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赵延林, 曹平. 裂隙岩体渗流—损伤—断裂耦合模型(扩展FLAC3D模型)与工程应用[J]. 岩土工程学报, 2010, 32(1).
引用本文: 赵延林, 曹平. 裂隙岩体渗流—损伤—断裂耦合模型(扩展FLAC3D模型)与工程应用[J]. 岩土工程学报, 2010, 32(1).
Coupling model of seepage-damage-fracture in fractured rock masses (extended flac3D model) and its appliance[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(1).
Citation: Coupling model of seepage-damage-fracture in fractured rock masses (extended flac3D model) and its appliance[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(1).

裂隙岩体渗流—损伤—断裂耦合模型(扩展FLAC3D模型)与工程应用

Coupling model of seepage-damage-fracture in fractured rock masses (extended flac3D model) and its appliance

  • 摘要: 摘 要:综合运用岩体结构力学、几何损伤力学及岩石流体力学理论,建立裂隙岩体渗流—损伤—断裂耦合数学模型(扩展FLAC3D模型),在FLAC现有计算模块的基础上,通过FISH研制了裂隙岩体渗流—损伤—断裂耦合分析程序。该模型的耦合机体现在:渗透水力梯度作为渗透体积力作用于损伤应力计算单元,裂隙渗透压作为面力作用于裂纹张开部分引起断续岩石裂纹的起裂,扩展导致岩体局部损伤;岩体裂纹的扩展引起岩体渗透系数的增加,导致渗流场的改变。对一复杂裂隙岸坡蓄水加载过程进行渗流—损伤—断裂耦合分析,得到不同蓄水时期,裂隙岸坡渗流场分布、损伤场的演化,初步探讨了水库蓄水过程中岸坡山体变形机制。耦合分析认为:山体变形是增量渗透力和增量浮托力共同作用于岸坡的结果;对蓄水相对高程较大的裂隙岸坡而言,库水位上升,裂隙渗透水压增加导致岩体裂纹起裂扩展,岩体损伤区增大且向岸坡深部扩展。高渗透压诱发岸坡不利断层带损伤区扩展,甚至贯通可能是导致岸坡失稳的重要原因。

     

    Abstract: Abstract: By comprehensive use of theory of structural mechanics of rock mass , geometrical damage mechanics and rock fluid mechanics,the model of seepage-damage-fracture coupling (extended FLAC3D model) was established. Baesd on FLAC3D existing computation modules,the programs of seepage-damage-fracture coupling in fractured rock masses were developed with the FISH language.Coupling mechanism of the model of seepage- damage-fracture coupling lies in that hydraulic gradient applies on the stress calculation units as permeate volume strength.Seepage pressure applies on the opening part of cracks as surface force, then lead rocks damage with discontinuous cracks splitting and growth; The cracks growth induce the increase of permeability coefficient, ultimately the change of seepage field.The seepage-damage-fracture coupling analysis on the fractured rock bank slope during the rising of water level in reservoir is shown.The laws of the distribution of the seepage field and rocks damage field evolution were obtained.A preliminary study on deformation of bank slope during the rising of water level in reservoir also was made .Coupling Analysis holds that deformation of bank slope is due to the interaction of increment seepage force and increment uplift force.For the fractured bank slope with the hight relative elevation of water storage , the increase of seepage pressure in fractures lead to damage zone growth with starting-crack and fracture propagation occuring.High seepage pressure lead to damage zone growth in unfavorable fault zone and even transfixion may be the important reasons which result in bank slope instability.

     

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