摘要
Based on a shallow-buried coal seam covered with thick loose layers in hilly loess areas of western China,we developed a mechanical model for a mining slope with slope stability analysis, and studied the mechanism of formation and development of a sliding ground fissure by the circular sliding slice method.Moreover, we established a prediction model of a sliding fissure based on a mechanical mechanism,and verified its reliability on face 52,304, an engineering example, situated at Daliuta coal mine of Shendong mining area in western China. The results show that the stress state of a mining slope is changed by its gravity and additional stress from the shallow-buried coal seam and gully terrain. The mining slope is found to be most unstable when the ratio of the down-sliding to anti-sliding force is the maximum, causing local fractures and sliding fissures. The predicted angles for the sliding fissure of face 52,304 on both sides of the slope are found to be 64.2° and 82.4°, which are in agreement with the experimental data.
Based on a shallow-buried coal seam covered with thick loose layers in hilly loess areas of western China, we developed a mechanical model for a mining slope with slope stability analysis, and studied the mech- anism of formation and development of a sliding ground fissure by the circular sliding slice method. Moreover, we established a prediction model of a sliding fissure based on a mechanical mechanism, and verified its reliability on face 52,304, an engineering example, situated at Daliuta coal mine of Shendong mining area in western China. The results show that the stress state of a mining slope is changed by its gravity and additional stress from the shallow-buried coal seam and gully terrain. The mining slope is found to be most unstable when the ratio of the down-sliding to anti-sliding force is the maximum, causing local fractures and sliding fissures. The predicted angles for the sliding fissure of face 52,304 on both sides of the slope are found to be 64.2° and 82.4°, which are in agreement with the experimental data.
基金
Projects funded by the National Key Basic Research Development Program(No.2013CB227904)
the National Natural Science Foundation of China(No.41272389)
China Postdoctoral Science Foundation(No.2014M561931)
the Natural Science Foundation of Hebei Province(No.D2014402007)
