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Volumn 53, Issue 1, 1996, Pages 825-837

Experimental study of surface segregation and wetting in films of a partially miscible polymer blend

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EID: 0001683340     PISSN: 1063651X     EISSN: None     Source Type: Journal    
DOI: 10.1103/PhysRevE.53.825     Document Type: Article
Times cited : (35)

References (79)
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    • PalphaMS is known to degrade upon pyrolysis yielding only monomer [47] and in order to check its temperature stability we carried out the following tests. Gel permeation chromatography (GPC) was performed on some PalphaMS (MW equal to 97 600) before and after annealing at 180 °C for a day. The result indicated negligible molecular weight degradation of the PalphaMS on annealing [48]. A thermal gravimetric analysis (TGA) experiment also indicated that the polymer was stable, with respect to decomposition to monomer, under annealing, since negligible mass change was observed after 16.5 h at 185 °C.
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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.
    • 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.
    • 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.
    • 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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