Persistence of Coffee-Ring Deposits in Concentrated Suspensions of Anisotropic Colloids
Samuel S. Nielsen, Ryker Fish, Brian C. Seper, Brennan Sprinkle, and Michelle M. Driscoll

TL;DR
This study investigates how physical parameters like particle concentration and sedimentation velocity influence coffee-ring deposit formation, revealing that particle shape does not significantly affect the phenomenon.
Contribution
The paper demonstrates that coffee-ring formation is primarily governed by sedimentation velocity rather than particle anisotropy, supported by experiments and hydrodynamic simulations.
Findings
Coffee-ring formation is independent of particle anisotropy.
Deposit geometry is controlled by the ratio of sedimentation velocity to evaporation interface velocity.
Hydrodynamic simulations accurately estimate sedimentation velocities.
Abstract
Evaporating a droplet containing dispersed colloids leaves behind a dried deposit whose shape is determined by capillary flows and the resulting particle transport. The classical coffee-ring effect occurs when an outward radial flow drives particles toward the droplet's contact line as the droplet evaporates, resulting in uneven deposition. This deposition is often studied in dilute concentration regimes where, hydrodynamically, the effects of particle shape are unimportant. As particle concentration increases, it is expected that particle anisotropy should play a larger role in modifying transport and potentially suppressing coffee-ring formation. We present experiments isolating the effects of particle shape, concentration, and density, as well as solvent temperature, on the geometry of the ring deposit. By analyzing the deposits using surface profilometry to more accurately…
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