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高原屏气潜水的心血管效应。

Cardiovascular effects of breath-hold diving at altitude.

机构信息

Master in Underwater and Hyperbaric Medicine, Sant'Anna School of Advanced Studies, Pisa - Italy.

CNR Institute of Clinical Physiology, Pisa - Italy.

出版信息

Undersea Hyperb Med. 2024 Second Quarter;51(2):189-196.

PMID:38985155
Abstract

Hypoxia, centralization of blood in pulmonary vessels, and increased cardiac output during physical exertion are the pathogenetic pathways of acute pulmonary edema observed during exposure to extraordinary environments. This study aimed to evaluate the effects of breath-hold diving at altitude, which exposes simultaneously to several of the stimuli mentioned above. To this aim, 11 healthy male experienced divers (age 18-52y) were evaluated (by Doppler echocardiography, lung echography to evaluate ultrasound lung B-lines (BL), hemoglobin saturation, arterial blood pressure, fractional NO (Nitrous Oxide) exhalation in basal condition (altitude 300m asl), at altitude (2507m asl) and after breath-hold diving at altitude. A significant increase in E/e' ratio (a Doppler-echocardiographic index of left atrial pressure) was observed at altitude, with no further change after the diving session. The number of BL significantly increased after diving at altitude as compared to basal conditions. Finally, fractional exhaled nitrous oxide was significantly reduced by altitude; no further change was observed after diving. Our results suggest that exposure to hypoxia may increase left ventricular filling pressure and, in turn, pulmonary capillary pressure. Breath-hold diving at altitude may contribute to interstitial edema (as evaluated by BL score), possibly because of physical efforts made during a diving session. The reduction of exhaled nitrous oxide at altitude confirms previous reports of nitrous oxide reduction after repeated exposure to hypoxic stimuli. This finding should be further investigated since reduced nitrous oxide production in hypoxic conditions has been reported in subjects prone to high-altitude pulmonary edema.

摘要

在暴露于特殊环境中时,会观察到急性肺水肿,其发病机制途径为体力活动时肺部血管中血液集中、缺氧以及心输出量增加。本研究旨在评估屏气潜水对高原的影响,因为这种潜水同时会暴露于上述多种刺激因素。为此,我们评估了 11 名健康的有经验潜水员(年龄 18-52 岁)(通过多普勒超声心动图、肺部超声评估评估超声肺部 B 线(BL)、血红蛋白饱和度、动脉血压、基础条件下(海拔 300 米)、海拔 2507 米)和海拔屏气潜水后的呼出气一氧化氮分数(一氧化氮)。在高原时,E/e' 比值(左心房压力的多普勒超声心动图指数)显著增加,潜水后无进一步变化。与基础条件相比,潜水后 BL 数量显著增加。最后,呼出气中一氧化氮分数在海拔高度显著降低;潜水后无进一步变化。我们的结果表明,缺氧暴露可能会增加左心室充盈压,并进而增加肺毛细血管压力。在高原进行屏气潜水可能会导致间质水肿(如 BL 评分所评估的),这可能是因为潜水期间的体力活动。在高原时呼出气中一氧化氮的减少证实了先前关于反复暴露于低氧刺激时一氧化氮减少的报告。由于在易发生高原肺水肿的人群中,低氧条件下一氧化氮生成减少的报道,因此应进一步研究这一发现。

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