This study statistically analyzes the correlation between the magnitude and duration of the anomalies in YSWT and earthquakes in the Tibetan block and its margins. The effectiveness of using observed YSWT data to predict earthquakes was quantitatively examined by the Molchan error diagram method. The results show that (1) the YSWT underwent several abnormal changes marked by “V”-shaped patterns, which might be related to several earthquakes that occurred in the Tibetan block and its margins. The extent and duration of the abnormal changes in the YSWT were linearly related to the magnitude of the earthquake; i.e., the higher the magnitude, the greater the change in the YSWT, and the shorter the duration. (2) Abnormal changes in the YSWT are somewhat predictive of earthquakes with magnitudes ≥5.5 (≥M5.5) within 800 km of the Yushu well and ≥M6.5 earthquakes in the Tibetan block and its margins. The prediction has a probability gain of approximately 2, and the most likely time period for an earthquake to occur is within approximately 3 months after the occurrence of an YSWT anomaly. Most of the anomalies in YSWT appeared before earthquakes in the thrust of block margins. Notably the larger strains from the earthquake did not produce any response. We speculate that the preseismic responses reflect the regional tectonics, such as the motion of the Indian plate, straining sub-blocks of the Tibetan block.
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Asteriadi, G., & Liverato, E. (1989). Pre-seismic responses of underground water level and temperature concerning a 4.8 magnitude earthquake in Greece on October 20. Tectonophysics, 170, 165–169.
Bilham, R., Vinod, K., & Molnar, P. (2001). Himalayan seismic hazard. Science, 293, 1442–1444.
Brodsky, E. E., Roeloffs, E., Woodcock, D., Gall, I., & Manga, M. (2003). A mechanism for sustained groundwater pressure changes induced by distant earthquakes. Journal of Geophysical Research: Solid Earth, 108(B8),2390.
Caine, J. S., & Minor, S. A. (2009). Structural and geochemical characteristics of faulted sediments and inferences on the role of water in deformation, Rio Grande Rift, New Mexico. Geological Society of America Bulletin, 121(9–10), 1325–1340.
Che, Y. T., Liu, W. Z., & Yu, J. Z. (1998). The relationship between crustal fluids and major earthquakes and its implications for earthquake prediction. Seismology and Geology (in Chinese), 20(4), 431–435.
Che, Y. T., & Yu, J. Z. (1997). The focal precursors, field precursors and remote precursors of ground fluid before strong earthquakes and their significance in the earthquake prediction. Earthquake (in Chinese), 17(3), 283–289.
Deng, Q. D., Cheng, S. P., Ma, J., et al. (2014). Seismic activities and earthquake potential in the Tibetan Plateau. Chinese J Geophys. (in Chinese), 57(7), 2025–2042. doi:10.6038/cjg20140701.
Deng, Q. D., Gao, X., Chen, G. H., & Yang, H. (2010). Recent tectonic activity of Bayankala fault-block and the Kunlun Wenchuan earthquakes series of the Tibetan Plateau. Earth Science Frontiers (in Chinese), 17(5), 163–178.
Du, L. T. (2007). Concept renewal from solid earth science to fluid one. Progress in Geophysics (in Chinese), 22(4), 1220–1224.
Faulkner, D. R., & Rutter, E. H. (2003). The effect of temperature, the nature of the pore fluid, and subyield differential stress on the permeability of phyllosilicate rich fault gouge. Journal of Geophysical Research: Solid Earth, 108(B5), 2227. doi:10.1029/2001JB001581.
Fu, Z. Z. (1988). Premonition and dynamic observation of terrestrial heat. Corpus of Crust Structure and Stress (in Chinese), 1, 1–7.
Hadley, K. (1973). Laboratory investigation of dilatancy and motion on fault surfaces at low confining pressures. In R. L. Kovach & A. Nur (Eds.), Proceedings of the conference on tectonic problems of the san andreas fault system (Vol. XIII). Stanford: Stanford University Publications, Geological Sciences.
He, A. H., Zhao, G., & Liu, C. L. (2012). The anomaly characteristics before Wenchuan earthquake and Yushu earthquake in Qinghai Yushu and Delingha geothermal observation wells. Chinese Journal of Geophysical (in Chinese), 55(4), 1261–1268. doi:10.6038/j.issn.0001-5733.2012.04.021.
Hsieh, P. A., Bredehoeft, J. D., & Rojstaczer, S. A. (1988). Response of well aquifer systems to Earth tides: Problem revisited. Water Resources Research, 24(3), 468–472.
Johnston, M. J. S., Hill, D. P., Linde, A. T., Langbein, J., & Bilham, R. (1995). Transient deformation during triggered seismicity from the 28 June 1992 Mw = 7.3 Landers earthquake at Long Valley volcanic caldera, California. Bulletin of the Seismological Society of America, 85, 787–795.
Jordan, T. H. (2006). Earthquake predictability, brick by brick. Seismological Research Letters, 77(1), 3–6. doi:10.1007/s10950-008-9147-6.
Kitagawa, Y., Koizumi, N., & Tsuskutta, T. (1996). Comparison of post-seismic groundwater temperature changes with earthquake-induced volumetric strain release: Yundani hot spring, Japan. Geophysical Research Letters, 23(22), 3147–3150.
Liu, L. B., Roeloffs, E., & Zheng, X. Y. (1989). Seismically induced water level fluctuations in the Wali well, Beijing, China. Journal of Geophysical Research: Solid Earth, 94(B7), 9453–9462, 1978–2012.
Manga, M., Beresnev, I., Brodsky, E. E., Elkhoury, J. E., Elsworth, D., Ingebritsen, S. E., et al. (2012). Changes in permeability caused by transient stresses: Field observations, experiments, and mechanisms. Review of Geophysics, 50, RG2004.
Mogi, K., Mochizuki, H., & Kurokawa, Y. (1989). Temperature changes in an artesian spring at Usami in the Izu Peninsula (Japan) and their relation to earthquakes. Tectonophysics, 159(1-2), 95–108.
Molchan, G. M. (1990). Strategies in strong earthquake prediction. Physics of the Earth and Planetary Interiors, 61(1–2), 84–98.
Molchan, G. M. (1991). Structure of optimal strategies of earthquake prediction. Tectonophysics, 193, 267–276.
Montgomery, D. R., & Manga, M. (2003). Streamflow and water well responses to earthquakes. Science, 300(5628), 2047–2049.
Orihara, Y., Kamogawa, M., & Nagao, T. (2014). Preseismic Changes of the Level and Temperature of Confined Groundwater related to the 2011 Tohoku Earthquake. Scientific reports, 4. doi:10.1038/srep06907
Roeloffs, E. A. (1998). Hydrologic precursors to earthquakes: A review. Pure and Applied Geophysics, 126, 177–209.
Sadovsky, M. A., Nersesov, I. L., Nigmatullaev, S. K., Latynina, L. A., Lukk, A. A., Semenov, A. N., Simbireva, V, I., Ulomov, V. I. (1972). The processes preceding strong earthquakes in some regions of middle Asia. Tectonophysics, 14(3), 295–307. doi: 10.1016/0040-1951(72)90078-9
Shi, Z., & Wang, G. (2014). Hydrological response to multiple large distant earthquakes in the Mile well, China. Journal of Geophysical Research: Earth Surface, 119, 2448–2459.
Shi, Z., & Wang, G. (2016). Aquifers switched from confined to semiconfined by earthquakes. Geophysical Research Letters, 43, 11,166–111,172.
Shi, Z., Wang, G., Manga, M., & Wang, C. Y. (2015). Mechanism of co-seismic water level change following four great earthquakes-insights from co-seismic responses throughout the Chinese mainland. Earth and Planetary Science Letters, 430, 66–74.
Shimamura, H., Ino, M., Hikawa, H., & Iwasaki, T. (1984). Groundwater microtemperature in earthquake regions. Pure and Applied Geophysics, 122(6), 933–946.
Simpson, D. W. (1986). Triggered earthquakes. Annual Review of Earth and Planetary Science, 14(1), 21–42.
Sun, X., & Liu, Y. (2012). Changes in groundwater level and temperature in induced by distant earthquakes. Geosciences Journal, 16(3), 327–337.
Venedikov, A. P., Arnoso, J., & Vieira, R. (2003). VAV: A program for tidal data processing. Computers & Geosciences, 29(4), 487–502. doi:10.1016/S0098-3004(03)00019-0.
Wakita, H. (1975). Water wells as possible indicators of tectonic strain. Science, 189(4202), 553–555.
Wang, C. Y., Liao, X., Wang, L. P., Wang, C. H., & Manga, M. (2016a). Large earthquakes create vertical permeability by breaching aquitards. Water Resources Research, 52(8), 5923–5937.
Wang, B., Ma, Y. C., & Ma, Y. H. (2016b). Variation of water temperature in Yushu well and its correlation with the big earthquakes occurred in Qinghai-Tibet block. Earthquake Research in China, 32(3), 461–468.
Wang, C. Y., Manga, M., Wang, C. H., & Chen, C. H. (2012). Transient change in groundwater temperature after earthquakes. Geology, 40, 119–122.
Wang, C. Y., Wang, L. P., Manga, M., Wang, C. H., & Chen, C. H. (2013). Basin-scale transport of heat and fluid induced by earthquakes. Geophysical Research Letters, 40, 1–5. doi:10.1002/grl.50738.
Yan, R., Wang, G., & Shi, Z. (2016). Sensitivity of hydraulic properties to dynamic strain within a fault damage zone. Journal of Hydrology, 543, 721–728.
Yang, X. F., Sun, L., Sun, C. L., & Li, Y. L. (2016). Relation between the water temperature anomaly of Yushu well and Nepal Ms8.1 earthquake. Plateau Earthquake Research (in Chinese), 28(2), 12–15.
Zechar, J. D., & Jordan, T. H. (2008). Testing alarm-based earthquake predictions. Geophysical Journal International, 172, 715–724.
Zhang, P. Z., Deng, Q. D., Zhang, G. M., et al. (2003). Strong earthquakes and active blocks in mainland China. Chinese Science: Series D, 33(Suppl.), 12–20. (in Chinese).
Acknowledgements
We would like to thank the Guest Editor Michael Manga and the reviewers for their constructive comments which greatly improve the manuscript. The authors wish to thank the China Earthquake Network Center and the Qinghai Provincial Seismological Bureau for providing the water temperature and level data in the Yushu well. This study was financially supported by the National Natural Science Foundation of China (41502239, U1602233) and the Monitoring, Prediction and Research-combined Project of the China Earthquake Administration under (163102).
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Sun, X., Xiang, Y., Shi, Z. et al. Preseismic Changes of Water Temperature in the Yushu Well, Western China. Pure Appl. Geophys. 175, 2445–2458 (2018). https://doi.org/10.1007/s00024-017-1579-x
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DOI: https://doi.org/10.1007/s00024-017-1579-x