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线性密度分层流体中游泳微生物之间的流体动力学相互作用。

Hydrodynamic interactions between swimming microorganisms in a linearly density stratified fluid.

作者信息

More Rishabh V, Ardekani Arezoo M

机构信息

School of Mechanical Engineering, Purdue University, West Lafayette, Indiana 47907, USA.

出版信息

Phys Rev E. 2021 Jan;103(1-1):013109. doi: 10.1103/PhysRevE.103.013109.

Abstract

Oceans and lakes sustain intense biological activity due to the motion of marine organisms, which has significant ecological and environmental impacts. The motion of individual organisms and their interactions with each other play a significant role in the collective motion of swimming organisms. However, ubiquitous vertical density stratification in these aquatic environments significantly alters the swimmer interactions as compared to in a homogeneous fluid. Furthermore, organisms have sizes varying over a wide range which results in finite inertia. To this end, we numerically investigate the interactions between a pair of model swimming organisms in two configurations: (1) approaching each other and (2) moving side by side with finite inertia in a linearly density stratified fluid. We use the archetypal reduced-order squirmer model to numerically model the swimming organisms. We present trajectories and the contact times of interacting squirmer (puller & pusher) pairs for different Re in the range 1-50 and Ri in the range 0-10. Depending on the squirmer Re and Ri we observe that the squirmer interactions can be categorized as (i) pullers getting trapped in circular loops at high Re and low Ri, (ii) pullers escaping each other with separating angle decreasing with increasing stratification at low Re and high Ri, (iii) pushers sticking to each other after the collision and deflecting away from the collision plane for either low Re or high Ri, (iv) pushers escaping otherwise with an angle of separation increasing with stratification. Stratification also increases the contact time for squirmer pairs. The presented results can be useful to understand the mechanisms behind the accumulation of planktonic organisms in horizontal layers in a stratified environment such as oceans and lakes.

摘要

由于海洋生物的运动,海洋和湖泊维持着强烈的生物活动,这对生态和环境有着重大影响。单个生物的运动及其相互作用在游泳生物的集体运动中起着重要作用。然而,与均匀流体相比,这些水生环境中普遍存在的垂直密度分层显著改变了游泳者之间的相互作用。此外,生物的大小范围很广,这导致了有限的惯性。为此,我们通过数值研究了一对模型游泳生物在两种配置下的相互作用:(1)相互靠近;(2)在具有线性密度分层的流体中以有限惯性并排移动。我们使用典型的降阶蠕动者模型对游泳生物进行数值建模。我们给出了不同雷诺数(Re)在1 - 50范围内和理查德森数(Ri)在0 - 10范围内相互作用的蠕动者(牵引者和推动器)对的轨迹和接触时间。根据蠕动者的Re和Ri,我们观察到蠕动者之间的相互作用可分为以下几类:(i)在高Re和低Ri时,牵引者被困在圆形回路中;(ii)在低Re和高Ri时,牵引者相互逃离,分离角度随分层增加而减小;(iii)对于低Re或高Ri,推动器在碰撞后相互粘连并偏离碰撞平面;(iv)否则,推动器以分离角度随分层增加的方式逃离。分层还增加了蠕动者对的接触时间。所呈现的结果有助于理解在海洋和湖泊等分层环境中浮游生物在水平层中聚集背后的机制。

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