离散断裂网络大尺度直剪试验模拟中断层抗剪强度的确定方法

Bona Kim
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摘要

在本研究中,为了更好地理解相对大规模直剪试验模型中剪切断层的行为,将3DEC建模与离散断裂网络(DFNs)技术相结合。DFNs明确地生成了两种不同的断裂面表面几何形状,表明表面呈阶梯状或光滑状,使用概率分布函数来生成离散裂缝的方向、裂缝密度(或频率)和大小。利用3DEC建模软件建立了百米的三维块体模型进行直剪试验。在完成直剪试验模拟后,通过反算估算出断面的抗剪强度。具有亚水平/垂直倾角的DFNs形成了瓦叠结构,导致了断裂面的阶梯式几何形状和强烈的剪切响应。在直接剪切作用下,断裂面需要先将凸起或块体破碎,然后才允许发生任何摩擦行为,否则断裂面将显著扩张。这导致了断裂面较高的抗剪强度。另一方面,倾斜倾角的DFNs形成了相对光滑的断平面表面。断裂面光滑的表面允许主要平行于断裂面的变形,并且在模型中只有少数破坏发生在岩块上。因此,3DEC模型使用两个截然不同的dfn明确地复制了断层面的复杂几何形状,并允许研究人员研究断层面的不同剪切行为作为地表条件的函数。
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Approaches to Determine Fault Shear Strength in Large-scale Direct Shear Test Simulations using Discrete Fracture Networks
In this study, 3DEC modeling in conjunction with the Discrete Fracture Networks (DFNs) technique was performed to better understand the behavior of shearing faults in a relatively large-scale direct shear test model. The DFNs explicitly generated two different geometries of the fault plane surface indicating the stepped or smooth waviness of the surface using probability distribution functions to generate orientation, fracture density (or frequency), and size of the discrete fractures. A 3-dimensional block model of hundreds of meters was constructed for the direct shear test using 3DEC modeling software. After the completion of the direct shear test simulations, a shear strength of the fault plane was estimated by back calculation. The DFNs with subhorizontal/vertical dip angles created an imbricate structure that resulted in a stepped geometry and strong shear response in the fault plane. Under direct shear, the fault plane needed to break the asperities or block before any frictional behavior was allowed or the fault plane would dilate significantly. This resulted in higher shear strength of the fault plane. On the other hand, the DFNs with oblique dip angles generated a relatively smooth surface of the fault plane. The smooth surface of the fault plane allowed deformation principally parallel to the fault plane, and only a few failures developed across the rock blocks in the model. Consequently, the 3DEC model explicitly replicated the complicated geometries of the fault plane using the two very contrasting DFNs and allowed researchers to investigate different shear behaviors of fault planes as a function of surface conditions.
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