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Morphogenesis Evolution of Calcite Crystals on Self-assembled Monolayers in the Presence of Block Copolymer Additives

机译:嵌段共聚物添加剂存在下自组装单层方解石晶体的形态发生演变

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Nature’s ability to precisely control over the size, orientation, and complex morphologies of biominerals has provided inspiration for the development of new synthetic routes for highly ordered inorganic materials. While the nucleation templates, including self-assembled monolayers (SAMs), Langmuir film, and solid matrices , define the crystal location and crystallographic orientation, the soluble additives such as acid-rich proteins,synthetic polymers,low molecular weight molecules,and inorganic ions selectively absorb on specific crystal faces and modify the crystal growth in terms of size, shape, polymorph, and morphology. Previously we have demonstrated morphogenesis evolution of CaCO3 calcite crystals on functional SAMs in the presence of Mg~(2+) additives. In comparison to Mg~(2+) ions as soluble additives, the organic molecules possess wider range of chemical functionalities and architectures, and their composition and molecular weight can be varied conveniently. Therefore, it is expected that organic additives may potentially offer more dramatic morphological changes and fine-tuning on calcite crystallization.
机译:大自然精确控制生物体的大小,取向和复杂形态的能力为高度有序无机材料开发新的合成途径提供了灵感。虽然核模板,包括自组装单层(SAM),朗缪尔膜和固体基质,定义晶体的位置和结晶取向,可溶性添加剂,如富酸蛋白质,合成聚合物,低分子量的分子,和无机离子选择性地吸收特定的晶面和修改晶体生长在大小,形状,多晶型物,和形态方面。此前,我们在Mg〜(2+)添加剂存在下表现出CaCO3方解石晶体的形态发生演变。与Mg〜(2+)离子相比,作为可溶性添加剂,有机分子具有更广泛的化学功能和架构,并且它们的组成和分子量可以方便地改变。因此,预计有机添加剂可能会提供更显着的形态学变化和对方解石结晶的微调。

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