Abstract.
Shock wave induced response of the berlinite form of FePO\(_4\) has been investigated up to 8.5 GPa. The X-ray diffraction measurements on the shock recovered samples reveal transition to the mixture of an amorphous phase and an orthorhombic phase around 5 GPa. The proportion of the amorphous material in the recovered sample is found to decrease at higher pressure. The results are interpreted in terms of a three-level free energy diagram for the crystal to amorphous transitions.
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Received 26 May 1997 / Accepted 1 September 1997
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Joshi, K., Suresh, N., Jyoti, G. et al. Shock wave induced phase transition in \(\alpha\)-FePO\(_4\) . Shock Waves 8, 173–176 (1998). https://doi.org/10.1007/s001930050110
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DOI: https://doi.org/10.1007/s001930050110