界面裂隙倾角对岩-煤组合体力学特性影响试验研究

Experimental study on effects of interfacial crack angle on mechanical properties of rock-coal composite sample

  • 摘要: 为探究界面裂隙倾角α(界面裂隙与竖直方向夹角)对岩-煤组合体力学特性的影响, 结合声发射系统和XTDIC三维全场应变测量系统, 对α为0°、15°、30°、60°、75°和90°的岩-煤组合体试样进行单轴压缩试验, 研究其特征应力、变形破坏与能量演化等特征。结果表明: 在轴向应力作用下, 煤样裂隙区域更易发生应力集中, 导致裂纹起裂并扩展, 组合体试样的起裂应力和损伤应力随α的增大而逐渐降低; 随轴向应力的增大, 岩样内裂隙区域将形成新生裂纹并发育扩展。界面裂隙会促进组合体试样内裂纹的产生、发育与扩展, 削弱了其整体承载能力; 组合体试样峰前弹性能密度、单轴抗压强度以及弹性模量均随α增大呈递减趋势。煤样、岩样内裂纹扩展与贯通导致组合体试样破坏, 随着α的增大, 其宏观破坏模式由拉-剪混合破坏(伴随局部弹射现象)转变为以拉伸破坏为主, 峰后盈余能密度逐渐降低; 煤样破坏导致岩样回弹变形, 随着α增加, 岩样回弹变形量与回弹变形率逐渐增加。

     

    Abstract: To investigate the influence of interfacial crack angle on the mechanical properties of coal-rock composite samples, uniaxial compression tests were conducted on samples with interface crack angles α (the angle between the interface crack and vertical direction) of 0°, 15°, 30°, 60°, 75°, and 90°. Combined with acoustic emission system and XTDIC three-dimensional full-field strain measurement system, the characteristics of characteristic stress, deformation and failure characteristics, and energy evolution of rock-coal composite samples with interfacial crack were studied. under axial stress, the fractured zones within the coal sample are more prone to developing stress concentrations, leading to crack initiation and propagation. As α increases, the crack initiation stress and damage stress of the composite specimen gradually decrease.Interfacial crack facilitate the initiation, development, and propagation of internal cracks within composite samples, thereby weakening their overall load-bearing capacity.With the increase of α, the pre-peak elastic energy density of the composite sample gradually decreases, and the uniaxial compressive strength and elastic modulus of the sample show a decreasing trend. The propagation and coalescence of internal cracks in coal and rock samples lead to the failure of composite samples.With the increase of α, the macroscopic failure mode transitions from a tensile-shear mixed mode accompanied by localized ejection failure to one predominantly characterized by tensile failure, with a gradual decrease in post-peak surplus energy density. Concurrently, the failure of coal sample leads to the rebound deformation of rock sample, and with the increase of α, both the magnitude and rate of rebound deformation in the rock sample progressively rise.

     

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