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金属矿山 ›› 2024, Vol. 53 ›› Issue (5): 84-.

• “矿业青年科学家”专题 • 上一篇    下一篇

硬岩矿体自然崩落过程成拱特征及其边界弱化

黄明清1 张厚缘1 郭晓强2 郑其伟1 刘青灵1   

  1. 1. 福州大学紫金地质与矿业学院,福建 福州350108;2. 紫金矿业集团股份有限公司,福建 上杭 364200
  • 出版日期:2024-05-15 发布日期:2024-06-14

Arching Characteristics and Boundary Weakening in Block Caving of Hard Orebodies

HUANG Minqing1 ZHANG Houyuan1 GUO Xiaoqiang2 ZHENG Qiwei1 LIU Qingling1   

  1. 1. Zijin School of Geology and Mining,Fuzhou University,Fuzhou 350108,China; 2. Zijin Mining Group Co. ,Ltd. ,Shanghang 364200,China
  • Online:2024-05-15 Published:2024-06-14

摘要: 硬岩矿体自然崩落过程中崩落顶板压力拱加剧了崩落边界的应力集中,崩落进程易受拱脚两侧的夹制 而受阻。通过崩落顶板压力拱极限自稳平衡计算及数值模拟分析硬岩崩落顶板成拱特征及崩落中止的潜在区域,进 而探讨通过边界弱化来预处理硬岩的工程措施。引入成拱系数及崩落损伤因子表征拉底上方不同区域岩体塑性区 的逐年发展趋势,采用塑性区相对位置反映割帮位置及割帮时机,从而解决边界弱化的时效性问题。结果表明:硬岩 矿体在上向崩落过程中,崩落顶板易形成自稳平衡拱并引起崩落减缓或中止,崩落顶板顶部压力和水平压力是引起 压力拱持续破坏的直接因素;拉底推进时崩落压力拱跨度以非均匀速率不断增加,压力拱边界随着拉底的推进而不 断前移,且拉底推进线前方始终处于高应力集中区域。当上盘矿岩交界处塑性区出现的时间滞后于拉底前锋时,可 采用割帮来破坏崩落拱平衡并促进持续崩落。研究结果有助于确定硬岩矿体自然崩落法边界弱化的区域与时机。

关键词: 自然崩落法 平衡拱 边界弱化 崩落损伤因子

Abstract: During block caving of hard rock orebodies,the pressure arch of the caving back intensifies the stress concentration at the caving boundary,and the caving process is easily hindered by the restraint on both sides of the arch feet. By calculating the ultimate self-stable balance of the pressure arch at the caving roof and analyzing the characteristics of the arch formation and the potential areas of caving cessation through numerical simulation,the engineering measures for pre-conditioning of hard rock by boundary weakening is proposed. The arching coefficient and caving damage factor are introduced to characterize the annual development trend of the plastic zone above the undercutting in different areas of the rock mass,and the relative position of the plastic zone is used to reflect the position and timing of slot cutting,thereby ascertaining the timeliness of boundary weakening. The results show that during the upward caving process of hard rock masses,the caving roof is prone to forming a self-stable arch,which causes the caving to slow down or cease. The vertical and horizontal pressures at the top of the caving back are the direct factors causing the continuous destruction of the pressure arch. As undercutting advances,the span of the caving pressure arch increases at a non-uniform rate,and the boundary of the pressure arch continuously moves forward with the advance of the undercutting,and the area in front of the undercutting line is always in a high stress concentration condition. When the plastic zone at the ore-rock boundary appears later than the undercutting forward line,slot cutting can be used to destroy the balance of the caving arch and promote propagative caving. The study results are helpful for determining the area and timing of boundary weakening of hard rock masses in block caving.

Key words: block caving,balancing arch,boundary weakening,caving damage factor