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Fractal theory and groundwater flow in fractured media.

机译:分形理论与地下水在裂隙介质中的流动。

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Numerous statistical models have been developed to study fluid flow in fractured media. However, the randomness assumption in these models is difficult to rationalize. In fact, experimentally and theoretically, it has been shown that rock fractures have predetermined paths of growth. Rock fracturing is a self-similar process in which properties of new fractures are controlled by the existing fractures. Unlike engineering materials, rock fracturing cannot be described by simple mathematical equations, neither by statistical models.; This research aims to develop a fractal model that overcomes limitations of the current statistical models. Iterated function systems (IFS) can create fractal objects. An arbitrary fracture set can be created by four “background” transformations and one “condensation set”. The challenge remains to identify the correct IFS whose attractor is “close” to limited field observations. An inverse fractal algorithm and associated graphical program provide the answer to this question. Subsequently, the fractal nature of fractures defines their hydraulic properties. Permeability tensors of all cells in a grid are calculated using “representative fractures”. The flow problem is then solved using a finite difference program (FLAC 2D). Limitations of the finite difference technique are discussed, as applied to fractured media. For a highly heterogeneous fracture network, it is recommended to use a discrete network model, as opposed to an equivalent continuum model.; In a physical experiment based on a Hele-Shaw model, good agreement was observed between the experiment and the fractal model. 30% difference in discharge was predicted due to the considerably smaller number of fractures in the experiment and the observations confirmed this prediction. As a practical example, some initial work on Yucca Mountain Project (YMP) showed that fracture patterns at this site have a fractal nature. The “shadow theorem of fractals” was used to simulate a fracture set with a fractal pattern.; This work opens new opportunities for fractal theory to be used in characterization of fractured media. The proposed model is a simple and easy to use technique that proved to be effective and accurate.
机译:已经开发出许多统计模型来研究裂缝介质中的流体流动。但是,这些模型中的随机性假设很难合理化。实际上,在实验和理论上,已经表明,岩石裂缝具有预定的生长路径。岩石压裂是一个自相似过程,其中新裂缝的性质由现有裂缝控制。与工程材料不同,岩石压裂不能用简单的数学方程式描述,也不能用统计模型描述。本研究旨在开发一种分形模型,以克服当前统计模型的局限性。迭代功能系统(IFS)可以创建分形对象。可以通过四个“背景”转换和一个“凝结集”来创建任意裂缝集。挑战仍然是确定正确的IFS,其吸引子“接近”有限的野外观测。反分形算法和相关的图形程序为该问题提供了答案。随后,裂缝的分形性质决定了它们的水力性质。使用“代表性裂缝”计算网格中所有单元的渗透率张量。然后使用有限差分程序(FLAC 2D )解决流动问题。讨论了适用于压裂介质的有限差分技术的局限性。对于高度异构的裂缝网络,建议使用离散网络模型,而不是等效的连续模型。在基于Hele-Shaw模型的物理实验中,观察到实验与分形模型之间的一致性。预计由于实验中的裂缝数量要少得多,因此放电差异将达到30%,观察结果证实了这一预测。作为一个实际例子,丝兰山区项目(YMP)的一些初步工作表明,该位置的裂缝类型具有分形特征。 “分形的影子定理”用于模拟具有分形图案的裂缝。分形理论为裂缝介质的表征提供了新的机会。所提出的模型是一种简单易用的技术,被证明是有效且准确的。

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