1. 山东科技大学 能源与矿业工程学院,山东,青岛,266590
2. 山东科技大学 矿山灾害预防控制省部共建国家重点实验室培育基地,山东,青岛,266590
网络首发:2022-10-03,
纸质出版:2022
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张东晓, 郭伟耀, 赵同彬, 等. 岩石I型裂纹定向扩展规律试验研究[J]. 岩土力学, 2022,43(S2):231-244.
ZHANG Dong-xiao, GUO Wei-yao, ZHAO Tong-bin, et al. Experimental study on directional propagation of rock type-Ⅰ crack[J]. 2022, 43(S2): 231-244.
张东晓, 郭伟耀, 赵同彬, 等. 岩石I型裂纹定向扩展规律试验研究[J]. 岩土力学, 2022,43(S2):231-244. DOI: 10.16285/j.rsm.2021.2188.
ZHANG Dong-xiao, GUO Wei-yao, ZHAO Tong-bin, et al. Experimental study on directional propagation of rock type-Ⅰ crack[J]. 2022, 43(S2): 231-244. DOI: 10.16285/j.rsm.2021.2188.
为精准获得岩石I型裂纹扩展演化全过程,采用一种简易裂纹定向扩展装置开展了不同岩性试样裂纹扩展试验研究,借助声发射及数字散斑技术对裂纹扩展全过程进行了监测,建立了裂纹定向扩展力学模型,分析了裂纹扩展过程中声发射及变形场的演化规律,提出了评价岩石I型裂纹扩展难易程度的能量指标CE,探讨了I型裂纹定向起裂扩展机制。结果表明:该简易裂纹定向扩展装置能够有效实现I型裂纹沿预定方向稳定扩展,其起裂角均小于10º,同时通过简化力学模型计算得到白砂岩、灰砂岩的裂纹扩展峰值强度与巴西劈裂抗拉强度相比偏差分别为22.76%、7.53%;根据变形场演化规律,可将裂纹扩展分为微裂隙发育(散斑变形场分区不明显)、主控裂纹孕育(散斑变形场出现分区现象)和主控裂纹扩展3个阶段;声发射演化过程可分为平静期、缓增期、急增期和降低期4个阶段,由于灰砂岩相较于白砂岩质地更致密、更坚硬,导致其声发射平静期长,而后3个阶段持续时间短;将载荷−位移曲线峰前与峰后的面积之比定义为评价岩石I型裂纹扩展难易程度的能量指标CE,计算得到灰砂岩、白砂岩的CE分别为13~16、1~2,表明CE可有效评价岩石I型裂纹扩展难易程度;岩石I型裂纹起裂扩展机制可概况为:在加载峰值前裂隙尖端受最大拉应力作用,存储的弹性能快速增加、耗散能缓慢增加,但在加载峰值后裂隙尖端存储弹性能超过其储能极限迅速释放,此时输入能大部分转化为耗散能促进主控裂纹快速扩展。后续将对裂纹定向扩展试验装置进一步优化改进,以期为裂纹扩展机制、岩石破坏前兆信息、裂纹止裂原理等研究提供一种新方法,同时为工程现场煤岩层定向爆破、压裂、止裂等相关技术优化提供理论指导。
To obtain the rock type-Ⅰ crack propagation process accurately
a simple crack directional propagation device was used to test the crack propagation of different rock types. The crack propagation process of rock is monitored with acoustic emission (AE) and digital image correlation method (DICM). A mechanical model of crack directional propagation was established. Then
AE and deformation field evolution laws during crack propagation process are analyzed
and a new crack propagation energy index (CE) is proposed to evaluate the difficulty of rock type-Ⅰ crack propagation and the crack initiation and propagation mechanism is discussed. The results show that
the simple crack directional propagation device can effectively realize the stable propagation of type-Ⅰ crack along the predetermined direction
the crack initiation angle is less than 10º
and the deviations between the peak strength of crack propagation calculated by simplified mechanical model and the tensile strength of Brazilian splitting are 22.76% and 7.53% for white sandstone and grey sandstone
respectively. According to the deformation field evolution law
the crack propagation can be divided into three stages: microcrack development (speckle deformation field is still uniform)
main crack propagation (zone phenomenon appears in speckle deformation field) and main crack propagation. Four stages including quiet stage
slow increase stage
rapid increase stage and decreasing stage can be identified in the AE evolution process. Compared with white sandstone
the gray sandstone is denser and the main cracks are fully developed
resulting in a long quiet stage of AE
while the last three stages are short. The area ratio of pre-peak area to post-peak areaof load-displacement curve was defined as CE
the CE of gray sandstone and white sandstone are 13−16
1−2
respectively
which shows that the CE can effectively evaluate the difficulty of type-I crack propagation. Rock type-I crack initiation and propagation mechanism can be summarized as follows: before the peak
the prefabricated crack tip is subjected to the maximum tensile stress
the elastic energy increases rapidly
and the dissipated energy increases slowly; nevertheless after the peak
elastic energy exceeds its energy storage limit and is released rapidly
most of the input energy is converted into dissipated energy
which results in a propagation rapid of crack. In the future
the crack directional propagation device will be optimized and improved
and it is expected to provide a new method for the study of crack propagation mechanism
rock fail precursor information and crack arrest principle
and to provide theoretical guidance for the optimization of coal strata directional blasting
fracturing
fracture arrest and other related technologies in the engineering site.
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