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首页> 外文期刊>Arabian journal of geosciences >Analysis of the distribution characteristics and laws of in situ stress in China's coal mines
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Analysis of the distribution characteristics and laws of in situ stress in China's coal mines

机译:中国煤矿原位应力分布特征及法律分析

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Based on the measured in situ stress data in China's coal mines, the relationship among the type of stress field, magnitude of stress, stress value, and the depth of burial was analyzed. The trends in the changes in side pressure coefficient and side pressure ratio were regressed and fitted with the increase in depth. This was compared to the Hoek-Brown curve, and the distribution characteristics and variation laws of underground stress field in China's coal mines were determined. (1) Generally, in situ stress increases with burial depth, but the geological structure and lithology render horizontal stress considerable. (2) In 87.72% of stress fields, which are considered typical tectonic stress fields, the horizontal stress comes into prominence. (3) About 64% working environment is the middle- and high-stress zones, and low- and ultrahigh-stress zones account for about 18% each. (4) The ratio of horizontal principal stress was distributed within a range of 1.0 similar to 2.5, and it was affected very little by burial depth. However, the difference increased continuously with burial depth, causing an obviously growing shear failure of coal and rock. (5) The side pressure coefficient is mostly distributed in 0.9 similar to 2.0, and it decreases with burial depth and is gradually close to 1.32. (6) Most side pressure ratio is in 0.5 similar to 1.6. When the burial depth is less than 700 similar to 750 m, the horizontal principal stress is lower than one in the world. Conversely, the magnitude of horizontal principal stress was more pronounced in deeper areas, but it always plays a leading role in the in situ stress field. (7) The seismic belt has a great influence on coalfield stress fields. Without affecting the stress field, the direction of maximum principal stress is approximately parallel or perpendicular to the trajectories of principal stress in China Continental Plate. However, under the composite effect of geological structure, the direction changed visibly. There is no apparent relationship between the two and no law to follow. The statistics of in situ stress are important reference values for understanding stress distribution in China's coal mines, and it also has a practical guiding significance for safely and efficiently mining underground.
机译:基于中国煤矿原位应力数据的测量,分析了应力场类型,压力,应力值的程度和埋藏深度之间的关系。侧压系数和侧压比变化的趋势是回归的,并装配深度增加。将这与Hoek-Brown曲线进行比较,并确定了中国煤矿地下应力场的分布特性和变化规律。 (1)通常,原位应力随埋藏深度而增加,但地质结构和岩性呈现横向应力相当大。 (2)在87.72%的压力场中,被认为是典型的构造应力场,水平应力突出。 (3)工作环境约为64%,是中高应力区域,低音和超高应力区域占约18%。 (4)水平主应力的比例在1.0的范围内分布于2.5的范围内,并且由于埋藏深度影响很少。然而,差异随着埋藏深度连续增加,导致煤炭和岩石的显然剪切失效。 (5)侧压系数大多数分布在0.9中,类似于2.0,它随着埋藏深度减少,逐渐接近1.32。 (6)大多数副压力比为0.5,类似于1.6。当埋藏深度小于700时,类似于750米,水平主要应力低于世界上的一个。相反,水平主要压力的大小在更深的区域中更加明显,但它始终在原位应力领域发挥着主导作用。 (7)地震皮带对煤田应力领域有很大影响。在不影响应力场的情况下,最大主应力的方向大致平行或垂直于中国大陆板块主压力的轨迹。然而,在地质结构的复合效果下,方向明显变化。两者之间没有明显的关系,也没有任何法律。原位应力的统计数据是了解中国煤矿中应力分布的重要参考价值,也具有安全有效地挖掘地下的实践指导意义。

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