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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Synthesis of nitrate sodalite: An in situ scanning calorimetric study
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Synthesis of nitrate sodalite: An in situ scanning calorimetric study

机译:硝酸钠方钠石的合成:原位扫描量热法研究

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摘要

The 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 degrees 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 socialite 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. (c) 2007 Elsevier Ltd. All rights reserved.
机译:硝酸钠方钠石的形成是DOE核废料存储地点回弹的重要组成部分,紧随其后的是烤箱合成,原位量热法(加热速率为0.01至0.1摄氏度/分钟)和X射线衍射的函数。确认了无定形沸石A-钠钙锰矿-铅锌矿的过渡序列。对于原位合成量热法,随着加热速率的增加,与沸石A形成有关的热流峰移至更高的温度。尽管最终产品主要是硝酸钠方钠石,但未检测到与A型沸石转化为社交名石有关的量热信号。这表明沸石A和方钠石的形成焓非常相似,并且沸石A到方钠石的转化焓很小。该结论与先前通过氧化物熔融溶液量热法的测量结果一致。 (c)2007 Elsevier Ltd.保留所有权利。

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