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首页> 外文期刊>Journal of Molecular Structure >FT-IR spectroscopic investigation of adsorption of 3-aminopyridine on sepiolite and montmorillonite from Anatolia
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FT-IR spectroscopic investigation of adsorption of 3-aminopyridine on sepiolite and montmorillonite from Anatolia

机译:FT-IR光谱法研究安那托利亚海泡石和蒙脱石上3-氨基吡啶的吸附

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The adsorption of 3-aminopyridine by natural sepiolite and montmorillonite from Eskisehir (Anatolia) was investigated in the temperature range from 20 to 125°C by infrared spectrometry using a variable temperature unit. The spectroscopic results indicate that the 3-aminopyridine molecules adsorbed on sepiolite are coordinated to Lewis acidic sites and/or surface hydro- xyls by H-bonding interaction throughpyridine ring nitrogen lone pairs. Surface Bronsted acid strength of sepiolite is weak and 3-aminopyridinium is not detected under the conditions applied in this study. It must be noted that the adsorption of amino- pyridine affected the hydroxyl group vibrations of sepiolite. The intercalation of 3-aminopyridine within montmorillonite has been shown by X-ray diffraction to increase the interlayer spacing. IR spectroscopy indicates that sorbed 3-aminopyridine .molecules by montmorillonite are mostly coordinated to exchangeable cations directly or indirectly through water bridges. The formation of 3-aminopyridinium cation is also detected at elevated temperatures.
机译:在20至125°C的温度范围内,使用可变温度装置,研究了Eskisehir(Anatolia)生产的天然海泡石和蒙脱石对3-氨基吡啶的吸附。光谱结果表明,吸附在海泡石上的3-氨基吡啶分子通过吡啶环氮孤对的H键相互作用与路易斯酸性位点和/或表面羟基配位。在本研究中应用的条件下,海泡石的表面布朗斯台德酸强度很弱,并且未检测到3-氨基吡啶鎓。必须注意的是,氨基吡啶的吸附影响了海泡石的羟基振动。 X射线衍射显示3-氨基吡啶在蒙脱石中的嵌入可增加层间间距。红外光谱表明,蒙脱石吸附的3-氨基吡啶分子大多直接或通过水桥间接地与可交换阳离子配位。在升高的温度下也检测到3-氨基吡啶鎓阳离子的形成。

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