黄锋, 周洋, 李天勇, 胡学涛. 软硬互层岩体力学特性及破坏形态的室内试验研究[J]. 煤炭学报, 2020, 45(S1): 230-238. DOI: 10.13225/j.cnki.jccs.2019.1388
引用本文: 黄锋, 周洋, 李天勇, 胡学涛. 软硬互层岩体力学特性及破坏形态的室内试验研究[J]. 煤炭学报, 2020, 45(S1): 230-238. DOI: 10.13225/j.cnki.jccs.2019.1388
HUANG Feng, ZHOU Yang, LI Tianyong, HU Xuetao. Laboratory experimental study on mechanical properties and failure modes of soft and hard interbedded rock mass[J]. Journal of China Coal Society, 2020, 45(S1): 230-238. DOI: 10.13225/j.cnki.jccs.2019.1388
Citation: HUANG Feng, ZHOU Yang, LI Tianyong, HU Xuetao. Laboratory experimental study on mechanical properties and failure modes of soft and hard interbedded rock mass[J]. Journal of China Coal Society, 2020, 45(S1): 230-238. DOI: 10.13225/j.cnki.jccs.2019.1388

软硬互层岩体力学特性及破坏形态的室内试验研究

Laboratory experimental study on mechanical properties and failure modes of soft and hard interbedded rock mass

  • 摘要: 软硬互层岩体是煤矿开采过程中常常遇到的不良地质,其构造的特殊性导致安全事故频发。为研究软硬互层岩体的力学特性及破坏机制,通过自制不同岩层倾角,不同层厚比的软硬互层岩体,采用室内岩石力学试验方法,得到:①软硬互层岩体的破坏从硬层开始,再逐步扩展到软层。单轴条件下,软层抑制裂隙扩展的能力随软层厚度的增加递增,但会引起峰值强度的下降;三轴条件下,随着软层厚度的增加,软层抑制裂隙扩展的能力先增加后降低,峰值强度呈倒“V”的规律、黏聚力显著下降,内摩擦角保持稳定。②单轴条件下,0°与30°试样均有应力跌落现象,不同的是30°下的应力应变曲线在应力跌落过后还有一段上升期,延性破坏特征更明显;三轴条件下,0°的岩体具有明显的峰后软化特征,而30°的岩体则不明显,多数为硬化流动破坏。随着软层厚度的增加,应变软化程度先增加后降低。③围压对软层、硬层的膨胀变形约束效果不同,容易引起软硬互层岩体的剪切破坏;随着围压的增加,峰后应力随应变的降低速率逐渐变缓、应变软化程度逐渐减弱、延性增大,软硬互层岩体峰值强度、峰值应变、弹性模量增大。④岩层存在倾角时,软弱互层连接处的敏感性增强,试件更容易产生贯穿裂隙;一定范围内的岩层倾角会弱化软硬互层岩体的力学性能,导致软硬互层岩体的弹性模量、峰值强度、内摩擦角下降。

     

    Abstract: Soft and hard interbedded rock mass is a bad geology body often encountered in engineering project,and its special structure leads to some frequent safety accidents. In order to study the mechanical properties and failure mechanism of soft and hard interbedded rock masses,using indoor rock mechanics test methods,the soft and hard interbedded rock masses with different rock layer dip angles and different layer thickness ratios were investigated. The study shows that ①soft and hard interbedded rock mass begins to break from the hard layer and then gradually expands to the soft layer. Under uniaxial conditions,as the thickness of the soft layer increases,the ability of the soft layer to inhibit crack propagation tends to increase,but it will cause the peak strength decrease. Under the triaxial condition,with the increase of soft layer thickness,the ability of soft layer to inhibit crack propagation first increases and then decreases,the peak intensity is inverted "V",the cohesive force is significantly decreased,and the internal friction angle is kept stable. ② Under uniaxial conditions,the 0° and 30° samples have a stress drop phenomenon,the difference is the stress-strain curve at 30° has a rising period after the stress drop,and the ductile failure characteristics are more obvious. Under the triaxial condition,the 0° rock mass has obvious post-peak softening characteristics,while the 30° rock mass does not have same obvious characteristics. Most are hardened flow damage. As the thickness of the soft layer increases,the degree of strain softening increases first and then decreases. ③Confining pressure has different effects on the expansion and deformation of soft and hard layers,which is easy to cause a shear failure of soft and hard interbedded rock mass. With the increase of confining pressure,the decreasing rate of partial stress-strain curves becomes slower and the degree of strain softening is gradually weakened and the ductility is increased. The peak strength,peak strain and elastic modulus of the soft and hard interbedded rock mass are increased. ④When the rock layer has an inclination angle,the sensitivity of the joint of the weak interbedded rock mass is enhanced,and the test sample is more likely to have a through crack. The dip angle of the rock within a certain range will weaken the mechanical properties of the soft and hard interbedded rock mass,resulting in the decrease of the elastic modulus,peak strength and internal friction angle of the soft and hard interbedded rock mass.

     

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