首页|基于关键层理论的导水裂隙带预测

基于关键层理论的导水裂隙带预测

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导水裂隙带高度是矿井水害防治的关键,为预测厚煤层开采条件下导水裂隙带高度,基于关键层理论计算了某工作面导水裂隙带的高度.结果表明,该工作面关键层主要由砂质泥岩和细粒砂岩构成,关键层的厚度为23.42~24.21 m,是所有岩层中厚度相对较大的岩层;黄土和红土等软岩层对导水裂隙带的发展起到了一定的抑制作用;基于关键层理论确定的最大导水裂隙带高度为136.9 m,与实测导水裂隙带高度十分接近,误差仅为6.08%.该成果可有助于准确判别矿井充水来源.
Prediction of water-conducting fracture zone based on key layer theory
The height of water-conducting fracture zone is a key to the prevention and control of mine water disaster.In order to calculate the height of water-conducting fracture zone under the conditions of thick coal seam mining,the height of water-conducting fracture zone in a working face of Northern Shaanxi coalfield is calculated based on the key layer theory.The re-sults show that the key layer of the working face is mainly sandy mudstone and fine sandstone.The thickness of the key layer is 23.42~24.21 m,which is relatively the thickest of all rock layers.The yellow and red soil-based soft rock layer plays a certain role in restraining the development of the water-conducting fracture zone.Based on the key layer theory,the maxi-mum height of the water-conducting fracture zone is determined as 136.9 m,which is very close to the measured height of the water-conducting fracture zone with an error of only 6.08%.This result can help to accurately identify the source of mine filling water.

Northern Shaanxi coalfieldkey layerwater-conducting fracture zone heightsoft rock

王力、来甲、齐晓华、薛伟、张利

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陕西煤业化工集团孙家岔龙华矿业有限公司,陕西榆林 719300

陕西省煤层气开发利用有限公司榆林分公司,陕西榆林 719300

陕北煤田 关键层 导水裂隙带高度 软岩

陕西省自然科学基础研究计划-陕煤联合基金重点项目陕西煤业化工集团重点科研项目

2019JLZ-032020SMHKJ-B-J-27

2024

陕西煤炭
陕西省煤炭工业协会 神华神东煤炭集团有限责任公司 陕西煤业化工集团有限责任公司

陕西煤炭

影响因子:0.204
ISSN:1671-749X
年,卷(期):2024.43(10)