Abstract
In clinical studies, the oxidation of 13C-labeled substrates to 13CO2 and the measurement of the appearance of excess 13CO2 in expiratory air has progressed to an increasingly common method as it is noninvasive and lacks the radiation exposure associated with the use of 14C. The collection of respiratory CO2 currently used occurs via trapping of CO2 in sodium hydroxide (trapping method), sometimes in conjunction with indirect calorimetry. The aim of the present study was to determine the accuracy of our direct nasopharyngeal sampling method for the collection of breath samples in preterm infants compared with the currently used trapping method. We present a method that simplifies the collection of breath samples in preterm infants. Seven preterm infants with a gestational age of 26–29 wk were studied on different postnatal days (range, 8–52 d) while receiving full enteral feeding. A primed constant 3-h intragastric infusion of [13C]bicarbonate was given, and breath samples were collected by means of direct nasopharyngeal sampling and by a sodium hydroxide trap simultaneously. Breath CO2 isotopic enrichments rose rapidly to reach a plateau by 120 min with <5% variation of plateau in both methods. 13CO2 breath isotopic enrichments obtained by the direct nasopharyngeal sampling method correlated highly (r2 = 0.933; p < 0.0001) with the trapping method. The Bland-Altman analysis showed no significant variability between the two methods and demonstrated that the 95% confidence interval is within ± 4.68 δ‰. These findings validate the simple method of direct nasopharyngeal sampling of expired air in neonates.
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Main
During the last three decades, stable isotopes have been used extensively to investigate whole-body protein metabolism in adults, children, and newborns (1–3). To determine the rate of substrate oxidation, the excretion of 13CO2 in expired air must be quantified. The rate of oxidation is calculated by multiplying the isotopic enrichment of CO2 in breath by the total rate of CO2 excreted, correcting for the incomplete recovery of 13C during an infusion of [13C]bicarbonate (1). This correction factor has to be used to adjust for the fractional recovery of CO2(4, 5). In addition, the V˙co2 needs to be measured.
Several methods are used to quantify V˙co2, but closed-circuit indirect calorimetry is the most commonly performed method and serves as gold standard for the estimation of V˙co2. This procedure requires the patient to breathe via a mouthpiece with the nares occluded or via a hood that catches all expired CO2(6). However, interpretation of the results obtained from indirect calorimetry may be difficult in particular. For instance, results are difficult to interpret when there is an unmeasured loss of expired gasses because of the use of uncuffed leaking endotracheal tubes in mechanically ventilated neonates (7). In addition, there is an increased possibility of error in the indirect calorimeter determination of oxygen consumption and V˙co2 with the low volumes of respiratory gas exchanged in small neonates (8) and the higher fraction of inspired oxygen used in critically ill patients (9). This error is of such a significant degree that the use of indirect calorimetry is not recommended in patients receiving more than 0.60 fraction of inspired oxygen (10).
Another method for measuring V˙co2 involves the infusion of a 14C-labeled substrate and the measurement of its specific activity and the rate of excretion of 14CO2 in breath for a period at isotopic steady-state (11). However, the use of radioactive isotopes in children is prohibited.
Numerous studies described the use of dilution of 13CO2 during the infusion of [13C]bicarbonate to calculate CO2 production, which avoids the quantification of total expired air (4, 12). However, this tracer technique uses a relatively complicated method to collect expired air. Breath samples must be collected using a closely fitted facemask and an inlet-outlet system with a low dead volume. Thereafter, the collected expired air has to pass through an all-glass spiral condenser containing sodium hydroxide. After liberating CO2 by adding phosphoric acid to the solution, the CO2 can be stored in a septum-capped tube until analysis (13). During all these procedures to liberate CO2, the fraction of 13CO2 might be decreased, resulting in an underestimation of the substrate oxidation.
To collect breath samples from preterm infants in a suitable manner, we applied the direct nasopharyngeal sampling technique previously described by Perman et al.(14). This method has been used in older children for the noninvasive diagnosis of sucrose or lactose malabsorption by a hydrogen breath test, and in preterm infants for the collection of expiratory air after administration of 13C-labeled substrates (14–16). However, in preterm infants, the direct nasopharyngeal sampling method has never been validated for the use in substrate oxidation studies. The direct sampling approach offers the advantage of being simple and not time-consuming, making it appropriate for use in preterm infants in combination with [13C]bicarbonate stable isotope dilution technique to estimate the CO2 production. Validation of such a method would provide a technique that could be used in a variety of clinical investigations in neonates and children.
The purpose of this study was to determine whether the direct nasopharyngeal sampling technique for the collection of expired air could be used to estimate CO2 production in preterm infants. We validated this technique against the method using CO2 trapping in sodium hydroxide for collection of expiratory air after [13C]bicarbonate infusion in preterm infants.
METHODS
Subjects.
Subjects included seven preterm infants admitted to the neonatal intensive care unit of the Erasmus MC-Sophia Children's Hospital. The study protocol was reviewed and approved by the Erasmus-MC Institutional Review Board, and written and informed consent was obtained from the parents of the preterm infants.
Direct nasopharyngeal sampling method and trapping method.
The collection of expired air was obtained by two different methods, i.e. the direct nasopharyngeal sampling method and the trapping method. In the direct nasopharyngeal sampling technique for the collection of expired air, we used a 6F gastric tube (6 Ch Argyle; Sherwood Medical, Tullamore, Ireland) as a collection device, which was placed carefully for 1 to 1.5 cm into the nasopharynx. When the infant received supplemental oxygen by nasal prong, the oxygen air had to pass a soda-lime filter (Erich Jaeger GmbH & Co. KG, Wurzburg, Germany) before entering the nasopharynx to supply CO2-free air. While observing the patient's normal breathing pattern, the examiner repeatedly aspirated 1 mL of each tidal volume late in the expiratory phase from the nasal prong connected to a 10-mL plastic syringe until 10 mL was obtained. Aliquots were transferred by syringe to a 10-mL Vacutainer (Van Loenen Instruments, Zaandam, The Netherlands).
The trapping method has been described for V˙co2 measurements in neonates (13, 17). In this method, breath samples are collected via a closely fitted facemask or canopy, which is placed around the head and chest of the neonate. The baby's head and neck were placed under the transparent Perspex canopy, and a partial seal is created by tucking the attached flexible material beneath the body and mattress to prevent any air leaks. We used a canopy as is used for indirect calorimetry studies in infants (18). An inlet-outlet system with a low dead volume is used to avoid dilution of the carbon dioxide <1.5–2.0%. Next, the collected expired air has to pass a sample of air leaving the ventilated hood through an all-glass spiral condenser, containing 10 mL of 1 M sodium hydroxide (Merck, Darmstadt, Germany). After liberating CO2 by adding phosphoric acid (Merck) to the solution, the CO2 can be stored in septum-capped tubes until analysis.
Validation of the collection method.
To demonstrate that the isotopic enrichment in the expired air collected by the direct nasopharyngeal sampling method showed a consistent relationship and to show that this collection of expired air is a reliable technique, comparison with the trapping method was performed. Validation of direct nasopharyngeal sampling technique and the trapping method was achieved by simultaneously obtaining duplicate paired samples of expired air according to both methods in seven clinically stable preterm infants without ventilatory support.
Tracer protocol.
After baseline expired breath samples were obtained according to both methods (Fig. 1), a primed (10.02 μmol/kg), 3-h continuous intragastric infusion (10.02 μmol·kg−1·h−1) of sterile pyrogen-free sodium [1-13C]bicarbonate (99 mol%13C; Cambridge Isotopes, Woburn, MA, U.S.A.) was administered. Five sets of duplicate CO2 breath samples were collected at 15-min intervals during the last hour of infusion by using both sampling techniques. Breath CO2 isotopic enrichment was plotted against time, and the plateau defined according to the convention of taking four or more consecutive points with a coefficient of variation of <5%.
Analytical methods.
Isotopic enrichment of expired CO2 was measured by monitoring ions at m/e 44 and 45 with a continuous flow isotope ratio mass spectrometer (ABCA; Europa Scientific, Van Loenen Instruments, Leiden, The Netherlands) (19). The ratio of the signals from the ionized species 13CO2 and 12CO2 each focused on one of the dual spectrometers is recorded and compared with the natural abundance of CO2 gas of known isotopic composition relative to the standard Pee Dee Belemnite (PDB). The results of this differential measurement are expressed as the delta per mille (δ‰) difference between the 13CO2/12CO2 ratio of the sample and standard (20).
where Ru is the difference between the 13CO2/12CO2 ratio of the sample, and Rs is the difference between the 13CO2/12CO2 ratio of the standard.
Steady-state values were obtained by determining the average CO2 isotopic enrichment after reaching plateau as previously described (21). RaCO2 was calculated using the standard steady-state equation (22):
where iB is the infusion rate of sodium [13C]bicarbonate (μmol·kg−1·h−1), IEI is the enrichment (mole percent excess) of [13C]bicarbonate in the bicarbonate infusate, and IEB is the 13CO2 enrichment in expiratory air at plateau during the sodium [13C]bicarbonate infusion (mole percent excess).
Statistics.
All values are expressed in mean ± SD. Statistical analyses were performed by ANOVA, t test, and Pearson correlation. Significance was determined as p < 0.05. Bland-Altman analysis was performed to test the variability between the two sampling methods (23).
RESULTS
All infants were appropriate for gestational age (median gestational age, 28 wk; range, 26–29 wk;Table 1). Seven patients who breathed spontaneously were studied; six of them received supplemental oxygen by a nasal prong. All infants were clinically stable at the time of the study. The median body weight at the time of study period was 1.2 kg (range, 1.0–1.5 kg), and the median postnatal age was 28 d (range, 8–52 d).
The estimated CO2 production was 37.04 ± 5.99 mmol·kg−1·h−1). Isotopic steady-state was achieved during sodium [13C]bicarbonate infusion with a coefficient of variation of 4.1% in the direct sampling method and 4.8% in the trapping method (Fig. 2). More importantly, the delta per mille difference determined from the direct nasopharyngeal sampling method correlated highly (r2 = 0.933; p < 0.0001) with the delta per mille difference obtained by the trapping technique. Furthermore, Bland-Altman analysis (Fig. 3) demonstrated agreement between the two methods to within ± 4.68 δ‰, i.e. 95% confidence interval.
DISCUSSION
The present study describes a methodology for the collection of expired air in preterm infants after administration of 13C-labeled material. In preterm neonates, isotopic steady-state of 13CO2 in breath obtained by our direct nasopharyngeal sampling technique during a [13C]bicarbonate infusion agreed closely with the isotopic steady-state obtained with the trapping technique during a [13C]bicarbonate infusion. This is demonstrated by the highly significant correlation between the measured values acquired from both methods. Therefore, in neonates the direct nasopharyngeal sampling technique can be used for the measurement of CO2 isotopic enrichment, which is necessary for estimation of V˙co2 and the quantification of oxidation of labeled substrates.
To determine the accuracy and precision of our technique in each individual subject in comparison with the trapping method we used the Bland-Altman analysis. Furthermore, by using this analysis we could assess the variability between the two methods (23). As shown in Figure 3, the 95% confidence interval of the two methods vary within an acceptable ± 4.68 δ‰. In other words, there is less then 5% probability that the two methods differ more than this amount.
Although we validated our direct sampling method only in nonventilated infants, we speculate that this technique will work in ventilated infants. Instead of sampling directly from the nasopharynx, expired air has to be withdrawn from the ventilation tube. The clinical applications of the direct sampling technique for the collection of breath are extensive, because whole-body flux and oxidation rates of nutrients can be quantified in adults and infants from primed constant infusion studies using 13C-labeled substrates with the collection of expired air (1–3). The methodology for measuring in vivo oxidation of substrates with the use of 13C-labeled material in clinical studies has been developed with the use of isotope ratio mass spectrometry analysis. The direct sampling method can also be used in breath tests for the noninvasive diagnosis of sucrose or lactose malabsorption and gastric emptying.
The excretion of labeled CO2 in breath after administration of 13C-labeled substrates is a function of the physical variables involved in CO2 metabolism, the kinetics of metabolism, and the delay associated with the passage through the whole-body bicarbonate pool before its expiration in the breath (24). For example, the labeled CO2 is temporarily retained in the bicarbonate pool of the bone, in larger organic molecules, and in smaller amounts in feces, sweat, and urine (24). That this bicarbonate pool is limited is shown by an almost complete recovery of CO2 during an extended infusion (24–48 h) and collection of expired air (25). In short-lasting studies in neonates, the CO2 retention varies between 70 and 84% and is correlated with the energy intake, metabolic rate, and V˙co2(5). Therefore, to determine the rate of oxidation of a labeled substrate, a correction factor is commonly used in the calculations (5). However, in previous studies in preterm infants without signs of infection or respiratory distress, we have shown that the correction factor can be left out assuming a constant V˙co2 for a few hours and by the use of a sequential [13C]bicarbonate and 13C-labeled substrate infusion (13, 17). Therefore, our direct sampling technique can be used very well to collect expired CO2 for mass spectrometric analysis.
CONCLUSIONS
We conclude that the presently described direct nasopharyngeal sampling method for the collection of expired air in preterm neonates is as good as other previously described breath collection methods for the calculation of substrate oxidation. This method is simple to use, and should provide new opportunities to study metabolism of various substrates in preterm infants, children, and adults.
Abbreviations
- V˙co2:
-
total carbon dioxide production
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Acknowledgements
The authors thank prof.dr. H.A. Büller for helpful comments and review of the manuscript. We also thank the parents who consented for their babies to participate in the study.
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Supported by The Sophia Foundation of Scientific Research (Kröger Foundation), the Royal Netherlands Academy of Arts and Science (Ter Meulen Fund), and the Nutricia Research Foundation.
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van der Schoor, S., de Koning, B., Wattimena, D. et al. Validation of the Direct Nasopharyngeal Sampling Method for Collection of Expired Air in Preterm Neonates. Pediatr Res 55, 50–54 (2004). https://doi.org/10.1203/01.PDR.0000099792.66562.7E
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DOI: https://doi.org/10.1203/01.PDR.0000099792.66562.7E