Rai D V, Darbari R, Aggarwal L M
Department of Biophysics, Panjab University, Chandigarh 160 014, India.
Indian J Biochem Biophys. 2005 Apr;42(2):127-30.
Age-related changes in bone composition within the age groups of 30, 60, 120 and 180 days in rats have been studied using thermogravimetery, elemental analysis and energy dispersive Xray (ED X-ray). The structural changes in rats the bone samples were monitored by IR spectroscopy. The main constituents of hydroxyapatite, namely Ca, P and their oxides were analyzed. Organic changes, such as C and N contents in the matrix were found to have a predominant role in the initial development of the bone. An incremental increase in the mineral content of bone with advancing age was also observed. Elemental composition (C and N contents) was observed to be independent of age at the initial stages. The amount of Ca and its oxide content was found to increase, and the P and its oxides showed a decreasing trend, with the advancing age. IR spectra revealed that the mineral phase comprised both amorphous and crystalline hydroxyapatite, even at maturity; the amorphous content being higher at the earlier stages (14.09%, at 30 days), but was gradually replaced by crystalline component with advancing age (63.09% at 180 days). The present data may be useful in explaining the ageing phenomenon and helpful in understanding the bone growth and remodeling.
利用热重分析法、元素分析和能量色散X射线(ED X射线)研究了30、60、120和180日龄大鼠骨成分的年龄相关变化。通过红外光谱监测大鼠骨样品的结构变化。分析了羟基磷灰石的主要成分,即钙、磷及其氧化物。发现基质中的碳和氮等有机变化在骨的初始发育中起主要作用。随着年龄的增长,还观察到骨矿物质含量逐渐增加。在初始阶段,元素组成(碳和氮含量)与年龄无关。随着年龄的增长,钙及其氧化物含量增加,而磷及其氧化物呈下降趋势。红外光谱显示,即使在成熟阶段,矿物相也包括无定形和结晶羟基磷灰石;无定形成分在早期阶段含量较高(30天时为14.09%),但随着年龄的增长逐渐被结晶成分取代(180天时为63.09%)。目前的数据可能有助于解释衰老现象,并有助于理解骨生长和重塑。