Experimental Study on Uniaxial Compression Failure Characteristics and Mechanical Properties of Composite Aquiclude Rock

IF 1.2 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Geofluids Pub Date : 2024-11-27 DOI:10.1155/gfl/6100598
Qiang Sun, Rui Zhao, Xiaolong Li, Hui Yuan
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Abstract

Composite aquiclude rock is an important part of the water barrier layer of coal seam floor, and its mechanical properties and failure characteristics have an important impact on the safety of coal seam mining. In order to explore the uniaxial compression failure characteristics and mechanical properties of composite aquiclude rocks, the mineral composition and microstructure of the composite cement rock were measured by XRD and SEM. Using a WAW-1000D electrohydraulic servo universal test system, uniaxial compression tests were carried out on samples of four structural types, namely, mudstone/siltstone, mudstone/fine sandstone, fine sandstone/siltstone, and siltstone/mudstone/fine sandstone composites soaked in saline water with various immersion periods and pH values. The experimental results show that the failure of composite rock samples was mainly concentrated in the mudstone part. With the increased proportion of soft rock in the structure, the rock samples exhibited changes in tensile, X-shaped conjugate inclined plane shear, and single inclined plane shear failure modes. The overall compressive strength of composite rock samples decreased with immersion time, and their failure mode shifted from shear to tensile with increasing immersion time. The strength-weakening effect of high-salinity water with different acidity and alkalinity on composite rock samples was significant. The increased pH promoted the tensile failure-shear failure-tensile failure evolution. The results of this study can provide important experimental data and theoretical basis for the stability control of composite aquiclude rock in coal mining.

复合水成岩单轴压缩破坏特征和力学性能的实验研究
复合含水岩是煤层底板隔水层的重要组成部分,其力学性能和破坏特征对煤层开采安全具有重要影响。为了探索复合含水岩的单轴压缩破坏特征和力学性能,采用 XRD 和 SEM 测量了复合胶结岩的矿物组成和微观结构。利用 WAW-1000D 电液伺服万能试验系统,对泥岩/粉砂岩、泥岩/细砂岩、细砂岩/粉砂岩和粉砂岩/泥岩/细砂岩四种结构类型的复合材料样品在不同浸泡时间和 pH 值的盐水中进行了单轴压缩试验。实验结果表明,复合岩样的破坏主要集中在泥岩部分。随着结构中软岩比例的增加,岩石样品表现出拉伸、X 形共轭斜面剪切和单斜面剪切破坏模式的变化。随着浸泡时间的延长,复合岩样的整体抗压强度降低,其破坏模式也从剪切转变为拉伸。不同酸碱度的高盐度水对复合岩样的强度减弱效应显著。pH 值的增加促进了拉伸破坏-剪切破坏-拉伸破坏的演变。该研究结果可为煤矿开采中复合含水岩的稳定性控制提供重要的实验数据和理论依据。
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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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