非均质多孔介质中反应输运的高阶自适应方案

Ricardo H. Deucher, H. Tchelepi
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引用次数: 1

摘要

二氧化碳的地下封存、污染物输送和提高采收率的过程往往涉及复杂的反应动力学。岩石-流体相互作用跨越了非常广泛的长度和时间尺度,对于数值解来说,正确地解决这些尺度是非常重要的。为了应对这些挑战,我们扩展了以前开发的用于模拟非均质多孔介质中反应性输移的自适应输移方案(Deucher和Tchelepi, 2021),以考虑(a)对流通量的高阶近似和(b)与连接到地球化学数据库的化学求解器的耦合。数值结果表明,当采用高阶近似时,自适应更有效。这是因为与低阶近似相比,数值色散水平较低,这有助于更准确地解决位移前沿。因此,经历显著浓度和饱和度梯度的区域更受限制,这导致自适应方案的计算效率提高。该方法的鲁棒性通过具有多井和可变总液率的高度非均质两相情况得到了验证。由于自适应方案的模块化,与化学求解器模块的耦合是直接的。在方解石储层基质中注入碳酸水的三维情况下,对该方案进行了测试。结果表明,该自适应方案在整个模拟过程中准确地表示了六种反应组分的参考浓度分布,并大大减少了实现该解决方案所需的单元更新次数。
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High-Order Adaptive Scheme for Reactive Transport in Heterogeneous Porous Media
Subsurface sequestration of carbon dioxide, contaminant transport, and enhanced oil recovery processes often involve complex reaction dynamics. The rock-fluid interactions span a very wide range of length and time scales, and it is important for the numerical solutions to resolve these scales properly. To address these challenges, we extend the adaptive transport scheme for the simulation of reactive transport in heterogeneous porous media developed previously (Deucher and Tchelepi, 2021) to account for (a) higher-order approximation of the convective fluxes and (b) coupling with a chemical solver connected to geochemical databases. The numerical results demonstrate that adaptivity is more effective when a higher-order approximation of the fluxes is used. This is because of lower levels of numerical dispersion compared with low-order approximations, which helps resolve the displacement fronts more accurately. As a result, the regions that experience significant concentration and saturation gradients are more confined, and that leads to improvements in the computational efficiency of the adaptive scheme. The robustness of the approach is demonstrated using a highly heterogeneous two-phase case with multiple wells and a variable total liquid-rate. Due to the modularity of the adaptive scheme, coupling with a chemical solver module is straightforward. The scheme is tested for a three-dimensional case that considers injection of carbonated water in a reservoir matrix of calcite. The results show that the adaptive scheme leads to an accurate representation of the reference concentration distributions of the six reactive components throughout the simulation and leads to a large reduction in the number of cell updates required to achieve the solution.
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