The Spatial Correlation between Crystalline and Amorphous Orientations of Isotactic Polypropylene during Plastic Deformation: An in situ Observation with FTIR Imaging
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The Spatial Correlation between Crystalline and Amorphous Orientations of Isotactic Polypropylene during Plastic Deformation: An in situ Observation with FTIR Imaging
Chinese Journal of Polymer ScienceVol. 33, Issue 4, Pages: 613-620(2015)
Affiliations:
National Synchrotron Radiation Lab and College of Nuclear Science and Technology, CAS Key Laboratory of Soft Matter Chemistry, University of Science and Technology of China, Hefei 230009, China
Wei Chen, Xiang-yang Li, Yan-ping Liu, et al. The Spatial Correlation between Crystalline and Amorphous Orientations of Isotactic Polypropylene during Plastic Deformation: An in situ Observation with FTIR Imaging[J]. Chinese Journal of Polymer Science, 2015, 33(4): 613-620. DOI: 10.1007/s10118-015-1613-3.
DOI:
Wei Chen, Xiang-yang Li, Yan-ping Liu, et al. The Spatial Correlation between Crystalline and Amorphous Orientations of Isotactic Polypropylene during Plastic Deformation: An in situ Observation with FTIR Imaging[J]. Chinese Journal of Polymer Science, 2015, 33(4): 613-620. DOI: 10.1007/s10118-015-1613-3.DOI:
The Spatial Correlation between Crystalline and Amorphous Orientations of Isotactic Polypropylene during Plastic Deformation: An in situ Observation with FTIR Imaging
we made a heterogeneous thin film of isotactic polypropylene (
i
PP) that contains a few large spherulites (~150 μm) which are surrounded by small spherulites (~15 μm) for tensile testing. The evolution processes of crystalline and amorphous orientations of
i
PP are monitored with its characteristic peaks at 998 and 973 cm
-1
respectively. By introducing the correlation images
the analysis demonstrates the relationships between the orientation evolutions of crystalline and amorphous phases in a space of 250 μm × 250 μm detecting area. During the plastic deformation
crystalline orientation is higher than amorphous orientation outside the large spherulite
while that is opposite inside the region. In addition
the evolutions of crystalline and amorphous orientations almost keep a positive correlation.
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