Abstract
AbstractThe high‐pressure crystallization of polyethylene in a diamond cell has been studied by infrared spectroscopy. The splitting of the CH2 rocking band at 720–730 cm−1 as a function of pressure was analyzed. It was found that pressure alone up to 3 kbar will not change the distance between methylene groups in the unit cell. However, this distance can be shortened by crystallization at this pressure. Intensities of selected crystalline (1176 and 1050 cm−1) and amorphous (1303, 1352, and 1368 cm−1) bands were measured on samples before and after high‐pressure crystallization, and also on samples of various densities crystallized under atmospheric pressure. The increase in the intensities of crystalline bands and concomitant decrease in amorphous bands, together with density changes, indicate that the crystallinity can be enhanced by crystallization under high pressure. Nevertheless, the crystallinity of polyethylene crystallized at high pressure is comparable with that of polyethylene crystallized at atmospheric pressure at low undercooling for long periods of time.
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