Optical absorption, EPR, Infrared and Raman spectral studies have been carried out on natural clinochlore mineral. The optical absorption spectrum exhibits bands characteristic of Fe 2+ and Fe 3+ ions. A band observed in the NIR region is attributed to an intervalence charge transfer (Fe 2+–Fe 3+) band. The room temperature EPR spectrum of single crystal of clinochlore mineral reveals the dominance of Fe 3+ ion exhibiting resonance signals at g=2.66; 3.68 and 4.31 besides one isotropic resonance signal at g=2.0. The EPR studies have been carried out for a polycrystalline sample in the temperature range from 103 to 443 K and for a single crystal of clinochlore mineral in the temperature range 123–297 K. The number of spins ( N) participating in resonance at g=4.3 signal of the single crystal of clinochlore mineral has been calculated at different temperatures. The paramagnetic susceptibility ( χ) is calculated from the EPR data at different temperatures for single crystal of clinochlore mineral. The Curie constant and Curie temperature values are evaluated from 1/ χ versus T graph. The infrared spectral studies reveal the formation of Fe 3+–OH complexes due to the presence of higher amount of iron in this mineral. The Raman spectrum exhibits bands characteristic of Si–O–Si stretching and Si–O bending modes.
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