Hysteretic wetting and dewetting of a thin sheet peeling off a liquid interface
ORAL
Abstract
We peel a thin polymeric sheet on and off an air-water interface with controlled velocity.
Under near-quasistatic conditions, measuring the force of peeling allows us to obtain contact
angles via force balance at various scales, as we have shown in prior work. This configuration
allows us to determine the local wetting angle at the 3-phase contact line between air, water
and sheet, and characterize the time-dependent wetting dynamics with higher temporal and
force resolution than is possible with imaging. In pulling up or pushing down the sheet, we find
that the contact line does not slip until we reach an angle close to the receding or advancing
contact angles, respectively. This point at which slip occurs is reproducible and independent of
velocity, while the final advancing or receding angle has a weak dependence on the speed of
peeling. Beyond this point, there is a steady state characterized by slipping and fluctuations of
the contact line. On stopping the peeling process, the contact angle relaxes very slowly to
equilibrium, with a time dependence that depends on whether the relaxation is from advancing
or receding conditions, also depending weakly on the speed of peeling. Repeated loops of
wetting and dewetting retain details of microscopic noise structure, which we identify as elastic
events occurring due to forcing at the contact line.
Under near-quasistatic conditions, measuring the force of peeling allows us to obtain contact
angles via force balance at various scales, as we have shown in prior work. This configuration
allows us to determine the local wetting angle at the 3-phase contact line between air, water
and sheet, and characterize the time-dependent wetting dynamics with higher temporal and
force resolution than is possible with imaging. In pulling up or pushing down the sheet, we find
that the contact line does not slip until we reach an angle close to the receding or advancing
contact angles, respectively. This point at which slip occurs is reproducible and independent of
velocity, while the final advancing or receding angle has a weak dependence on the speed of
peeling. Beyond this point, there is a steady state characterized by slipping and fluctuations of
the contact line. On stopping the peeling process, the contact angle relaxes very slowly to
equilibrium, with a time dependence that depends on whether the relaxation is from advancing
or receding conditions, also depending weakly on the speed of peeling. Repeated loops of
wetting and dewetting retain details of microscopic noise structure, which we identify as elastic
events occurring due to forcing at the contact line.
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Presenters
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Nuoya Zhou
University of Massachusetts Amherst
Authors
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Nuoya Zhou
University of Massachusetts Amherst