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1 Human Performance Laboratory, School of Sport and Exercise Sciences, The University of Birmingham, Birmingham, United Kingdom
2 School of Biosciences, The University of Birmingham, Birmingham, United Kingdom
3 City Hospital, Physics and Nuclear Medicine, Birmingham, United Kingdom
* To whom correspondence should be addressed. E-mail: a.e.jeukendrup{at}bham.ac.uk.
The purpose of this study was to assess the level of agreement between two techniques commonly used to measure exogenous carbohydrate oxidation (CHOEXO). To accomplish this seven healthy male subjects (24 ± 3 y, 74.8 ± 2.1 kg, 62 ± 4 mL/kg/min) exercised at 50 % of their peak power for 120 min on 2 occasions. During these exercise bouts subjects ingested a solution containing either 144 g glucose (8.7 % w.v. GLU) or water (WATER). The glucose solution contained trace amounts of both [U-13C]-glucose and [U-14C]-glucose to allow CHOEXO to be quantified simultaneously. The water trial was used to correct for background 13C enrichment. 13C appearance in the expired air was measured using isotope ratio mass spectrometry while 14C appearance was quantified by trapping expired CO2 in solution (using hyamine hydroxide) and adding a scintillator before counting radioactivity. CHOEXO measured with 13C-glucose (13C-CHOEXO) was significantly greater than CHOEXO measured with 14C-glucose (14C-CHOEXO) from 30-120 min. There was a 15 ± 4 % difference between 13C-CHOEXO and 14C-CHOEXO such that the absolute difference increased with the magnitude of CHOEXO. Further investigations suggest that the difference is not due to losses of CO2 from the trapping solution prior to counting or an underestimation of the 'strength' of the trapping solution. Previous research suggests that the degree of isotopic fractionation is small (Kalhan et al. (1977)). Therefore, the explanation for the discrepancy in calculated exogenous CHO oxidation remains to be fully understood.
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