To identify the crystalline structure, Fourier transform infrared (FTIR) spectroscopy in attenuated total reflection (ATR) mode Bruker Alpha II spectrometer with platinum ATR attachment and a diamond crystal was used. Spectra in the 400–1500 cm
−1 range with a resolution of 1 cm
−1 was collected to characterize the crystalline structure of the samples. The degree of β crystallinity phase in the samples was calculated as follows (Cai et al., 2017 (
link); Xin et al., 2018 (
link); Kaspar et al., 2020 (
link)) the degree was calculated using Eq.
1:
where Aα and Aβ are the absorbance values at 763 cm
−1 (CH
2 in-plane bending or rocking and CF
2 bending and skeletal bending) and 840 cm
−1 (CH
2 rocking and CF
2 asymmetrical stretching), respectively.
To confirm the crystalline structure, X-ray diffractometer (XRD) X'Pert Pro PANalytical equipped with Cu/Kα radiation (wavelength 0.15418 nm) in the 2θ range of 0°–50° at a scanning speed of 0.1°/min, was used and crystalline content was analysed according to Eq.
2:
where the Iα, Iγ, and Iβ correspond to the intensity peaks of the α, γ, and β phases, respectively. The XRD peaks for the monoclinic α phase are 18.7° (020), 19.8° (110), and 26.5° (021), while the 20.7° (110/200), 36.6° (101) and 56° (221) peaks correspond to the orthorhombic β phase peak, and the γ phase peak can be attributed to 40° (002) (Cai et al., 2017 (
link); Xin et al., 2018 (
link); Kaspar et al., 2020 (
link)):
The average crystallite size (D) was identified using the Scherrer using Eq.
3:
where λ is the wavelength of 1.54 Å, B is the Full Width at Half Maximum (FWHM), θ is Bragg’s and K is a constant 0.94 [54]. The obtained data was analysed using the GraphPad Prism 10 software.