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Reactive clays for the fixation and stabilization of dye precursors in interactive papers

机译:用于在交互式纸中固定和稳定染料前体的反应性粘土

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Abstract: Swelling clays are known for their ability to intercalate organic and inorganic species in their interlamellar space. For example, Montmorillonite and Vermiculite interact strongly with organic and inorganic guests, which provoke dimensional changes upon intercalation. Unlike other minerals like zeolites, clays present geometrical changes at the molecular scale by penetration of polar species of suitable size into the layers. The anionic charge of swelling clays attract positive ions which remain fixed on the flakes surface until other ions exchange. The intermediate charge densities, i.e. 57 - 100 square angstroms of interlayer surface per unit charge, which are typical of vermiculites and smectites that swell easily, are different to the high surface charges of about 12 - 30 square angstroms per unit charge that are typical for non swelling micas like Muscovite. In Ca- Monmorillonite, the basal spacing d(100) expands proportionally to the carbon number of monohydric alcohols. One and two layer complexes having the organic molecules parallel to the basal surfaces were reported for the polyethyleneglicol ester of the oleic acids in Na-, Ca- and Mg-montmorillonite. This has proved that intercalation of high molecular weight materials can readily occur from aqueous solutions. In addition, smectites form colored complexes with a number of bases, i.e. Pyridine, which are adsorbed into well outgassed natural montmorillonites, giving rise to blue complexes which become gray upon humidification with water steam. Also, glycine and its peptides, as well as a variety of other aminoacids are sorbed by Na-, Ca- and H-Montmorillonites from aqueous solutions. Also, photochromic molecules were reported to intercalate readily in montmorillonite type clays. On the other hand, spiropyrans are molecules with long alkyl chains and their use as 3-D memory devices has been proposed. The molecules are formed by two $pi@-moieties which are set orthogonally to each other, exhibiting the individual absorption spectra rather than the conjugated spectrum. In this view, swelling clays may be used to host reactive molecules for optical, thermal or electrical recording in paper. Most of the clays that are introduced already into the composition of paper, i.e. kaolin paper clays, can host molecules externally and are potentially useful for the design of interactive papers. In this work, the interaction of dyes and clays was investigated, based on the reactive forms of spiropyrans, which are sensitive materials for recording optical and electrical signals. !13
机译:摘要:溶胀粘土以在层间空间中插入有机和无机物质的能力而闻名。例如,蒙脱石和Ver石与有机和无机客体强烈地相互作用,这会在插层时引起尺寸变化。与沸石等其他矿物不同,粘土通过将适当大小的极性物质渗透到层中,在分子尺度上呈现几何变化。膨胀粘土的阴离子电荷吸引正离子,这些正离子保持固定在片状表面上,直到其他离子交换为止。中间电荷密度,即单位电荷中间层表面的57-100平方埃,这是容易膨胀的sm石和蒙脱石的典型特征,不同于典型的for电荷和每单位电荷大约12-30平方埃的高表面电荷。非膨胀云母,如白云母。在钙蒙脱石中,基间距d(100)与一元醇的碳原子数成正比扩展。据报道,Na-,Ca-和Mg-蒙脱土中油酸的聚乙二醇酯与有机分子平行于基底表面的一层和两层络合物。这已经证明,高分子量材料的嵌入可以容易地从水溶液中发生。另外,蒙脱石形成具有许多碱的有色配合物,即吡啶,它们被吸附到充分除气的天然蒙脱石中,产生蓝色配合物,该配合物在用水蒸汽加湿后变成灰色。同样,甘氨酸及其肽以及多种其他氨基酸也被Na-,Ca-和H-蒙脱石从水溶液中吸附。另外,据报道光致变色分子容易插入到蒙脱石型粘土中。另一方面,螺吡喃是具有长烷基链的分子,并且已经提出将其用作3-D存储装置。分子由彼此正交设置的两个π-部分形成,表现出单独的吸收光谱而不是共轭光谱。根据这种观点,溶胀粘土可用于容纳反应性分子,以在纸上进行光学,热或电记录。已经引入纸组合物中的大多数粘土,即高岭土纸粘土,可以在外部容纳分子,并且对于交互式纸的设计潜在地有用。在这项工作中,基于螺吡喃的反应形式对染料和粘土的相互作用进行了研究,螺吡喃是用于记录光和电信号的敏感材料。 !13

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