Relationship between Water Temperature Anomaly and Earthquake in Yunnan
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摘要: 云南地区地震频发, 水温观测点分布也最集中, 为研究水温异常与地震的关系提供了便利条件.通过收集已经公开发表关于该区域"十五"之前的水温异常与地震的对应关系的文章, 较系统地研究了水温异常持续时间、异常空间位置与地震之间的关系.结果表明: 水温异常主要是地震短临异常, 强震前也存在水温中期趋势异常; 一般情况下, 地震震级越大, 异常范围越广, 发震地点通常出现在水温异常集中的区域.Abstract: In Yunnan, earthquakes happened frequently, as well as groundwater temperature observation points are mostly centralized for its distribution. It is comprehensively collected for seismic cases on water temperature anomaly before the reform, the relationships of seism with water temperature anomaly duration and abnormal space is researched systematically. The result shows that water temperature anomaly is mainly impending-earthquake anomalies, however it has mid-term tendency anomalies before strong earthquakes. Generally, the greater earthquake magnitude, the vaster anomaly range, earthquakes were occurred during anomaly concentration area. The studying achievement has great significance for earthquake prediction and station setting.
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图 1 云南地区水温前兆观测点分布
图中圆点和三角形都为云南地区水温观测点，三角形为本文所统计中地震前出现异常的水温点
Fig. 1. Distribution of observation points of water temperature in Yunnan
图 2 水温观测资料正常动态特征
a.浙江宁波井; b.安徽霍山井; c.安徽庐江井; d.安徽巢湖井; e.四川北川井; f.天津王3井
Fig. 2. The characteristics of water temperature normal dynamic
图 4 地震震级与异常水温测点距离关系
Fig. 4. The relationship between magnitude and distance of earthquake and the abnormal temperature station
图 5 异常水温点与地震距离关系
Fig. 5. The relationship between distance and the abnormal temperature station
图 6 水温异常持续时间与地震关系
Fig. 6. The relationship between earthquake and duration of the abnormal temperature
图 7 水温短临异常与中期异常统计
Fig. 7. The pie chart of short-impending anomalies and medium term anomalies of water temperature
表 1 云南地区水温前兆异常与地震关系统计
Table 1. Water temperature anomalies and earthquakes in Yunnan
台站名称 异常信息 地震信息 异常开始时间 最大异常量(℃) 异常开始距发震时间(d) 异常类型 发震时间 震级M 地点 震中距(km) 保山 1996-01-16 0.009 6 18 升温型 1996-02-03 7.0 丽江 259 保山 2001-05-10 0.030 8 170 畸变型 2001-10-27 6.0 永胜 187 保山 2004-09-30 0.024 0 19 畸变型 2004-10-19 5.0 保山 17 大姚 1986-06-06 0.124 6 67 升温型 1986-08-12 5.2 盐源 185 1987-04-21 0.049 1 27 升温型 1987-05-18 5.3 鹤庆 120 1988-06-27 0.193 4 132 降温型 1988-11-06 7.6 澜沧-耿马 385 1995-02-12 0.150 1 254 升温型 1995-10-24 6.5 武定 87 1998-03-01 0.234 0 263 降温型 1998-11-19 6.2 宁蒗 179 1999-09-25 0.047 6 112 升温型 2000-01-15 6.5 姚安 37 2001-01-15 0.047 6 176 升温型 2001-07-10 5.3 楚雄 94 2001-01-15 0.047 6 285 降温型 2001-10-27 6.0 永胜 91 2002-10-11 0.100 0 283 升温型 2003-07-21 6.2 大姚 33 2002-10-11 0.100 0 370 升温型 2003-10-16 6.1 大姚 29 2004-03-15 * 148 降温型 2004-08-10 5.6 昭通 278 2004-03-15 0.135 7 286 升温-降温型 2004-12-26 5.0 楚雄-双柏 117 2007-03-16 0.248 7 79 畸变型 2007-06-03 6.4 宁洱 306 迪庆 1996-01-19 0.000 8 15 降温-升温型 1996-02-03 7.0 丽江 167 峨山 1999-05-09 0.023 2 200 升温-降温型 1999-11-25 5.2 澄江 56 峨山 1999-05-09 0.021 3 251 升温-降温型 2000-01-15 6.5 姚安 198 峨山 2001-06-11 0.002 3 34 降温型 2001-07-15 5.1 江川 25 峨山 2007-01-08 0.004 5 146 升温型 2007-06-03 6.4 宁洱 184 洱源 1996-02-02 0.008 1 1 降温-升温型 1996-02-03 7.0 丽江 125 建水 2001-03-12 0.006 1 125 畸变型 2001-07-15 5.1 江川 104 建水 2007-03-14 0.003 9 81 降温-升温型 2007-06-03 6.4 宁洱 147 景东 2007-04-29 0.004 4 35 升温型 2007-06-03 6.4 宁洱 161 澜沧 1995-03-21 0.632 6 103 畸变型 1995-07-02 7.3 孟连西 88 丽江 2007-04-23 0.028 4 41 升温-降温型 2007-06-03 6.4 宁洱 439 临沧 2007-02-18 0.001 3 105 畸变型 2007-06-03 6.4 宁洱 143 孟连 2007-05-21 13.900 0 13 畸变型 2007-06-03 6.4 宁洱 173 弥渡 1988-01-06 0.001 3 4 降温-升温型 1988-01-10 5.5 宁蒗 195 弥渡 1988-10-18 0.053 4 19 降温型 1988-11-06 7.6 澜沧-耿马 321 弥渡 2001-07-01 0.001 8 118 降温型 2001-10-27 6.0 永胜 95 弥渡 2007-04-15 0.031 3 49 降温型 2007-06-03 6.4 宁洱 269 弥勒 2005-01-10 0.096 1 215 降温-升温型 2005-08-13 5.3 交山 124 曲江 2007-05-09 0.797 0 25 升温型 2007-06-03 6.4 宁洱 204 思茅 2004-12-10 0.021 4 47 升温型 2005-01-26 5.0 思茅 26 思茅 2005-01-23 0.019 2 202 降温-升温型 2005-08-13 5.3 交山 323 下关 2004-05-19 0.026 0 221 降温-升温型 2004-12-26 5.0 楚雄-双柏 161 易门 1999-04-21 0.026 5 269 降温型 2000-01-15 6.5 姚安 139 永胜 1999-06-08 0.009 4 221 降温型 2000-01-15 6.5 姚安 135 鱼洞 2003-10-25 0.001 6 21 升温型 2003-11-15 5.1 鲁旬 42 鱼洞 2003-10-25 0.001 6 32 降温型 2003-11-26 5.0 鲁旬 42 昭通 1996-01-11 0.001 8 23 降温型 1996-02-03 7.0 丽江 280 1998-04-16 0.008 1 217 降温型 1998-11-19 6.2 宁蒗 221 2000-05-31 0.002 6 82 升温型 2000-08-21 5.1 武定 183 2001-08-19 0.000 5 69 降温型 2001-10-27 6.0 永胜 277 2003-10-25 0.002 5 21 升温型 2003-11-15 5.1 鲁旬 45 2003-10-25 0.002 5 32 升温型 2003-11-26 5.0 鲁旬 46 2004-07-01 0.004 7 40 升温型 2004-08-10 5.6 鲁旬-昭通 46 
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[1] Baker, E.T., Fox, C.G., Cowen, J.P., 1999. Insitu Observations of the Onset of Hydrothermal Discharge during the 1998 Submarine Eruption of Axial volcano, Juan de Fuca Ridge. The Letter of Geophysics Research, 26(23): 3445-3448. doi: 10.1029/1999GL002331 [2] Cao, X.L., Zhang, Z.G., Wang, Q.C., 1995. Anomalous Variations of Shallow Layer Geotemperature before Strong Earthquakes. North China Earthquake Sciences, 13(4): 9-17(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-HDKD504.001.htm [3] Che, Y.T., Liu, C.L., Yu, J.Z., 2008. Micro-Behavior of Well-Water Temperature and Its Mechanism. Earthquake, 28(4): 20-28(in Chinese with English abstract). http://www.researchgate.net/publication/293236129_Micro-behavior_of_well-water_temperature_and_its_mechanism [4] Che, Y.T., Yu, J.Z., Liu, C.G., 1996. The Observation and Study on Groundwater Temperature Characteristics in China. Hydrogeology & Engineering Geology, 28(4): 34-37(in Chinese with English abstract). [5] Chen, Y.J., Yao, B.S., 1999. The Features of Geotemperature in Short-Term Precursory Anomalies before the Zhangbei Earthquake with Ms6.2. Earthquake, 19(2): 179-782(in Chinese with English abstract). http://www.researchgate.net/publication/298505184_The_features_of_geotemperature_in_short-term_precursory_anomalies_before_the_Zhangbei_earthquake_with_Ms_62 [6] Dziak, R.P., Chadwick, W.W., Fox, C.G., et al., 2003. Hydrothermal Temperature Changes at the Southern Juan de Fuca Ridge Associated with Mw6.2 Blanc Transform Earthquake. Geology, 31(2): 119-122. doi: 10.1130/0091-7613(2003)031 [7] He, Z.T., Ma, B.Q., Li, Y.S., et al., 2012. Width and Hanging Wall Effect of Surface Rupture Caused by Wenchuan Earthquake. Acta Scientiarum Naturalium Universitatis Pekinensis, 48(6): 886-894(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-BJDZ201206004.htm [8] Johnson, H.P., Hutnak, M., Dziak, R.P., et al., 2000. Earthquake-Induced Changes in a Hydrothermal System on the Juan de Fuca Mid-Ocean Ridge. Nature, 407: 174-177. doi: 10.1038/35025040 [9] Liu, Y.W., 2006. Review of the Exploration Seismic Underground Fluid in China. China Earthquake Research in China, 22(3): 222-235 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZGZD200603001.htm [10] Liu, Y.W., Chen, H.J., Che, Y.T., 2006. Retrospect and Prospect of Observation and Study on Seismic Underground Fluid in China. Recent Developments in World Seismology, (7): 3-12(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GJZT200607002.htm [11] Liu, Y.W., Sun, X.L., Wang, S.Q., et al., 2008. Relationship of Bore-Hole Water Temperature Anomaly and the 2007 Ning'er Ms6.4 Earthquake. Journal of Seismological Research, 31(4): 347-353(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZYJ200804009.htm [12] Lu, M.Y., Liu, Y.W., Fan, X.F., et al., 2009. Preliminary Study on Subsurface Fluid Long-Time Trend Change and Strong Earthquake Prediction. Journal of Seismological Research, 32(4): 323-332(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZYJ200904002.htm [13] 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. doi: 10.1016/0040-1951(89)90172-8 [14] Sohn, R.A., Fornari, D.J., von Damm, K.L., et al., 1998. Seismic and Hydrothermal Evidence of Acracking Event on the East Pacific Rise Crest at 9°50′N. Nature, 396(12): 159-161. doi: 10.1038/24146 [15] Sun, X.L., Liu, Y.W., 2006. Summaries of the Micro Temperature Variations of Underground Water Caused by Loading Stresses. Recent Developments in World Seismology, (7): 17-26(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GJZT200607004.htm [16] Tian, H., Zhong, Y., Zhang, Z.L., 1994. The Relation between Earthquakes and Anomalous Variations of Geothermal Temperature in Beijing Observatory. Seismological and Geomagnetic Observation and Research, 5(3): 9-14(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DZGJ403.001.htm [17] Xu, G.M., Feng, Z.S., Tang, Z.F., 2002. Study of Normal Dynamic and Earthquake Samples of Jiangsu Digital Geothermal Data. Earthquake, 22(4): 130-135 (in Chinese with English abstract). http://www.researchgate.net/publication/296437410_Study_of_normal_dynamics_and_earthquake_samples_of_Jiangsu_digital_geothermal_data [18] Yang, Z.Z., Deng, Z.H., Yang, X.H., et al., 2010. Study on the Influencing Factors of Well Water-Temperature Changes. Earthquake, 30(2): 71-79(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DIZN201002009.htm [19] Zhang, B., Liu, Y.W., Yang, X.H., 2013. Contrastive Study on Co-Seismic Response Characteristics of Well Water Temperature in Wenchuan (M8.0), Yushu (M7.1), Lushan (M7.0) and Minxian (M6.6) Earthquakes. China Earthquake Engineering Journal, 35(3): 535-541 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZBDZ201303023.htm [20] Zhao, G., Wang, J., He, A.H., et al., 2009. Study of Normal Geothermal Dynamics. Earthquake, 29(3): 109-116(in Chinese with English abstract). http://www.researchgate.net/publication/298515070_Study_of_normal_geothermal_dynamics [21] 曹新来, 张子广, 王勤彩, 1995. 浅层地温强震前的异常变化. 华北地震科学, 13(4): 9-17. https://www.cnki.com.cn/Article/CJFDTOTAL-HDKD504.001.htm [22] 车用太, 鱼金子, 刘春国, 1996. 我国地震地下水温动态观测与研究. 水文地质工程地质, 28(4): 34-37. https://www.cnki.com.cn/Article/CJFDTOTAL-SWDG604.010.htm [23] 车用太, 刘成龙, 鱼金子, 2008. 井水温度微动态及其形成机制. 地震, 27(4): 20-28. doi: 10.3969/j.issn.1000-3274.2008.04.003 [24] 陈沅俊, 姚宝树, 1999. 张北6.2级地震地温短临异常特征. 地震, 19(2): 179-782. doi: 10.3969/j.issn.1000-3274.1999.02.010 [25] 何仲太, 马保起, 李玉森, 等, 2012. 汶川地震地表破裂带宽度与断层上盘效应. 北京大学学报: 自然科学版, 48(6): 886-894. https://www.cnki.com.cn/Article/CJFDTOTAL-BJDZ201206004.htm [26] 刘耀炜, 2006. 我国地震地下流体科学40年探索历程回顾. 中国地震, 22(3): 222-235. doi: 10.3969/j.issn.1001-4683.2006.03.002 [27] 刘耀炜, 陈华静, 车用太, 2006. 我国地震地下流体观测研究40年发展与展望. 国际地震动态, 7: 3-12. doi: 10.3969/j.issn.0253-4975.2006.07.003 [28] 刘耀炜, 孙小龙, 王世芹, 等, 2008. 井孔水温异常与2007年宁洱6.4级地震关系分析. 地震研究, 31(4): 347-353. doi: 10.3969/j.issn.1000-0666.2008.04.009 [29] 陆明勇, 刘耀炜, 范雪芳, 等, 2009. 地下流体长趋势异常变化与强震预测的初步研究. 地震研究, 32(4): 323-332. doi: 10.3969/j.issn.1000-0666.2009.04.001 [30] 孙小龙, 刘耀炜, 2006. 应力加载作用引起地下水微温度场变化的研究综述. 国际地震动态, (7): 17-26. doi: 10.3969/j.issn.0253-4975.2006.07.005 [31] 田华, 仲阳, 张之立, 1994. 白家疃地温异常变化与地震的对应关系. 地震地磁观测与研究, 15(3): 9-14. https://www.cnki.com.cn/Article/CJFDTOTAL-DZGJ403.001.htm [32] 杨竹转, 邓志辉, 杨贤和, 等, 2010. 井孔水温动态变化的影响因素探讨. 地震, 30(2): 71-79. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZN201002009.htm [33] 徐桂明, 冯志生, 唐振芳, 2002. 江苏地区数字化地热正常动态及震例初步研究. 地震, 22(4): 130-135. doi: 10.3969/j.issn.1000-3274.2002.04.020 [34] 张彬, 刘耀炜, 杨选辉, 2013. 中国大陆井水温对汶川8.0级、玉树7.1级、庐山7.0及和岷县6.6及地震响应特征的对比研究. 地震工程学报, 35(3): 535-541. doi: 10.3969/j.issn.1000-0844.2013.03.0535 [35] 赵刚, 王军, 何案华, 等, 2009. 地热正常动态特征的研究. 地震, 29(3): 109-116. https://www.cnki.com.cn/Article/CJFDTOTAL-DIZN200903014.htm -
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