Dispersion of a gyrotactic micro-organism suspension in a vertical pipe: the buoyancy-flow coupling effect

被引:4
|
作者
Wang, Bohan [1 ]
Jiang, Weiquan [2 ]
Chen, Guoqian [1 ,2 ]
机构
[1] Peking Univ, Coll Engn, Lab Syst Ecol & Sustainabil Sci, Beijing 100871, Peoples R China
[2] Macau Univ Sci & Technol, Macao Environm Res Inst, Macau 999078, Peoples R China
基金
中国国家自然科学基金; 中国博士后科学基金;
关键词
micro-organism dynamics; suspensions; GENERALIZED TAYLOR DISPERSION; SWIMMING MICROORGANISMS; ORIENTATION DISTRIBUTION; BIOCONVECTION; SOLUTE; MODEL;
D O I
10.1017/jfm.2023.279
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
Understanding the transport of micro-organisms in pipes is crucial to many fundamental problems, such as bioconvection and biodiesel production. In this work, we investigate the velocity profile and dispersion of a suspension of negatively buoyant, gyrotactic micro-organisms in a vertical pipe. With an imposed flow rate, the non-uniform radial cell concentration typical of gyrotaxis distorts the simple Poiseuille flow through inhomogeneous buoyancy, which in turn affects the cell concentration distribution. By solving the fundamental Smoluchowski equation and the Navier-Stokes equation simultaneously, we account for this bidirectional buoyancy-flow coupling effect. Asymptotic dispersion coefficients, namely, drift velocity and dispersivity, are further calculated with the obtained radial velocity and cell concentration profiles, which are assumed to be steady, symmetric and axially invariant. Using the gyrotactic micro-organism Chlamydomonas augustae as an example, detailed results are given to illustrate the effect of buoyancy-flow coupling. In downwelling flows, the buoyancy-flow coupling effect intensifies with the Richardson number Ri quantifying the mean cell concentration, but is strongest at a moderate flow strength. The buoyancy-flow coupling effect significantly enhances the velocity and cell concentration in the central region, as well as the drift velocity and dispersivity. In contrast, the buoyancy-flow coupling effect is comparatively limited in upwelling flows, due to the dominant influence of the no-slip boundary condition imposed at the wall. Comparisons with predictions of existing approximate models are also presented.
引用
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页数:25
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