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基于水动力的典型矿山泥石流运动模式研究

常鸣 唐川

水利学报Issue(11):1318-1326,9.
水利学报Issue(11):1318-1326,9.DOI:10.13243/j.cnki.slxb.2014.11.007

基于水动力的典型矿山泥石流运动模式研究

Study on typical movement model in mine debris flow based on hydrodynamic force conditions

常鸣 1唐川1

作者信息

  • 1. 成都理工大学 地质灾害防治与地质环境保护国家重点实验室,四川 成都 610059
  • 折叠

摘要

Abstract

Some artificial accumulations of slag become more broken caused by“4·20”Lushan earthquake in 2013. Hougou is a typical mines debris flow susceptible region in earthquake zone of Shimian County. The motion pattern of its debris flow is closely related with terrain, hydrologic, static and dynamic, and material conditions. Since there are differences in motion patterns of man-made and natural debris flows, this study started with the four conditions and took Hougou debris flow as an example to discuss the mo⁃tion pattern of mine debris flow in detail. The results show that the process of Hougou debris flow involves the following five aspects:(a) stability of waste slag reduced by initial rainfall;(b) slag slope eroded by continuous rainfall;(c) channel slag moving stimulated by rainwater;(d) debris flow forming with high content of slag torrent,and (e) debris flow scale enhanced by slag erosion along the gully.

关键词

矿山泥石流/矿渣/水动力

Key words

mine debris flow/slag/hydrodynamic force

分类

天文与地球科学

引用本文复制引用

常鸣,唐川..基于水动力的典型矿山泥石流运动模式研究[J].水利学报,2014,(11):1318-1326,9.

基金项目

西南地形急变带地质灾害综合调查与风险制图(2011FY110100-3);高等学校博士学科点专项基金;汶川震区滑坡泥石流演化规律与活动规律预测研究 ()

水利学报

OA北大核心CSCDCSTPCD

0559-9350

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