多煤层叠加开采覆岩离层演化规律与开度预测研究
Study on the evolution law of bed separation and aperture variation in overlying strata under multi-coal seam superimposed mining
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                            摘要: 随着深部煤炭资源开采规模的扩大,多煤层叠加开采导致的顶板离层水害已成为主要灾害,其演化规律与离层开度预测是研究热点。以红阳煤田西一采区为研究对象,利用相似材料、3DEC数值模拟等手段,系统研究了多煤层叠加开采下覆岩离层的时空演化特征及其开度变化规律。结果表明,覆岩离层动态演化受关键层破断、采动应力场耦合及煤层开采顺序的显著影响,7煤层与12煤层间高位离层受多场耦合作用最大开度达3.5 m,而3煤层顶板近场离层因关键层协同作用仅发育至0.6 m。基于关键层理论与岩层碎胀效应,构建离层开度预测模型,通过301工作面实测数据验证,预测值与实测值误差小于15%。Abstract: As deep coal mining expands,water damage resulting from roof separation during the overlapping extraction of multiple coal seams has become a significant hazard and a key research focus. This study examines the West 1st Mining Area of the Hongyang Coalfield to systematically analyze the spatial and temporal evolution and aperture variation of overlying strata separation under multi-seam mining conditions,by using similar materials, 3DEC numerical simulation and other means. The results indicate that the development of bed separation is strongly influenced by the rupture of key strata,interactions within the mining-induced stress field,and the sequence of seam extraction. High-level separation between coal seams 7to12 can reach a maximum aperture of 3. 5 meters under combined field effects,while immediate roof separation above coal seam 3 is limited to 0. 6 meters due to key stratum interaction. Based on these findings,a predictive model for bed separation aperture was developed, incorporating key stratum theory and the effects of rock fragmentation and bulking. Field measurements from working face 301 show that model predictions deviate by less than 15%.
 
             
						  
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