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Particle-Attachment-Mediated and Matrix/Lattice-Guided Enamel Apatite Crystal Growth

机译:颗粒连接介导和基质/晶格引导的搪瓷磷灰石晶体生长

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摘要

Tooth enamel is a hard yet resilient biomaterial that derives its unique mechanical properties from decussating bundles of apatite crystals. To understand enamel crystal nucleation and growth at a nanoscale level and to minimize preparation artifacts, the developing mouse enamel matrix was imaged in situ using graphene liquid cells and atomic resolution scanning transmission electron and cryo-fracture electron microscopy. We report that 1-2 nm diameter mineral precipitates aggregated to form larger 5 nm particle assemblies within ameloblast secretory vesicles or annular organic matrix subunits. Further evidence for the fusion of 1-2 nm mineral precipitates into 5 nm mineral aggregates via particle attachment was provided by matrix-mediated calcium phosphate crystal growth studies. As a next step, aggregated particles organized into rows of 3-10 subunits and developed lattice suprastructures with 0.34 nm gridline spacings corresponding to the (002) planes of apatite crystals. Mineral lattice suprastructures superseded closely matched organic matrix patterns, suggestive of a combination of organic/inorganic templates guiding apatite crystal growth. Upon assembly of 2-5 nm subunits into crystal ribbons, lattice fringes indicative of the presence of larger ordered crystallites were observed surrounding elongating crystal ribbons, presumably guiding the c-axis growth of composite apatite crystals. Cryo-fracture micrographs revealed reticular networks of an organic matrix on the surface of elongating enamel crystal ribbons, suggesting that protein coats facilitate c-axis apatite crystal growth. Together, these data demonstrate (i) the involvement of particle attachment in enamel crystal nucleation, (ii) a combination of matrix-and lattice-guided crystal growth, and (iii) fusion of individual crystals via a mechanism similar to Ostwald ripening.
机译:牙釉质是一种难以且有弹性的生物材料,其来自磷灰石晶体的典范束的独特力学性能。为了了解纳米级水平的搪瓷晶体成核和生长,并最小化制备伪像,使用石墨烯液体细胞和原子分辨率扫描透射电子和冷冻裂隙电子显微镜原位成像发育小鼠搪瓷基质。我们认为1-2nm直径的矿物沉淀物聚集在Ameloblast分泌囊泡或环形有机基质亚基内形成较大的5nm颗粒组件。通过基质介导的磷酸钙晶体生长研究提供将1-2nm矿物质沉淀成5nm矿物质聚集体的进一步证据。作为下一步,聚集颗粒组织成3-10个亚基的行,并开发了与磷灰石晶体的(002)平面相对应的0.34nm格栅间距的晶格超法。矿物晶格超法取代了与有机基质模式紧密匹配,暗示了有机/无机模板引导磷灰石晶体生长的组合。在将2-5nm亚基组装成晶带时,围绕伸长晶带观察到围绕伸长晶状体的较大有序微晶的存在的晶格状,可能引导复合磷灰石晶体的C轴生长。冷冻裂缝显微照片显示了伸长釉质晶带表面的有机基质的网状网络,表明蛋白质涂层促进了C轴磷灰石晶体生长。这些数据一起证明(i)粒子附着在搪瓷晶体成核中的参与,(ii)通过类似于Ostwald成熟的机制的机制,(iii)融合的基质 - 和晶格引导晶体生长的组合,以及(iii)各个晶体的融合。

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