Kurihara Takashi, Aridome Msato, Ayade Heev, Zaid Irwin, Mizuno Daisuke
Kyushu University, Fukuoka 812-8581, Japan.
Rudolf Peierls Center for Theoretical Physics, University of Oxford, Oxford OX1 3NP, United Kingdom.
Phys Rev E. 2017 Mar;95(3-1):030601. doi: 10.1103/PhysRevE.95.030601. Epub 2017 Mar 9.
We investigate the hydrodynamic fluctuations in suspensions of swimming microorganisms (Chlamydomonas) by observing the probe particles dispersed in the media. Short-term fluctuations of probe particles were superdiffusive and displayed heavily tailed non-Gaussian distributions. The analytical theory that explains the observed distribution was derived by summing the power-law-decaying hydrodynamic interactions from spatially distributed field sources (here, swimming microorganisms). The summing procedure, which we refer to as the physical limit operation, is applicable to a variety of physical fluctuations to which the classical central limiting theory does not apply. Extending the analytical formula to compare to experiments in active swimmer suspensions, we show that the non-Gaussian shape of the observed distribution obeys the analytic theory concomitantly with independently determined parameters such as the strength of force generations and the concentration of Chlamydomonas. Time evolution of the distributions collapsed to a single master curve, except for their extreme tails, for which our theory presents a qualitative explanation. Investigations thereof and the complete agreement with theoretical predictions revealed broad applicability of the formula to dispersions of active sources of fluctuations.
我们通过观察分散在介质中的探针粒子来研究游动微生物(衣藻)悬浮液中的流体动力学涨落。探针粒子的短期涨落是超扩散的,并且呈现出重尾非高斯分布。通过对来自空间分布场源(此处为游动微生物)的幂律衰减流体动力学相互作用进行求和,推导出了解释观测分布的解析理论。我们将这种求和过程称为物理极限运算,它适用于经典中心极限理论不适用的各种物理涨落。将解析公式扩展以与活性游动体悬浮液中的实验进行比较,我们表明观测分布的非高斯形状与诸如力产生强度和衣藻浓度等独立确定的参数同时符合解析理论。除了其极端尾部外,分布的时间演化塌缩为一条单一的主曲线,我们的理论对此给出了定性解释。对其进行研究并与理论预测完全一致,揭示了该公式对涨落活性源分散体系具有广泛的适用性。