• journal_title：American Mineralogist
• Contributor：P.S.R. Prasad ; V. Krishna Chaitanya ; K. Shiva Prasad ; D. Narayana Rao
• Publisher：Mineralogical Society of America
• Date：2005-
• Format：text/html
• Language：en
• Identifier：10.2138/am.2005.1742
• journal_abbrev：American Mineralogist
• issn：0003-004X
• volume：90
• issue：4
• firstpage：672
• section：Articles

d="p-1">The dehydration mechanism of natural single crystals of gypsum was investigated in the temperature range 300–430 K by in situ infrared (FTIR) spectroscopy. The thermal evolution of the second-order modes of H₂O and SO₄ groups in gypsum, in the wavenumber range 4850–5450 cm⁻¹ and 2050–2300 cm⁻¹ respectively, were used to probe the dehydration and rehydration sequence. A total disappearance of the combination modes of H₂O and the replacement of four SO₄⁻² bands (2245, 2200, 2133, and 2117 cm⁻¹) observed at room temperature by three bands (2236, 2163, and 2131 cm⁻¹) observed at 390 K indicates the direct formation of γ-CaSO₄ upon heating. Upon cooling water re-enters into the γ-CaSO₄ structure at around 363 K to form bassanite. This observation, that the dehydration of gypsum directly yields γ-CaSO₄ (anhydrite) without the intermediate formation of hemi-hydrate (bassanite), is further corroborated by the dehydration behavior of bassanite. The second-order SO₄ modes of bassanite observed around 2218, 2136, and 2096 cm⁻¹ were replaced with the bands of γ-CaSO₄ at about 378 K upon heating.