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INFLUENCE OF SYNTHESIS CONDITIONS ON THE FORMATION OF A KAOLINITE-METHANOL COMPLEX AND SIMULATION OF ITS VIBRATIONAL SPECTRA

机译:合成条件对高岭石-甲醇配合物形成的影响及其振动光谱的模拟

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摘要

Kaolinite is often used as a base for the synthesis of new organo-mineral nanomaterials designed for applications in industry and in environmental protection. To make the mineral structure more likely to interact with organic molecules, a kaolinite-methanol complex (KM) can be used. In the present study, different experimental procedures were tested to investigate the formation of the KM. The kaolinite-dimethyl sulfoxide intercalation compound (KDS), either wet or dried, was used as a pre-intercalate. The samples obtained were characterized using X-ray diffraction, Fourier-transform infrared spectroscopy, CHNS elemental analysis, ~(13)C CP-magic angle spinning nuclear magnetic resonance (MAS NMR), and ~(27)Al and ~(29)Si MAS NMR techniques. The method of density functional theory with dispersion corrections (DFT-D2) was used to explain the structure and to simulate the vibrational spectra of KM. Theoretical results were compared with experimental data. The most effective formation of the KM (d_(001) = 11.1 A -wet; d_(001) = 8.7 A - dried) was observed when the dried KDS precursor was used. In such conditions the degree of intercalation reached ~98% after 24 h of reaction time. As indicated by the CHNS elemental analysis, ~1/6 of the inner-surface OH groups were grafted by OCH3 groups. The esterification reaction was less efficient at higher temperatures or when wet KDS was used. In the latter case, the excess of very polar dimethyl sulfoxide molecules prevented intercalation of methanol and further grafting. Detailed analysis of the results of theoretical simulations revealed that the reaction of the KDS with methanol led to the formation of kaolinite with both grafted methoxy groups and intercalated methanol, and water molecules in the interlayer space. The spectra calculated revealed the contribution of individual vibrational modes into the complex bands, i.e. the energy of C-H vibrations was in the order: v_(as)CH_(met) > v_(as)CH_(mtx) > v_sCH_(met) > v_sCH_(mtx).
机译:高岭石通常被用作合成新型有机矿物纳米材料的基础,这些材料设计用于工业和环境保护。为了使矿物结构更可能与有机分子发生相互作用,可以使用高岭石-甲醇复合物(KM)。在本研究中,测试了不同的实验程序以研究KM的形成。湿的或干燥的高岭石-二甲基亚砜插层化合物(KDS)均用作预插层。使用X射线衍射,傅立叶变换红外光谱,CHNS元素分析,〜(13)C CP-魔术角旋转核磁共振(MAS NMR)以及〜(27)Al和〜(29)对获得的样品进行表征。 Si MAS NMR技术。使用带有弥散校正的密度泛函理论方法(DFT-D2)来解释结构并模拟KM的振动谱。理论结果与实验数据进行了比较。当使用干燥的KDS前体时,观察到最有效的KM形成(d_(001)= 11.1 A-湿; d_(001)= 8.7 A-干燥)。在这种条件下,反应24小时后,插层度达到〜98%。如CHNS元素分析所示,内表面OH基团的约1/6被OCH3基团接枝。在较高温度或使用湿KDS时,酯化反应效率较低。在后一种情况下,极极性二甲基亚砜分子的过量阻止了甲醇的嵌入和进一步的接枝。对理论模拟结果的详细分析表明,KDS与甲醇的反应导致高岭石的形成,该高岭石同时具有接枝的甲氧基和插入的甲醇,并且在层间空间中存在水分子。计算得出的光谱揭示了单个振动模式对复杂频带的贡献,即,CH振动的能量的顺序为:v_(as)CH_(met)> v_(as)CH_(mtx)> v_sCH_(met)> v_sCH_ (mtx)。

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  • 来源
    《Clays and clay minerals》 |2012年第3期|p.227-239|共13页
  • 作者单位

    Department of Mineralogy, Petrography and Geochemistry, Faculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, al. Mickiewicza 30, 30-059 Krakow, Poland;

    Institute of Inorganic Chemistry, Slovak Academy of Sciences, Dubravska Cesta 9, SK-845 36 Bratislava, Slovak Republic;

    Institute of Inorganic Chemistry, Slovak Academy of Sciences, Dubravska Cesta 9, SK-845 36 Bratislava, Slovak Republic,Institut fuer Bodenforschung, Universitaet fuer Bodenkultur, Peter-Jordan-Strasse 82b, A-1190 Vienna, Austria;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    DFT-D2; grafting; intercalation; kaolinite; methanol; vibrational spectra;

    机译:DFT-D2;嫁接;插层高岭石甲醇振动光谱;

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