Determination of the hydrogen positions in the sulphate mineral Bloedite
High-pressure synchrotron X-ray experiments on the mineral Bloedite have shown that dehydration does not occur under pressure, and that rather surprisingly, there is no phase transition up to 14GPa. This mineral may be widely distributed in the crust of icy satellites, such as the satellites of Jupiter. We wish to determine accurately the H-atom positions, and whether they are ordered or disordered, in this intriguing mineral, at room temperature and at lower temperatures, and for this we ask for 6 days on D19.
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KATERINOPOULOU Anna; Balic-Zunic Tonci; COMODI Paola and MASON, Sax A.. (2013). Determination of the hydrogen positions in the sulphate mineral Bloedite. Institut Laue-Langevin (ILL) doi:10.5291/ILL-DATA.5-11-404
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