Study on the Application of Finite Difference in Geological Mine Fault Groups: A Case Study

Author:

Yuan Jianbo12ORCID,Wang Chao34,Liu Zhigang124,Lyu Jingchao34,Lu Yajun34,You Wuchao5ORCID,Yan Jiazheng6

Affiliation:

1. State Key Laboratory of Strata Intelligent Control and Green Mining Co-Founded by Shandong Province and the Ministry of Science and Technology, Shandong University of Science and Technology, Qingdao 266590, China

2. Institute of Mining Engineering, Shandong University of Science and Technology, Tai’an 271019, China

3. Yan Kuang Energy Group Co., Ltd., Zoucheng 273500, China

4. Shandong Energy Group, Jinan 250013, China

5. Shandong Jingtai Engineering Technology Co., Ltd., Zibo 255425, China

6. Linyi City Development Group Co., Ltd., Linyi 276037, China

Abstract

Fault structures can cause a bad mining environment and increase the stress of surrounding coal pillar faults. The study investigates the stress evolution characteristics within fault structure groups and their surrounding coal pillars and explores the extent to which these fault structure groups influence the stress distribution in coal pillars. Based on three-dimensional modeling technology, a transparent geological model of the geological environment of fault structure groups was constructed and finite difference software was used to generate a numerical simulation model. Two survey lines and four survey points were arranged to analyze the stress distribution of a coal pillar fault. The results show that the fault structure groups have obvious stress barrier effects. There is a 35 m stress reduction zone in the hanging wall of the fault and a 30 m stress increase zone in the footwall of the fault. Both FL-1 and FL-3 faults have a stress barrier effect in the hanging wall. The obvious stress increases in the footwall of the fault are 37.7 MPa and 33.5 MPa, respectively. The stress of the FL-2 fault as a whole appears to be a more obvious superposition at the end of mining, and the peak stress reaches 41.5 MPa.

Publisher

MDPI AG

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