首页|基于FLAC3D数值模拟的砂岩顶板导水裂隙带高度及突水性研究

基于FLAC3D数值模拟的砂岩顶板导水裂隙带高度及突水性研究

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随着开采深度的不断增加,新集二矿1煤组开采活动引起上覆厚层坚硬砂岩岩层的断裂变形现象可能威胁矿井的安全生产.为研究新集二矿煤层深部开采条件下的"上三带"发育规律以及突水危险性,以新集二矿2401采区为研究对象,对新集二矿构造地质条件、水文地质条件进行了详细剖析,确定了1煤组煤层顶板含水层的充水条件;利用经验公式和数值模拟手段预测了2401采区1上煤层回采过程中导水裂隙带发育高度;在此基础上分析了回采后煤层顶板突水危险性,结果表明新集二矿上覆推覆体含水层对2401采区的开采基本不产生影响,影响采区开采的主要充水水源为1煤组顶板砂岩水及1煤组底板太原组灰岩裂隙水,对采后涌水量进行了准确预测;含水层富水性受断层及裂隙发育影响,需利用瞬变电磁物探手段对顶板砂岩富水性进行探查,圈定顶板砂岩富水区并对底板灰岩进行超前探测,查明底板灰岩构造及水文地质特征.通过研究认为数值模拟方法对研究导水裂隙带发育高度和矿井突水预测有一定理论参考价值,也可对煤矿安全生产提供较高的参考价值.
Research on the Height and Water in Rush Behavior of Water Conducted Zones in Sandstone Roof Based on FLAC3D Numerical Simulation
With the continuous increase of mining depth,the mining activities of the 1 coal group in Xinji No.2 mine may cause fracture deformation of the overlying thick and hard sandstone layer,which may threaten the safety production of the mine. In order to study the development law of the "upper three zones" and the risk of water inrush under the deep mining conditions of the coal seam in Xinji No. 2 mine,taking 2401 mining area of Xinji No. 2 mine as the research object,a detailed analysis was conducted on the structural geological and hydrogeological conditions of Xinji No.2 mine,and the water filling conditions of the roof aquifer of No.1 group of coal seams were determined;Using empirical formulas and numerical simulation methods,the development height of the water conducted zones during the backfilling process of No. 1U coal seam in 2401 mining area was predicted,and the post mining water inflow was accurately predicted;On this basis,the risk of water inrush from the roof of the coal seam after mining was analyzed. The results showed that the aquifer of the overlying strata of Xinji No.2 mine had little impact on the mining of the 2401 mining area. The main water sources affecting the mining area were the sandstone water in the roof of No.1 group of coal seams and the fissure water in the Taiyuan Formation limestone in the floor of No.1 group of coal seams. The water rich property was affected by the development of faults and fissures,and transient electromagnetic geophysical exploration methods were needed to explore the water rich property of the roof sandstone,delineate the water rich area of the roof sandstone,and conduct advanced detection of the floor limestone to identify the structure and hydrogeological characteristics of the floor limestone. Through research,it is believed that numerical simulation methods can provide a theoretical basis for development height of water conducted zones and predicting mine water inrush and also offer high reference value for coal mine safety production.

water conducted zonesnumerical simulationroof water damageFLAC3DXinji No.2 mine

汪有清、吴明、王猛、刘卞禹、王阳

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中煤新集能源股份有限公司新集二矿,安徽淮南 232000

中国矿业大学煤层气资源与成藏过程教育部重点实验室,江苏徐州 221008

中国矿业大学资源与地球科学学院,江苏徐州 221116

导水裂隙带 数值模拟 顶板水害 FLAC3D 新集二矿

2024

中国煤炭地质
中国煤炭地质总局

中国煤炭地质

CSTPCD
影响因子:0.652
ISSN:1674-1803
年,卷(期):2024.36(12)