Bone mineral turnover in a patient with osteogenesis imperfecta estimated by fluoride excretion.

G B Forbes, D R Taves, F A Smith, R W Kilpper
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引用次数: 5

Abstract

A child with severe osteogenesis imperfecta was treated with NaF for 8 years, at the end of which time his iliac bone contained 29 mg F/g Ca. Urine F was assayed at intervals for 4.5 years after discontinuing treatment. After the first few days the decline in urinary F excretion can be described by a two component exponential function, with half-times of 5.4 months (10%) and 8.9 years (90%). The latter half-time value is of the same order of magnitude as those observed for F and other "bone-seeking" elements in normal subjects, which suggests that the turnover rate of bone mineral is normal in this disease. Three methods for estimating the attained body F burden at the end of NaF treatment--namely, metabolic balance, bone biopsy, and integration of the exponential function--yielded comparable values.

通过氟化物排泄估计成骨不全患者的骨矿物质转换。
一名患有严重成骨不全症的儿童接受NaF治疗8年,治疗结束时其髂骨含有29 mg F/g Ca。停止治疗后每隔4.5年检测一次尿F。在最初几天后尿氟排泄的下降可以用双分量指数函数来描述,半衰期为5.4个月(10%)和8.9年(90%)。后半时间值与正常受试者中观察到的F和其他“寻骨”元素具有相同的数量级,这表明该疾病中骨矿物质的周转率正常。估计NaF治疗结束时获得的体F负荷的三种方法——即代谢平衡、骨活检和指数函数的整合——产生了可比较的值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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