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Lung Diffusion in a 14-Day Swimming Altitude Training Camp at 1850 Meters

Bibliographic Data

ID15510855
AuthorsIker García (0000-0003-1844-5705, Universitat de Barcelona), Franchek Drobnic (0000-0001-8594-4294, Medical Services Shenhua Greenland FC, Shanghai 201315, China), Teresa Galera (Universitat de Barcelona), Victoria Pons (0000-0001-6712-1139, Centre d’Alt Rendiment (CAR) de Sant Cugat, Av. Alcalde Barnils s/n, E-08173 Sant Cugat del Vallés, 08174 Barcelona, Spain), Ginés Viscor (0000-0003-4942-2346, Universitat de Barcelona, corresponding author)
Year2020
Volume17
Issue10
Pages3501-3501
Publication date2020-05-17
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueInternational Journal of Environmental Research and Public Health (JOURNAL)
Journal identifiersISSN: 1661-7827 • E-ISSN: 1660-4601
PublisherMultidisciplinary Digital Publishing Institute (PUBLISHER • CH)
DOI10.3390/ijerph17103501
PMID32429560
OpenAlexW3025364881
LanguageEN
Citations received1
References cited58

Swimming exercise at sea level causes a transient decrease in lung diffusing capacity for carbon monoxide (DL CO ). The exposure to hypobaric hypoxia can affect lung gas exchange, and hypoxic pulmonary vasoconstriction may elicit pulmonary oedema. The purpose of this study is to evaluate whether there are changes in DL CO during a 14-day altitude training camp (1850 m) in elite swimmers and the acute effects of a combined training session of swimming in moderate hypoxia and 44-min cycling in acute normobaric severe hypoxia (3000 m). Participants were eight international level swimmers (5 females and 3 males; 17-24 years old; 173.5 ± 5.5 cm; 64.4 ± 5.3 kg) with a training volume of 80 km per week. The single-breath method was used to measure the changes in DL CO and functional gas exchange parameters. No changes in DL CO after a 14-day altitude training camp at 1850 m were detected but a decrease in alveolar volume (VA; 7.13 ± 1.61 vs. 6.50 ± 1.59 L; p = 0.005; d = 0.396) and an increase in the transfer coefficient of the lung for carbon monoxide (K CO ; 6.23 ± 1.03 vs. 6.83 ± 1.31 mL·min -1 ·mmHg -1 ·L -1 ; p = 0.038; d = 0.509) after the altitude camp were observed. During the acute hypoxia combined session, there were no changes in DL CO after swimming training at 1850 m, but there was a decrease in DL CO after cycling at a simulated altitude of 3000 m (40.6 ± 10.8 vs. 36.8 ± 11.2 mL·min -1 ·mmHg -1 ; p = 0.044; d = 0.341). A training camp at moderate altitude did not alter pulmonary diffusing capacity in elite swimmers, although a cycling session at a higher simulated altitude caused a certain degree of impairment of the alveolar-capillary gas exchange

Anesthesia · Cardiology · Diffusing capacity · DLCO · Effects of high altitude on humans · Hypobaric chamber · Hypoxia (environmental · Hypoxic pulmonary vasoconstriction · Lung · Lung function · Lung volumes · Oxygen · Pulmonary Diffusing Capacity · Pulmonary function testing · Cardiovascular and Diving-Related Complications · Chemistry · Chronic Obstructive Pulmonary Disease (COPD) Research · High Altitude and Hypoxia · Medicine · Anatomy · Internal Medicine

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Unique citing works1
Citations per year0.25
Citation span2022 - 2022 (1)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 1

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