首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Multiscale fracture network characterization and impact on flow: A case study on the Latemar carbonate platform
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Multiscale fracture network characterization and impact on flow: A case study on the Latemar carbonate platform

机译:多尺度裂缝网络特征及其对流动的影响-以Latemar碳酸盐岩台地为例

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A fracture network arrangement is quantified across an isolated carbonate platform from outcrop and aerial imagery to address its impact on fluid flow. The network is described in terms of fracture density, orientation, and length distribution parameters. Of particular interest is the role of fracture cross connections and abutments on the effective permeability. Hence, the flow simulations explicitly account for network topology by adopting Discrete-Fracture-and-Matrix description. The interior of the Latemar carbonate platform (Dolomites, Italy) is taken as outcrop analogue for subsurface reservoirs of isolated carbonate build-ups that exhibit a fracture-dominated permeability. New is our dual strategy to describe the fracture network both as deterministic-and stochastic-based inputs for flow simulations. The fracture geometries are captured explicitly and form a multiscale data set by integration of interpretations from outcrops, airborne imagery, and lidar. The deterministic network descriptions form the basis for descriptive rules that are diagnostic of the complex natural fracture arrangement. The fracture networks exhibit a variable degree of multitier hierarchies with smaller-sized fractures abutting against larger fractures under both right and oblique angles. The influence of network topology on connectivity is quantified using Discrete-Fracture-Single phase fluid flow simulations. The simulation results show that the effective permeability for the fracture and matrix ensemble can be 50 to 400 times higher than the matrix permeability of 1.0.10(-14) m(2). The permeability enhancement is strongly controlled by the connectivity of the fracture network. Therefore, the degree of intersecting and abutting fractures should be captured from outcrops with accuracy to be of value as analogue.
机译:在一个孤立的碳酸盐岩平台上,从露头和航拍图像中量化裂缝网络的布置,以解决其对流体流动的影响。该网络是根据裂缝密度,方向和长度分布参数来描述的。特别令人感兴趣的是裂缝的交叉连接和基台对有效渗透率的作用。因此,流模拟通过采用离散断裂和矩阵描述来明确考虑网络拓扑。 Latemar碳酸盐台地(意大利多洛米蒂)的内部被认为是孤立的碳酸盐岩层地下储层的露头类似物,这些碳酸盐岩层表现出以裂缝为主导的渗透率。新的双重策略是将裂缝网络描述为流量模拟的确定性输入和随机输入。通过整合露头,机载图像和激光雷达的解释,可以清晰地捕获裂缝的几何形状,并形成多尺度数据集。确定性网络描述构成了描述规则的基础,该描述规则可诊断复杂的自然裂缝布置。裂缝网络表现出不同程度的多层层次结构,较小的裂缝在直角和斜角下都与较大的裂缝邻接。网络离散度对网络连通性的影响可以通过离散-断裂-单相流体流动模拟来量化。仿真结果表明,裂缝和基质整体的有效渗透率可以比基质渗透率1.0.10(-14)m(2)高50到400倍。渗透率的提高受到裂缝网络连通性的强烈控制。因此,应准确地从露头中捕获相交和邻接的裂缝的程度,以作为类似物。

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