Effect of Particle Thermophoresis on Convection of Magnetic Fluids in Narrow Channels Heated from Below

IF 1 4区 工程技术 Q4 MECHANICS Fluid Dynamics Pub Date : 2023-05-02 DOI:10.1134/S0015462822601863
A. F. Glukhov, A. S. Sidorov
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Abstract

The effect of positive thermodiffusion of colloidal particles under convection of magnetic fluids in connected vertical channels of 3.2 × 3.2 mm2 square cross-section and height 50 mm heated from below is analyzed. Below the critical Rayleigh number, particle thermophoresis in vertical generates unstable density stratification in fluid at rest. This leads to rapid bursts (~1 min) of concentration convection arising periodically (~4 h). Under developed convection, above the critical Rayleigh number particle thermophoresis in horizontal direction generates concentration inhomogeneities in the neighborhood of the channel walls and provokes convective flow instability that leads to the periodic change (~1 h) in the direction of convective stream. The reasons of the oscillatory instability of mechanical equilibrium observed experimentally at positive sign of the Soret coefficient are discussed.

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颗粒热泳动对从下加热的狭窄通道中磁流体对流的影响
分析了从下加热的3.2 × 3.2 mm2平方截面、高度为50mm的连通垂直通道中,在磁流体对流作用下胶体颗粒正热扩散的影响。低于临界瑞利数,颗粒在垂直方向上的热泳运动在静止流体中产生不稳定的密度分层。这导致浓度对流周期性(~4 h)快速爆发(~1 min)。在对流不发达的情况下,高于临界瑞利数的颗粒在水平方向上的热泳现象在通道壁面附近产生浓度不均匀性,引起对流不稳定,导致对流方向周期性变化(~1 h)。讨论了索莱特系数为正号时实验观察到的力学平衡振荡不稳定的原因。
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来源期刊
Fluid Dynamics
Fluid Dynamics MECHANICS-PHYSICS, FLUIDS & PLASMAS
CiteScore
1.30
自引率
22.20%
发文量
61
审稿时长
6-12 weeks
期刊介绍: Fluid Dynamics is an international peer reviewed journal that publishes theoretical, computational, and experimental research on aeromechanics, hydrodynamics, plasma dynamics, underground hydrodynamics, and biomechanics of continuous media. Special attention is given to new trends developing at the leading edge of science, such as theory and application of multi-phase flows, chemically reactive flows, liquid and gas flows in electromagnetic fields, new hydrodynamical methods of increasing oil output, new approaches to the description of turbulent flows, etc.
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