In situ characterization of strain-induced crystallization of natural rubber by synchrotron radiation wide-angle X-ray diffraction: construction of a crystal network at low temperatures. Issue 4 (11th January 2019)

• Record Type: Journal Article
• Authors: Chen, Pinzhang; Zhao, Jingyun; Lin, Yuanfei; Chang, Jiarui; Meng, Lingpu; Wang, Daoliang; Chen, Wei; Chen, Liang; Li, Liangbin
• Is Part Of: Soft matter. Volume 15:Issue 4(2018)
• Page Start: 734
• Page End: 743
• Publication Date: 2019-01-11
• Subjects: Soft condensed matter -- Periodicals; 530.413
• DOI: 10.1039/c8sm02126k
• Languages: English
• ISSNs: 1744-683X

Abstract

Abstract : The structural evolution of NR during stretching at −40 °C and in the strain–temperature space. Abstract : Strain-induced crystallization (SIC) of natural rubber (NR) at descending temperatures as low as −60 °C is systematically investigated by in situ synchrotron radiation wide-angle X-ray diffraction (SR-WAXD) measurement. The detailed structural evolution of NR during SIC is studied in the strain–temperature space, where up to four regions are defined depending on the SR-WAXD results. In region I, the molecular chains begin to be oriented under tensile loading. The onset of crystallization happens in the very beginning of region II, and the NR crystal acts as a new physical cross-linking point to form a crystal network, namely the series model. The further increment of crystallinity (> ca. 8%) leads to the transition of the crystal network from the series model to the parallel model in region III. The crystal network is finally accomplished in region IV, where the crystallinity remains almost constant. Interestingly, regions III and IV exist only in the intermediate-temperature zone II (−40 °C to −10 °C), which are missing in zones I (−10 °C to 25 °C) and III (−60 °C to −40 °C). This suggests that sufficient crystallinity ( χ II–III > ca. 8%) is required to form the parallel model. The new crystal network provides a deep understanding of SIC of NR considering the microscopic features, i.e. oriented amorphous component, the onset of crystallization and crystallinity evolution and its correlation with the macroscopic stress–strain curve.