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3, 0.15%; CaO, 15.1%; MgO, 19.2%) reveals that the clay he used must have been a trioctahedral mineral (very low content in aluminum), very likely hectorite (the natural equivalent of Laponite). Such a mineral is classically associated with calcium carbonate impurities, which explains the high content in CaO. In view of this high amount of impurity and considering the known chemical instability of hectorite, the assignment of the observed phase transition could be questionable.
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0011294442
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Further information on the experimental setup can be found on the web at the address
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Further information on the experimental setup can be found on the web at the address http://www.esrf.fr/exp_facilities/ID21/.
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