芦山地震灾区地震前后地质灾害发育规律与对比
文献类型：期刊论文
| 作者 | 孔纪名
|
| 刊名 | 山地学报
 |
| 出版日期 | 2014 |
| 卷号 | 32期号:1页码:111-116 |
| 关键词 | 地质灾害 发育规律 对比研究 芦山地震 |
| 其他题名 | efore and after the Lushan Earthquake Contrast Geohazards in Earthquake-stricken Areas |
| 通讯作者 | 孔纪名 |
| 合作状况 | 国内 |
| 中文摘要 | 为了研究芦山地震前后地质灾害在不同环境中的分布规律，对研究区震前3 814 处和震后新增1 337 处地质灾害与各环境因素的关系进行了统计和分析，得出以下结论: 1． 震后新增灾害数量的88. 41% 分布在距震中100km 范围内，密度随距震中距离的增大而减小; 新增灾害67. 31%分布在地震烈度Ⅶ度及其以上地区，灾害密度随地震烈度减小而逐渐减小。2． 震前和震后新增灾害数量和密度均随距河流距离的增大而减小。3． 震前和新增地质灾害数量和密度在砂砾岩和花岗岩中较为发育。4． 震后和新增灾害数量和密度均以海拔500 ～ 1 000 m 和1 000 ～1 500 m 较大。5． 震前和震后新增灾害总数的94. 99% 和91. 85% 发生在坡度小于40°的范围; 震前灾害密度在随坡度增大逐渐减小，震后新增灾害密度随坡度变化规律不明显，其主要原因是震前灾害以滑坡为主，而震后新增灾 害崩塌和滑坡数量相当。 |
| 英文摘要 | For revealing the distribution of geohazards in environmental factors，3 814 geohazards before Lushan earthquake and 1 337 geohazards after Lushan earthquake were used to statistics and analysis the relationship between geohazards and environmental factors． The main results of the paper can be summarized as follows． (1) 88. 41% of geohazards after earthquake distributed in the range of 100 km from the epicenter and the density of geohazards decreased with the increase of distance from epicenter． About 67. 31% of geohazards after earthquake distributed in area with or more than seismic intensity VII and the density of geohazards decreased with the increase of seismic intensity． ( 2) The amount and density of geohazards before earthquake and geohazards after earthquake all decreased with the increase of distance from rivers． ( 3) The amount and density of geohazards before earthquake and geohazards after earthquake were maximum in conglomerate and granite． ( 4) The amount and density of geohazards before earthquake and geohazards after earthquake were maximum in relief from 500 to 1 000 meters and 1 000 to 1 500 meters． ( 5) About 94. 99% of geohazards before earthquake and 91. 85% of geohazards after earthquake were in area where the slope was less than 40°． The density of geohazards before earthquake decreased with the increase of slope but the density of geohazards after earthquake did not changed obviously with the slope． |
| 分类号 | P694;X43 |
| 收录类别 | CSCD |
| 资助信息 | 国家高技术研究发展计划(863计划) 项目(2012AA121302);西南科技大学博士基金(11zx7160);国家自然科学基金项目(41272297，41371185) |
| 语种 | 中文 |
| CSCD记录号 | CSCD:5135246 |
| 公开日期 | 2014-05-20 |
| 源URL | [http://ir.imde.ac.cn/handle/131551/6940]  |
| 专题 | 成都山地灾害与环境研究所_成都山地所知识仓储（2009年以前） 成都山地灾害与环境研究所_山地灾害与地表过程重点实验室 |
| 推荐引用方式 GB/T 7714 | 孔纪名. 芦山地震灾区地震前后地质灾害发育规律与对比[J]. 山地学报,2014,32(1):111-116. |
| APA | 孔纪名.(2014).芦山地震灾区地震前后地质灾害发育规律与对比.山地学报,32(1),111-116. |
| MLA | 孔纪名."芦山地震灾区地震前后地质灾害发育规律与对比".山地学报 32.1(2014):111-116. |
入库方式： OAI收割
来源：成都山地灾害与环境研究所
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