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EMANATION THERMAL ANALYSIS OF NATURAL AND CHEMICALLY-MODIFIED VERMICULITE

机译:天然和化学改性石的散发热分析

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Emanation thermal analysis (ETA), based on radon release measurements from previously labeled samples, was used for the first time in the characterization of the thermal behavior of natural Mg~(2+)-vermiculite (Santa Olalla, Huelva, Spain) and of Na~+- and NH_4~+-exchanged vermiculite samples. In addition, vermiculite samples subjected to a chemical treatment with an aqueous solution of (NH_4)_2SiF_6 and partially or totally re-saturated with Na~+ ions were also investigated by ETA. The ETA results of natural Mg~(2+)-vermiculite, Na~+-vermiculite and NH_4~+-vermiculite gave supplementary information about microstructure changes of the samples observed under dynamic heating conditions. The method has proved to be very useful for characterization of microstructure changes due to modification in the interlayer space of samples during the heat treatment. The crystallization of vermiculite into new phases, such as enstatite (for NH_4~+-vermiculite and Mg~(2+)-vermiculite) and forsterite (for Na~+-vermiculite) was also observed by ETA.
机译:辐射热分析(ETA)基于先前标记的样品中的release释放量测量,首次用于表征天然Mg〜(2 +)-ver石(Santa Olalla,韦尔瓦,西班牙)和Na〜+-和NH_4〜+交换的ver石样品。另外,还通过ETA研究了用(NH_4)_2SiF_6的水溶液进行化学处理并且部分或全部被Na〜+离子再饱和的ver石样品。天然Mg〜(2 +)-石,Na〜+-石和NH_4〜+-石的ETA结果为样品在动态加热条件下的微观结构变化提供了补充信息。事实证明,该方法对于表征由于热处理过程中样品的层间空间发生变化而引起的微观结构变化非常有用。通过ETA还观察到ul石结晶为新相,例如顽辉石(对于NH_4〜+-石和Mg〜(2 +)-石)和镁橄榄石(对于Na〜+-石)。

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