THE ROLE OF CO-UNITS IN POLYMER CRYSTALLIZATION AND MELTING - NEW INSIGHTS FROM STUDIES ON SYNDIOTACTIC POLY(PROPENE-CO-OCTENE)

Citation
G. Hauser et al., THE ROLE OF CO-UNITS IN POLYMER CRYSTALLIZATION AND MELTING - NEW INSIGHTS FROM STUDIES ON SYNDIOTACTIC POLY(PROPENE-CO-OCTENE), Macromolecules, 31(18), 1998, pp. 6250-6258
Citations number
14
Categorie Soggetti
Polymer Sciences
Journal title
ISSN journal
00249297
Volume
31
Issue
18
Year of publication
1998
Pages
6250 - 6258
Database
ISI
SICI code
0024-9297(1998)31:18<6250:TROCIP>2.0.ZU;2-#
Abstract
The effect of noncrystallizable units on the crystallization and melti ng was studied for two octene copolymers of syndiotactic polypropylene , in an extension of previous investigations on a homopolymer sample w ith 3% meso dads. Using time and temperature dependent SAXS experiment s and DSC, we determined the dependencies of the crystal thickness, th e rate of crystallization, and the melting point on the chosen crystal lization temperature. With an increase in the content of noncrystalliz able units (octene units or meso dads; both show equal effects), we ob served, as expected, a shift of the melting points to lower temperatur es and similar shifts of the growth rate versus temperature curves, bu t surprisingly, no effect at all on the crystal thickness. The thickne sses of all three samples show a common temperature dependence, being inversely proportional to the supercooling below the equilibrium melti ng point of perfect syndiotactic polypropylene. The latter is located at 196 degrees C, as determined by an extrapolation based on measured melting points. Data demonstrate that the popular Hoffman-Weeks plot w hen applied to random copolymers does not yield the respective equilib rium melting points; it can only be used for perfect homopolymers. Cry stal thicknesses and growth rates are, according to the observations, independent properties. The thicknesses are those of a specific native crystal form with high surface free energy. DSC experiments indicate that all crystals first form this native state and then become stabili zed by relaxation processes that decrease the surface energy. These st abilization processes, which produce the difference between the temper atures of crystallization and melting, leave the crystallite thickness unchanged.