Predicting the height of the water-conducting fractured zone using multiple regression analysis and GIS

被引:30
|
作者
Liu, Yong [1 ]
Yuan, Shichong [1 ,2 ]
Yang, Binbin [3 ,4 ]
Liu, Jiawei [1 ]
Ye, Zhaoyong [1 ,5 ]
机构
[1] China Univ Min & Technol, Sch Resources & Geosci, 1 Univ Rd, Xuzhou 221116, Jiangsu, Peoples R China
[2] North China Engn Invest Inst Co Ltd, 39 Huitong Rd, Shijiazhuang 050021, Hebei, Peoples R China
[3] Xuchang Univ, Sch Civil Engn, 88 Bayi Rd, Xuchang 461000, Henan, Peoples R China
[4] China Univ Min & Technol, Inst Mine Water Hazards Prevent & Controlling Tec, 1 Univ Rd, Xuzhou 221116, Jiangsu, Peoples R China
[5] Shanxi Xishan Jinxing Energy Corp Ltd, Xiegou Coal Mine, Lvliang 033600, Shanxi, Peoples R China
基金
国家重点研发计划;
关键词
Information entropy theory; Water-conducting fractured zone; Water and sand inrushes; Nonlinear multiple regression; Fully mechanized cave mining; COAL SEAMS; INRUSH; MINE;
D O I
10.1007/s12665-019-8429-3
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The water-conducting fractured zone induced by mining under aquifers is channels for water and sand inrushes. A method based on multiple regression analysis and a geographic information system (GIS) is proposed to predict the height of the water-conducting fractured zone in this paper. Five main indicators are found to control the height of the water-conducting fractured zone during fully mechanized caving mining under aquifers in which the thickness of the coal seam is more than 3 m: thickness of the coal seam, proportion of hard rock, length of the panel, mined depth and dip angle. The height of water-conducting fractured zone and the predictive variables from eighteen coal mines in China are investigated. Based on information entropy theory, a nonlinear multiple regression model and the weight of the indicators are considered, and the nonlinear multiple regression model is used in the GIS. Then, the approach is validated with a case study of the Xiegou Coalmine in the Shanxi province of China, in which the thickness of the coal seam which is under aquifers is more than 3 m. Error analysis of the approach is calculated with different hydrogeology classification. The results indicate that this model is a useful tool for predicting and analyzing the height of the water-conducting fractured zone, since the height of the water-conducting fractured zone can be quantitatively calculated and visualized.
引用
收藏
页数:15
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