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Temperature Oscillation Modulated Self-Assembly of Periodic Concentric Layered Magnesium Carbonate Microparticles

机译:周期性同心层状碳酸镁微粒的温度振荡调制自组装

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摘要

Intriguing patterns of periodic, concentric, layered, mineral microstructure are present in nature and organisms, yet they have elusive geneses. We hypothesize temperature oscillation can be an independent factor that causes the self-assembly of such patterns in mineral phases synthesized in solution. Static experiments verify that rhythmic concentric multi-layered magnesium carbonate microhemispheres can be synthesized from bicarbonate solution by temperature oscillation, without use of a chemical template, additive or gel-diffusion system. Appropriate reactant concentration and initial pH value can restrain the competitive growth of other mineral generations. Polarized light microscopy images indicate the microhemispheres are crystalline and the crystallinity increases with incubation time. The thickness of a single mineral layer of microhemisphere in microscale is precisely controlled by the waveform parameters of the temperature oscillation, while the layer number, which can reach tens to about one hundred, is constrained by the temperature oscillation period number. FT-IR spectra show that these microhemispheres synthesized under different conditions can be identified as the basic form of magnesium carbonate, hydromagnesite (Mg5(CO3)4(OH)2⋅4H2O). SEM images exhibit the characteristic microscopic texture of the alternating dark and light rings of these microhemispheres. TEM images and ED patterns suggest the nanoflakes of microhemispheres are present in polycrystalline form with some degree of oriented assembly. The temperature oscillation modulated self-assembly may offer a new mechanism to understand the formation of layered microstructure of minerals in solution, and provide a non-invasive and programmable means to synthesize hierarchically ordered materials.
机译:周期性,同心,分层,矿物微观结构的有趣模式存在于自然界和有机体中,但是它们具有难以捉摸的成因。我们假设温度振荡可能是导致溶液中合成的矿物相中此类模式自组装的独立因素。静态实验证明,可以通过温度振荡从碳酸氢盐溶液中合成有节奏的同心多层碳酸镁微半球,而无需使用化学模板,添加剂或凝胶扩散系统。适当的反应物浓度和初始pH值可以限制其他矿物世代的竞争性增长。偏光显微镜图像表明微半球是结晶的,并且结晶度随孵育时间的增加而增加。微半球的单个矿物层的厚度在微尺度上是由温度振荡的波形参数精确控制的,而可达到数十至约一百的层数受温度振荡周期数的限制。 FT-IR光谱表明,在不同条件下合成的这些微半球可以被识别为碳酸镁,菱镁矿(Mg5(CO3)4(OH)2⋅4H2O)的基本形式。 SEM图像显示了这些微半球交替的暗环和亮环的特征微观纹理。 TEM图像和ED模式表明,微半球的纳米片以多晶形式存在,并具有一定程度的定向组装。温度振荡调制自组装可能会提供一种新的机制,以了解溶液中矿物质的分层微观结构的形成,并提供一种非侵入性和可编程手段来合成分层有序的材料。

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