Orientational deformations leading to temperature-induced structural phase transition in Prehnite using Raman, Infrared, and Terahertz spectroscopy.

[Display omitted] • Reported high-temperature Raman, infrared, Terahertz studies on Prehnite mineral. • Orientational change of AlO 6 octahedra & SiO 4 tetrahedra breaks symmetry at 800 °C. • Extinction of Raman & abrupt change of FIR modes confirm symmetry change at 800 °C. • Spectral changes supported by XRD studies indicate structural phase transition. Understanding molecular and structural properties of naturally extracted minerals under varying thermodynamic parameters such as pressure (P) and temperature (T) helps us to explore vital information regarding various geological processes. Here, we present the comprehensive results of Raman, infrared (IR), and Terahertz (THz) spectroscopic investigations on Prehnite (Ca 2 Al(AlSi 3 O 10)(OH) 2) mineral from ambient (25 °C) to 1000 °C in the 6.6 – 4000 cm−1 wide spectral range. The results indicate a substantial distortion in orientation between AlO 6 octahedron and SiO 4 tetrahedron layer leads to the strengthening of hydrogen bonds (HBs) in the Prehnite structure around 800 °C. Consequently, the disappearance of Raman active modes and abrupt change in frequency (ω) of Far-IR modes (obtained using THz spectroscopy) around 800 °C are spectral signatures of symmetry change in the structure. Eventually, these orientational changes at the molecular level trigger structural phase transition around 800 °C, supported by X-ray diffraction (XRD) measurements. Thus, the present study depicts the pivotal role of inter- and intra-molecular interactions in Prehnite, which determines its bonding and structural characteristics and hence its physicochemical properties under diverse environments. [ABSTRACT FROM AUTHOR]