埃洛石
高岭石
化学
粉末衍射
傅里叶变换红外光谱
粘土矿物
红外光谱学
矿物
矿物学
核化学
化学工程
结晶学
有机化学
工程类
作者
Beata Szczepanik,P. M. Słomkiewicz,Magdalena Garnuszek,K. Czech,D. Banaś,A. Kubala‐Kukuś,I. Stabrawa
标识
DOI:10.1016/j.molstruc.2014.12.008
摘要
The effect of chemical modification of halloysite from a Polish strip mine “Dunino” on the chemical composition and structure of this clay mineral was studied using infrared spectroscopy (ATR FT-IR), wavelength dispersive X-ray fluorescence (WDXRF), and X-ray powder diffraction (XRPD) methods. The results obtained by the WDXRF technique confirm that the content of silica and alumina was the highest for bleached halloysite samples and the lowest for acid-treated halloysite. A higher content of Fe2O3 in comparison to halloysite samples coming from other countries was observed for raw halloysite samples. XRPD diffraction pattern obtained for raw halloysite confirmed the presence of halloysite, kaolinite, hematite, and calcite minerals in the sample. Bleaching the halloysite removes (or significantly reduces) the content of other minerals present in the raw halloysite. The FT-IR spectra of the studied halloysite samples show in the 3700–3600 cm−1 region well-defined hydroxyl stretching bands characteristic for the kaolin-group minerals and bands associated with the vibrations of the aluminium–silicon skeleton in the 1400–1000 cm−1 region. Modifying halloysite with 4-chloro-aniline causes successive incorporation of amine into the BH sample.
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