强震区震后地质灾害长期活动性研究综述

杨志华; 兰恒星; 张永双; 郭长宝

强震区震后地质灾害长期活动性研究综述

1.
中国地质科学院地质力学研究所, 北京 100081
2.
中国科学院地理科学与资源研究所, 北京 100101
3.
中国地质环境监测院, 北京 100081

基金项目:

国家自然科学基金项目 41502313

中国地质调查项目 DD20160271

详细信息

作者简介:
杨志华(1982-), 男, 博士, 助理研究员, 主要从事地质灾害研究。E-mail:yangzh99@163.com

中图分类号: P694
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- 文章访问数: 574
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- 被引次数: 0
出版历程
- 收稿日期: 2017-03-21
- 刊出日期: 2017-10-01

RESEARCH REVIEW ON LONG-TERM ACTIVITY OF POST-EARTHQUAKE GEOHAZARD IN STRONG SEISMIC-DISTURBED REGIONS

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China
3.
China Institute of Geo-Environment Monitoring, Beijing 100081, China

摘要

摘要: 地震通过改变地表岩体的物理力学性质而使得震区滑坡、泥石流等地质灾害显著增强的现象在震后持续相当长的一段时间。在研究分析国内外学者对地震地质灾害研究成果的基础上，系统总结了目前在地震诱发地质灾害的发育分布规律及其演化趋势方面的研究方法及成果，探讨了研究中存在的问题及薄弱环节，并对未来的研究方向及趋势进行了展望。研究认为目前国内外对地震地质灾害长期活动性的研究还没有形成体系，尚缺乏有效的研究方法与技术，并且研究成果存在较大差异性。地震扰动区地质灾害长期活动性研究可为震后地质灾害的长期防灾减灾和风险管控提供科学支持，也能对地震地质灾害相关问题的进一步深入研究提供参考。
- 地震 /
- 地质灾害 /
- 长期活动性 /
- 活跃周期 /
- 综述
Abstract: Earthquake can significantly change the physical and mechanical properties of surface rock masses, which leads to an obvious geohazard increase after earthquake for a long period of time. Based on the review and analysis of the current research status of long-term activity of post-earthquake geohazard, the current research methods and achievements of development, distribution rule and evolution trend of earthquake-induced geohazard are systematically summarized, the problems and weaknesses during the research process are discussed, and the prospects and the future research directions and trends are presented. At present, there is no perfect research system and effective research methods and techniques for long-term activity of post-earthquake geohazard, and the research results have a big difference. In-depth scientific research on long-term activity of post-earthquake geohazard in seismic-disturbed regions can provide scientific support for long-term disaster prevention, mitigation and risk control of geohazard after the earthquake and also present a reference for further study of this scientific problem.
- earthquake /
- geohazard /
- long-term activity /
- active cycle /
- review

HTML全文

图 1 汶川地震滑坡与环境因子的关系

a-坡向^[6]; b-地震烈度^[7]

Figure 1. Relationship between Wenchuan earthquake-induced landslides and environmental factors

下载: 全尺寸图片幻灯片

图 2 台湾集集地震扰动区触发泥石流的小时降雨量和累积降雨量^[44]

Figure 2. Plot of the maximum hourly percipitation versus the maximum accumulated precipitation for debris flow events in the Chi-chi earthquake-disturbed areas

下载: 全尺寸图片幻灯片

图 3 日本关东地震后滑坡强度变化规律^{[15, 20]}

Figure 3. The change rule of landslide intensity from 1896 to 1990 after Kanto earthquake in Japan

下载: 全尺寸图片幻灯片

图 4 汶川震后几年来的典型地质灾害及防治工程破坏实例

Figure 4. Typical cases of destruction scenes of geo-hazard control engineering after the Wenchuan earthquake

下载: 全尺寸图片幻灯片

图 5 汶川震区2000年以来灾难性滑坡发展趋势^[15~16]

Figure 5. Variation of geohazard number with time in the Wenchuan earthquake-disturbed area since 2000

下载: 全尺寸图片幻灯片

图 6 台湾集集地震前后的降雨诱发滑坡强度变化规律^{[21, 44~45]}

Figure 6. Change rule of landslide intensity induced by rainfalls before and after the Chi-Chi earthquake in Taiwan, China

下载: 全尺寸图片幻灯片

表 1 中国典型地震震后有效松弛时间^[65]

Table 1. Post-seismic effective relaxation cycles of typical earthquakes in China

地震名称	震级(M_s)	发震时间	测段名称	资料年限	有效松弛时间/年	最大形变量/mm	同震形变/mm
唐山	7.8	1976.7.28	山津26-22	1976—1992	21.6	127.1	206
邢台	7.2	1966.3.22	冯巨7-11	1966—1976	11.1	131.6	273
通海	7.8	1970.1.5	高大1-4	1970—1981	5.5	32.8	未测
炉霍	7.6	1973.2.6	虚墟B-C	1973—1981	4.9	6.5	未测
共和	7.0	1900.4.26	倒花15-18	1990—1995	4.0	25.5	43

下载: 导出CSV

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