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钟秀梅, 陈文凯, 侯景瑞, 袁中夏. 汶川地震触发武都区和文县地质灾害发育特征研究[J]. 岩土工程学报, 2011, 33(zk1): 349-353.
引用本文: 钟秀梅, 陈文凯, 侯景瑞, 袁中夏. 汶川地震触发武都区和文县地质灾害发育特征研究[J]. 岩土工程学报, 2011, 33(zk1): 349-353.
ZHONG Xiu-mei, CHEN Wen-kai, HOU Jing-rui, YUAN Zhong-xia. Distribution rules of geo-hazards induced by Wenchuan Earthquake[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(zk1): 349-353.
Citation: ZHONG Xiu-mei, CHEN Wen-kai, HOU Jing-rui, YUAN Zhong-xia. Distribution rules of geo-hazards induced by Wenchuan Earthquake[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(zk1): 349-353.

汶川地震触发武都区和文县地质灾害发育特征研究

Distribution rules of geo-hazards induced by Wenchuan Earthquake

  • 摘要: 汶川地震在甘肃省触发了大量的崩塌、滑坡等地质灾害,武都区和文县的地质灾害尤为发育,占甘肃省灾害总量的 75% ,因此,通过灾后对地震地质灾害的现场调查和遥感解译,共获得该区地质灾害点 993 处。在此基础上,利用 GIS 技术对地震地质灾害的分布与河流水系、烈度、高程等因素的关系进行统计分析。研究得出:①地震地质灾害在区域上具有沿河流水系成线状分布的特点;②地震地质灾害密度随烈度的增加而增大;③大部分地震地质灾害分布在高程 1000 ~ 2000 m 的中高山地貌区;④地形坡度是地震地质灾害发育的控制性因素之一,绝大部分灾害集中在坡度 10 °~ 40 °的范围内; ⑤坡向对地震地质灾害的发育也有影响,正南坡向和东南坡向的地质灾害较为发育 。

     

    Abstract: Wenchuan Earthquake causes a large number of geo-hazards in Wudu District and Wenxian County of Gansu Province. After a field investigation and the interpretation of remote-sensing images taken after the earthquake , 993 earthquake-induced geo-hazards are obtained. Then, the distribution of these geo-hazards is investigated statistically using GIS techniques to determine how the occurrence of geo-hazards correlates with distance from the rivers, slopes, elevations and aspect s. The main results of this research can be summarized as follows: (1) the geo-hazards triggered by earthquake show the feature of zonal distribution along the rivers; (2) the geo-hazards density increases with the increase of earth intensity; (3) the earthquake-induced geo-hazards have corresponding relationship with the elevation, and for most hazards occur below the elevation of 1000 to 2000 m; (4) the slope steepness is a main factor which controls the development of earthquake-induced geo-hazards and a vast majority of geo-hazards are distributed within the range of 10 ° to 40 ° ; (5) aspect influences on the geo-hazards triggered by the Earthquake, and more hazards occur in aspect of due south and southeast.

     

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