中国安全科学学报 ›› 2019, Vol. 29 ›› Issue (9): 138-143.doi: 10.16265/j.cnki.issn1003-3033.2019.09.022

• 安全工程技术科学 • 上一篇    下一篇

破碎围岩结构面特征及稳定性分析

赵康1,2 副教授, 王庆2, 王军强1, 索天元1, 郝蛟龙1, 柳小胜3   

  1. 1 灵宝金源矿业股份有限公司,河南 灵宝 472500;
    2 江西理工大学 建筑与测绘工程学院,江西 赣州 341000;
    3 长沙矿山研究院有限责任公司,湖南 长沙 410012
  • 收稿日期:2019-05-12 修回日期:2019-07-15 出版日期:2019-09-28 发布日期:2020-10-30
  • 作者简介:赵 康 (1980—),男,河南周口人,博士,副教授,主要从事工程岩体监测及稳定性、岩土工程数值计算方面的教学与研究工作。E-mail:zhaok_666666@163.com。
  • 基金资助:
    国家自然科学基金资助(51764013);中国博士后基金面上资助(2019M652277);江西省自然科学基金重点资助(20192ACBL21014);研究生创新专项资金资助(XS2018-S012、ZS2018-S031)。

Structural plane characteristics and stability of broken surrounding rocks

ZHAO Kang1,2, WANG Qing2, WANG Junqiang1, SUO Tianyuan1, HAO Jiaolong1, LIU Xiaosheng3   

  1. 1 Lingbao Jinyuan Mining Company Limited, Lingbao Henan 472500, China;
    2 School of Architectural and Surveying & Mapping Engineering, Jiangxi University of Science and Technology, Ganzhou Jiangxi 341000, China;
    3 Changsha Institute of Mining Research Limited Company, Changsha Hunan 410012, China
  • Received:2019-05-12 Revised:2019-07-15 Online:2019-09-28 Published:2020-10-30

摘要: 为评价某金矿极破碎围岩的稳定性,测量并分析该矿围岩Ⅳ、Ⅴ级微型裂隙结构面,选取+260、+295、+330 m等3个生产中段;利用详细测线法分析节理间距、产状、起伏形态、粗糙度、张开度、渗水性对围岩稳定性的影响,使用极点图、玫瑰花图探讨优势结构面产状的分布特性。结果表明:该矿围岩节理裂隙较发育,节理分布较为紧密,平均间距小于1 m,且主要集中在0.2~0.6 m,围岩整体属于破碎、极破碎岩体,稳定性较差;该矿+260、+295和+330 m中段的产状优势结构面相似,都具有明显集中现象,倾向主要集中在324~360 °和0~35 °,倾角主要集中在70~79 °;结构面的起伏状态多为平直型,对结构面稳定性影响较大;结构面之间结合较为紧密,填充物较少,对结构面的稳定性影响较小。

关键词: 破碎围岩, 围岩稳定性, 结构面特征, 节理裂隙, 详细测线法

Abstract: In order to evaluate the stability of extremely fractured surrounding rocks in a gold mine, micro-fracture structural planes of the IV and V grade of the surrounding rocks in the mine were measured and analyzed in three production sections of +260, +295 and +330 m. The influences of joint spacing, occurrence, undulating shape, roughness, openness and seepage on surrounding rock stability were analyzed by scanline method. The distribution characteristics of dominant structural planes occurrence were discussed by using pole plot and rose plot. The results show that the surrounding rock joints are well developed and closely distributed, and the average spacing is less than 1m and is mainly concentrated in 0.2-0.6 m. The surrounding rocks are broken and extremely broken rock mass with poor stability. The dominant occurrence has obvious concentration in the middle of +260, +295 and +330 m. The dip is mainly concentrated at 324-360 ° and 0-35 °, and the dip direction is mainly concentrated at 70-79 °. The undulating state of the structural plane is mostly straight, which has a great influence on the stability of the structural plane. The structural surfaces are tightly combined with less filler, which has less influence on the structural surface stability.

Key words: broken surrounding rocks, surrounding rock stability, structural plane characteristics, joint crack, scanline method

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