| 引用本文: | 段书苏,姚令侃,郭沉稳.山区复杂大流域地貌发育阶段判识方法及应用[J].哈尔滨工业大学学报,2016,48(3):147.DOI:10.11918/j.issn.0367-6234.2016.03.025 |
| DUAN Shusu,YAO Lingkan,GUO Chenwen.Tendency prediction of collapse-landslide caused by earthquake based on the erosion cycle theory[J].Journal of Harbin Institute of Technology,2016,48(3):147.DOI:10.11918/j.issn.0367-6234.2016.03.025 |
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| 山区复杂大流域地貌发育阶段判识方法及应用 |
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段书苏1, 姚令侃1,2,3, 郭沉稳1
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(1.西南交通大学 土木工程学院,610031 成都; 2.抗震工程技术四川省重点实验室 道路与铁道工程抗震技术研究所,610031 成都;3.高速铁路线路工程教育部重点实验室,610031 成都)
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| 摘要: |
| 为确定山区复杂大流域的地貌发育阶段及其在地震、暴雨等触发条件下的灾害区域严重程度.基于地貌循环理论和山区复杂大型流域的分阶段发育的理论，将斯特拉勒积分的计算方法与坡降指标（SL指标）结合，以确定山区复杂大流域的发育阶段.利用DEM（digital elevation model）和ArcGIS技术，计算发育阶段并据此评价崩塌滑坡在触发条件具备时的区域严重程度.在山区复河流复杂大流域内，分支小流域的斯特拉勒积分的变化点，SL指标的突变点均可以作为发育阶段的分界点；在同一发育阶段内，斯特拉勒积分值分布集中，整个发育阶段的斯特拉勒积分可以作为处于这一发育阶段的所有分支小流域发育阶段的代表值.处于幼年晚期和壮年期的流域，斯特拉勒积分处于0.45~0.6之间，崩塌滑坡最严重.
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| 关键词: 侵蚀循环理论 河流分阶段发育理论 斯特拉勒积分 坡降指标SL 地震触发崩塌滑坡 |
| DOI：10.11918/j.issn.0367-6234.2016.03.025 |
| 分类号:U211.9 |
| 文献标识码:A |
| 基金项目:国家自然科学基金面上项目(41172321)； 国家自然科学基金重点项目(41030742)； 中国铁路总公司科技研究开发计划课题(2013G014-A). |
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| Tendency prediction of collapse-landslide caused by earthquake based on the erosion cycle theory |
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DUAN Shusu1, YAO Lingkan1,2,3, GUO Chenwen1
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(1. School of Civil Engineering, Southwest Jiaotong University, 610031 Chengdu, China; 2. Road and Railway Engineering Research Institute, Sichuan Key Laboratory of Seismic Engineering and Technology, 610031 Chengdu, China; 3.MOE Key Laboratory of High-speed Railway Engineering,610031 Chengdu, China)
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| Abstract: |
| A method of determining the stage of geomorphic development is built up in complicated mountainous river basin, which can also be used to regional assessment of the regional severity of collapse-landslide caused by earthquake or heavy rainstorm. Based on the theory of the erosion cycle and the theory of river's developing by stages, the stage of geomorphic development is estimated by combining the Strahler's integral (HI) and the stream-gradient indices (SL indices). Then regional severity of collapse-landslide is estimated by development stage with DEM (digital elevation model) and ArcGIS technique. Both of the change point of HI of branch basins and the breakpoint of SL indices can be the cut-off point of development stage. In the same development stage, HIs are very similar. HI of the whole same development stage can be the representative HI of all the HIs of branch basins. The basins in development stage of late youth and maturity have the severest regional disasters, with HI change from 0.45~0.6.
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| Key words: erosion cycle theory theory of river basin development by stage Strahler’s integral (HI) stream-gradient indices (SL indices) collapse-landslide caused by earthquake |
