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在高海拔和海平面运动时的肺动脉压、心输出量和动脉血氧饱和度。

Pulmonary pressure, cardiac output, and arterial oxygen saturation during exercise at high altitude and at sea level.

机构信息

Cardiovascular Laboratory, High Altitude Research Institute, Peruvian University "Cavetano Heredia," Lima, Perú.

出版信息

Circulation. 1966 Feb;33(2):249-62. doi: 10.1161/01.cir.33.2.249.

Abstract

The response elicited by exercise on pulmonary pressure, cardiac output, and arterial oxygen saturation in 35 lifetime residents of high altitude has been studied at high altitude (14,900 feet above sea level), and 22 residents of low altitude have been studied at sea level. A procedure combining cardiac catheterization, arterial cannulation, and spirometry was carried out. The exercise was moderate and was performed in supine position using a bicycle ergometer, the work load being 300 kg-m/min/m2 and the average increase of the oxygen uptake being 4.7 times at sea level and 4.8 times at high altitude. Both at .sea level and at high altitude the cardiac output augmented during exercise proportionally to the increase in oxygen uptake, and thus followed the pattern of response described by other authors. The cardiac output as well as the oxygen intake, for the magnitude of exertion performed in this study, was almost the same at sea level and at high altitude. The cardiac output rose during exercise almost exclusively as a result of an increase in the heart rate, with the stroke volume remaining practically constant. Despite similar increase in cardiac output, the response of pulmonary pressure was smaller for sea-level subjects than for the high-altitude subjects. Increments of mean pulmonary pressure bf nearly 50% and 100% were observed on exercise at sea level and at high altitude, respectively. During exercise the arterial oxygen saturation did not change in the sea-level studies, but decreased significantly in the high-altitude studies. The decrement observed in high-altitude residents is related to a fall in arterial pO2 which at resting conditions is placed on the steep part of the oxygen dissociation curve.

摘要

本研究旨在探讨长期居住在高原(海拔 14900 英尺)的 35 名居民和低海拔(海平面)的 22 名居民在运动时对肺动脉压、心输出量和动脉血氧饱和度的反应。采用心脏导管插入术、动脉插管术和肺量测定法进行了一项联合程序。运动强度适中,在仰卧位使用自行车功量计进行,负荷为 300kg-m/min/m2,平均耗氧量在海平面和高原分别增加了 4.7 倍和 4.8 倍。在海平面和高原,心输出量随着耗氧量的增加而成比例增加,因此遵循了其他作者描述的反应模式。在本研究中进行的运动强度下,心输出量和耗氧量在海平面和高原几乎相同。心输出量在运动期间几乎完全由于心率增加而增加,而每搏量保持几乎不变。尽管心输出量增加相似,但肺动脉压的反应在海平面组中小于高原组。在海平面和高原运动时,平均肺动脉压分别增加了近 50%和 100%。在海平面研究中,运动期间动脉血氧饱和度没有变化,但在高原研究中显著下降。在高原居民中观察到的下降与动脉 pO2 下降有关,在静息状态下,动脉 pO2 处于氧离解曲线的陡峭部分。

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