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- W2120142216 abstract "Chrysotile, a variety of serpentine minerals has been investigated through optical absorption and EPR studies. High magnification electron micrographs have shown the existence of a tube-like structure of the layers. The optical absorption indicated the presence of Fe2+ and Fe3+ ions. The bands at 10,989, 11,111, 15,873 19,608, 22,727 and 26,316 cm− 1 we assigned to Fe3+ and the other bands at 9260, 10,526, 11,628, 12,048 and 21,739 cm− 1 Fe2+. The g-values indicated that Fe3+ have entered in to the lattice by replacing Mg2+ ions. The IR spectrum of trioctahedral chrysotile shows two bands at 3694 and 3648 cm− 1 in the OH stretching region. This sample was highly disordered as reflected by the X-ray diffraction pattern." @default.
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- W2120142216 date "2008-12-01" @default.
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- W2120142216 title "Structural analysis, optical absorption and EPR spectroscopic studies on chrysotile" @default.
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- W2120142216 doi "https://doi.org/10.1016/j.clay.2008.01.011" @default.
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