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特厚煤层综放工作面覆岩移动规律及冲击地压防治

Overlying strata movement law and rockburst prevention & control for fully mechanized top coal caving face in extra-thick coal seams.

作者信息

Rong Hai, He Longyue, Wang Yadi, Wei Xiangzhi, Wei Shilong, Yang Suihan, Li Jincheng, Chen Linlin

机构信息

College of Mining, Liaoning Technical University, Fuxin, 123000, China.

Graduate School of Liaoning Technical University, Fuxin, 123000, China.

出版信息

Sci Rep. 2025 Feb 8;15(1):4750. doi: 10.1038/s41598-025-89133-7.

Abstract

To investigate the movement law of overlying strata in the fully mechanized top-coal caving face of extra-thick coal seams and further achieve the effective prevention and control of rock burst. Taking the 12,240 working face of Gengcun Coal Mine as the engineering background, initially, the calculation formula for the collaborative deformation load of hard rock strata and the formula for the instability scale of hard rock strata are employed to precisely ascertain the position and instability scale of the key strata. Subsequently, a UDEC calculation model is established to comprehensively investigate the instability characteristics of the overlying hard rock strata. Simultaneously, a meticulous analysis of the working resistance of the on-site supports is carried out to validate the theoretical computations. Eventually, in light of the research findings, a rational determination of the cutting scale is made so as to offer a scientific foundation and efficacious guidance for the execution of roof pre-splitting blasting operations. The research results show that within 50 m above the 12,240 working face, there is one low-position hard strata and three medium-position hard strata. Under the influence of mining, the displacement field of the overlying hard strata is symmetrically distributed with respect to the central axis of the goaf. The stress rise areas on both sides of the goaf present a "hyperbolic" distribution, and the stress of the goaf roof and floor is released, showing an "elliptical parabolic belt" distribution. The periodic instability occurred about 8 m after the initial instability of the low-level hard rock layer, and the periodic instability occurred about 20 m after the initial instability of the middle hard rock layer 1. The goaf of the 12,220 working face in the north of the working face is a crucial reason for the support resistance of the upper part of the 12,240 working face being greater than that of the middle part and the middle part being greater than that of the lower part. When the working face advances 20-30 m, a distinct pressure accumulation area emerges in the middle of the working face and is regularly distributed as the working face advances. The monitoring results indicate that microseismic events are concentrated in the basic roof and medium-position strata 1, and energy events of 10 J are prone to occur. The basic roof and medium-position strata 1 are the key points for rock burst prevention of the working face. A roof cutting scale of no more than 10 m for the low-position hard strata can effectively reduce the rock burst risk. The research results provide theoretical support for roof pre-splitting and rock burst prevention of the 12,240 working face in Gengcun Coal Mine and can offer guidance for the prediction and prevention and control of rock burst risk in mines and working faces under similar conditions.

摘要

为研究特厚煤层综放开采工作面覆岩运动规律,进一步实现冲击地压的有效防治。以耿村煤矿12240工作面为工程背景,首先采用硬岩层协同变形载荷计算公式和硬岩层失稳尺度公式精确确定关键层位置及失稳尺度,随后建立UDEC计算模型全面研究覆岩硬岩层失稳特征,同时对现场支架工作阻力进行细致分析以验证理论计算,最终根据研究结果合理确定割煤尺度,为顶板预裂爆破作业实施提供科学依据和有效指导。研究结果表明,12240工作面上方50 m范围内存在一层低位硬岩层和三层中位硬岩层。在采动影响下,覆岩硬岩层位移场相对于采空区中轴线对称分布,采空区两侧应力升高区呈“双曲线”分布,采空区顶底板应力释放,呈“椭圆抛物线带”分布。低位硬岩层初次失稳后约8 m发生周期失稳,中位硬岩层1初次失稳后约20 m发生周期失稳。工作面北部12220工作面采空区是导致12240工作面上部支护阻力大于中部、中部大于下部的关键原因。当工作面推进20 - 30 m时,工作面中部出现明显的压力积聚区,并随工作面推进呈规律分布。监测结果表明,微震事件集中在基本顶和中位岩层1,易发生能量为10 J的能量事件。基本顶和中位岩层1是工作面冲击地压防治的重点。低位硬岩层顶板切割尺度不超过10 m可有效降低冲击地压风险。研究成果为耿村煤矿12240工作面顶板预裂和冲击地压防治提供了理论支撑,可为类似条件矿井及工作面冲击地压风险预测与防治提供指导。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/afbf/11807143/e1fd51866fc4/41598_2025_89133_Fig1_HTML.jpg

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