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示踪放射性铁与体内铁的平衡

Equilibration of tracer radioiron with body iron.

作者信息

Charlton R W, Fatti L P, Lynch S R, Torrance J D, Bothwell T H

出版信息

Clin Sci (Lond). 1980 Jan;58(1):93-100. doi: 10.1042/cs0580093.

Abstract
  1. The degree to which a tracer quantity of 55Fe bound to transferrin and introduced into the plasma 36 months previously had equilibrated with the body iron was studied in a subject who was phlebotomized repeatedly until iron-deficiency anaemia developed. 2. Analysis of the results with two mathematical models showed that equilibration with haemoglobin iron and storage iron was complete. 3. Estimates of the quantity of iron initially stored in the body by three different methods yielded values of 37.3, 33.1 and 34.8 mmol. 4. Since the previously determined mean initial plasma ferritin concentration was 185 micrograms/1 (462 pmol/1), there was 0.179-0.197 mmol of stored iron per 1 microgram of plasma ferritin/1. 5. The study suggests that the assumption on which currently accepted values for daily body iron loss were calculated is valid.
摘要
  1. 研究人员在一名受试者身上进行了实验,该受试者反复进行静脉放血直至出现缺铁性贫血,以此来探究36个月前注入血浆的与转铁蛋白结合的微量55Fe与体内铁达到平衡的程度。2. 运用两种数学模型对结果进行分析,结果表明与血红蛋白铁和储存铁的平衡已完成。3. 通过三种不同方法估算出的体内最初储存的铁量分别为37.3、33.1和34.8毫摩尔。4. 由于先前测定的平均初始血浆铁蛋白浓度为185微克/升(462皮摩尔/升),每1微克血浆铁蛋白/升对应0.179 - 0.197毫摩尔的储存铁。5. 该研究表明,目前计算每日身体铁流失的公认值所依据的假设是有效的。

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