Computational Earth Science (EES-16), Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA.
Applied Mathematics and Plasma Physics (T-5), Theoretical Division, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA.
Phys Rev E. 2018 Mar;97(3-1):033304. doi: 10.1103/PhysRevE.97.033304.
Fractures form the main pathways for flow in the subsurface within low-permeability rock. For this reason, accurately predicting flow and transport in fractured systems is vital for improving the performance of subsurface applications. Fracture sizes in these systems can range from millimeters to kilometers. Although modeling flow and transport using the discrete fracture network (DFN) approach is known to be more accurate due to incorporation of the detailed fracture network structure over continuum-based methods, capturing the flow and transport in such a wide range of scales is still computationally intractable. Furthermore, if one has to quantify uncertainty, hundreds of realizations of these DFN models have to be run. To reduce the computational burden, we solve flow and transport on a graph representation of a DFN. We study the accuracy of the graph approach by comparing breakthrough times and tracer particle statistical data between the graph-based and the high-fidelity DFN approaches, for fracture networks with varying number of fractures and degree of heterogeneity. Due to our recent developments in capabilities to perform DFN high-fidelity simulations on fracture networks with large number of fractures, we are in a unique position to perform such a comparison. We show that the graph approach shows a consistent bias with up to an order of magnitude slower breakthrough when compared to the DFN approach. We show that this is due to graph algorithm's underprediction of the pressure gradients across intersections on a given fracture, leading to slower tracer particle speeds between intersections and longer travel times. We present a bias correction methodology to the graph algorithm that reduces the discrepancy between the DFN and graph predictions. We show that with this bias correction, the graph algorithm predictions significantly improve and the results are very accurate. The good accuracy and the low computational cost, with O(10^{4}) times lower times than the DFN, makes the graph algorithm an ideal technique to incorporate in uncertainty quantification methods.
断裂是低渗透岩石中地下流体流动的主要通道。因此,准确预测裂缝系统中的流动和传输对于提高地下应用的性能至关重要。这些系统中的裂缝尺寸可以从毫米到公里不等。尽管由于离散裂缝网络(DFN)方法中包含详细的裂缝网络结构,因此使用离散裂缝网络(DFN)方法来模拟流动和传输被认为更加准确,但在如此广泛的范围内捕捉流动和传输仍然是计算上不可行的。此外,如果要量化不确定性,则必须运行这些 DFN 模型的数百个实现。为了降低计算负担,我们在 DFN 的图形表示上求解流动和传输。我们通过比较基于图形和高保真 DFN 方法的突破时间和示踪粒子统计数据,研究了图形方法的准确性,对于具有不同数量的裂缝和异质性程度的裂缝网络。由于我们最近在能够对具有大量裂缝的裂缝网络进行 DFN 高保真模拟的能力方面取得了进展,因此我们处于执行此类比较的独特位置。我们表明,与 DFN 方法相比,图形方法的突破时间具有一致的偏差,偏差高达一个数量级。我们表明,这是由于图形算法对给定裂缝上交叉点的压力梯度的低估,导致示踪粒子在交叉点之间的速度较慢,旅行时间较长。我们提出了一种偏置校正方法,该方法可以减小图形算法与 DFN 预测之间的差异。我们表明,通过这种偏置校正,图形算法的预测得到了显著改善,结果非常准确。良好的准确性和低计算成本(比 DFN 低 O(10^{4})倍),使得图形算法成为不确定性量化方法中理想的技术。