Davies S, Spanel P, Smith D
Centre for Science and Technology in Medicine, School of Postgraduate Medicine, Keele University, UK.
Physiol Meas. 2001 Nov;22(4):651-9. doi: 10.1088/0967-3334/22/4/301.
The ability to measure total body water accurately, non-invasively and rapidly with results that are immediately available would represent an important advance in body composition research. Flowing afterglow mass spectrometry (FA-MS) has been developed to enable immediate measurement of deuterium content in breath water from single exhalations, which when combined with oral D2O loading enables measurement of total body water. We report here its first use in normal subjects, demonstrating the dispersal kinetics of deuterium in the body by monitoring deuterium in breath water following ingestion. Ten studies were performed in six normal subjects. After obtaining baseline samples, each subject ingested 0.3 g x kg(-1) of 99.9% pure D2O. Subsequently, breath samples were obtained every 3-5 minutes until equilibration had occurred. Three distinct phases in breath deuterium content were observed: an initial immediate peak due to HDO remaining in the oral cavity, a secondary peak reflecting gastrointestinal absorption and finally equilibration with the body water. The incremental increase in breath deuterium abundance between baseline and equilibration was used to calculate the total body water. Mathematical fitting of this final equilibration phase demonstrated that the measured deuterium abundance was within 0.2% of the ideal (asymptotic) value within 2 hours in all cases. We conclude that FA-MS is a powerful new method that, when combined with oral D2O loading, enables measurement of the dispersal kinetics of HDO and the calculation of total body water within 2 hours.
能够准确、无创且快速地测量全身水含量,并能立即获得结果,这将代表身体成分研究的一项重要进展。流动余辉质谱法(FA-MS)已被开发出来,用于立即测量单次呼气中呼出水中的氘含量,当与口服重水(D2O)负荷相结合时,可用于测量全身水含量。我们在此报告其在正常受试者中的首次应用,通过监测摄入后呼出水中的氘来证明氘在体内的扩散动力学。对6名正常受试者进行了10项研究。在获取基线样本后,每个受试者摄入0.3 g·kg-1的99.9%纯重水。随后,每3 - 5分钟采集一次呼气样本,直至达到平衡。观察到呼出氘含量有三个不同阶段:由于口腔中残留的重水(HDO)导致的初始即刻峰值,反映胃肠道吸收的第二个峰值,以及最终与身体水分达到平衡。利用基线与平衡之间呼出氘丰度的增量增加来计算全身水含量。对这个最终平衡阶段的数学拟合表明,在所有情况下,测量的氘丰度在2小时内都在理想(渐近)值的0.2%以内。我们得出结论,FA-MS是一种强大的新方法,当与口服重水负荷相结合时,能够在2小时内测量重水的扩散动力学并计算全身水含量。