共查询到20条相似文献,搜索用时 125 毫秒
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Novel organic–inorganic hybrid pigments were prepared by in situ imidization of poly(styrene-co-maleic anhydride) (SMA) aqueous dispersion with ammonia in the presence of inorganic pigments, i.e. kaolin (K) or a mixture of kaolin (K)/alumina trihydrate (ATH). The objective was to allow the organic nano-particles of poly(styrene-co-maleimide) (SMI) to precipitate during their formation onto the surface of the inorganic pigment(s) and to investigate their potential in paper coatings. The produced hybrid pigments were characterized by Diffuse Reflectance Infrared Fourier Transform Spectroscopy (DRIFT-FTIR), scanning electron microscopy (SEM), wide-angel X-ray diffraction (WXRD) spectroscopy and their particle sizes were determined by dynamic light scattering technique. By FTIR measurements the formation of maleimide was confirmed and the existence of strong hydrogen bonding between organic and inorganic components could also be detected. Whereas, the SEM images revealed that the surface of silicate layers had successfully been to a large extent covered by the organic nano-particles to give raise to novel hybrid particles. In addition, the particle size measurements support the observation that the organic nanoparticles for the most part had been chemically or physically attached to the larger inorganic particles. Thus, this in situ imidization process in the presence of clay particles provides a neat method of dispersing the formed nanoparticles onto the inorganic surface through hydrogen bonding. The produced hybrids were applied as auxiliary pigments in paper coating where they improved gloss without roughening the paper surface. 相似文献
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John B. Murray 《Fuel》1973,52(2):105-111
The inorganic constituents of low-rank Victorian brown coal, which are mainly present as inherent inorganic combinations attached to the coal molecule, are different from the minerals present in higher-rank coals. Changes in the state of combination of the inorganics in the chars of these coals have been studied by determining the minerals formed when chars are prepared at various temperatures. It is shown that when brown coals containing inorganic carboxylates are carbonized, the reactive functional groups which are present will begin to decompose below 400 °C and their decomposition is completed by 600 °C. The inorganic elements released will form mineral combinations depending on the carbonizing temperature and the reduction potential of the metal. Sodium carbonate, calcium oxide, magnesium oxide (periclase) and iron oxide (magnetite) are usually the chief minerals that may be formed. Mineral constituents present in the original coal may also change during carbonization. As the temperature increases, hydrated oxides of iron, clay and aluminium will lose water of crystallization and become dehydrated, forming magnetite, dried clay and alumina. Pyrite will lose up to half its sulphur at 400–450 °C. If the carbonization temperature is over 600 °C, metallic iron may be formed from the magnetite, and sodium chloride (and later sodium carbonate) will volatilize. Quartz remains unaltered. 相似文献
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The catalytic power of 14 inorganic materials, namely, 4 synthetic short-range ordered oxides, 4 CBD-treated clay minerals, and 6 primary minerals in the abiotic synthesis of humic acids (HA) through the oxidative polymerization of hydroquinone was investigated. The promoting effect of Mn oxide is much higher than that of short-range ordered oxides of Fe, Al and Si. The accelerating effects of montmorillonite and tephroite are highest among the respective mineral groups studied. Among all inorganic materials studied, the catalytic power of tephroite (Mn2SiO4) and especially Mn oxide is most striking. The Mn oxide and tephroite rapidly convert hydroquinone to HA and the IR spectra of these synthesized HA are similar to those of soil HA. Compared to the clay minerals, the transition metal-bearing primary minerals have a stronger promoting effect on the synthesis of hydroquinone-derived HA.The data obtained indicate the sequence of the catalytic power of selected short-range ordered oxides, clay minerals, and primary minerals in the formation of hydroquinone-derived HA. The powerful promoting effects of the Mn oxide and tephroite on the synthesis of HA strongly indicate that Mn-bearing oxides and silicates deserve close attention in the formation of humic substances. 相似文献
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粘土矿物的药理作用及其医药应用 总被引:4,自引:1,他引:3
粘土矿物因有大的比表面积,丰富的孔隙率,良好的吸附性能,较高的吸附容量和离子交换能力等,已作为很多药物的活性成分和药物辅料,被广泛用于胃、肠道疾病,急慢性腹泻,皮肤病及风湿病的治疗。随着人们对粘土矿物性能和治病机理研究的深入,粘土矿物作为天然无毒副作用药物材料的研究越来越受到重视。通过近年来国内外粘土药物研究报道及实验室的研究成果,综合介绍粘土矿物的特点、性能、药理作用及其临床应用,预测粘土矿物在医药、化妆品领域中的应用前景。 相似文献
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化学吸附储热技术近年来在太阳能利用和中低温余热领域得到了广泛关注,与传统的显热储热和相变储热技术相比具有储热密度高、储热损失小、可实现冷热双储等优点,然而其传质传热问题和液解问题导致的吸附性能和循环稳定性能的降低限制了其规模化应用。本文综述了利用矿物基多孔结构材料对化学吸附材料进行封装的方法以解决上述问题,总结了近年来石墨、蛭石等不同矿物基化学吸附储热材料的特点及其在化学吸附系统中的应用,主要介绍了矿物基化学吸附材料的两种体系(无机盐-水体系和氯盐-氨体系)的传质传热、化学吸附热等性能,并进一步指出了矿物基化学吸附储热技术未来的发展趋势,提出开发新型矿物基复合材料和优化化学吸附系统是未来的研究热点。 相似文献
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Effect of the layer charge of clay minerals on optical properties of organic dyes. A review 总被引:1,自引:0,他引:1
Juraj Bujdk 《Applied Clay Science》2006,34(1-4):58
Interactions between clay minerals and cationic organic dyes cause significant changes in the optical, spectral and chemical properties of the chromophores. These changes are due to the formation of supramolecular assemblies of dye cations, called molecular aggregates. Numerous experiments indicate that dye molecular aggregation is sensitively controlled by the layer charge of a clay mineral. Interpretations are based on a detailed analysis of papers investigating reactions of dyes with clay minerals but also considering the reactions with other inorganic solid materials and templates. Older papers dealing with the subject and alternative interpretations of the phenomenon are analysed and critically reviewed. Significance for clay science, material sciences, nanotechnology and potential industrial applications are discussed. 相似文献
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