煤矿开采中破碎煤块和岩块的压实和渗流特性:实验室试验综述

Cun Zhang , Yanhong Chen , Zhaopeng Ren , Fangtian Wang
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引用次数: 0

摘要

破碎煤岩(BCR)是煤巷(或煤壁)塌陷区的重要组成介质,也是断层破碎带和塌陷柱的主要充填材料。碎屑岩的压实渗流特性直接影响煤矿的安全高效开采。因此,大量实验室研究都集中在 BCR 的压实渗流特性上。本文首先概述了煤矿开采过程中 BCR 所涉及的工程问题,包括漏风、自燃、瓦斯排放和煤层中的地下水库。与断层和塌陷柱等构造相关的涌水以及与煤矸石充填和开采相关的地表沉降也涉及到 BCR 的压实渗流特性。基于碱性催化还原的现场问题,人们在实验室试验中进行了许多模拟现场环境的尝试。首先对 BCR 的实验设备(空腔尺寸和形状、声发射、CT 等)和实验设计进行了综述。实验室分析的主要对象可分为压实试验和渗流试验。在压实试验中,主要研究 BCR 的承载变形特征(应力-应变曲线)、孔隙演化特征和再破碎特征。渗流试验主要以气体或水为主要介质,研究不同压实应力条件下的渗透性演变特征。在实验室试验中,通常要考虑煤和岩体的类型、颗粒大小、颗粒形状、水压、温度和应力路径等因素。BCR 的横向压缩试验可分为三个阶段,包括自我调整阶段、破碎阶段、弹性阶段或稳定阶段。在每个阶段,应力、变形、孔隙度、能量、粒度和破碎率都有各自的特点。有关 BCR 透水性实验的渗流试验实际上属于变质渗流。而实验测试的重点仍然是应力对 BCR 孔隙结构在气体渗透性方面的影响。最后,讨论了未来与煤炭开采相关的 BCR 实验测试,包括扩大规模、长期加载和水浸泡、开采应力路径匹配等。
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Compaction and seepage characteristics of broken coal and rock masses in coal mining: A review in laboratory tests

Broken coal and rock (BCR) are an important component medium of the caving zone in the goaf (or gob), as well as the main filling material of fault fracture zone and collapse column. The compaction seepage characteristics of BCR directly affect the safe and efficient mining of coal mines. Thus, numerous laboratory studies have focused on the compaction seepage characteristics of BCR. This paper first outlines the engineering problems involved in the BCR during coal mining including the air leakage, the spontaneous combustion, the gas drainage, and the underground reservoirs in the goaf. Water inrush related to tectonics such as faults and collapse columns and surface subsidence related to coal gangue filling and mining also involve the compaction seepage characteristics of BCR. Based on the field problems of BCR, many attempts have been made to mimic field environments in laboratory tests. The experimental equipment (cavity size and shape, acoustic emission, CT, etc.) and experimental design for the BCR were firstly reviewed. The main objects of laboratory analysis can be divided into compression tests and seepage test. During the compaction test, the main research focuses on the bearing deformation characteristics (stress-strain curve), pore evolution characteristics, and re-crushing characteristics of BCR. The seepage test mainly uses gas or water as the main medium to study the evolution characteristics of permeability under different compaction stress conditions. In the laboratory tests, factors such as the type of coal and rock mass, particle size, particle shape, water pressure, temperature, and stress path are usually considered. The lateral compression test of BCR can be divided into three stages, including the self-adjustment stage, the broken stage, and the elastic stage or stable stage. At each stage, stress, deformation, porosity, energy, particle size and breakage rate all have their own characteristics. Seepage test regarding the water permeability experiment of BCR is actually belong to variable mass seepage. While the experimental test still focuses on the influence of stress on the pore structure of BCR in terms of gas permeability. Finally, future laboratory tests focus on the BCR related coal mining including scaling up, long term loading and water immersion, mining stress path matching were discussed.

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