由爽, 李飞, 纪洪广, 王洪涛, 张乘菡. 高应力高水压下深部花岗岩力学响应联动机制[J]. 煤炭学报, 2020, 45(S1): 219-229. DOI: 10.13225/j.cnki.jccs.2019.1389
引用本文: 由爽, 李飞, 纪洪广, 王洪涛, 张乘菡. 高应力高水压下深部花岗岩力学响应联动机制[J]. 煤炭学报, 2020, 45(S1): 219-229. DOI: 10.13225/j.cnki.jccs.2019.1389
YOU Shuang, LI Fei, JI Hongguang, WANG Hongtao, ZHANG Chenghan. Linkage mechanism of mechanical response of deep granite under high stress and high water pressure[J]. Journal of China Coal Society, 2020, 45(S1): 219-229. DOI: 10.13225/j.cnki.jccs.2019.1389
Citation: YOU Shuang, LI Fei, JI Hongguang, WANG Hongtao, ZHANG Chenghan. Linkage mechanism of mechanical response of deep granite under high stress and high water pressure[J]. Journal of China Coal Society, 2020, 45(S1): 219-229. DOI: 10.13225/j.cnki.jccs.2019.1389

高应力高水压下深部花岗岩力学响应联动机制

Linkage mechanism of mechanical response of deep granite under high stress and high water pressure

  • 摘要: 深部高应力环境下,岩体通常处于应力峰后段,裂隙发育,岩石破碎,在这样的环境下,高水压对岩体性能的影响将更为明显。本研究针对千米以深的岩体峰后特性开展试验研究工作。采用水力耦合条件下的三轴循环加卸载试验,获得全应力-应变曲线。通过获取起裂应力、扩容应力、峰值应力、残余应力等应力阈值,对岩石各个应力应变阶段进行划分。通过计算各变形参数及渗透率获取岩石水力参数的演化规律;针对高围压、高渗透压环境下花岗岩破坏后表现出的较高残余强度,对比分析不同围压等级下残余强度与峰值强度的比值,获得不同高围压等级对于花岗岩石峰值破坏时强度衰减的影响曲线;通过分析峰后残余段初始渗透率较峰值处渗透率的损失值,揭示岩石受围压因素影响从峰值处至残余段渗透性能变化过程,获得不同高围压等级与渗透率波动的相关性。最后通过拟合岩石扩容阶段、残余阶段损伤变量与渗透率演化曲线,研究两者之间的相关性。结果表明:碎裂质花岗岩受高围压、高水压耦合作用下,表现出无压密段、起裂点低、较长的屈服阶段与扩容阶段以及破坏后保留较高承载能力的力学特性;弹性模量在峰前阶段呈现下降趋势,在峰后残余阶段表现出先上升后下降的趋势,泊松比的演化规律正好相反;岩石的损伤变量随峰前循环次数增加表现先下降后上升趋势,在峰后残余阶段损伤变量稳定上升,渗透率也呈现相似规律。扩容阶段岩石的渗透率与损伤变量呈现对数函数关系,而残余阶段则两者呈现出良好的指数函数关系;残峰比与围压等级呈负相关性,而渗透率损失率随围压呈正相关性。

     

    Abstract: Under high stress and high water pressure,the rocks are usually in the post-peak stage,some cracks are developed and some internal structures are broken. The variability of mechanical behavior of rock mass is seriously presented. Therefore,this paper performed a series of triaxial cyclic loading and unloading experiments under hydraulic-mechanics coupling to investigate the post-peak characteristics of granite drilled from more than 1 000 m in metal mine. Through the complete stress-strain curves,the mechanical and hydraulic parameters are correspondingly calcu-lated. By obtaining the threshold values of crack initiation stress,dilatancy stress,peak stress and residual stress,the stress-strain stages of rock are divided. Given the high residual strength of granite after failure,the ratio of residual strength to peak strength under different confining pressures is analyzed and compared,and the influence curve of different confining pressures on the strength loss of granite is built. By comparing the difference between the initial permeability at the residual stage and the maximum permeability before the peak stage,the permeability change affected by confining pressure factors is revealed,and the relationship between different high confining pressures and permeability changes is obtained. Finally,the response mechanism among the rock expansion,damage evolution on residual stages and permeability are explicated. The results show that under the coupling of high confining pressure and high water pressure,the cataclastic granite shows the mechanical characteristics of no compaction section,low initiation point,long yield stage and expansion stage,and high bearing capacity after failure. The elastic modulus shows a downward trend in the pre-peak stage,and an upward and then downward trend in the residual stage,and the evolution law of Poisson's ratio is opposite. With the increase of the number of cycles,the damage variable of rock shows a trend of decrease first and then increase,and increases steadily in the residual stage after peak,the permeability shows similar law. The relationship between the permeability and damage variable of rock can be described by logarithmical function in the expansion stage and an exponent function in the residual stage. There is a negative correlation between the ratio of residual strength to peak strength and the confining pressure,while the permeability loss rate has a positive correlation with the confining pressure.

     

/

返回文章
返回