不同含水率花岗岩力学特性及声发射特征研究
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1.鞍钢集团矿业弓长岭有限公司露采分公司, 辽宁 辽阳 111008 ; 2.中国恩菲工程技术有限公司, 北京 100038 ; 3.北京科技大学金属矿山高效开采与安全教育部重点实验室, 北京 100083

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王峰(1984—),男,山西泽州人,硕士,工程师,主要从事煤矿安全生产管理工作。

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P584

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弓长岭独木采区西北帮地下开采及地质环境影响研究(项目号:2023-科A04)


Study on Mechanical Properties and Acoustic Emission Characteristics of Granite With Different Water Content
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    摘要:

    含水率是影响花岗岩力学性能及破坏模式的关键因素,为探究不同含水率对花岗岩力学性能和破坏模式的影响,开展了3组不同含水率(干燥、天然、饱水)花岗岩单轴压缩和声发射试验,从试样的力学行为、破裂模式和声发射参数特征来探讨含水率对花岗岩的影响。结果表明:随着含水率的增加,花岗岩的峰值应力和弹性模量逐渐降低,相较于干燥试样,饱水试样的峰值应力降低了约5152%、弹性模量降低了约2277%,峰值应变则呈现先降低后升高的变化趋势。天然状态下花岗岩峰值应变最低,约为0694%;泊松比则呈线性递增的趋势,由021增至025。含水率的越高的花岗岩试样的应力-应变曲线出现应力跌落现象越明显。随着含水率的增加,花岗岩试样表面的张拉裂纹数量减少,岩石崩落的块体体积增大。岩石的破坏模式由劈裂破坏转为拉剪混合破坏,最后为X型共轭剪切破坏。随着含水率的增加,水化反应削弱颗粒间的粘聚力越强,岩石更容易发生微裂纹的扩展和相对滑动,导致饱水花岗岩试样的损伤曲线突变点出现最早,约为4523s。花岗岩声发射信号主要集中在低频和中频,且以低幅信号为主。随着含水率的增加,低中频之间的声发射信号向加载后期转移。无论花岗岩是否含水在加载后期均观察到高幅现象。

    Abstract:

    Moisture content is a key factor affecting the mechanical properties and failure modes of granite. In order to explore the influence of different moisture contents on the mechanical properties and failure modes of granite, three groups of uniaxial compression and acoustic emission tests of granite with different moisture contents (dry, natural and saturated) were carried out. The influence of moisture content on granite was discussed from the mechanical behavior, fracture mode and acoustic emission parameter characteristics of samples. The results show that with the increase of water content, the peak stress and elastic modulus of granite decrease gradually. Compared with dry samples, the peak stress of saturated samples decreases by about 5152%, and the elastic modulus decreases by about 2277%. The peak strain decreases first and then increases. The peak strain of granite in natural state is the lowest, about 0694%. Poissons ratio increased linearly from 021 to 025. The higher the water content, the more obvious the stress drop phenomenon in the stress-strain curve of the granite sample. With the increase of water content, the number of tensile cracks on the surface of granite samples decreases, and the volume of rock collapse increases. The failure mode of rock changes from splitting failure to tensile-shear mixed failure, and finally to X-type conjugate shear failure. With the increase of water content, the hydration reaction weakens the cohesion between particles, and the rock is more prone to micro cracks.

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王峰, 洪大华, 王宇驰, 等.不同含水率花岗岩力学特性及声发射特征研究[J].中国矿山工程,2025,54(5):43-48.

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  • 在线发布日期: 2025-12-24
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