长江科学院院报 ›› 2017, Vol. 34 ›› Issue (8): 111-119.DOI: 10.11988/ckyyb.20160484

• 岩土工程 • 上一篇    下一篇

我国倾倒变形体发育规律研究

陆文博1, 晏鄂川1, 邹浩1, 张世殊2   

  1. 1.中国地质大学(武汉) 工程学院,武汉 430074;
    2.中国电建集团 成都勘测设计研究院有限公司,成都 610072
  • 收稿日期:2016-05-19 修回日期:2016-06-24 出版日期:2017-08-01 发布日期:2017-08-18
  • 作者简介:陆文博(1992-),男,湖北孝昌人,硕士研究生,主要从事岩土体稳定性评价与利用的研究,(电话)18062651007(电子信箱)lwblwb21@126.com。

Development Rules of Toppling Deformation Slopes in China

LU Wen-bo1, YAN E-chuan1, ZOU Hao1, ZHANG Shi-shu2   

  1. 1.Faculty of Engineering, China University of Geosciences, Wuhan 430074, China;
    2.Chengdu Engineering Corporation Limited, Power China, Chengdu 610072, China
  • Received:2016-05-19 Revised:2016-06-24 Online:2017-08-01 Published:2017-08-18
  • Supported by:
    中国电建集团成都勘测设计研究院有限公司科技项目(P225-2014)

摘要: 倾倒变形体发育规律研究在倾倒变形防治规划及水电工程选址中具有重要意义。统计国内的倾倒变形体,有助于分析我国倾倒变形体发育规律。根据倾倒变形体的分布提出倾倒变形体区域地质易发性分区研究范围,选取地貌、地层时代、地震烈度、构造应力分布为影响因子,针对倾倒变形体进行区域地质易发性区划评价。选择在西部地区发育的11条主要河流上的水电工程倾倒变形体进行地理位置易发性区划评价,分析不同等级中倾倒变形体分布特点与发育要素(岩性、坡高、坡角、发育高程、水平及垂直发育深度)的对应关系。结果表明:倾倒变形体主要分布在四川、青海、云南3省;横断山脉“极大、大起伏高山”区属于倾倒变形体地质极易发区;雅砻江中游、澜沧江中上游、黄河上游、大渡河上游、岷江上游等河流属于倾倒变形体地理位置易发性较高区段。通过此研究,可为西南倾倒变形体防治规划及水电工程选址提供一定的参考依据。

关键词: 倾倒变形体, 区域地质, 西部水电工程, 地理位置, 易发性, 发育规律

Abstract: Researches on the development rule of toppling deformation slopes is of great significance in prevention planning for toppling deformation and site selection for hydropower projects. And statistical research is conducive to the analysis of toppling deformation slopes in China. In this article, the west region of China is determined as the study area in view of the distribution of toppling deformation slopes. Four influencing factors are selected for geographical susceptibility zoning evaluation, namely landform, stratigraphic age, seismic intensity and tectonic stress distribution. Toppling deformation slopes of 11 rivers in west China are taken as examples for the evaluation of geographical position susceptibility. The relations between distribution features and development factors (lithology, slope height, slope angle, elevation, horizontal depth and vertical depth) are revealed according to the zoning results. Results show that 1) toppling deformation slopes mainly exist in Sichuan, Qinghai and Yunnan provinces; 2) Hengduan Mountains with extremely large and large heaves belong to the zone of extremely high susceptibility; 3) areas of high susceptibility are located in the middle reach of Yalong River, the middle and upper reaches of Lancang River, the upstream of Yellow River, Dadu River and Minjiang River. The research results offer reference for prevention planning of toppling deformation and site selection for hydropower projects in southwest China.

Key words: toppling deformation slope, regional geology, hydropower projects in west China, geographical position, susceptibility, development rule

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