淮北临涣矿区地层非采动沉降分析
General Trend of Non-Mining -Induced Subsidence and Deformation in Lin-Huan Coal Production Aress
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摘要: 本文是基于设置在临涣和海孜两矿工业广场煤柱内新生界地层沉降变形孔的监测、地表水准测量、有关水文孔观测资料以及土工试验结果,对临涣矿区巨厚松散地层内部非采动沉降变形的特征与机理进行了较全面的分析。并简要分析该矿区地层非采动沉降对井筒稳定性的影响。以及与一般情况城市地表沉降的差异。Abstract: Based on the observed data of the subsidence and deformation of Cainozoic Era layers inLinhuan Coalfield,levelling of the surface,as well as,some hydro-geological data and the result of soiltests,this paper discusses the general rules and mechanism of non-mining-induced subsidence and de-formation of the layers in Linhuan Coalfield,and presents the difference between the non-mining-induced subsidence and deformation of the layers in the coalfield and the surface subsidence in cities.