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关闭煤矿倾斜煤层裂隙场模拟与遗留煤层气资源评价

Simulation of fracture field in inclined coal seams of closed coal mines and coalbed methane resource assessment

  • 摘要: 随“双碳”目标的提出,重庆市煤炭行业整体退出,关闭煤矿中赋存大量的煤层气资源,其资源和安全属性逐渐受到关注。为摸清松藻煤矿遗留煤层气的资源潜力,利用UDEC软件模拟了倾斜煤层群采空区覆岩裂隙场的空间分布特征,在此基础上构建了倾斜煤层采空区体积计算方法和关闭煤矿遗留煤层气资源的评价方法。倾斜煤层群重复采动覆岩裂隙呈非对称非等腰梯形,采空区中部被压实裂隙闭合,采动裂隙主要分布在工作面两端,且工作面顶端采动裂隙的规模、开度及连通性远高于工作面底端,采空区四周形成了“O”形圈,其顶部是遗留煤层气的富集区域;随煤厚的增加,K2B、K1和K3B煤层的采动裂隙率(2.28%、2.60%和3.09%)和分形维数(1.087、1.202和1.458)整体增大;基于构建的倾斜煤层采空区体积计算模型评估松藻煤矿采空区体积共4175.41万m3,主要分布在采空区中部的矩形体区域,工作面顶端终采线一侧的楔形五面体垮落带和裂隙带体积是底端楔形五面体的1.40倍和1.36倍;构建了松藻煤矿遗留煤层气资源“分类—分区(分水平)—分源叠加”的评价流程,估算了松藻煤矿遗留煤层气资源总量129906.21万m3,原位区、采空区和积水区占比为91.11%、7.84%和1.05%;K1、K2B和K3B煤层占比35.58%、3.21%和61.21%;原位区和采空区煤层气以吸附态为主(92.34%和78.73%),主要赋存在K3B煤层(60.97%和52.09%),采空区遗留煤层气主要分布在一水平(47.38%)和二水平(38.06%),游离煤层气主要分布在采空区裂隙带中(82.55%)。

     

    Abstract: With the introduction of the “dual carbon” goals, the coal industry in Chongqing has largely exited, and many coal mines have closed, leaving behind significant amounts of coalbed methane (CBM) resources. These resources and their safety properties are gradually gaining attention. To assess the resource potential of the leftover coalbed methane at Songzao Coal Mine, UDEC software was used to simulate the spatial distribution characteristics of the overburden fracture field in the inclined coal seam mining area. Based on this, a method for calculating the volume of the inclined coal seam gob area and an evaluation method for the leftover coalbed methane resources in closed mines were developed. The fractures in the overburden of the inclined coal seam group due to repeated mining are asymmetric and non-isosceles trapezoids. The fractures in the middle of the gob area are compressed and closed, while the mining fractures mainly occur at both ends of the working face. Moreover, the scale, aperture, and connectivity of the mining fractures at the top of the working face are significantly higher than those at the bottom. An “O”-shaped ring forms around the gob area, with the top being the enrichment region for the leftover coalbed methane. As the coal thickness increases, the mining fracture rate (2.28%, 2.60%, and 3.09%) and fractal dimension (1.087, 1.202, and 1.458) of K2B, K1, and K3B coal seams increase overall. Based on the constructed volume calculation model for the inclined coal seam gob area, the gob volume of Songzao Coal Mine is estimated to be 41.7541 million m3, mainly distributed in the rectangular body area of the gob. The volume of the wedge-shaped pentagonal collapse zone and fracture zone on the side of the final mining line at the top of the working face is 1.40 times and 1.36 times that of the wedge-shaped pentagonal area at the bottom. The evaluation process for the leftover coalbed methane resources at Songzao Coal Mine is constructed in a “classification-zone (horizon)-source overlay” manner. The total amount of leftover coalbed methane is estimated to be 1.299 billion m3, with in-situ, gob, and water accumulation areas accounting for 91.11%, 7.84%, and 1.05%, respectively. The K1, K2B, and K3B coal seams account for 35.58%, 3.21%, and 61.21%, respectively. The coalbed methane in the in-situ and gob areas is mainly in adsorbed form (92.34% and 78.73%), primarily hosted in the K3B coal seam (60.97% and 52.09%). The leftover coalbed methane in the gob area is mainly distributed in the first horizon (47.38%) and second horizon (38.06%), with free coalbed methane predominantly located in the fracture zones of the gob area (82.55%).

     

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