SYNTHESIS OF NITRATE SODALITE: AN IN SITU SCANNING CALORIMETRIC STUDY

dc.contributor.authorLiu Q.
dc.contributor.authorNavrotsky A.
dc.date.accessioned2026-02-21T09:20:53Z
dc.date.issued2007
dc.description.abstractThe formation of nitrate sodalite, an important constituent of the resilient heels at DOE nuclear waste storage sites, was closely followed by oven synthesis, in situ calorimetry as a function of heating rate from 0.01 to 0.1 °C/min and X-ray diffraction. A transition sequence of amorphous-zeolite A-sodalite-cancrinite was confirmed. For in situ synthesis calorimetry, the heat flow peaks related to zeolite A formation are shifted to higher temperatures as heating rate increases. Although the end products are mostly nitrate sodalite, no calorimetric signals associated with zeolite A to sodalite conversion are detected. This suggests that the enthalpy of formation of zeolite A and sodalite are very similar and the zeolite A to sodalite conversion enthalpy is small. This conclusion is in accord with previous measurements by oxide melt solution calorimetry. © 2007 Elsevier Ltd. All rights reserved.
dc.identifierhttps://elibrary.ru/item.asp?id=31369571
dc.identifier.citationGeochimica et Cosmochimica Acta, 2007, 71, 8, 2072-2078
dc.identifier.doi10.1016/j.gca.2007.01.011
dc.identifier.issn0016-7037
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/51226
dc.subjectnitrate sodalite
dc.titleSYNTHESIS OF NITRATE SODALITE: AN IN SITU SCANNING CALORIMETRIC STUDY
dc.typeСтатья

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