煤炭科学技术2024,Vol.52Issue(3) :1-12.DOI:10.13199/j.cnki.cst.2022-1926

厚煤层大采高综放工作面覆岩断裂演化规律研究

Study on evolution law of overburden fracture in fully-mechanized top-coal caving face with large mining height in thick coal seam

刘洪涛 罗紫龙 韩子俊 韩洲 陈小港 彭佳琛
煤炭科学技术2024,Vol.52Issue(3) :1-12.DOI:10.13199/j.cnki.cst.2022-1926

厚煤层大采高综放工作面覆岩断裂演化规律研究

Study on evolution law of overburden fracture in fully-mechanized top-coal caving face with large mining height in thick coal seam

刘洪涛 1罗紫龙 1韩子俊 1韩洲 1陈小港 1彭佳琛1
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作者信息

  • 1. 中国矿业大学(北京)能源与矿业学院,北京 100083
  • 折叠

摘要

大采高综放开采易形成强烈的矿压显现,上覆岩层的断裂演化规律对工作面安全生产至关重要.以羊场湾煤矿160206工作面为工程背景,运用相似模拟试验、数值模拟和理论分析的综合研究方法,对大采高综放工作面覆岩的断裂过程与覆岩运移规律进行系统研究.研究表明:导水裂隙带内岩层随工作面推进表现为"台阶下沉",同层岩层下沉趋势沿走向表现为"急剧下降—稳定(最大值)—快速上升—稳定(最小值)".工作面覆岩运动场由两区分布(加速下沉区、缓慢下沉区)演化为三区分布(加速下沉区、缓慢下沉区、稳定区).对离层演化与地表下沉规律进行了定量描述,运用理论计算表达式深入地剖析了地表的动态下沉机理及其相关因素.结合相似模拟与数值模拟的试验结果,提出了覆岩断裂演化的形态变化特征:覆岩断裂形态由"单等腰梯形"演化为"双等腰梯形",表土层影响区由"矩形"演化为"倒梯形".分析了覆岩中垮落区、离层区、压实区、裂隙富集区的动态演化过程:垮落区逐渐增大至一定程度,高度小幅度降低并趋于稳定,离层区由下至上逐渐发育并随工作面向前移动,离层区逐渐闭合形成压实区,且压实区逐渐增大并最终保持稳定,裂隙富集区位于采空区前后端部并随工作面向前移动.

Abstract

Fully mechanized top-coal caving mining with large mining height is easy to form strong strata behavior,and the fracture evolu-tion law of overlying strata is very important for safe production of working face.Taking the 160206 working face of Yangchangwan Coal Mine as the engineering background,the comprehensive research methods of similar simulation test,numerical simulation and theoretical analysis are used to systematically study the overburden fracture process and overburden migration law of the fully mechanized top coal caving working face with large mining height.The research shows that the strata in the water flowing fracture zone show"bench sinking"with the advance of the working face,and the subsidence trend of the same strata along the strike shows"sharp decline-stability(maxim-um)-rapid rise-stability(minimum)".The overburden movement field of the working face has evolved from two areas(accelerated sub-sidence area and slow subsidence area)to three areas(accelerated subsidence area,slow subsidence area and stable area).The evolution of abscission layer and the law of surface subsidence are quantitatively described,and the dynamic subsidence mechanism of the surface and its related factors are deeply analyzed by using theoretical calculation expressions.Combined with the experimental results of similar sim-ulation and numerical simulation,the morphological change characteristics of overburden fracture evolution are proposed:the overburden fracture morphology evolves from"single isosceles trapezoid"to"double isosceles trapezoid",and the influence area of topsoil layer evolves from"rectangle"to"inverted trapezoid".The dynamic evolution process of collapse area,separation area,compaction area and fracture enrichment area in overburden is analyzed:The caving zone gradually increases to a certain extent,the height decreases slightly and tends to be stable,the separation zone gradually develops from bottom to top and moves forward with the working face,the separation zone gradually closes to form a compaction zone,and the compaction zone gradually increases and finally remains stable,and the fracture enrichment zone is located at the front and back ends of goaf and moves forward with the working face.

关键词

大采高综放/相似模拟/覆岩运动场/覆岩运移/覆岩断裂形态

Key words

fully-mechanized top-coal caving with large mining height/similar simulation/overburden sports ground/overburden mi-gration/overburden fracture morphology

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基金项目

国家自然科学基金(U22A20165)

国家自然科学基金(52004289)

国家自然科学基金(2022XJNY01)

出版年

2024
煤炭科学技术
煤炭科学研究总院

煤炭科学技术

CSTPCDCSCD北大核心
影响因子:2.095
ISSN:0253-2336
参考文献量20
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