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Studies of cyclic and linear poly(dimethyl siloxanes): 5. Diffusion behaviour in dilute solution
Authors:CJC Edwards  RFT Stepto  JA Semlyen
Affiliation:1. Department of Chemistry, University of York, Heslington, York YO1 5DD, UK;2. Department of Polymer and Fibre Science, The University of Manchester Institute of Science and Technology (UMIST), Manchester M60 1QD, UK
Abstract:The diffusion coefficients of cyclic and linear oligomeric and polymeric dimethyl siloxanes, containing number-average numbers of skeletal bonds in the range 6 < n?n < 650, have been measured in toluene solution at 298K. Impermeable diffusion behaviour was observed for all the siloxanes studied, in agreement with previous findings for ethylene oxide and hexamethylene oxide oligomers and polymers. The ratio of the friction coefficients frfl for the ring (r) and linear (l) dimethyl siloxanes was found to be 8 (within the limits of experimental error) over the whole range of molecular weights studied. Values of the expansion factor αf for the linear poly(dimethyl siloxanes) (obtained from the diffusion measurements) were found to be approximately equal to the corresponding values for αη (found previously by viscometric studies) for small values of the excluded volume parameter z; and αf was larger than αη for large z, as predicted by first-order perturbation theory. Mean-square radii of gyration 〈s2G〉 were calculated from the diffusion data for both cyclic and linear poly(dimethyl siloxanes) assuming Gaussian statistics, and found to be in good agreement with the corresponding values obtained by neutron scattering. However, the values of 〈s2G,l〉 for the short chain poly(dimethyl siloxanes) did not agree with the corresponding values of 〈s2O,l〉, calculated using the rotational isomeric state model of Flory, Crescenzi and Mark. This discrepancy is thought to arise from deviations from Gaussian behaviour, and considerably better agreement between experiment and theory was achieved by using appropriate values of a function ψl(x), which relates radii of gyration and impermeable hydrodynamic diffusion radii.
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