超前工作面巷道变形和顶板能量累积的灾害机理研究

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2025-04-16 DOI:10.1155/gfl/9692590
Long Cheng
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引用次数: 0

摘要

顶板能量积累导致煤矿超前破坏和巷道破坏是煤矿面临的重要灾害之一。识别顶板能量聚集的位置,可以预测顶板超前破坏和巷道变形的位置,从而采取预防措施。基于两种广义位移梁,研究了不同荷载、不同厚度、不同悬臂长度作用下顶煤壁弯矩和能量密度的累积规律。得出以下结论:(1)在不同荷载条件下,弯矩峰值和能量密度峰值均出现在煤壁前方10m处,达到峰值后迅速减小至0,不再变化。弯矩峰值随荷载的增加呈线性增加,关系式为M =−143.32q−286.63。弯矩峰值随荷载的增加呈指数变化,关系为Ue = 200.46e0.42q。(2)在不同厚度下,厚度对岩层的弯矩在峰值处呈不规则分布。当厚度为12.5和15 m时,变化趋于一致,当厚度为7.5和10 m时,厚度为17.5 m时顶板弯矩较小。当厚度小于17.5 m时,厚度越小,峰值越大,峰值越超前。屋面厚度越小,能量密度积累的范围越小。(3)在不同悬臂长度下,随着悬臂长度的增加,峰值弯矩呈线性增加,关系为Me =−158.22 L + 137.4,弯矩积累范围随着顶板悬臂长度的增加而增大。随着悬臂梁长度的增加,顶板的峰值能量密度呈指数增长,关系为Ue = 3.5536e1.1067L,顶板的引线能量积累距离增大。(4)当顶板厚度为10 m时,应力峰值在工作面前方5 ~ 15 m范围内出现频率较高,很好地验证了理论分析的正确性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Study on Disaster Mechanism of Roadway Deformation and Roof Energy Accumulation in Advance Working Face

Study on Disaster Mechanism of Roadway Deformation and Roof Energy Accumulation in Advance Working Face

It is one of the important disasters faced by coal mine that roof energy accumulation leads to its advance failure and roadway failure. Identifying the position of roof energy accumulation can predict the position of roof advance failure and roadway deformation, so as to take preventive measures. Based on two generalized displacement beams, the accumulation law of the bending moment and energy density of the top coal wall under different loads, different thicknesses, and different cantilever lengths is investigated. The following conclusions are drawn: (1) Under different load conditions, the peak of the bending moment and energy density both appear at 10 m in front of the coal wall and rapidly decrease to 0 after reaching the peak and no longer change. The peak value of the bending moment increases linearly with the increase of the load, and the relation is M = −143.32q − 286.63. The peak value of bending moment changes exponentially with the increase of load, and the relation is Ue = 200.46e0.42q. (2) Under different thicknesses, the bending moment of the thickness to the rock layer has an irregular distribution at the peak value. When the thickness is 12.5 and 15 m, the change tends to be consistent, and when the thickness is 7.5 and 10 m, the bending moment of the roof is small when the thickness is 17.5 m. When the thickness is less than 17.5 m, the smaller the thickness is, the larger the peak value is, and the more advanced the peak value is. The smaller the thickness of the roof, the smaller the range of energy density accumulation. (3) Under different cantilever lengths, with the increase of cantilever length, the peak bending moment presents a linear increase, and the relationship is Me = −158.22 L + 137.4, and the range of bending moment accumulation increases with the increase of the roof cantilever length. With the increase of the cantilever length, the peak energy density of the roof increases exponentially, and the relationship is Ue = 3.5536e1.1067L, and the lead energy accumulation distance of the roof increases. (4) When the thickness of the roof is 10 m, the stress peak occurs more frequently within 5–15 m in front of the working face, which well confirms the correctness of the theoretical analysis.

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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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