大采高浅埋深开采地表裂缝成因分析研究
Analysis on surface cracking causes by high cutting and shallow depth coal mining
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摘要: 为了掌握大采高浅埋深开采地表裂缝发育规律,以超化煤矿22001工作面为研究对象,通过现场监测和理论分析,获取地表裂缝分布特征及变形参数,分析了地表非连续变形的形成原因。结果表明:动态裂缝超前距为38.5 m,发育周期19 d;裂缝最终呈现密度大、宽度小、无台阶型发育、压缩变形区域小、裂缝角偏小的特征。上覆岩层中关键层的破断是地表裂缝产生的根本原因,因覆岩岩性较软,松散层较厚,应力在传递过程中受到削弱,进而降低了台阶裂缝发育的可能性;黄土层抗拉能力弱,故地表形成了密集分布、无台阶发育的裂缝特征。Abstract: in order to maser the surace cracking develogment law of the high cutting and shallo w depth mining,.based on No.22001 cal mining face in Chaohua/Mine as the study object theste monitring and theoetical analysis were applied to obtain the surface cracking distrbution features and the deformaton parameters and to analyze the formation causes of the surace discontinuous deformaton. The resuits showed that the pilot distance of the dynamic cracking was 38.5 m and the development period was 19 days.The cracks fnally would have the features with high density.narrow width,no bench type development.small compresson deformation region and small cracking angle, The breaking of the key layer in he overburden strata was the basic causeof the suface ground cracking ocured. Due to the litholegyof the overburden strata was soft and thelose layer was thick,.the stress was relaxed during the transtion perod and thus the posstilty fthe bench cracking development was decreased.The tensie perormanceof the loess ayer was weak and the surface ground would have the cracking features withdense distributin and no bench development.