赵各庄井地下流体的映震响应
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摘要
赵各庄井位于首都圈地区,是夏垫断裂带北端的地震观测井。其地下流体同震响应的统计数据显示,在对6级以上远场地震的响应次数上,赵各庄井的水位较水温更显著;在对MS 7.0井水位的响应幅度变化范围为3.0mm—770.0mm,典型水温的响应幅度为0.0129℃,井水位响应幅度明显强于水温,响应形态以振荡型为主。赵各庄井水温、水位的异常变化和夏垫断裂带的活动性密切相关,同时也会影响断裂带的活动性。综合分析认为,在对赵各庄井水温和水位两大测项进行观测时,应以水位为主,还应关注夏垫断裂带的活动性。同时,为了监测夏垫断裂带的活动性,应对赵各庄井水位和水温进行长期监测,以保证首都圈地区的人民生产安全。
The Zhaogezhuang well is loacated in the capital zone and it's an earthquake observation well along the Xiadian Fault zone. In this poper we conducted sfatistical study of the co-seismic corresponding of and we fand that respcmse of groundwater level is more remarkable than that of temperature for MS≥6.0 earthquakes on responding times and MS≥7.0 earthquakes on responding minute as well; Responding amplitude ranges from 3.0—770.0 mm for groundwater level and 0.0129℃ for typical groundwater temperature, and the variation of groundwater level is more obvious than that of temperature. Oscillation mode is the main responsive form. The anomaly of groundwater level and temperature is related to the activity of the Xiadian fault zone in consideration of its location and maybe impact the fault activity. In conclusion, groundwater level of the Zhaogezhuang well should be paid more attention in order to monitor the activity of Xiadian fault zone. Meanwhile, in order to monitor the Xiadian fault zone activity,the observation should be conducted in long-time of the guarantee of production safety of capital circle people.
The Zhaogezhuang well is loacated in the capital zone and it's an earthquake observation well along the Xiadian Fault zone. In this poper we conducted sfatistical study of the co-seismic corresponding of and we fand that respcmse of groundwater level is more remarkable than that of temperature for MS≥6.0 earthquakes on responding times and MS≥7.0 earthquakes on responding minute as well; Responding amplitude ranges from 3.0—770.0 mm for groundwater level and 0.0129℃ for typical groundwater temperature, and the variation of groundwater level is more obvious than that of temperature. Oscillation mode is the main responsive form. The anomaly of groundwater level and temperature is related to the activity of the Xiadian fault zone in consideration of its location and maybe impact the fault activity. In conclusion, groundwater level of the Zhaogezhuang well should be paid more attention in order to monitor the activity of Xiadian fault zone. Meanwhile, in order to monitor the Xiadian fault zone activity,the observation should be conducted in long-time of the guarantee of production safety of capital circle people.
引文
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1 http://data.earthquake.cn
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陈亮,丁富雄,张蕾等,2012.建水地下流体监测井水位骤降异常分析.地震研究,35(4):471-476.
陈运泰,刘瑞丰,2004.地震的震级.地震地磁观测与研究,25(6):1-12.
邓前辉,王继军,汤吉等,2000.三河-平谷8级大震区地壳上地幔电性结构特征.见:中国地震学会第八次学术大会论文摘要集.北京:地震学报出版社,282.
邓前辉,王继军,汤吉等,2001.三河-平谷8级大震区地壳上地幔电性结构特征研究.地震地质,23(2):178-185.
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巩浩波,郭卫英,李光科等,2015.重庆井网水位水温同震响应特征分析.震灾防御技术,10(S1):794-804.
郭履灿,1971.华北地区的地方性震级ML和面波震级MS经验关系.见:全国地震工作会议.1-10.
韩孔艳,赵健,2016.赵各庄地震观测井观测现状分析及改造方案探讨.煤炭与化工,39(7):129-132.
韩晓昆,李营,杜建国等,2013.夏垫断裂中南段土壤气体地球化学特征.物探与化探,37(6):976-982.
何付兵,白凌燕,王继明等,2013.夏垫断裂带深部构造特征与第四纪活动性讨论.地震地质,35(3):490-505.
黄辅琼,陈顒,白长清等,2005.八宝山断层的变形行为与降雨及地下水的关系.地震学报,27(6):637-646.
贾辉,何正勤,叶太兰,2008.用瞬态多道瑞利波法研究夏垫隐伏断裂附近的浅层速度结构变化.地震地磁观测与研究,29(1):15-19.
江娃利,1999.北京平谷地区地表陡坎的成因识别.地震地质,21(4):309-315.
江娃利,侯治华,肖振敏等,2000.北京平原夏垫断裂齐心庄探槽古地震事件分析.地震地质,22(4):413-422.
兰双双,迟宝明,姜纪沂,2011.地下水位对近震和远震异常响应的比较--以汶川地震和苏门答腊地震为例.吉林大学学报(地球科学版),41(1):145-152.
李梁,张世红,蔡向民等,2011.北京市平原区夏垫断裂活动性的磁学研究.见:中国地球物理学会第二十七届年会论文集.长沙:中国地球物理学会,161.
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廖欣,刘春平,石云等,2014.川06井水位固体潮效应变化初探.地震学报,36(2):299-305.
刘瑞丰,蔡晋安,彭克银等,2007.地震科学数据共享工程.地震,27(2):9-16.
刘耀炜,陆明勇,付虹等,2010.地下流体动态信息提取与强震预测技术研究.北京:地震出版社.
陆丽娜,李静,沈军等,2016.夏垫活动断层土壤氡地球化学特征.震灾防御技术,11(4):736-746.
陆丽娜,杨明,李静等,2018.土壤气汞探测在夏垫断裂带的应用研究.地质与勘探,54(1):112-120.
陆明勇,黄辅琼,刘善华等,2005.地壳变形与地下水相互作用及其异常关系初探.地震,25(1):67-73.
毛昌伟,丁锐,龚正等,2010.1679年三河-平谷8级地震地表断层陡坎的GPS测量.地壳构造与地壳应力文集,(22):11-18.
牛安福,张晶,吉平,2005.强地震引起的同震形变响应.内陆地震,19(1):1-7.
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1 http://data.earthquake.cn