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From spinodal decomposition to alternating layered structure within single crystals of biogenic magnesium calcite

机译:从旋节线分解到生物方解石镁单晶内的交替层状结构

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摘要

As organisms can form crystals only under ambient conditions, they demonstrate fascinating strategies to overcome this limitation. Recently, we reported a previously unknown biostrategy for toughening brittle calcite crystals, using coherently incorporated Mg-rich nanoprecipitates arranged in a layered manner in the lenses of a brittle star, Ophiocoma wendtii. Here we propose the mechanisms of formation of this functional hierarchical structure under conditions of ambient temperature and limited solid diffusion. We propose that formation proceeds via a spinodal decomposition of a liquid or gel-like magnesium amorphous calcium carbonate (Mg-ACC) precursor into Mg-rich nanoparticles and a Mg-depleted amorphous matrix. In a second step, crystallization of the decomposed amorphous precursor leads to the formation of high-Mg particle-rich layers. The model is supported by our experimental results in synthetic systems. These insights have significant implications for fundamental understanding of the role of Mg-ACC material transformation during crystallization and its subsequent stability.
机译:由于生物只能在环境条件下形成晶体,因此它们展现出了吸引人的策略来克服这一局限性。最近,我们报道了一种以脆性方解石(Ophiocoma wendtii)的晶状体以层状方式连贯结合的富含Mg的纳米沉淀物,用于增韧脆性方解石晶体的生物策略。在这里,我们提出了在环境温度和有限的固体扩散条件下这种功能分层结构的形成机理。我们建议通过液体或凝胶状无定形碳酸镁(Mg-ACC)前体的旋节线分解进入富含Mg的纳米颗粒和贫Mg的无定形基质来进行形成。在第二步骤中,分解的无定形前体的结晶导致形成高镁颗粒富集层。该模型得到合成系统中实验结果的支持。这些见解对于结晶过程中Mg-ACC材料转化的作用及其后续稳定性具有基本意义。

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