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张国庆, 黄霆. 综放工作面回采初期采空区涌水预测[J]. 煤炭科学技术, 2013, (12).
引用本文: 张国庆, 黄霆. 综放工作面回采初期采空区涌水预测[J]. 煤炭科学技术, 2013, (12).
ZHANG Guo-qing HUANG Ting, . Prediction on Water Flow in Goaf at Initial Mining Period of Fully-Mechanized Top Coal Caving Face[J]. COAL SCIENCE AND TECHNOLOGY, 2013, (12).
Citation: ZHANG Guo-qing HUANG Ting, . Prediction on Water Flow in Goaf at Initial Mining Period of Fully-Mechanized Top Coal Caving Face[J]. COAL SCIENCE AND TECHNOLOGY, 2013, (12).

综放工作面回采初期采空区涌水预测

Prediction on Water Flow in Goaf at Initial Mining Period of Fully-Mechanized Top Coal Caving Face

  • 摘要: 为了有效预测综放工作面初采期采空区的涌水情况,采用经验公式计算出综放工作面垮落带高度和导水裂缝带高度,根据钻孔资料确定常村煤矿9号含水层位于导水裂缝带内。在此基础上,利用FLAC3D模拟综放工作面回采过程,得出上覆岩层的垂直位移导致的垮落带和导水裂缝带分布规律,导水裂缝带与9号含水层导通是工作面采空区涌水水源。结果表明:在未达到充分采动时,导水裂缝带为"拱形",数值模拟了工作面回采至108—112 m与现场回采到106 m工作面采空区涌水较为吻合,验证了数值模拟可准确预测综放工作面现场采空区涌水。

     

    Abstract: In order to effectively predict water flow in goaf at the initial mining period of fully-mechanized top coal caving face,an empirical formula was applied to C alculate the height of the roof falling zone and the height of the water flow zone in fully-mechanized top caving face. According to the borehole information,No. 9 aquifer was located in a water flow zone as determined. Based on the circumstances,a FLAC3Dsoftware was applied to simulate the mining process of fully-mechanized coal C aving face, the distribution law of the roof falling zone and water flow fracture zone occurred by the vertical displacement of the overburden strata was obtained and the i nterconnection between the water flow fracture zone and No. 9 aquifer would be the water sources of the water flow in the goaf of the coal mining face. The results sho wed that before a full mining reached,the water flow fracture zone was arch shape and the water flow in goaf,numerical simulation on the coal mining at 108- -112 m of t he coal mining face and the site mining at 106 m of the coal mining face was fitted. Thus the results verified the numerical simulation could accurately predict the water flow in goaf.

     

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