期刊文献+

脆性岩石破裂过程损伤与渗流耦合数值模型研究 被引量:38

STUDY ON MODEL OF DAMAGE AND FLOW COUPLING IN BRITTLE ROCK FAILURE PROCESS
在线阅读 下载PDF
导出
摘要 大量的实验结果表明,脆性岩石的渗透性不是一个常量,而是应力和应力诱发损伤破裂的函数.建立了一个描述非均匀岩石渗流-应力-损伤耦合数学模型(FSD Model),开发出岩石破裂过程渗流-应力-损伤耦合分析计算系统(F-RFPA^(2D).在该系统中,单元的力学、水力学性质根据统计分布而变化,以体现材料的随机不均质性,材料在开裂破坏过程中流体压力传递通过单元渗流-损伤耦合迭代来实现.该系统能够对岩石试件在孔隙水压力和双轴荷载作用下裂纹的萌生、扩展过程中渗透率演化规律及其渗流-应力耦合机制进行模拟分析.最后,给出两个算例:算例1模拟载荷作用下岩石应力应变-渗透率全过程.模拟结果表明,非均匀性对岩石的应力峰值强度、峰值前后其渗透性演化规律及其破裂机制影响十分明显,模拟结果和实验结果较为一致;算例2模拟孔隙水压力作用下岩石拉伸断裂过程,通过和物理实验对比验证,验证了模型计算结果的可靠性. Experimental results provide strong evidence that rock permeability cannot be a constant but a function of stresses and stress-induced damage. In this paper, a numerical code Rock Failure Process Analysis (F-RFPA2D) is implemented by introducing a flow-stress-damage (FSD Model) coupling model for heterogeneous rocks and taking into account the growth of the existing cracks and the formation of new fractures. In this FSD model, material is discribed by many elements with the same size and different mechanical and permeability parameters in order to reflect the heterogeneity of rock. The water fluid pressure during failure process is obtained by flow and stress coupling iteration. A coupling analysis of flow and damage under hydraulic fracturing on rock is attained to simulate the fracture process of rock, and this model has been used to investigate the behavior of fluid flow, damage evolution and their coupling action in samples subjected to both hydraulic and biaxial compressive loading. Two numerical simulations are given. The results of the first simulation suggest that the nature of fluid flow in rocks varies from material to material and the peak strength of the rock samples and the change of rock permeability during progressive failure process depend strongly upon the heterogeneity of the rocks, and the numerical results compare well with the corresponding experimental results. Another simulation result presents a failure process subjected to tensile stress caused by pore pressure. It shows that the FSD model is valid by comparing with the experimental results.
出处 《力学学报》 EI CSCD 北大核心 2003年第5期533-541,共9页 Chinese Journal of Theoretical and Applied Mechanics
基金 国家自然科学基金(50204003) 国家自然科学基金(50134040) 香港专项研究基金(HKU7029/02E)
关键词 脆性岩石 破裂过程 损伤 渗流 耦合 数值模型 渗透性 F-RFPA^2D系统 failure process, heterogeneity, brittleness, permeability, F-RFPA2D
  • 相关文献

参考文献22

二级参考文献25

  • 1张守良,沈琛,邓金根.岩石变形及破坏过程中渗透率变化规律的实验研究[J].岩石力学与工程学报,2000,19(z1):885-888. 被引量:45
  • 2赵阳升.煤体—瓦斯耦合数学模型及数值解法[J].岩石力学与工程学报,1994,13(3):220-239. 被引量:70
  • 3李世平,李玉寿,吴振业.岩石全应力应变过程对应的渗透率-应变方程[J].岩土工程学报,1995,17(2):13-19. 被引量:109
  • 4陶振宇.水库诱发地震预测的新途径.第二次全国岩石力学与工程学术会议论文集[M].知识出版社,1989..
  • 5朱珍德.裂隙岩体非稳态渗流场与损伤耦合问题的研究:博士学位论文[M].上海:同济大学出版社,1997..
  • 6Schlangen E,van Mier JGM.Simple lattice model for numerical simulation of fracture of concrete materials and structures.Materials and Structures.1992,25:534~542
  • 7Frantziskonis G,Renaudin P,Breysse D.Heterogeneous solids-Part I: analytical and numerical 1-D results on boundary effects.Eur J Mech,A/Solids,1997,16(3): 409~423
  • 8Blair SC,Cook NG.Analysis of compressive fracture in rock using statistical techniques: Part I.a non-linear rule-based model.Int J Rock Mech Min Sci,1998,35(7): 837~848
  • 9Blair SC,Cook NG.Analysis of compressive fracture in rock using statistical techniques: Part II.effect of microscale heterogeneity on macroscopic deformation.Int J Rock Mech Min Sci,1998,35(7): 849~861
  • 10Tang CA,Kaiser PK.Numerical simulation of cumulative damage and seismic energy release during brittle rock failure Part I: fundamentals.Int J Rock Mech Min Sci,1998,35(2): 113~121

共引文献265

同被引文献458

引证文献38

二级引证文献388

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部