煤炭工程 ›› 2025, Vol. 57 ›› Issue (5): 107-116.doi: 10. 11799/ ce202505015

• 研究探讨 • 上一篇    下一篇

急倾斜煤层长壁采场底板应力传递路径倾角效应研究

朱开鹏   

  1. 中煤科工西安研究院(集团)有限公司
  • 收稿日期:2024-12-11 修回日期:2025-01-24 出版日期:2025-05-13 发布日期:2025-07-03
  • 通讯作者: 朱开鹏 E-mail:61387363@qq.com

Dip angle effect of stress transfer path in floor of longwall stope in steeply pitching coal seam#br#

  • Received:2024-12-11 Revised:2025-01-24 Online:2025-05-13 Published:2025-07-03

摘要:

为探究急倾斜煤层长壁采场底板采动应力传递路径的倾角效应,以新疆2130煤矿急倾斜长壁综采工作面为工程背景,采用物理相似模拟与数值计算相结合的研究方法,在全面厘定并分析底板非对称变形破坏一般规律的基础上,对底板采动应力的传递路径及其倾角效应进行了研究,量化表征了急倾斜煤层底板主应力大小渐变以及方向偏转的演化特征。结果表明: 在急倾斜煤层开采过程中,受煤层倾角影响,底板采动应力传递路径呈非对称反拱形态;在应力拱内部,直接底以及工作面倾向中下部区域的基本底处于受拉状态;在应力拱外部,以应力偏转界线为界限,底板主应力向倾向两侧煤体传递。并且,随着煤层倾角的增大,底板应力拱的拱高以及工作面倾向下侧煤体底板的应力集中系数均呈的演化趋势;底板第一主应力的大小和卸荷系数逐渐降低,最大卸荷位置向工作面倾向下侧煤体迁移;第一主应力向x轴正方向偏转,使得底板破坏深度逐渐减小。受此影响,底板的最大破坏深度位于工作面倾向中下部区域;同时,在采空区矸石的非均衡约束作用下,工作面倾向中上部区域的底板块体结构更易出现失稳滑移,且在持续的采动影响下底板滑移区易向上扩展。基于此,可通过对底板易破坏滑移区域采取重点关注、区域治理的防治措施,改善该区域底板的应力环境和结构特征,以期实现对急倾斜煤层长壁采场底板的稳定性控制。

关键词:

急倾斜煤层 , 底板 , 采动应力 , 倾角效应

Abstract: The stability control of the floor is the basis of the stability control of the ' support-surrounding rock ' system in steeply inclined coal seam mining. Based on the engineering background of a steeply inclined long-wall fully mechanized mining face in a mine, this paper adopts the research method of combining physical similarity simulation and numerical calculation. On the basis of comprehensively determining and analyzing the general law of asymmetric deformation and failure of floor, the transmission path of floor mining stress and its dip angle effect are studied, and the evolution characteristics of principal stress gradient and direction deflection of floor in steeply inclined stope are quantitatively characterized. The results show that in steeply inclined coal seam mining, the transmission path of mining-induced stress in the floor exhibits an asymmetric anticlinal shape under the influence of the coal seam dip angle. Within the stress arch, the immediate floor and the basic floor in the middle-lower region of the working face are under tensile stress, with the principal stress direction nearly parallel to the coal seam. Outside the stress arch, the principal stress in the floor deviates toward both sides of the coal body, with the stress deflection boundary serving as the demarcation line. Furthermore, as the coal seam dip angle increases, the arch height of the floor stress arch and the support pressure on the lower side of the working face floor exhibit a decrease-increase-decrease trend. The magnitude of the first principal stress and the unloading coefficient gradually decrease, with the maximum unloading position migrating toward the coal body on the lower side of the working face. The direction of the first principal stress gradually deflects towards the coal seam, resulting in a gradual reduction in the depth of floor failure. As a result, the maximum failure depth of the floor is located in the middle-lower region of the working face. Meanwhile, influenced by the unequal confinement effect of the goaf's waste rock, the floor block structure in the middle-upper region of the working face is more prone to instability and sliding, with upward expansion likely under continued mining disturbance. Based on these findings, targeted preventive measures such as "key monitoring and regional treatment" can be implemented in areas prone to failure and sliding. These measures aim to improve the stress environment and structural characteristics of the floor in these regions, thereby achieving effective stability control of the floor in steeply inclined longwall mining faces.