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LOW-TEMPERATURE FTIR STUDY OF KAOLIN-GROUP MINERALS

机译:高岭土矿物的低温FTIR研究

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Low-temperature FTIR spectroscopy was used to characterize the ν(OH) region of kaolin-group minerals including well ordered to poorly ordered kaolins from Georgia, Brazil, and England, along with samples of discrete dickite and nacrite. Low-temperature FTIR spectra were useful in resolving dickite- and nacrite-like features present in the spectra of kaolins when cooled to <30 K. These features were not resolved at room temperature and only partially resolved at liquid N_2 temperature (77 K). The room-temperature and low-temperature positions of the ν(OH) bands of kaolinite, dickite, and nacrite were linearly correlated with the interatomic OH··· O distances and this relationship served as the basis for polytype/disorder identification. Dickite or dickite-like disorder was found in high Hinckley-Index kaolinite from Keokuk, Iowa, and from Cornwall, England. Dickite- and nacrite-like features were observed in both high- and low-Hinckley-index kaolinite and the amounts of these stacking sequences generally increased with decreasing Hinckley Index.
机译:低温FTIR光谱用于表征高岭土类矿物的ν(OH)区域,包括佐治亚州,巴西和英国的有序至有序的高岭土,以及离散的闪锌矿和珍珠陶土的样品。低温FTIR光谱可用于解析冷却至<30 K时出现在高岭土光谱中的重沸石和类似钠长石的特征。这些特征在室温下不分解,而在液态N_2温度(77 K)下仅部分分解。高岭石,地开石和珍珠陶土的ν(OH)谱带的室温和低温位置与原子间OH···O距离呈线性相关,该关系为多型/无序识别提供了基础。在爱荷华州Keokuk和英格兰康沃尔郡的高欣克利指数高岭石中发现了迪克石或类似迪克石的失调。在高欣克利指数和低欣克利指数的高岭石中均观察到了像Dickite和nacrite的特征,并且这些堆叠序列的数量通常随欣克利指数的降低而增加。

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