García-Ruiz Juan Manuel, Melero-García Emilio, Hyde Stephen T
Laboratorio de Estudios Cristalográficos, Instituto Andaluz de Ciencias de la Tierra, Consejo Superior de Investígacìones Cientificas-Universidad de Granada, Avenida del Conocimiento, Parque Tecnológico, Ciencias de la Salud, 18100 Armilla, Spain.
Science. 2009 Jan 16;323(5912):362-5. doi: 10.1126/science.1165349.
The precipitation of barium or strontium carbonates in alkaline silica-rich environments leads to crystalline aggregates that have been named silica/carbonate biomorphs because their morphology resembles that of primitive organisms. These aggregates are self-assembled materials of purely inorganic origin, with an amorphous phase of silica intimately intertwined with a carbonate nanocrystalline phase. We propose a mechanism that explains all the morphologies described for biomorphs. Chemically coupled coprecipitation of carbonate and silica leads to fibrillation of the growing front and to laminar structures that experience curling at their growing rim. These curls propagate in a surflike way along the rim of the laminae. We show that all observed morphologies with smoothly varying positive or negative Gaussian curvatures can be explained by the combined growth of counterpropagating curls and growing laminae.
在富含二氧化硅的碱性环境中,碳酸钡或碳酸锶的沉淀会形成晶体聚集体,这些聚集体被称为二氧化硅/碳酸盐生物形态,因为它们的形态类似于原始生物。这些聚集体是完全无机起源的自组装材料,其非晶态二氧化硅相与碳酸盐纳米晶相紧密交织在一起。我们提出了一种机制,该机制解释了所描述的生物形态的所有形态。碳酸盐和二氧化硅的化学耦合共沉淀导致生长前沿的纤维化以及在其生长边缘处发生卷曲的层状结构。这些卷曲以类似波浪的方式沿着薄片边缘传播。我们表明,所有观察到的具有平滑变化的正或负高斯曲率的形态都可以通过反向传播的卷曲和生长的薄片的联合生长来解释。