Singh Priya A, Orford Elise R, Donkers Kevin, Bluck Leslie J C, Venables Michelle C
Stable Isotope Facility, MRC Elsie Widdowson Laboratory, 120 Fulbourn Road, Cambridge, CB1 9NL, UK.
Rapid Commun Mass Spectrom. 2018 Dec 30;32(24):2122-2128. doi: 10.1002/rcm.8291.
Variation in O natural abundance can lead to errors in the calculation of total energy expenditure (TEE) when using the doubly labelled water (DLW) method. The use of Bayesian statistics allows a distribution to be assigned to O natural abundance, thus allowing a best-fit value to be used in the calculation. The aim of this study was to calculate within-subject variation in O natural abundance and apply this to our original working model for TEE calculation.
Urine samples from a cohort of 99 women, dosed with 50 g of 20% H O, undertaking a 14-day breast milk intake protocol, were analysed for O. The within-subject variance was calculated and applied to a Bayesian model for the calculation of TEE in a separate cohort of 36 women. This cohort of 36 women had taken part in a DLW study and had been dosed with 80 mg/kg body weight H O and 150 mg/kg body weight H O.
The average change in the δ O value from the 99 women was 1.14‰ (0.77) [0.99, 1.29], with the average within-subject O natural abundance variance being 0.13‰ (0.25) [0.08, 0.18]. There were no significant differences in TEE (9745 (1414), 9804 (1460) and 9789 (1455) kJ/day, non-Bayesian, Bluck Bayesian and modified Bayesian models, respectively) between methods.
Our findings demonstrate that using a reduced natural variation in O as calculated from a population does not impact significantly on the calculation of TEE in our model. It may therefore be more conservative to allow a larger variance to account for individual extremes.
使用双标记水(DLW)法时,氧自然丰度的变化会导致总能量消耗(TEE)计算出现误差。贝叶斯统计方法允许为氧自然丰度分配一个分布,从而在计算中使用最佳拟合值。本研究的目的是计算个体内氧自然丰度的变化,并将其应用于我们最初的TEE计算工作模型。
对99名女性组成的队列的尿液样本进行氧分析,这些女性摄入了50 g 20%的H₂¹⁸O,并遵循14天的母乳摄入方案。计算个体内方差,并将其应用于贝叶斯模型,以计算另一组36名女性的TEE。这36名女性参与了一项DLW研究,她们按体重每千克80 mg的H₂¹⁸O和每千克150 mg的H₂³H¹⁶O进行了剂量摄入。
99名女性的δ¹⁸O值平均变化为1.14‰(0.77)[0.99,1.29],个体内氧自然丰度的平均方差为0.13‰(0.25)[0.08,0.18]。不同方法之间的TEE无显著差异(非贝叶斯模型、Bluck贝叶斯模型和改良贝叶斯模型分别为9745(1414)、9804(1460)和9789(1455)kJ/天)。
我们的研究结果表明,在我们的模型中,使用根据群体计算得出的氧自然变化减少值对TEE的计算没有显著影响。因此,允许更大的方差以考虑个体极端情况可能更为保守。