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通过测量呼出一氧化碳浓度评估血红素周转的昼夜节律。

Diurnal rhythm of heme turnover assessed by breath carbon monoxide concentration measurements.

作者信息

Levitt M D, Ellis C, Levitt D G

机构信息

Research Service, Minneapolis Veterans Affairs Medical Center, MN 55417.

出版信息

J Lab Clin Med. 1994 Sep;124(3):427-31.

PMID:8083586
Abstract

Measurements of pulmonary carbon monoxide (CO) excretion can be used as a quantitative indicator of heme turnover. We determined whether a diurnal variation of heme turnover occurs by using a recently described technique that estimates breath CO excretion from measurements of alveolar CO concentration corrected for environmental CO to yield an endogenous PCO. This simple technique, unlike the previously employed rebreathing method, makes it possible to repeatedly measure CO excretion throughout a 24-hour period. Nine studies in seven healthy adult subjects demonstrated a diurnal rhythm of CO excretion with a peak excretion rate at about noon that was 26% greater than the nadir, which occurred at about midnight. The rhythm of CO production underlying the observed breath CO excretion was calculated to have an amplitude of about twice that of CO excretion and a phase shift relative to excretion of about 4 hours. We conclude that a diurnal variation in the rate of heme turnover occurs, and when CO determinations are used to assess minor alterations in heme turnover, consideration must be given to the time of day at which the measurements are obtained.

摘要

肺一氧化碳(CO)排泄量的测量可作为血红素周转的定量指标。我们通过一种最近描述的技术来确定血红素周转是否存在昼夜变化,该技术通过对环境CO进行校正后测量肺泡CO浓度来估算呼出CO量,从而得出内源性PCO。与之前采用的重复呼吸法不同,这种简单的技术使得在24小时内反复测量CO排泄量成为可能。对7名健康成年受试者进行的9项研究表明,CO排泄存在昼夜节律,排泄率峰值出现在中午左右,比午夜左右出现的最低点高26%。据计算,观察到的呼出CO排泄背后的CO产生节律的幅度约为CO排泄幅度的两倍,且相对于排泄有大约4小时的相位偏移。我们得出结论,血红素周转速率存在昼夜变化,当使用CO测定来评估血红素周转的微小变化时,必须考虑测量的时间。

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