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X-ray Diffraction Studies Of The Thermal Behaviour Of Commercial Vermiculites

机译:商业Ver石热行为的X射线衍射研究

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For the purpose of knowing the vermiculites which would have larger capability to retain contaminating substances heating commercial samples from different places have been identified and their thermal behaviour at several temperatures has been investigated by X-ray diffraction (XRD), electron microprobe, thermal analysis (TG and DTA), scanning electron microscopy (SEM), and transmission electron microscopy (TEM). The commercial vermiculites can be divided into two types: type 1 (Sta. Olalla, Piaui and Goias) with Mg~(2+) and K~+ (< 1) as the principal cations in the interlayer space, and type 2 (China E, China W, China G and Palabora) with K~+ (approximately=or > 1) and/or Na~+ and/or Ca~(2+) with or without Mg~(2+) as the principal interlayer cations. The process of dehydration in situ with the temperature seems restricted to interlamellar water monolayers of 1 -WLHS type-1 of vermiculites, without dehydration to a zero-water-layer-hydration state (0-WLHS) and the dehydroxylation starts at lower temperatures than in vermiculites of type 2. The maximum hydration state exhibited by the type-2 samples at ambient temperature was equal or lower than the monolayer hydrate, the dehydration process in situ with the temperature was slower and the dehydrated vermiculite coexists with a mica-like structure. The behaviour of vermiculites at elevated temperature examined in situ can be understood considering that the vermiculites constitute a complex system not necessarily in equilibrium and where kinetics plays an important role. Commercial vermiculites heated abruptly at 1000 ℃ during 1 min transform to mica-like or mica-like coexisting with enstatite, in contrast to the purest Sta. Olalla vermiculite, with only magnesium interlayer cations, which changes to enstatite.
机译:为了知道the石具有更大的保留污染物能力的substances石,已经鉴定了从不同地方加热商业样品的and石,并通过X射线衍射(XRD),电子微探针,热分析研究了它们在几个温度下的热行为( TG和DTA),扫描电子显微镜(SEM)和透射电子显微镜(TEM)。商业ver石可分为两种类型:中间层空间中以Mg〜(2+)和K〜+(<1)为主要阳离子的1型(Sta。Olalla,Piaui和Goias)和2型(中国)。 E,中国W,中国G和Palabora),其中K〜+(大约等于或> 1)和/或Na〜+和/或Ca〜(2+),有或没有Mg〜(2+)作为主要层间阳离子。温度下的原位脱水过程似乎仅限于1-WLHS类型为1的of石的层间水单层,而没有脱水至零水层水合状态(0-WLHS),并且脱羟基作用的起始温度低于在类型2的石中。类型2样品在环境温度下表现出的最大水合状态等于或低于单层水合物,随温度的原位脱水过程较慢,并且脱水的ul石共存为云母状结构。考虑到the石构成了一个不一定处于平衡状态且动力学起重要作用的复杂系统,因此可以理解examined石在高温下的行为。与最纯的Sta不同,商品石在1000℃下突然加热1分钟后转变为云母状或云母状与顽辉石共存。 Olalla mic石,只有镁中间层阳离子,会变成顽辉石。

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