{"title":"相干涉在多孔介质稳态两相流中的作用","authors":"Jiafan Guo , Zhechao Wang , Liping Qiao , Hao Feng","doi":"10.1016/j.advwatres.2025.104981","DOIUrl":null,"url":null,"abstract":"<div><div>When two fluids flow simultaneously in a porous medium at a low flow rate, known as steady-state two-phase flow, the total pressure drop deviates from a linear relationship with the Darcy flux. This deviation is primarily caused by the capillary pressure drop induced by interphase interference at pore throats. This study aims to estimate the capillary pressure drop based on fluid–fluid interfacial area at the pore scale. Recognizing that steady-state two phase flow typically exhibits discontinuous behavior, we proposed a simple equation to explain the relationship between total pressure drop, viscous pressure drop, and capillary pressure drop. Experiments were conducted in transparent micromodels to investigate the effects of flow rate, average viscosity and pore structure under both drainage and imbibition conditions. The results indicate a linear relationship between capillary pressure drop and the specific interfacial area of the moving wetting and moving non-wetting phase. Additionally, the slope of the capillary pressure drop-specific interfacial area curve is only related to the flow rate. Moreover, we established and verified the relationship between the specific interfacial area and relative permeability. This study provides new insights into the nonlinear relationship between Darcy flux and pressure drop in two-phase flow.</div></div>","PeriodicalId":7614,"journal":{"name":"Advances in Water Resources","volume":"202 ","pages":"Article 104981"},"PeriodicalIF":4.0000,"publicationDate":"2025-05-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The role of phase interference in steady-state two-phase flow in porous media\",\"authors\":\"Jiafan Guo , Zhechao Wang , Liping Qiao , Hao Feng\",\"doi\":\"10.1016/j.advwatres.2025.104981\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>When two fluids flow simultaneously in a porous medium at a low flow rate, known as steady-state two-phase flow, the total pressure drop deviates from a linear relationship with the Darcy flux. This deviation is primarily caused by the capillary pressure drop induced by interphase interference at pore throats. This study aims to estimate the capillary pressure drop based on fluid–fluid interfacial area at the pore scale. Recognizing that steady-state two phase flow typically exhibits discontinuous behavior, we proposed a simple equation to explain the relationship between total pressure drop, viscous pressure drop, and capillary pressure drop. Experiments were conducted in transparent micromodels to investigate the effects of flow rate, average viscosity and pore structure under both drainage and imbibition conditions. The results indicate a linear relationship between capillary pressure drop and the specific interfacial area of the moving wetting and moving non-wetting phase. Additionally, the slope of the capillary pressure drop-specific interfacial area curve is only related to the flow rate. Moreover, we established and verified the relationship between the specific interfacial area and relative permeability. This study provides new insights into the nonlinear relationship between Darcy flux and pressure drop in two-phase flow.</div></div>\",\"PeriodicalId\":7614,\"journal\":{\"name\":\"Advances in Water Resources\",\"volume\":\"202 \",\"pages\":\"Article 104981\"},\"PeriodicalIF\":4.0000,\"publicationDate\":\"2025-05-07\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Advances in Water Resources\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0309170825000958\",\"RegionNum\":2,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"WATER RESOURCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Advances in Water Resources","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0309170825000958","RegionNum":2,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"WATER RESOURCES","Score":null,"Total":0}
The role of phase interference in steady-state two-phase flow in porous media
When two fluids flow simultaneously in a porous medium at a low flow rate, known as steady-state two-phase flow, the total pressure drop deviates from a linear relationship with the Darcy flux. This deviation is primarily caused by the capillary pressure drop induced by interphase interference at pore throats. This study aims to estimate the capillary pressure drop based on fluid–fluid interfacial area at the pore scale. Recognizing that steady-state two phase flow typically exhibits discontinuous behavior, we proposed a simple equation to explain the relationship between total pressure drop, viscous pressure drop, and capillary pressure drop. Experiments were conducted in transparent micromodels to investigate the effects of flow rate, average viscosity and pore structure under both drainage and imbibition conditions. The results indicate a linear relationship between capillary pressure drop and the specific interfacial area of the moving wetting and moving non-wetting phase. Additionally, the slope of the capillary pressure drop-specific interfacial area curve is only related to the flow rate. Moreover, we established and verified the relationship between the specific interfacial area and relative permeability. This study provides new insights into the nonlinear relationship between Darcy flux and pressure drop in two-phase flow.
期刊介绍:
Advances in Water Resources provides a forum for the presentation of fundamental scientific advances in the understanding of water resources systems. The scope of Advances in Water Resources includes any combination of theoretical, computational, and experimental approaches used to advance fundamental understanding of surface or subsurface water resources systems or the interaction of these systems with the atmosphere, geosphere, biosphere, and human societies. Manuscripts involving case studies that do not attempt to reach broader conclusions, research on engineering design, applied hydraulics, or water quality and treatment, as well as applications of existing knowledge that do not advance fundamental understanding of hydrological processes, are not appropriate for Advances in Water Resources.
Examples of appropriate topical areas that will be considered include the following:
• Surface and subsurface hydrology
• Hydrometeorology
• Environmental fluid dynamics
• Ecohydrology and ecohydrodynamics
• Multiphase transport phenomena in porous media
• Fluid flow and species transport and reaction processes