中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
冕宁县牦牛坪稀土矿区“ 7`18”水石流灾害

文献类型:期刊论文

作者马东涛; 陈英
刊名山地学报
出版日期2014
卷号32期号:6页码:732-738
关键词水石流 形成条件 特征 稀土矿区 危害
其他题名An Approach about Water stone Flow Hazards Occurred in July 18th,2013 in Maoniuping Rare Earth Mining Area in Mianning,Sichuan
通讯作者马东涛
中文摘要2013-07-17T20:00—2013-07-18T3:00,冕宁县牦牛坪稀土矿区7 h降雨219 mm,瓦维埃河及支沟发生6处水石流,对采矿场、选矿厂、地面站、弃土场、排洪沟、矿山公路及矿山环境造成严重危害。研究发现:牦牛坪矿区具备水石流发育的充分条件,泥石流沟处于发育壮年期,但泥石流处于衰退期。“7·18”水石流是在100 a一遇强暴雨激发下,沟床及岸坡老泥石流堆积物和沟床堆积物在山洪冲蚀下切、侧蚀下形成的,暴雨和水石流暴发频率同步。其水石流具有固体物质粗大(最大粒径8 m),块砾石含量高(80%以上),粉、粘粒含量极低(小于1%),容重高(16~185 t/m3),冲淤变化大(最大冲深10 m,最大淤积5 m),规模大(总冲出量50×104 m3)等特点。
英文摘要Waterstone flow is a special type of debris flow,which usually breaks out in granite,limestone,marble area and in rare rainstorm. In July 18,2013,a heavy rainstorm with rainfall of 219 mm in 7 hours in Maoniuping rareearth mining area of Mianning County,Sichuan,China triggered 6 waterstone flow and 2 mining debris flow in Waweiai River Basin and its tributaries. The mining fields,ore dressing plant,ground station,dump,flood discharge trench,mining road et al and mine environment suffered serious harms. The study shows that the studied region has sufficient conditions for waterstone flow developing,and the debris flow is in the stage of maturity while the debris flow is in a recession. July 18 waterstone flows are induced by a strong rainfall with frequency of 100 years,which eroded and incised old debris flow bank and bed deposits along with flash flood. The frequency of heavy rain and outbreak of waterstone flow has same synchronization. The waterstone flow has some features such as coarse solids (maximum diameter of 8 m),very low content of powder and clay (less than 1%),high bulk density (1.6~1.85 t/m3),strong scouring and silting changes in gully bed (maximum scour depth 10 meters,the largest deposition depth of 5 meters),large scale (with total capacity of 50×104 m3 of solid materials ) etc.
分类号P642.23
语种中文
公开日期2014-09-05
源URL[http://ir.imde.ac.cn/handle/131551/7194]  
专题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
马东涛,陈英. 冕宁县牦牛坪稀土矿区“ 7`18”水石流灾害[J]. 山地学报,2014,32(6):732-738.
APA 马东涛,&陈英.(2014).冕宁县牦牛坪稀土矿区“ 7`18”水石流灾害.山地学报,32(6),732-738.
MLA 马东涛,et al."冕宁县牦牛坪稀土矿区“ 7`18”水石流灾害".山地学报 32.6(2014):732-738.

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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