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Order-Disorder Effects in Minerals

If the various aluminosilicate units present in a mineral can be resolved sufficiently for their relative populations to be simulated, the Al-for-Si disorder can in principle be determined. In practice, the resonances from the various structural units often overlap, making it necessary to deconvolute the broad spectral envelope by curve-fitting procedures. Gaussian peaks are most commonly fitted, since they allow good visual fits to [Pg.208]

Determination of the distribution of Si over the various aluminosilicate units by curve fitting provides an accurate and eonvenient method of obtaining the Si/Al ratio of the aluminosilicate framework by applying Loewenstein s Rule. This proeedure has been used in conjunction with Al NMR in a structural study of NaY zeolite stabilised [Pg.209]

The availability of NMR probes capable of operating at elevated temperatures up to 600-700°C has opened up the possibility of studying temperature-induced processes in minerals. The thermal changes in analcime have been studied in situ by multinuclear NMR including Si (Kim and Kirkpatrick 1998). Pre-melting processes in lithium and sodium metasilicates have also been studied by Si NMR at temperature (George et al. 1998). [Pg.211]


See other pages where Order-Disorder Effects in Minerals is mentioned: [Pg.199]    [Pg.208]   


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