Bosco Gerardo, Rizzato Alex, Martani Luca, Schiavo Simone, Talamonti Ennio, Garetto Giacomo, Paganini Matteo, Camporesi Enrico M, Moon Richard E
Environmental Physiology and Medicine Laboratory, Department of Biomedical Sciences, University of Padova, Padova, Italy.
ATIP Center for Hyperbaric Medicine, Padova, Italy.
Front Physiol. 2018 Nov 5;9:1558. doi: 10.3389/fphys.2018.01558. eCollection 2018.
The present study aimed to evaluate the partial pressure of arterial blood gases in breath-hold divers performing a submersion at 40 m. Eight breath-hold divers were enrolled for the trials held at "Y-40 THE DEEP JOY" pool (Montegrotto Terme, Padova, Italy). Prior to submersion, an arterial cannula in the radial artery of the non-dominant limb was positioned. All divers performed a sled-assisted breath-hold dive to 40 m. Three blood samplings occurred: at 10 min prior to submersion, at 40 m depth, and within 2 min after diver's surfacing and after resuming normal ventilation. Blood samples were analyzed immediately on site. Six subjects completed the experiment, without diving-related problems. The theoretically predicted hyperoxia at the bottom was observed in 4 divers out of 6, while the other 2 experienced a reduction in the partial pressure of oxygen (paO) at the bottom. There were no significant increases in arterial partial pressure of carbon dioxide (paCO) at the end of descent in 4 of 6 divers, while in 2 divers paCO decreased. Arterial mean pH and mean bicarbonate ( ) levels exhibited minor changes. There was a statistically significant increase in mean arterial lactate level after the exercise. Ours was the first attempt to verify real changes in blood gases at a depth of 40 m during a breath-hold descent in free-divers. We demonstrated that, at depth, relative hypoxemia can occur, presumably caused by lung compression. Also, hypercapnia exists at depth, to a lesser degree than would be expected from calculations, presumably because of pre-dive hyperventilation and carbon dioxide distribution in blood and tissues.
本研究旨在评估在40米深度进行屏气潜水的潜水员的动脉血气分压。招募了8名屏气潜水员参加在“Y - 40深度之乐”泳池(意大利帕多瓦省蒙特格罗托泰尔梅)进行的试验。在潜水前,在非优势肢体的桡动脉放置动脉插管。所有潜水员均进行了雪橇辅助的屏气潜水至40米深度。进行了三次血液采样:潜水前10分钟、40米深度时、潜水员浮出水面并恢复正常通气后2分钟内。血液样本在现场立即进行分析。6名受试者完成了实验,未出现与潜水相关的问题。6名潜水员中有4名在水底观察到理论预测的高氧状态,而另外2名在水底时氧分压(paO)降低。6名潜水员中有4名在潜水结束时动脉二氧化碳分压(paCO)没有显著升高,而2名潜水员的paCO降低。动脉平均pH值和平均碳酸氢盐( )水平变化较小。运动后动脉平均乳酸水平有统计学意义的升高。我们是首次尝试在自由潜水员屏气下潜至40米深度时验证血气的实际变化。我们证明,在深度时可能会出现相对低氧血症,推测是由肺压缩引起的。此外,在深度时存在高碳酸血症,其程度低于计算预期,推测是由于潜水前过度通气以及血液和组织中二氧化碳的分布。