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Thermo-XRD-analysis of Co-, Ni- and Cu-montmorillonite treated with anionic alizarinate - Curve-fitting

机译:阴离子硅铝酸盐处理的钴,镍和铜蒙脱石的热X射线分析-曲线拟合

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Co- and Ni-montmorillonites adsorb in aqueous suspensions up to 13 mmol alizarinate per 100 g clay, onto the broken-bonds whereas Cu-clay adsorbs up to 25 mmol dye per 100 g clay into the interlayer space. Unloaded Co-, Ni- and Cu-clays and samples loaded with increasing amounts of alizarinate, were gradually heated in air to 360 degrees C and analyzed by X-ray diffraction. All diffractograms were curve-fitted. Fitted diffractograms of non-heated samples, showed two peak components labeled C and D, at approximate to 1.22 and approximate to 1.32 nm, characterizing tactoids with mono- and non-complete bilayers of water, respectively. After heating at 120 degrees C component D decreased or disappeared and two new components A and B appeared at approximate to 0.99 and approximate to 1.08 nm, representing collapsed tactoids and tactoids with interlamellar oxy-cations, respectively. At 250 degrees C C and D decreased or disappeared but A and B appeared in all fitted diffractograms. Co- and Ni- clay after heating at 360 degrees C did not show C and D. Components A and B proved that these clays collapsed indicating that initially there was no alizarinate in the interlayers. At 360 degrees C C and D persisted in the fitted-diffractograms of Cu-clay, representing tactoids with interlamellar charcoal formed from the partial oxidation of adsorbed dye initially located in the interlayers.
机译:钴和镍蒙脱石在水性悬浮液中的吸附力高达每100 g粘土13毫摩尔的叠氮酸盐,而铜粘土则每100 g粘土将高达25毫摩尔的染料吸附到中间层空间中。在空气中将未负载的Co,Ni和Cu粘土以及负载了越来越多的茜素酸盐的样品逐渐加热到360摄氏度,并通过X射线衍射进行分析。所有衍射图都是曲线拟合的。未加热样品的拟合衍射图显示出两个标记为C和D的峰成分,分别位于约1.22和约1.32 nm处,分别表征了具有单层和不完全双层水的触针。在120℃加热后,组分D减少或消失,两个新的组分A和B出现在大约0.99和大约1.08 nm处,分别代表塌陷的类触针和带有层间氧阳离子的类触针。在250摄氏度时,C和D降低或消失,但所有拟合的衍射图中都出现A和B。在360℃下加热后的Co-和Ni-粘土没有显示C和D。组分A和B证明这些粘土塌陷,表明最初在中间层中没有铝合酸盐。在360摄氏度下,C和D持续存在于Cu-粘土的拟合衍射图中,代表类触针具有层状炭,该层状炭是由最初位于夹层中的吸附染料的部分氧化形成的。

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