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

IF 3.5 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Weihang Sun, Yongqi Wang
{"title":"Modeling Phase Separation in Grain-Fluid Mixture Flows by a Depth-Averaged Approach With Dilatancy Effects","authors":"Weihang Sun,&nbsp;Yongqi Wang","doi":"10.1029/2023JF007416","DOIUrl":null,"url":null,"abstract":"<p>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.</p>","PeriodicalId":15887,"journal":{"name":"Journal of Geophysical Research: Earth Surface","volume":"129 12","pages":""},"PeriodicalIF":3.5000,"publicationDate":"2024-12-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2023JF007416","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Earth Surface","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2023JF007416","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0

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.

Abstract Image

求助全文
约1分钟内获得全文 求助全文
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
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信