Abstract
Objective:
The definition of bronchopulmonary dysplasia (BPD) among very-low birth weight (VLBW) infants is based upon oxygen requirement at 36 weeks gestation, but oxygen may be required at altitude because of hypoxia. This study determined the effect of altitude on BPD rates.
Study Design:
For 63 VLBW infants at high altitude, oxygen concentrations were measured by a hood oxygenation test (HOT) and BPD rates were determined with altitude adjustment.
Result:
BPD rates before and after altitude adjustment were 71.8 and 26.7%, respectively. Of oxygen-dependent infants analyzed by HOT, 33.3% needed room air. HOT oxygen requirement correlated with gestational age of last apnea episode (r=0.42, P<0.001).
Conclusion:
Although BPD rates may be adjusted for altitude with the HOT, the test does not accurately predict clinical oxygen need. Persistent requirement for supplemental oxygen beyond that needed in the HOT may be partially due to immaturity of respiratory control mechanisms.
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Acknowledgements
The author wishes to thank Sue Danielson for assistance with data tabulation.
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Appendix
Appendix
Calculation of oxygen concentration required at altitude to simulate an oxygen concentration at sea level
The behavior of gases is governed by the Ideal Gas Equation:
where P=pressure, V=volume, n=number of moles, R=ideal gas constant, and T=temperature.
At sea level (s) and altitude (a), gas may be described by respective equations
and
Dividing the equation at altitude by the equation at sea level yields
Assuming constant temperature and volume (constant tidal volume and minute ventilation) yields
This equation gives the ratio of the number of oxygen molecules in a given volume at altitude to the number in the same volume at sea level. In Denver Pa=630 mm Hg and at sea level Ps=760 mm Hg. Therefore, in Denver there are only 630/760=0.829 as many oxygen molecules in a given volume of air as there are at sea level. The inverse of this ratio allows the calculation of the number of additional molecules of oxygen, or alternatively the fraction of inspired oxygen (FIO2)a, required at a given altitude to simulate an (FIO2)s at sea level: (FIO2)a=(FIO2)s (Ps/Pa). For room air at sea level (FIO2)s is 0.21. So for Denver, Ps/Pa=1.21 and (FIO2)a=0.253 to simulate room air at sea level.
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Britton, J. Altitude, oxygen and the definition of bronchopulmonary dysplasia. J Perinatol 32, 880–885 (2012). https://doi.org/10.1038/jp.2012.6
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DOI: https://doi.org/10.1038/jp.2012.6
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