摘要
为了研究巨厚砾岩下特厚煤层开采地表形变规律,以概率积分模型为原型,建立了基于叠加原理的三维空间分布式优化求参模型。以常村煤矿2113工作面地表移动观测站实测资料为依据,采用下沉和水平移动求参模型求取了地表形变预计参数。结合工程地质资料,从岩层运移机理对参数的分布规律进行了分析。结果表明,巨厚砾岩关键层的初次破断距为367 m,悬臂梁周期破断距为179 m,关键层破断后地表非连续变形显现强烈,巨厚砾岩层的悬臂支承作用是造成地表沉陷盆地出现偏态下沉的根本原因,与实测结果相吻合。
In order to research ground surface deformation law of extra-thick coal mining under the condition of massive conglomerate stratum, according to probability integral model, 3D distributed mathematical functions to determine optimum parameters have been made based on superposition principle. In response to ground surface movement surveying datum of 2113 panel of Changcun colliery, surface deformation prediction parameters have been obtained by using subsidence and horizontal movement functions. Associated with engineering geological data, parameters distribution law has been analyzed from overburden terrane movement mechanism. The results show that first weighing interval of thick conglomerate is 367 m, while period weighing interval of cantilever is 179 m. Ground surface discrete deformation present intensively after key-strata collapses. And the cantilever bear action of massive conglomerate stratum mainly causes dissymmetry subsidence basin. The results are in accord-ance with field surveying datum.
出处
《采矿与安全工程学报》
EI
CSCD
北大核心
2015年第4期628-633,共6页
Journal of Mining & Safety Engineering
基金
国家自然科学基金项目(41101520
41071328
51074064)
河南理工大学博士基金项目(B2011-025)
关键词
巨厚砾岩
开采沉陷
优化求参
运移机理
关键层
massive conglomerate
mining subsidence
optimum obtaining parameter
movement mechanism
key stratum