我国水库诱发地震监测技术进展
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摘要
从1962年新丰江水库诱发地震监测工作开始,我国的水库诱发地震监测工作已经走过了半个世纪,水库诱发地震监测工作对于水库诱发地震的发生、发展以及对正确引导舆论导向有重要意义。本文系统阐述了水库诱发地震监测工作的目的和意义,对我国的水库诱发地震监测工作进展进行了综述,水库诱发地震监测工作经过三个阶段的发展,已经全面进入了数字化和远程传输时代。文章对最新一代水库诱发地震系统的遥测地震台站、台网管理中心和数据传输与中继系统进行了介绍。最后,对设台条件等相关问题进行了讨论。
An Ms.6.1 earthquake induced by the Xinfengjiang reservoir occurred in 1962. Since then,the reservoir-induced earthquake monitoring work has had a history of 50 years in our country. In this paper,we expound the purpose and meaning of reservoir-induced earthquake monitoring. Reservoir-induced earth quake monitoring makes it possible to accurately judge the reservoir-induced earthquake'occurrence and de velopment trends,and to correctly guide the direction of public opinion. For half a century,after the three stages of development,the work has fully entered the digitization and remote transmission period. The reser voir-induced earthquake monitoring system composition and operational requirements were described in de tail. In the end,the setting station conditions and some other relevant issues were discussed.
An Ms.6.1 earthquake induced by the Xinfengjiang reservoir occurred in 1962. Since then,the reservoir-induced earthquake monitoring work has had a history of 50 years in our country. In this paper,we expound the purpose and meaning of reservoir-induced earthquake monitoring. Reservoir-induced earth quake monitoring makes it possible to accurately judge the reservoir-induced earthquake'occurrence and de velopment trends,and to correctly guide the direction of public opinion. For half a century,after the three stages of development,the work has fully entered the digitization and remote transmission period. The reser voir-induced earthquake monitoring system composition and operational requirements were described in de tail. In the end,the setting station conditions and some other relevant issues were discussed.
引文
[1]夏其发,汪雍熙.试论水库诱发地震的地质分类[J].水文地质工程地质,1984(1):9-13.
[2]易立新,车用太.水库诱发地震及其水文地质条件和诱震机理[J].中国地质灾害与防治学报,2000,11(2):46-50.
[3]夏其发.《世界水库诱发地震震例基本参数汇总表》暨水库诱发地震评述[J].中国地震灾害与防治,1992,3(4):95-100.
[4]欧作畿.水库诱发地震的研究[J].云南水利发电,2005,21(3):18-21.
[5]王秋月,朱守彪.水库诱发地震讨论及其动力学机制分析[C]//地壳构造与地壳应力文集.北京:地震出版社,2009.
[6]沈崇刚,陈厚群,等.新丰江水库地震及其对大坝的影响[J].中国科学,1974(2):184-205.
[7]杨晓源.我国近年水库地震综述[J].地震地磁观测与研究,1999,20(2):3-15.
[8]JSGC-01,中国数字测震台网技术规程[S].
[9]GB 50287-2006,水利水电工程地质勘察规范[S].
[10]GB 21075-2007,水库诱发地震危险性评价[S].
[11]中华人民共和国国务院令第409号.水库地震监测管理条例[Z].2006年10月16日.
[2]易立新,车用太.水库诱发地震及其水文地质条件和诱震机理[J].中国地质灾害与防治学报,2000,11(2):46-50.
[3]夏其发.《世界水库诱发地震震例基本参数汇总表》暨水库诱发地震评述[J].中国地震灾害与防治,1992,3(4):95-100.
[4]欧作畿.水库诱发地震的研究[J].云南水利发电,2005,21(3):18-21.
[5]王秋月,朱守彪.水库诱发地震讨论及其动力学机制分析[C]//地壳构造与地壳应力文集.北京:地震出版社,2009.
[6]沈崇刚,陈厚群,等.新丰江水库地震及其对大坝的影响[J].中国科学,1974(2):184-205.
[7]杨晓源.我国近年水库地震综述[J].地震地磁观测与研究,1999,20(2):3-15.
[8]JSGC-01,中国数字测震台网技术规程[S].
[9]GB 50287-2006,水利水电工程地质勘察规范[S].
[10]GB 21075-2007,水库诱发地震危险性评价[S].
[11]中华人民共和国国务院令第409号.水库地震监测管理条例[Z].2006年10月16日.
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