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We have performed similar experiments with polystyrene particles in the presence of non-adsorbing polymer. In this case, the system does not cream but rather sediments along the gravitational direction; as a result there are no depletion interactions with the upper liquid-air interface. Consistent with this, we find no delay time
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We have performed similar experiments with polystyrene particles in the presence of non-adsorbing polymer. In this case, the system does not cream but rather sediments along the gravitational direction; as a result there are no depletion interactions with the upper liquid-air interface. Consistent with this, we find no delay time.
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15
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60049083735
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The fraction for gelation is taken from [8, which contains the phase diagram for our experimental system
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The volume fraction for gelation is taken from [8], which contains the phase diagram for our experimental system.
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16
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84864156867
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The length scale of a pixel in one of our images is 10 μm. We thus expect that the structure of the colloidal suspension should not greatly affect the transmission through the sample. We also assume that contributions arising from the scattering from other parts of the cell are negligible compared to the transmission [17
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The length scale of a pixel in one of our images is 10 μm. We thus expect that the structure of the colloidal suspension should not greatly affect the transmission through the sample. We also assume that contributions arising from the scattering from other parts of the cell are negligible compared to the transmission [17].
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19
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A.D. Dinsmore, V. Prasad, I. Wong, D.A. Weitz, Phys. Rev. Lett. 96, 185502 (2007).
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Dinsmore, A.D.1
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20
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60049087990
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In the initial compression stages, the gel does not change appreciably its fraction. As a result, the elastic stress gradient in equation (9) can be neglected. The initial stages are thus determined by the balance between the gravitational and frictional stress gradients. This is used to determine the initial permeability of the gel from the slope of the interface evolution with time. See [4] for further details
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In the initial compression stages, the gel does not change appreciably its volume fraction. As a result, the elastic stress gradient in equation (9) can be neglected. The initial stages are thus determined by the balance between the gravitational and frictional stress gradients. This is used to determine the initial permeability of the gel from the slope of the interface evolution with time. See [4] for further details.
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