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2025, 02, No.261 34-36+41
某高原沟谷型泥石流发育特征及其影响分析
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摘要:

该文从地质构造及地层岩性两方面,分析了西藏某矿山泥石流物源颗粒的组成及形成背景。根据矿区泥石流发育特征,计算得到泥石流容重、流速、流量及一次输移量等参数。以N2泥石流为例,经分析,N2区域泥石流的规模较小、中等发育、处于发展期,并对该处拟建排土场的潜在风险进行评价,提出了解决建议。

Abstract:

This paper analyzes the composition and formation background of debris flow source materials in a mining area in Tibet from the perspectives of geological structure and stratigraphic lithology. Based on the development characteristics of debris flow in the mining area, key parameters such as unit weight, velocity, discharge, and single transport volume of the debris flow is calculated. Taking the N2 debris flow as an example, the analysis indicates that the debris flow in the N2 area is small in scale, moderately developed, and currently in a developmental stage. The study also evaluates the potential risks posed to the proposed waste disposal site in the area and offers corresponding mitigation suggestions.

参考文献

[1] 屈永平,朱静,卜祥航,等.西藏林芝地区冰川降雨型泥石流起动实验初步研究.岩石力学与工程学报,2015,34(增刊1):3256~3266.

[2] 刘建康,程尊兰.西藏古乡沟泥石流与气象条件的关系.科学技术与工程,2015,15(09):45~49,55.

[3] 李金洋,尹国龙,黄海,等.藏东高原浅丘红层区泥石流发育特征及活动性研究.钻探工程,2024 ,51 (03):45~53.

[4] 喻涌麒,周南,秦龙华,等.云南玉龙县雾露湾泥石流成因机制分析及治理措施.云南地质,2024 ,43 (02):274~278.

[5] 中国地质环境监测院.地质灾害危险性评估规范:GB/T 40112—2021.北京:中国标准出版社,2021.

[6] 中华人民共和国国土资源部.泥石流灾害防治工程勘查规范:DZ/T 0220—2006.北京:中华人民共和国国土资源部,2006.

基本信息:

中图分类号:P642.23

引用信息:

[1]王斌,曹鑫,姜士磊.某高原沟谷型泥石流发育特征及其影响分析[J].勘察科学技术,2025,No.261(02):34-36+41.

发布时间:

2025-04-20

出版时间:

2025-04-20

引用

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