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胜利露天煤矿边坡稳定性预测研究
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摘要
胜利露天煤矿位于内蒙古锡林浩特市北郊6km。地理座标:东经115°30'~116°26',北纬43°57'~44°14'。1979年12月投入生产, 2004年4月,完成该矿的初步设计。5煤层已形成50~60m高的帮坡,6煤层出露后边坡高度将达到150m,排土场最终排弃高度为60m。自2005年起,在非工作帮的中区、北区及北端帮已多次发生滑坡、坍塌。根据边坡变形性质、发育特征、运动形式,将滑坡分为松散层滑坡和沿基岩接触面滑坡两种类型。
     影响边坡稳定性的自然因素有:地质构造、软弱夹层、水等;主要诱发因素是降水及爆破震动。软弱层岩性以泥岩或炭质泥岩为主,为边坡失稳的主要滑动面。
     根据滑坡类型不同,以东部非工作帮中部(DH2)为研究区,以网格状形式布置监测点14个,并将坡顶后缘拉裂缝附近和前缘弯曲隆起部位的监测点作为监测重点。
     根据边坡变形特点,滑坡位移─时间曲线可认为是二次曲线和指数曲线组合,构造新灰色预测模型,对边坡变形进行预测。预测过程中为提高预测精度,该模型在计算中改进了背景值的计算方法并采用了数据新陈代谢法。
     将新灰色预测模型与尖点突变模型相结合,构造了灰色─突变模型,用失稳判别式对边坡的稳定性进行预测。
Sheng Li Open-pit Coal Mine locates 6km away from North suburbs of Xi Lin Hao Te city of Inner Mongolia. Geographical coordinate is E115°30'~116°26', N 43°57'~44°14'. Sheng Li Open-pit Coal Mine worked from December ,1979.The initially plan of Sheng Li Open-pit Coal Mine was done in April,2004.The hight of 5th coals has reached 50~60m and the hight of 6th coals has reached 150m. Slide and collapse has occurred many times in the middle and north of easten non-workable side and north side from 2005. Based on the comprehensive analysis on the deformation, fissures development, movement style and the induced factors of the landslide, two types of landslide were generalized including unconsolidated formation sliding and sliding along the contact plane of bedrock.
     According to diffrent slope types, the middle easten non-workable side is considered as researching zone.Placing 14 supervision dots in net, mainly use the data of the front side to forecast.
     Considering the character of open-pit mine side slope, slope distortion forecasting method has been constructed. To get higher degree of accuracy, a modified calculation method of background value and a data metabolism method were used.
     Combined with the modified grey model and mutation forcasting model, the suitable method of landslide catastrophe forecasting has been given. A discriminant formula and related formation has been used to forecast stability of slope.
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