Evaluation of coal mines’ rock mass gas permeability in the equivalent stress zone

Q3 Engineering
O. M Shahsenko, V. A Cherednyk, N. V Khoziaikina, S. M Hapieiev
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Abstract

Purpose. Based on a comparative analysis of the internal mechanism of shape change of rock samples, which were loaded in specified deformations mode, and geomechanical and gas-dynamic processes in coal mass, to establish a causal link between these phenomena. To qualitatively characterise their gas permeability as a function of the rock’s volume expansion. To justify the possibility of using a full “stress-strain” diagram as a technogenic methane deposit formation model and its spatial localisation. Methodology. Theoretical research is based on using the solid mechanic constitutive principles and results of studying the rock samples failure in the mode of specified strains. Findings. The ability to use a full “stress-strain” diagram for detecting and localising methane reservoirs during the coal seams excavation was proved during the research. It was found that the compaction threshold coincides with the bearing pressure maximum in front of the longwall face. This area corresponds to the rock mass with minimal porosity and minimal filtration, which allows considering it as an envelope of an artificial gas deposit. Regularities that connect the three-dimensional equivalent stress state with the final gas permeability of the gas-saturated coal mass were obtained. These data allow creating a predictive numerical geomechanical model of methane migration paths. Originality. The ability to use a full “stress-strain” diagram in the controlled strain mode for numerical modelling of gas permeability of a methane-saturated coal mass during the mining of coal seams and the determination of technogenic gas deposit boundaries are justified. Dependences of the current and final gas permeability on the rock’s mechanical characteristics in a post-peak strain state are obtained. Practical value. Functional dependencies based on geomechanical models are obtained that allow the identification and localisation of technogenic methane reservoirs in mines during coal seam excavation, with subsequent utilisation of the extracted gas. Furthermore, methane removal enhances mining safety by reducing the risk of gas dynamic phenomena while decreasing gas emissions into the atmosphere contributes to reducing the greenhouse effect.
煤矿岩体等效应力区透气性评价
目的。通过对比分析在特定变形模式下加载的岩样形状变化的内在机理与煤体的地质力学和气体动力过程,建立了这些现象之间的因果关系。以岩石体积膨胀的函数定性表征它们的透气性。为了证明使用完整的“应力-应变”图作为技术甲烷矿床形成模型及其空间定位的可能性。方法。理论研究是基于固体力学本构原理和岩样在特定应变模式下的破坏研究成果。发现。在研究过程中,证明了在煤层开挖过程中使用完整的“应力-应变”图来探测和定位甲烷储层的能力。研究发现,压实阈值与长壁工作面前方的最大承载压力一致。该区域对应于孔隙率最小、过滤最小的岩体,因此可以将其视为人工气矿床的包络层。得到了三维等效应力状态与含气煤体最终渗透率之间的联系规律。这些数据可以建立一个预测甲烷运移路径的数值地质力学模型。创意。利用控制应变模式下的完整“应力-应变”图对煤层开采过程中含甲烷饱和煤体的渗透性进行数值模拟和确定技术成因气藏边界是合理的。得到了峰后应变状态下岩石力学特性与当前和最终渗透率的关系。实用价值。基于地质力学模型的功能依赖关系可以在煤层开挖过程中识别和定位矿井中的技术甲烷储层,并随后利用所提取的气体。此外,甲烷的清除通过降低气体动力现象的风险来提高开采安全性,同时减少气体排放到大气中有助于减少温室效应。
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来源期刊
CiteScore
1.70
自引率
0.00%
发文量
148
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