Fractures are normally present in the underground and are, for some physical processes, of paramount importance. Their accurate description is fundamental to obtain reliable numerical outcomes useful, e.g., for energy management. Depending on the physical and geometrical properties of the fractures, fluid flow can behave differently, going from a slow Darcian regime to more complicated Brinkman or even Forchheimer regimes for high velocity. The main problem is to determine where in the fractures one regime is more adequate than others. In order to determine these low-speed and high-speed regions, this work proposes an adaptive strategy which is based on selecting the appropriate constitutive law linking velocity and pressure according to a threshold criterion on the magnitude of the fluid velocity itself. Both theoretical and numerical aspects are considered and investigated, showing the potentiality of the proposed approach. From the analytical viewpoint, we show existence of weak solutions to such model under reasonable hypotheses on the constitutive laws. To this end, we use a variational approach identifying solutions with minimizers of an underlying energy functional. From the numerical viewpoint, we propose a one-dimensional algorithm which tracks the interface between the low- and high-speed regions. By running numerical experiments using this algorithm, we illustrate some interesting behaviors of our adaptive model on a single fracture and small networks of intersecting fractures.
翻译:裂缝通常存在于地下,对于某些物理过程来说,是最重要的。准确描述对于获得可靠的数字结果(例如,对于能源管理来说)至关重要。根据断裂的物理和几何特性,流体可以采取不同的行为,从慢的达西安制度到更复杂的布林克曼制度,甚至高速度的福赫海默制度。主要问题是确定断裂中一个制度比其他制度更适当。为了确定这些低速度和高速区域,这项工作提出了一个适应性战略,其基础是选择适当的组织法,将速度和压力与流体速度本身的临界标准联系起来。考虑和调查理论和数字方面,显示拟议方法的潜力。从分析角度看,我们在构件法的合理假设下对这种模型存在薄弱的解决办法。为此,我们采用一种变式方法,确定与基本能源功能的最小化者一起找到解决办法。从数字角度出发,我们建议采用一维的算算算法,用以跟踪我们低序和高速度网络之间的界面。我们用一个有趣的数字模型,用这个模型来说明我们进行低序和高速度的模型。