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Formation of amorphous calcium carbonate and its transformation into mesostructured calcite

机译:无定形碳酸钙的形成及其向介孔方解石的转化

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Amorphous calcium carbonate (ACC) is a key precursor of crystalline CaCO3 biominerals and biomimetic materials. Despite recent extensive research, its formation and amorphous-to-crystalline transformation are not, however, fully understood. Here we show that hydrated ACC nanoparticles form after spinodal liquid-liquid phase separation and transform via dissolution/(re) precipitation into poorly hydrated and anhydrous ACC nanoparticles that aggregate, forming a range of 1D, 2D and 3D structures. The formation of these structures appears to be achieved by oriented attachment (OA), facilitated by the calcite medium-range order of ACC nanoparticles. Both electron irradiation processes in the TEM and under humid air exposure at room temperature of the latter ACC structures result in pseudomorphs of single crystalline mesostructured calcite. While the high-vacuum/e-beam heating leads to solid-state transformation, the transformation in air occurs via an interface-coupled dissolution/precipitation mechanism. Our results differ significantly from the currently accepted model, which considers that the low T ACC-to-calcite transformation in air and during biomineralization is a solid-state process. These results may help to better understand how calcite biominerals form after ACC and offer the possibility of biomimetically preparing single crystalline calcite structures after ACC by tuning pH(2)O at room temperature.
机译:非晶态碳酸钙(ACC)是结晶CaCO3生物矿物和仿生材料的关键前体。尽管最近进行了广泛的研究,但是其形成和从非晶态到结晶态的转变还没有被完全理解。在这里,我们显示了水合ACC纳米粒子在旋节线液相分离后形成,并通过溶解/(再)沉淀转变为水合不良的无水ACC纳米粒子,这些纳米粒子聚集在一起,形成了一系列1D,2D和3D结构。这些结构的形成似乎是通过定向附着(OA)来实现的,方解石的ACC纳米粒子的方解石中等范围的顺序促进了这种结构。后者的ACC结构在TEM中的电子辐照过程以及在室温下在潮湿空气中的辐照过程均会导致单晶介孔方解石的假晶型。虽然高真空/电子束加热导致固态转变,但空气中的转变是通过界面耦合的溶解/沉淀机制发生的。我们的结果与当前接受的模型有显着差异,后者认为空气中和生物矿化过程中低的T ACC向方解石转化是固态过程。这些结果可能有助于更好地了解ACC后方解石生物矿物的形成方式,并提供了在ACC后通过在室温下调节pH(2)O仿生制备单晶方解石结构的可能性。

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