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Large apparent interfacial slippage at polyelectrolyte-perfluorocarbon interfaces on a quartz crystal resonator
Mikko Salomäki1, Jouko Kankare
1Department of Chemistry, University of Turku, FIN-20014 Turku, Finland.
Langmuir : the ACS Journal of Surfaces and Colloids
|August 25, 2004
Summary
Interfacial slippage between polyelectrolyte multilayers and perfluorocarbon liquids causes apparent negative mass densities. The de Gennes model, involving a gas layer, best explains this phenomenon, though other models were considered.
Area of Science:
- Materials Science
- Physical Chemistry
- Surface Science
Background:
- Quartz crystal resonators are sensitive to mass loading.
- Polyelectrolyte multilayers exhibit complex interactions with liquids.
- Apparent negative areal mass densities suggest phenomena beyond simple mass addition.
Purpose of the Study:
- To explain the observed negative areal mass densities in polyelectrolyte multilayer systems.
- To investigate the role of interfacial slippage in resonator measurements.
- To compare different physical models of interfacial slippage.
Main Methods:
- Utilized quartz crystal resonator measurements in contact with perfluorocarbon liquids.
- Modeled the interfacial slippage zone as a distinct layer with physical parameters.
- Analyzed three slippage models: de Gennes (gas cavity), water layer, and true slipping (velocity discontinuity).
- Calculated slippage admittances, slippage lengths, and corrected areal mass densities.
Main Results:
- Interfacial slippage was identified as the cause of apparent negative areal mass densities.
- All three models provided calculated parameters, but with varying degrees of fit.
- The de Gennes model showed slightly less variation in calculated parameters, suggesting greater credibility.
Conclusions:
- Interfacial slippage is a critical factor in interpreting quartz crystal resonator data for multilayers in liquids.
- The de Gennes model offers a plausible explanation for the observed phenomenon.
- Further experimental validation is needed to definitively favor one slippage model.