矿化(土壤科学)
纤维
胶原纤维
生物矿化
材料科学
生物物理学
电子显微镜
矿化组织
各向异性
基质(化学分析)
结晶学
化学
复合材料
化学工程
牙本质
光学
生物
物理
工程类
有机化学
氮气
作者
Yifei Xu,Fabio Nudelman,E. Deniz Eren,Maarten Wirix,Bram Cantaert,Wouter H. Nijhuis,Daniel Hermida‐Merino,Giuseppe Portale,Paul H. H. Bomans,Christian Ottmann,Heiner Friedrich,Wim Bras,Anat Akiva,Joseph Orgel,Fiona C. Meldrum,Nico A. J. M. Sommerdijk
标识
DOI:10.1038/s41467-020-18846-2
摘要
Abstract The mineralized collagen fibril is the basic building block of bone, and is commonly pictured as a parallel array of ultrathin carbonated hydroxyapatite (HAp) platelets distributed throughout the collagen. This orientation is often attributed to an epitaxial relationship between the HAp and collagen molecules inside 2D voids within the fibril. Although recent studies have questioned this model, the structural relationship between the collagen matrix and HAp, and the mechanisms by which collagen directs mineralization remain unclear. Here, we use XRD to reveal that the voids in the collagen are in fact cylindrical pores with diameters of ~2 nm, while electron microscopy shows that the HAp crystals in bone are only uniaxially oriented with respect to the collagen. From in vitro mineralization studies with HAp, CaCO 3 and γ-FeOOH we conclude that confinement within these pores, together with the anisotropic growth of HAp, dictates the orientation of HAp crystals within the collagen fibril.
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