作为纳米材料的矿化组织:原子力显微镜分析。

L Bozec, J de Groot, M Odlyha, B Nicholls, M A Horton
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引用次数: 16

摘要

矿化组织,如骨,由两种物质相组成:胶原蛋白原纤维,形成结构模型,矿物质羟基磷灰石钙随后沉积在结构模型上。在骨骼生长或修复的骨转换过程中,胶原蛋白和矿物质被破骨细胞以三维的方式移除,基质蛋白被成骨细胞的合成活性所取代,然后钙化。原子力显微镜的分辨率和未修饰的、完全钙化的样品的使用使得整个骨骼和牙本质结构的成像成为可能,包括胶原蛋白和矿物相。在未修饰的骨和牙本质中分别发现了直径在225 nm到1.4微米之间的矿物晶体。在酸处理后的牙本质和破骨细胞介导的基质吸收后的骨中观察到d带状胶原;轴向周期性值分别约为67 nm和69 nm。这些实验方法使矿化组织的结构能够在原生样品中进行检查,并将促进骨骼重要临床疾病(如骨质疏松症)的骨结构研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mineralised tissues as nanomaterials: analysis by atomic force microscopy.

Mineralised tissues, such as bone, consist of two material phases: collagen protein fibrils that form the structural models upon which the mineral, calcium hydroxyapatite, is subsequently deposited. Collagen and mineral are removed in a three-dimensional manner by osteoclasts during bone turnover in skeletal growth or repair, and matrix proteins are replaced by the synthetic activity of osteoblasts and then calcify. The resolution of atomic force microscopy and use of unmodified, fully calcified samples has enabled the imaging of the overall bone and dentine structure, including collagen and mineral phases. Mineral crystals, in the diameter size range of 225 nm up to 1.4 microm, were found in unmodified bone and dentine respectively. D-banded collagen is observed in dentine after acid treatment and in bone after osteoclast-mediated matrix resorption; axial periodicity values of approximately 67 and 69 nm are observed, respectively. These experimental approaches have enabled the structure of mineralised tissues to be examined in native samples and will facilitate the study of bone structure in important clinical disorders of the skeleton, such as osteoporosis.

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