湖南省数字化井水位对尼泊尔M 8.1地震的同震响应特征分析
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摘要
通过分析湖南省数字化井水位对尼泊尔M 8.1地震的同震响应特征,我们发现,同一地震在不同观测井中引起的同震响应特征各不相同.湖南省井水位的同震响应形态以水震波为主,而且对于波动伴随阶变的同震响应类型,总是先记录到水震波然后才产生阶变.认为,同震响应形态的差异性以及初动响应时间的快慢可能与仪器、井况、井孔的构造环境以及水文地质条件等因素有关.湖南省水位观测井对远场大震的远场效应反映较灵敏,能反映区域应力场变化引起的含水层应力应变的变化.
The co-seismic response characteristics of digital well water level in Hunan Province to the Nepal M 8. 1 earthquake are analyzed in this paper, the results display that the co-seismic response characteristics caused by the same earthquake differ from one another in different wells. The main co-seismic response form is water earthquake wave in Hunan Province,and it is always recorded before than water level step in the co-seismic form of water earthquake wave accompanied with water level step. We think,the otherness of co-seismic response forms and the speed of first motion response time are possibly related to instrument,well condition,structural environment,hydrogeological condition of well and et al.The observation wells in Hunan Province are sensitive to the far field effect caused by teleseism,which can reflect the stress-strain change of water-bearing stratum caused by the change of region stress field.
The co-seismic response characteristics of digital well water level in Hunan Province to the Nepal M 8. 1 earthquake are analyzed in this paper, the results display that the co-seismic response characteristics caused by the same earthquake differ from one another in different wells. The main co-seismic response form is water earthquake wave in Hunan Province,and it is always recorded before than water level step in the co-seismic form of water earthquake wave accompanied with water level step. We think,the otherness of co-seismic response forms and the speed of first motion response time are possibly related to instrument,well condition,structural environment,hydrogeological condition of well and et al.The observation wells in Hunan Province are sensitive to the far field effect caused by teleseism,which can reflect the stress-strain change of water-bearing stratum caused by the change of region stress field.
引文
Che Y T,Wang T C,Yu J Z.1989.The current situation and trend of research on earthquake wave in China[J].Earthquake(in Chinese),(1):70-72.
Che Y T,Yu J Z.2006.Underground Fluids and Earthquake(in Chinese)[M].Beijing:China Meteorological Press.
Chen D Q,Liu Y W,Yang X H,et al.2007.Co-seismic water level,temperature responses of some wells to far-field strong earthquakes and their mechanisms[J].Seismology and Geology(in Chinese),29(1):122-132.
Fu H,Liu L F,Wang S Q,et al.2002.Research on coseismic and post seismic effect of ground water for the local and near earthquake[J].Earthquake(in Chinese),22(4):55-66.
Fu H,Wu C D,Liu Q,et al.2007.Abnormal water level records caused by indonesia large earthquakes in Yunnan and its significance[J].Seismology and Geology(in Chinese),29(4):873-882.
Jing S Q,Wang J W.2001.Analysis on seismic effect and its mechanism of Changsha well’s dynamic ground water level for the MS7.6 Jiji earthquake,Taiwan[J].South China Journal of Seismology(in Chinese),21(1):32-37.
Liao L X,Wang M L.2008.The characteristic analysis of response to the M8 large earthquake of Indonesia of water level network of Fujian Province[J].Seismological and Geomagnetic Observation and Research(in Chinese),29(4):67-72.
Liao L X,Wang M L,Wu S Z.2009.Study on coseismic effects of water level as observed by Fujian well network and its implication to earthquake prediction[J].Acta Seismologica Sinica(in Chinese),31(4):432-441.
Liu X Y,Zheng X J,Wang L,et al.2009.Response analysis of the well-water-level system in confined aquifer[J].Chinese Journal Geophysics(in Chinese),52(12):3147-3157,doi:10.3969/j.issn.0001-5733.2009.12.025.
Liu Y W,Yang X H,Liu Y M,et al.2005.Response characters of subsurface fluid to the MW9.0 Earthquake in Sumatra[M].//Department of Earthquake Monitoring and Prediction,China Earthquake Administration.The 2004 M 8.7 Earthquake in Sumatra,Indonesia and Its Influence on China Main Land(in Chinese).Beijing:Seismological Press,131-285.
Sun X L,Liu Y W.2008.Characteristics and mechanism of co-seismic responses in the Tayuan well[J].Earthquake Research in China(in Chinese),24(2):105-115.
Wang C M.1990.The Dynamic Observation Network of Earthquake Groundwater in China(in Chinese)[M].Beijing:Seismological Press,289-290.
Wang C M,Che Y T,Wan D K,et al.1988.The Micro-dynamic Study on Groundwater(in Chinese)[M].Beijing:Seismological Press.
Yan R,Huang F Q.2009.Preliminary study on coseismic response of Huanghua well water level to 5 times of Sumatra earthquakes[J].Earthquake Research in China(in Chinese),25(3):325-332.
Yang Z Z.2011.Coseismic variations of well water-level and temperature caused by seismic waves and their generating mechanisms(in Chinese)[Ph.D.thesis].Beijing:Institute of Geology,China Earthquake Administration.
Yang Z Z,Deng Z H,Liu C G,et al.2008.Coseismic changes of water level and water temperature caused by MS8.0 Wenchuan Earthquake[J].Seismology and Geology(in Chinese),30(4):895-905.
Yang Z Z,Deng Z H,Yang X H,et al.2014.Comparison and analysis of well water-level variations caused by Lushan MS7.0 earthquake in2013 and Wenchuan MS8.0 earthquake in 2008[J].Seismology and Geology(in Chinese),36(2):380-391.
Yu J Z,Che Y T,Liu C L,et al.2012.Coseismic responses of water level and temperature in wells of the Jinshajiang ground water observation network to the Japan MS9.0 earthquake:Characteristics and mechanism[J].Earthquake(in Chinese),32(1):59-69.
Yu J Z,Che Y T,Wang A Y,et al.1993.Preliminary study on relations between the anomalies of seismic wave of water level and the earthquake risk[J].Earthquake(in Chinese),(4):30-37.
Zhang B,Cheng H H,Shi Y L.2015.Calculation of the co-seismic effect of MS8.1 earthquake,Apirl 25,2015,Nepal[J].Chinese Journal Geophysics(in Chinese),58(5):1794-1803,doi:10.6038/cjg20150529.
Zhang B,Liu Y W,Gao X Q,et al.2015.Correlation analysis on coseismic response between well water level and temperature caused by the Nepal MS8.1 earthquake[J].Acta Seismologica Sinica(in Chinese),37(4):533-540.
Zhang Q X,Chen Y,Zheng X J,et al.2012.The analyze of coseismic response characteristics of magnitude 9.0 earthquake in Japan from the digital water level and temperature in Fujian Province[J].Seismological and Geomagnetic Observation and Research(in Chinese),33(3-4):61-66.
Zhang Z D,Chi Z L,Chen H M,et al.2000.Vibration of water level in well and earthquake wave[J].Journal of Seismological Research(in Chinese),23(4):418-425.
车用太,王铁城,鱼金子.1989.我国水震波研究的现状与动向[J].地震,(1):70-72.
车用太,鱼金子.2006.地震地下流体学[M].北京:气象出版社.
陈大庆,刘耀炜,杨选辉,等.2007.远场大震的水位、水温同震响应及其机理研究[J].地震地质,29(1):122-132.
付虹,刘丽芳,王世芹,等.2002.地方震及近震地下水同震震后效应研究[J].22(4):55-66.
付虹,邬成栋,刘强,等.2007.印尼巨大地震引起的云南水位异常记录及其意义[J].地震地质,29(4):873-882.
敬少群,王佳卫.2001.长沙井动水位对台湾集集7.6级地震的震时效应及其机理分析[J].华南地震,21(1):32-37.
廖丽霞,王玫玲.2008.福建水位观测网对印度尼西亚8级巨震的响应特征分析[J].地震地磁观测与研究,29(4):67-72.
廖丽霞,王玫玲,吴绍祖.2009.福建省流体台网井水位的同震效应及其地震预测意义[J].地震学报,31(4):432-441.
刘序俨,郑小菁,王林,等.2009.承压井水位观测系统对体应变的响应机制分析[J].地球物理学报,52(12):3147-3157,doi:10.3969/j.issn.0001-5733.2009.12.025.
刘耀炜,杨选辉,刘永铭,等.2005.地下流体苏门答腊8.7级地震的响应特征[M].//中国地震局监测预报司.2004年印度尼西亚苏门答腊8.7级大地震及其对中国大陆地区的影响.北京:地震出版社,131-285.
孙小龙,刘耀炜.2008.塔院井水位和水温的同震响应特征及其机理探讨[J].中国地震,24(2):105-115.
汪成民.1990.中国地震地下水动态观测网[M].北京:地震出版社,289-290.
汪成民,车用太,万迪堃,等.1988.地下水微动态研究[M].北京:地震出版社.
杨竹转.2011.地震波引起的井水位水温同震变化及其机理研究[博士论文].北京:中国地震局地质研究所.
杨竹转,邓志辉,刘春国,等.2008.中国大陆井水位与水温动态对汶川MS8.0地震的同震响应特征分析[J].地震地质,30(4):895-905.
杨竹转,邓志辉,杨贤和,等.2014.2013年芦山MS7.0地震和2008年汶川MS8.0地震井水位同震变化的比较分析[J].地震地质,36(2):380-391.
鱼金子,车用太,刘成龙,等.2012.金沙江水网对日本9.0级地震的同震响应及其特征与机理[J].地震,32(1):59-69.
鱼金子,车用太,王爱英,等.1993.水震波异常与中期强震危险性关系初探[J].地震,(4):30-37.
张彬,刘耀炜,高小其,等.2015.2015年尼泊尔MS8.1地震引起的井水位与井水温同震效应及其相关性分析[J].地震学报,37(4):533-540.
张贝,程惠红,石耀霖.2015.2015年4月25日尼泊尔MS8.1大地震的同震效应[J].地球物理学报,58(5):1794-1803,doi:10.6038/cjg20150529.
张清秀,陈莹,郑小菁,等.2012.福建省数字化水位、水温对日本9级地震的同震响应[J].地震地磁观测与研究,33(3-4):61-66.
张昭栋,迟镇乐,陈会民,等.2000.井水位的振荡与地震波[J].地震研究,23(4):418-425.
晏锐,黄辅琼.2009.黄骅井水位对苏门答腊5次地震的同震响应初步研究[J].中国地震,25(3):325-332.
Che Y T,Yu J Z.2006.Underground Fluids and Earthquake(in Chinese)[M].Beijing:China Meteorological Press.
Chen D Q,Liu Y W,Yang X H,et al.2007.Co-seismic water level,temperature responses of some wells to far-field strong earthquakes and their mechanisms[J].Seismology and Geology(in Chinese),29(1):122-132.
Fu H,Liu L F,Wang S Q,et al.2002.Research on coseismic and post seismic effect of ground water for the local and near earthquake[J].Earthquake(in Chinese),22(4):55-66.
Fu H,Wu C D,Liu Q,et al.2007.Abnormal water level records caused by indonesia large earthquakes in Yunnan and its significance[J].Seismology and Geology(in Chinese),29(4):873-882.
Jing S Q,Wang J W.2001.Analysis on seismic effect and its mechanism of Changsha well’s dynamic ground water level for the MS7.6 Jiji earthquake,Taiwan[J].South China Journal of Seismology(in Chinese),21(1):32-37.
Liao L X,Wang M L.2008.The characteristic analysis of response to the M8 large earthquake of Indonesia of water level network of Fujian Province[J].Seismological and Geomagnetic Observation and Research(in Chinese),29(4):67-72.
Liao L X,Wang M L,Wu S Z.2009.Study on coseismic effects of water level as observed by Fujian well network and its implication to earthquake prediction[J].Acta Seismologica Sinica(in Chinese),31(4):432-441.
Liu X Y,Zheng X J,Wang L,et al.2009.Response analysis of the well-water-level system in confined aquifer[J].Chinese Journal Geophysics(in Chinese),52(12):3147-3157,doi:10.3969/j.issn.0001-5733.2009.12.025.
Liu Y W,Yang X H,Liu Y M,et al.2005.Response characters of subsurface fluid to the MW9.0 Earthquake in Sumatra[M].//Department of Earthquake Monitoring and Prediction,China Earthquake Administration.The 2004 M 8.7 Earthquake in Sumatra,Indonesia and Its Influence on China Main Land(in Chinese).Beijing:Seismological Press,131-285.
Sun X L,Liu Y W.2008.Characteristics and mechanism of co-seismic responses in the Tayuan well[J].Earthquake Research in China(in Chinese),24(2):105-115.
Wang C M.1990.The Dynamic Observation Network of Earthquake Groundwater in China(in Chinese)[M].Beijing:Seismological Press,289-290.
Wang C M,Che Y T,Wan D K,et al.1988.The Micro-dynamic Study on Groundwater(in Chinese)[M].Beijing:Seismological Press.
Yan R,Huang F Q.2009.Preliminary study on coseismic response of Huanghua well water level to 5 times of Sumatra earthquakes[J].Earthquake Research in China(in Chinese),25(3):325-332.
Yang Z Z.2011.Coseismic variations of well water-level and temperature caused by seismic waves and their generating mechanisms(in Chinese)[Ph.D.thesis].Beijing:Institute of Geology,China Earthquake Administration.
Yang Z Z,Deng Z H,Liu C G,et al.2008.Coseismic changes of water level and water temperature caused by MS8.0 Wenchuan Earthquake[J].Seismology and Geology(in Chinese),30(4):895-905.
Yang Z Z,Deng Z H,Yang X H,et al.2014.Comparison and analysis of well water-level variations caused by Lushan MS7.0 earthquake in2013 and Wenchuan MS8.0 earthquake in 2008[J].Seismology and Geology(in Chinese),36(2):380-391.
Yu J Z,Che Y T,Liu C L,et al.2012.Coseismic responses of water level and temperature in wells of the Jinshajiang ground water observation network to the Japan MS9.0 earthquake:Characteristics and mechanism[J].Earthquake(in Chinese),32(1):59-69.
Yu J Z,Che Y T,Wang A Y,et al.1993.Preliminary study on relations between the anomalies of seismic wave of water level and the earthquake risk[J].Earthquake(in Chinese),(4):30-37.
Zhang B,Cheng H H,Shi Y L.2015.Calculation of the co-seismic effect of MS8.1 earthquake,Apirl 25,2015,Nepal[J].Chinese Journal Geophysics(in Chinese),58(5):1794-1803,doi:10.6038/cjg20150529.
Zhang B,Liu Y W,Gao X Q,et al.2015.Correlation analysis on coseismic response between well water level and temperature caused by the Nepal MS8.1 earthquake[J].Acta Seismologica Sinica(in Chinese),37(4):533-540.
Zhang Q X,Chen Y,Zheng X J,et al.2012.The analyze of coseismic response characteristics of magnitude 9.0 earthquake in Japan from the digital water level and temperature in Fujian Province[J].Seismological and Geomagnetic Observation and Research(in Chinese),33(3-4):61-66.
Zhang Z D,Chi Z L,Chen H M,et al.2000.Vibration of water level in well and earthquake wave[J].Journal of Seismological Research(in Chinese),23(4):418-425.
车用太,王铁城,鱼金子.1989.我国水震波研究的现状与动向[J].地震,(1):70-72.
车用太,鱼金子.2006.地震地下流体学[M].北京:气象出版社.
陈大庆,刘耀炜,杨选辉,等.2007.远场大震的水位、水温同震响应及其机理研究[J].地震地质,29(1):122-132.
付虹,刘丽芳,王世芹,等.2002.地方震及近震地下水同震震后效应研究[J].22(4):55-66.
付虹,邬成栋,刘强,等.2007.印尼巨大地震引起的云南水位异常记录及其意义[J].地震地质,29(4):873-882.
敬少群,王佳卫.2001.长沙井动水位对台湾集集7.6级地震的震时效应及其机理分析[J].华南地震,21(1):32-37.
廖丽霞,王玫玲.2008.福建水位观测网对印度尼西亚8级巨震的响应特征分析[J].地震地磁观测与研究,29(4):67-72.
廖丽霞,王玫玲,吴绍祖.2009.福建省流体台网井水位的同震效应及其地震预测意义[J].地震学报,31(4):432-441.
刘序俨,郑小菁,王林,等.2009.承压井水位观测系统对体应变的响应机制分析[J].地球物理学报,52(12):3147-3157,doi:10.3969/j.issn.0001-5733.2009.12.025.
刘耀炜,杨选辉,刘永铭,等.2005.地下流体苏门答腊8.7级地震的响应特征[M].//中国地震局监测预报司.2004年印度尼西亚苏门答腊8.7级大地震及其对中国大陆地区的影响.北京:地震出版社,131-285.
孙小龙,刘耀炜.2008.塔院井水位和水温的同震响应特征及其机理探讨[J].中国地震,24(2):105-115.
汪成民.1990.中国地震地下水动态观测网[M].北京:地震出版社,289-290.
汪成民,车用太,万迪堃,等.1988.地下水微动态研究[M].北京:地震出版社.
杨竹转.2011.地震波引起的井水位水温同震变化及其机理研究[博士论文].北京:中国地震局地质研究所.
杨竹转,邓志辉,刘春国,等.2008.中国大陆井水位与水温动态对汶川MS8.0地震的同震响应特征分析[J].地震地质,30(4):895-905.
杨竹转,邓志辉,杨贤和,等.2014.2013年芦山MS7.0地震和2008年汶川MS8.0地震井水位同震变化的比较分析[J].地震地质,36(2):380-391.
鱼金子,车用太,刘成龙,等.2012.金沙江水网对日本9.0级地震的同震响应及其特征与机理[J].地震,32(1):59-69.
鱼金子,车用太,王爱英,等.1993.水震波异常与中期强震危险性关系初探[J].地震,(4):30-37.
张彬,刘耀炜,高小其,等.2015.2015年尼泊尔MS8.1地震引起的井水位与井水温同震效应及其相关性分析[J].地震学报,37(4):533-540.
张贝,程惠红,石耀霖.2015.2015年4月25日尼泊尔MS8.1大地震的同震效应[J].地球物理学报,58(5):1794-1803,doi:10.6038/cjg20150529.
张清秀,陈莹,郑小菁,等.2012.福建省数字化水位、水温对日本9级地震的同震响应[J].地震地磁观测与研究,33(3-4):61-66.
张昭栋,迟镇乐,陈会民,等.2000.井水位的振荡与地震波[J].地震研究,23(4):418-425.
晏锐,黄辅琼.2009.黄骅井水位对苏门答腊5次地震的同震响应初步研究[J].中国地震,25(3):325-332.