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This paper presents a high-throughput method for the simultaneous determination of deuterium and oxygen-18 (18O) enrichment of water samples isolated from blood. This analytical method enables rapid and simple determination of these enrichments of microgram quantities of water. Water is converted into hydrogen and carbon monoxide gases by the use of a high-temperature conversion elemental analyzer (TC-EA), that are then transferred on-line into the isotope ratio mass spectrometer. Accuracy determined with the standard light Antartic precipitation (SLAP) and Greenland ice sheet precipitation (GISP) is reliable for deuterium and 18O enrichments. The range of linearity is from 0 up to 0.09 atom percent excess (APE, i.e. -78 up to 5725 delta per mil (dpm)) for deuterium enrichment and from 0 up to 0.17 APE (-11 up to 890 dpm) for 18O enrichment. Memory effects do exist but can be avoided by analyzing the biological samples in quintuplet. This method allows the determination of 1440 samples per week, i.e. 288 biological samples per week.

Whole body protein turnover and energy expenditure before and during an oral glucose tolerance test (1 g/kg body wt) were studied on separate occasions in six healthy young men before and during 3 days of simulated microgravity using the 6 degrees head-down tilt (HDT) method. After 42-47 h of HDT, basal insulin concentrations increased significantly from 9.4 +/- 1.9 to 13.1 +/- 0.1 microU/ml (P < 0.002). No significant differences in glycemia, insulinemia, or free fatty acid concentrations were observed in response to the oral glucose load. With HDT, increases were observed in basal postabsorptive resting metabolic rate (8%; P < 0.05), lipid oxidation (33 +/- 2 to 51 +/- 5 mg/min; P < 0.02), and the thermic effect of glucose (7.7 +/- 1 to 10.7 +/- 0.6%; not significant). Protein turnover (arithmetic mean of ammonia and urea flux rates) was unchanged by HDT, but a significant increase was seen when calculated from ammonia alone (P < 0.02). The present data show that HDT results in an increased energy requirement through elevations in both the basal metabolic rate and the thermic response to food ingestion. These changes may have been brought about by a cephalic shift of body fluids similar to that experienced in microgravity.

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