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首页> 外文期刊>Journal of Thermal Analysis and Calorimetry >Thermal analyis of hexadecyltrimethylammonium–montmorillonites Part 1. Thermogravimetry, carbon and hydrogen analysis and thermo-IR spectroscopy analysis
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Thermal analyis of hexadecyltrimethylammonium–montmorillonites Part 1. Thermogravimetry, carbon and hydrogen analysis and thermo-IR spectroscopy analysis

机译:十六烷基三甲基铵-蒙脱石的热分析第1部分。热重分析,碳氢分析和热红外光谱分析

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Na-montmorillonite (Na-MONT) was loaded with hexadecyltrimethylammonium cations (HDTMA) by replacing 41 and 90% of the exchangeable Na with HDTMA, labeled OC-41 and OC-90, respectively. Na-MONT, OC-41, and OC-90 were heated in air up to 900 °C. Unheated and thermally treated organoclays heated at 150, 250, 360, and 420 °C are used in our laboratory as sorbents of different hazardous organic compounds from waste water. In order to get a better knowledge about the composition and nature of the thermally treated organoclays Na-MONT and the two organo-clays were studied by thermogravimetry (TG) in air and under nitrogen. Carbon and hydrogen contents in each of the thermal treated sample were determined and their infrared spectra were recorded. The present results showed that at 150 °C both organoclays lost water but not intercalated HDTMA cations. At 250 °C, many HDTMA cations persisted in OC-41, but in OC-90 significant part of the cations were air-oxidized into H2O and CO2 and the residual carbon formed charcoal. After heating both samples at 360 °C charcoal was present in both organo clays. This charcoal persisted at 420 °C but was gradually oxidized by air with further rise in temperature. TG runs under nitrogen showed stepwise degradation corresponding to interlayer water desorption followed by decomposition of the organic compound, volatilization of small fragments and condensation of non-volatile fragments into quasi-charcoal. After dehydroxylation of the clay the last stages of organic matter pyrolysis and volatilization occurred.
机译:通过用HDTMA(分别标记为OC-41和OC-90)替换41%和90%的可交换钠,将十六烷基三甲基铵阳离子(HDTMA)装入钠蒙脱石(Na-MONT)。将Na-MONT,OC-41和OC-90在空气中加热到900°C。在我们的实验室中,加热到150、250、360和420°C的未经加热和热处理的有机粘土用作废水中各种有害有机化合物的吸附剂。为了更好地了解经过热处理的有机粘土的组成和性质,在空气中和氮气下通过热重分析(TG)研究了Na-MONT和两种有机粘土。测定每个热处理样品中的碳和氢含量,并记录其红外光谱。目前的结果表明,两种有机粘土在150°C时都会失水,但不会插入HDTMA阳离子。在250°C下,许多HDTMA阳离子保留在OC-41中,但在OC-90中,很大一部分阳离子被空气氧化成H 2 O和CO 2 残留的碳形成木炭。两种样品均在360°C加热后,两种有机粘土中均含有木炭。这种木炭在420°C下持续存在,但随着空气的温度逐渐升高,逐渐被空气氧化。 TG在氮气下运行,显示出逐步降解,与层间水解吸相对应,随后有机化合物分解,小碎片挥发和非挥发性碎片凝结为准木炭。粘土脱羟基后,发生了有机物热解和挥发的最后阶段。

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