工作面采场底板损伤深度试验与数值模拟

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS Geofluids Pub Date : 2023-09-13 DOI:10.1155/2023/2184880
Xipeng Cui, Hongqi Shao, Kailei Zhao
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引用次数: 0

摘要

本研究旨在探讨新枝煤矿东四矿区岩层破裂发育深度,分析采场底板发育规律。采用两种压水试验方法和数值模拟方法对新县煤矿东四采区工作面底板破坏特征进行了研究。结果表明:工作面底板破坏始于工作面前方一定范围;随着工作面推进,开采底板破坏深度不断增大。同时,由于掘进和回采的双重扰动,回采巷道的破坏范围略大于工作面底板的破坏范围。压水试验结果表明,破裂深度为8.98 ~ 9.03 m。底板破坏深度数值模拟结果显示其破坏深度约为8.7 m,与压水试验基本一致。为类似煤层开采底板破坏的超前预勘探提供参考。
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Damage Depth Test and Numerical Simulation of Stope Floor in Mining Face
The purpose of this study is to explore the development depth of rock layer rupture and analyze the developmental regularity of mining floor in Dongsi mining area of Xinzhi Coal Mine. Two kinds of pressure water testing methods and numerical simulation are used to study the failure characteristics of the bottom plate of the working face in Dongsi mining area of Xinxian Coal Mine. The results show that the failure of working face bottom plate starts from a certain range in front of the working face. With the advance of working face, the failure depth of mining bottom plate increases continuously. At the same time, the failure range of mining roadway is slightly larger than the failure range of working face bottom plate due to the double disturbance of tunneling and mining. The pressure water test shows that the rupture depth occurs at 8.98-9.03 m. The numerical simulation results of floor failure depth show that its depth is about 8.7 m, which is basically consistent with the pressure water test. It provides a reference for the advanced preexploration of mining bottom plate failure in similar coal seam.
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来源期刊
Geofluids
Geofluids 地学-地球化学与地球物理
CiteScore
2.80
自引率
17.60%
发文量
835
期刊介绍: Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines. Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.
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