深厚煤层长壁开采空侧巷道底鼓特性研究

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2026-04-08 DOI:10.1155/gfl/5536664
Yinghao Hao, Jinhai Liu, Xiaodong Miu, Guoli Ding, Pei Qi, Hao Wu, Linsheng Gao
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引用次数: 0

摘要

随着工作面开采深度的增加,底鼓控制在工程实践中越来越突出。以葫芦苏煤矿21404工作面采空区为工程背景,对煤层深、厚、密工作面采空区底鼓进行了研究。工作面开采前,采空区侧巷道出现轻微底鼓,底板硬化体出现裂缝。方正前底鼓量明显增大。巷道中段隆起,最高底隆起约500mm。平方化后回风入口底鼓明显增大。它从两边挤到了马路中间。巷道中部存在底鼓现象。巷道在距工作面小于90 m时变形加速,巷道底鼓量最大为500 mm,巷道两侧最大收敛量为300 mm。底鼓量大于两侧底鼓量。采空区巷道底部存在一个斜三角形位移区。固体边的煤移到了巷道上。采空区边巷底鼓严重,边巷煤柱变形广泛。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

A Study on the Floor Heave Characteristics of a Gob-Side Entry in Deep-Thick Coal Seam During Longwall Mining

A Study on the Floor Heave Characteristics of a Gob-Side Entry in Deep-Thick Coal Seam During Longwall Mining

Floor heave control becomes more and more prominent in engineering practice with the increased mining depth of the working face. The gob-side entry of the 21404 working face in Hulusu Coal Mine was taken to be the engineering background to study the gob-side entry’s floor heave in the working face with a deep, thick, and dense layer of coal. There was slight floor heave in the gob-side entry before mining the working face, and cracks appeared in the hardened bodies of the floor. The floor heave amount increased significantly before squaring. The roadway’s middle floor was heaved, and the highest floor heave was about 500 mm. The floor heave of the return-air entry increased significantly after squaring. It was squeezed from the two sides to the roadway’s middle part. Additionally, there was floor heave in the roadway’s middle part. The deformation of the roadway was accelerated when it was less than 90 m away from the working face, with a maximum floor-heave amount of 500 mm and a maximum two-side convergence of 300 mm. The amount of floor heave was greater than that of the two sides. There was an oblique triangular displacement area at the roadway side’s bottom in the gob-side entry. Coal on the solid sides moved to the roadway. The gob-side entry’s floor heave was serious, with coal pillars’ extensive deformation on the sides.

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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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