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arXiv 2602.08049cond-mat.soft
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运动可逆性下胶体悬浮液的连续统统计动力学

Continuum-statistical dynamics of colloidal suspensions under kinematic reversibility

International School Michel Lucius(米歇尔·卢修斯国际学校)

Jerome Burelbach

AI总结:

提出线性响应理论,通过洛伦兹互易定理在运动可逆性下的应用,建立胶体运动中昂萨格互易性的连续统力学起源,并推导出胶体扩散的所有非平衡贡献。

摘要:

我们提出一个线性响应理论,建立了胶体运动中昂萨格互易性的连续统力学起源。通过解耦静水应力和流体动力应力,我们证明了当洛伦兹互易定理在运动可逆性下应用于胶体沉降的辅助流动问题时,昂萨格互易关系出现。我们的框架适用于包含多种微粒种类的悬浮液,并通过单次应用洛伦兹互易定理推导出胶体扩散的所有非平衡贡献,无论胶体表面施加滑移还是无滑移流体动力边界条件。此外,边界层处理仅假设用于纤毛运动,而产生非平衡热力学运动的静水压力在边界层近似之外被完全解析。特别地,我们的框架与通过半透膜的经典渗透一致,其中流体流动在没有界面势相互作用的情况下发生。对于由于溶质的体积排斥引起的扩散泳,我们的结果因此预测对于薄的体积排斥层,胶体向更高溶质浓度运动,而对于较长程、中等排斥势,则恢复相反趋势。

英文摘要:

We present a linear response theory that establishes the continuum-mechanical origin of Onsager reciprocity in colloidal motion. By decoupling hydrostatic and hydrodynamic stress, we show that Onsager reciprocal relations emerge when the Lorentz reciprocal theorem is applied under kinematic reversibility to the auxiliary flow problem of colloidal sedimentation. Our framework applies to suspensions containing multiple species of microparticles and derives all non-equilibrium contributions to colloidal diffusion from a single application of the Lorentz reciprocal theorem, irrespective of whether a slip or no-slip hydrodynamic boundary condition is imposed at the colloidal surface. Furthermore, a boundary-layer treatment is only assumed for ciliary motion, while the hydrostatic forces giving rise to non-equilibrium thermodynamic motion are fully resolved beyond the boundary-layer approximation. In particular, our framework is consistent with classical osmosis through a semi-permeable membrane, where fluid flow occurs without interfacial potential interactions. For diffusiophoresis due to volume exclusion of a solute, our results therefore predict colloidal motion towards higher solute concentration for thin excluded-volume layers, whereas the opposite trend is recovered for longer-ranged, moderately repulsive potentials.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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