Analysis of the Impact of Geological Factors on the Distribution of Abutment Pressure in Deep-Buried Longwall Faces

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2025-06-12 DOI:10.1155/gfl/2736614
Man Wang, Huidong Zhang, Songtao Ji, Wending Zhang, Zehua Niu, Rui Min, Huice Jiao, Yong Liu
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引用次数: 0

Abstract

To investigate the control factors of mine disasters induced by high ground pressure, this paper takes a longwall face of Pingdingshan No. 10 coal mine as the engineering background. By employing the analytical model and numerical simulation methods, this study quantified the movement characteristics of the hard roof strata and the evolution of mining-induced stress. The control mechanisms of various geological factors on the distribution of the abutment pressure were evaluated. The results indicate that (1) the PFC-FLAC coupled numerical model can effectively simulate and predict the characteristics of roof collapse and the distribution characteristics of abutment pressure. (2) The first weighting distance, the peak of the abutment pressure, and the influence range of the abutment pressure can be measured by the proposed model, whereas the periodic weighting barely can be observed. (3) The tensile strength and thickness of the hard roof directly control the peak value of the abutment pressure and the first weighting distance. As the strength and thickness of the hard roof increase, both the peak value and influence distance of the abutment pressure significantly increase. When the tensile strength of the hard roof reaches a high value, the development of fractures in the hard roof shows a clear periodicity pattern. The vertical stress significantly affects the movement and fracturing of the overburden, while the horizontal stress has a limited impact on the movement and fracturing of the overburden. The proposed methods provide technical guidance and theoretical support for controlling ground pressure in deep-buried longwall faces.

地质因素对深埋长壁工作面支承压力分布的影响分析
为探讨高地压矿井灾害的控制因素,本文以平顶山十矿某长壁工作面为工程背景。采用解析模型和数值模拟方法,定量分析了硬顶板岩层的移动特征和采动应力演化规律。评价了各种地质因素对桥台压力分布的控制机制。结果表明:(1)PFC-FLAC耦合数值模型能有效地模拟和预测顶板坍塌特征和桥台压力分布特征;(2)该模型可以测量第一次加权距离、台压力峰值和台压力影响范围,而不能观测到周期加权。(3)硬顶板的抗拉强度和厚度直接控制着支承压力峰值和首重距离。随着硬顶板强度和厚度的增加,支承压力峰值和影响距离均显著增大。当硬顶板抗拉强度达到较高值时,硬顶板裂缝发育呈现明显的周期性规律。竖向应力对覆岩的移动和破裂影响显著,而水平应力对覆岩的移动和破裂影响有限。该方法为深埋长壁工作面地压控制提供了技术指导和理论支持。
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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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