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骨单位骨特性相对于组织和动物年龄的空间变化。

Spatial variation in osteonal bone properties relative to tissue and animal age.

作者信息

Gourion-Arsiquaud Samuel, Burket Jayme C, Havill Lorena M, DiCarlo Edward, Doty Stephen B, Mendelsohn Richard, van der Meulen Marjolein C H, Boskey Adele L

机构信息

Hospital for Special Surgery, Mineralized Tissue Laboratory, Research Division, New York, New York, USA.

出版信息

J Bone Miner Res. 2009 Jul;24(7):1271-81. doi: 10.1359/jbmr.090201.

Abstract

Little is known about osteonal bone mineral and matrix properties, although these properties are of major importance for the understanding of bone alterations related to age and bone diseases such as osteoporosis. During aging, bone undergoes modifications that compromise their structural integrity as shown clinically by the increase of fracture incidence with age. Based on Fourier transform infrared (FTIR) analysis from baboons between 0 and 32 yr of age, consistent systematic variations in bone properties as a function of tissue age are reported within osteons. The patterns observed were independent of animal age and positively correlated with bone tissue elastic behavior measured by nano-indentation. As long as tissue age is expressed as a percentage of the entire osteon radius, osteonal analyses can be used to characterize disease changes independent of the size of the osteon. These mineral and matrix analyses can be used to explain bone fragility. The mineral content (mineral-to-matrix ratio) was correlated with the animal age in both old (interstitial) and newly formed bone tissue, showing for the first time that age-related changes in BMC can be explain by an alteration in the mineralization process itself and not only by an imbalance in the remodeling process.

摘要

尽管骨单位骨矿物质和基质特性对于理解与年龄相关的骨骼变化以及骨质疏松症等骨骼疾病至关重要,但人们对其了解甚少。随着年龄增长,骨骼会发生改变,损害其结构完整性,临床上表现为骨折发生率随年龄增加。基于对0至32岁狒狒的傅里叶变换红外光谱(FTIR)分析,研究报告了骨单位内骨骼特性随组织年龄变化的一致系统性差异。观察到的模式与动物年龄无关,且与通过纳米压痕测量的骨组织弹性行为呈正相关。只要将组织年龄表示为整个骨单位半径的百分比,骨单位分析就可用于表征疾病变化,而与骨单位大小无关。这些矿物质和基质分析可用于解释骨骼脆性。矿物质含量(矿物质与基质的比率)在老龄(间隙)和新形成的骨组织中均与动物年龄相关,首次表明与年龄相关的骨矿物质含量变化可由矿化过程本身的改变来解释,而不仅仅是由重塑过程中的失衡所致。

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