Modeling Phase Separation in Grain-Fluid Mixture Flows by a Depth-Averaged Approach With Dilatancy Effects

IF 3.8 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Journal of Geophysical Research: Earth Surface Pub Date : 2024-12-20 DOI:10.1029/2023JF007416
Weihang Sun, Yongqi Wang
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Abstract

In this work, we propose a comprehensive two-layer depth-averaged model to study the dynamic behavior of grain-fluid mixtures, which considers the granular dilatancy effects and the different frictional rheologies of grains in different states. Unlike single-phase flows, not only the interaction between granular and fluid phases significantly influence the dynamics of mixtures, but also the phase separation, so that different flow regimes can occur. These include five different possible regimes: two-layer regimes of (a) under-saturated mixture and (b) over-saturated mixture as well as single-layer regimes of (c) saturated mixture, (d) pure grains and (e) pure fluid. Most depth-averaged models in previous studies have considered only one of these flow regimes. The present model is an improved and integrated version of these depth-averaged models. Taking into account that the pure grains and pure fluid in the upper layer, which occur in the regimes of the under-saturated and over-saturated grain-fluid mixtures, respectively, exhibit different flow features than in the lower layer of the saturated mixture, we use a two-phase two-layer depth-averaged model to describe these regimes. This proposed model is possibly the first to employ a two-layer structure to describe all possible different flow regimes simultaneously. The proposed model is then solved numerically using a high-resolution central-upwind scheme and shows its ability to handle different flow regimes. To demonstrate the robustness of the numerical implementation and to evaluate the performance of the model, the numerical results are compared with several experiments reported in the literature, showing a certain qualitative agreement.

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考虑剪胀效应的颗粒-流体混合流动相分离深度平均模拟
在这项工作中,我们提出了一个综合的两层深度平均模型来研究颗粒-流体混合物的动态行为,该模型考虑了颗粒的膨胀效应和颗粒在不同状态下的不同摩擦流变学。与单相流动不同,颗粒相和流体相之间的相互作用不仅会显著影响混合物的动力学,而且还会影响相分离,因此会出现不同的流动形式。这包括五种不同的可能状态:(a)不饱和混合物的两层状态和(b)过饱和混合物的两层状态,以及(c)饱和混合物的单层状态,(d)纯颗粒和(e)纯流体。在以前的研究中,大多数深度平均模型只考虑了这些流态中的一种。本模型是这些深度平均模型的改进和综合版本。考虑到上层的纯颗粒和纯流体分别出现在欠饱和和过饱和的颗粒-流体混合物中,与饱和混合物的下层相比,它们表现出不同的流动特征,我们使用两相两层深度平均模型来描述这些状态。该模型可能是第一个采用两层结构来同时描述所有可能的不同流型的模型。然后,采用高分辨率的中心迎风格式对所提出的模型进行了数值求解,并显示了其处理不同流型的能力。为了证明数值实现的鲁棒性和评估模型的性能,将数值结果与文献中报道的几个实验进行了比较,显示出一定的定性一致性。
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来源期刊
Journal of Geophysical Research: Earth Surface
Journal of Geophysical Research: Earth Surface Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
6.30
自引率
10.30%
发文量
162
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