Shock-driven jamming and periodic fracture of particulate rafts

A tenuous monolayer of hydrophobic particles at the air-water interface often forms a scum or raft. When such a monolayer is disturbed by the localized introduction of a surfactant droplet, a radially divergent surfactant shock front emanates from the surfactant origin and packs the particles into a...

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Bibliographic Details
Published in:Europhysics letters Vol. 96; no. 3; p. 36008
Main Authors: Bandi, M. M, Tallinen, T, Mahadevan, L
Format: Journal Article
Language:English
Published: IOP Publishing 01-11-2011
EPS, SIF, EDP Sciences and IOP Publishing
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Summary:A tenuous monolayer of hydrophobic particles at the air-water interface often forms a scum or raft. When such a monolayer is disturbed by the localized introduction of a surfactant droplet, a radially divergent surfactant shock front emanates from the surfactant origin and packs the particles into a jammed, compact, annular band with a packing fraction that saturates at a peak packing fraction φ*. As the resulting two-dimensional, disordered elastic band grows with time and is driven radially outwards by the surfactant, it fractures to form periodic triangular cracks with robust geometrical features. We find that the number of cracks N and the compaction band radius R* at fracture onset vary monotonically with the initial packing fraction (φinit). However, the compaction band's width W* is constant for all φinit. A simple geometric theory that treats the compaction band as an elastic annulus, and accounts for mass conservation allows us to deduce that N≃2πR*/W*≃4πφRCP/φinit, a result we verify both experimentally and numerically. We show that the essential ingredients for this phenomenon are an initially low enough particulate packing fraction that allows surfactant-driven advection to cause passive jamming and eventual fracture of the hydrophobic particulate interface.
Bibliography:istex:8FC5FCDC740AEDEA2F58A1FCB67ED63674E063BB
publisher-ID:epl13954
ark:/67375/80W-Z36SFGZT-1
ISSN:0295-5075
1286-4854
DOI:10.1209/0295-5075/96/36008