Jones P J
School of Dietetics and Human Nutrition, McGill University, Montreal, Québec.
Obes Res. 1995 Mar;3 Suppl 1:41-8. doi: 10.1002/j.1550-8528.1995.tb00006.x.
Doubly labeled water (DLW) is an accurate, portable method for measuring free-living energy expenditure. However, under certain conditions shifts in baseline abundance of deuterium and oxygen-18 tracers used in the method may produce errors in derivation of both turnover (k) rates and calculated energy expenditure. Present objectives were to examine during what experimental situations baseline errors arise and to address means of correcting for such baseline shifts so that consequent errors in energy expenditure calculations are minimized. Under conditions where shifts in baseline abundance for deuterium and oxygen-18 parallel abundances corresponding to the natural meteoric water ratio, self-compensating changes in k values for both deuterium and oxygen will result in minimal error to the DLW energy expenditure calculations, provided that the dose ratio of isotopes also mimics the meteoric water line. However, in situations where relative shifts in abundance of each isotope across the measurement period are not in parallel relative to the natural meteoric water line, then the potential for larger DLW errors exists. Optimally, subjects should equilibrate with the new water source. Failing this, correction for shifting baseline can be accomplished by measuring isotopic abundance changes in a control group of subjects not given the DLW dose, but performing similar tasks and consuming the same diet as the group given DLW. Alternatively, theoretically based correction values can be calculated given knowledge of the abundances of the final drinking water and the interval time that subjects consumed the new fluid.
双标记水(DLW)是一种测量自由生活状态下能量消耗的准确且便携的方法。然而,在某些条件下,该方法中使用的氘和氧 - 18示踪剂的基线丰度变化可能会在周转率(k)和计算出的能量消耗推导过程中产生误差。当前的目标是研究在哪些实验情况下会出现基线误差,并探讨校正此类基线变化的方法,以便将能量消耗计算中的后续误差降至最低。在氘和氧 - 18的基线丰度变化与对应于天然雨水比例的丰度平行的条件下,氘和氧的k值的自补偿变化将导致DLW能量消耗计算的误差最小,前提是同位素的剂量比也模拟雨水线。然而,在测量期间每种同位素的丰度相对变化相对于天然雨水线不平行的情况下,则存在较大的DLW误差的可能性。最佳情况下,受试者应与新水源达到平衡。若无法做到这一点,可以通过测量未给予DLW剂量但执行类似任务且饮食与给予DLW的组相同的对照组受试者的同位素丰度变化来完成对基线变化的校正。或者,在已知最终饮用水的丰度和受试者消耗新液体的间隔时间的情况下,可以计算基于理论的校正值。