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年龄和镁缺乏对大鼠骨镁池的影响。

Effect of age and magnesium depletion on bone magnesium pools in rats.

作者信息

Alfrey A C, Miller N L, Trow R

出版信息

J Clin Invest. 1974 Nov;54(5):1074-81. doi: 10.1172/JCI107851.

Abstract

In vivo and in vitro studies were carried out to characterize the exchangeable bone magnesium pool and determine what effect age and magnesium depletion has on bone magnesium. A highly significant correlation was found between the size of the in vitro elutable and in vivo exchangeable bone magnesium (r=0.97). To show that the exchangeable bone magnesium was the surface-limited bone magnesium, elution studies were performed 4 h after the in vivo administration of radiomagnesium. Specific activity in the eluant was 85% of that found in the serum at time of death, suggesting that the elutable and exchangeable bone magnesium pools were largely the same pool. Bone magnesium concentration fell with increasing age. The entire fall in bone magnesium was a result of a decrease in the surface-limited fraction. Since bone crystals have been shown to enlarge with aging with resulting contraction of the surface area, this would be the most apparent explanation for this finding. During magnesium depletion, magnesium concentration in both the exchangeable and nonexchangeable pools decreased. The fractional change in the exchangeable pool was much larger than the change in total or nonexchangeable bone magnesium, suggesting that the surface-limited magnesium pool is available during magnesium depletion. The change in size of the nonexchangeable bone magnesium pool appeared to be more related to the duration of magnesium depletion than the change in serum magnesium levels. The fall in magnesium concentration in this pool is probably a consequence of continuing formation of low magnesium bone during the depletion period.

摘要

开展了体内和体外研究,以表征可交换骨镁池,并确定年龄和镁缺乏对骨镁有何影响。体外可洗脱的骨镁与体内可交换骨镁的大小之间存在高度显著的相关性(r = 0.97)。为了表明可交换骨镁是表面受限的骨镁,在体内给予放射性镁4小时后进行洗脱研究。洗脱液中的比活性是死亡时血清中比活性的85%,这表明可洗脱和可交换骨镁池在很大程度上是同一个池。骨镁浓度随年龄增长而下降。骨镁的整体下降是表面受限部分减少的结果。由于已表明骨晶体随年龄增长而增大,导致表面积收缩,这将是对此发现最明显的解释。在镁缺乏期间,可交换池和不可交换池中的镁浓度均降低。可交换池中的分数变化远大于总骨镁或不可交换骨镁的变化,这表明在镁缺乏期间表面受限的镁池是可用的。不可交换骨镁池大小的变化似乎与镁缺乏的持续时间比与血清镁水平的变化更相关。该池中镁浓度的下降可能是在缺乏期持续形成低镁骨的结果。

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