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We estimate the reptation time from the ratio [Formula Presented]approx [Formula Presented]/[Formula Presented] using a value of [Formula Presented], the d-PS tracer diffusion coefficient, of app [Formula Presented] cm[Formula Presented] s[Formula Presented] obtained from interdiffusion coefficient measurements on this blend [66]. Direct measurements of [Formula Presented] on different d-PS–PalphaMS blends [70] further corroborate this result.
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We estimate the reptation time from the ratio τrepapprox Rg2/Dstar using a value of Dstar, the d-PS tracer diffusion coefficient, of app 10-13 cm2 s-1 obtained from interdiffusion coefficient measurements on this blend [66]. Direct measurements of Dstar on different d-PS–PalphaMS blends [70] further corroborate this result.
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We have approximated the concentration gradient to [ [Formula Presented]- [Formula Presented]([Formula Presented])]/ (2 sqrt Dt ). This is equivalent to replacing the depletion layer depicted in Fig. 12 by a uniform gradient decreasing linearly to [Formula Presented] from [Formula Presented] over a length 2 sqrt Dt. The factor of 2 is necessary for conservation of material.
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We have approximated the concentration gradient to [ φm- φd(zstar)]/ (2 sqrt Dt ). This is equivalent to replacing the depletion layer depicted in Fig. 12 by a uniform gradient decreasing linearly to φd from φm over a length 2 sqrt Dt. The factor of 2 is necessary for conservation of material.
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In this article the domains considered are rich in the nonwetting phase. There is no reason, however, to suppose that such anisotropic domains do not exist in our experiments, nor that they do not affect the growth of the wetting layer.
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In this article the domains considered are rich in the nonwetting phase. There is no reason, however, to suppose that such anisotropic domains do not exist in our experiments, nor that they do not affect the growth of the wetting layer.
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