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海平面及模拟高原环境下正常人运动时的通气-灌注不均

Ventilation-perfusion inequality in normal humans during exercise at sea level and simulated altitude.

作者信息

Gale G E, Torre-Bueno J R, Moon R E, Saltzman H A, Wagner P D

出版信息

J Appl Physiol (1985). 1985 Mar;58(3):978-88. doi: 10.1152/jappl.1985.58.3.978.

Abstract

To investigate the effects of both exercise and acute exposure to high altitude on ventilation-perfusion (VA/Q) relationships in the lungs, nine young men were studied at rest and at up to three different levels of exercise on a bicycle ergometer. Altitude was simulated in a hypobaric chamber with measurements made at sea level (mean barometric pressure = 755 Torr) and at simulated altitudes of 5,000 (632 Torr), 10,000 (523 Torr), and 15,000 ft (429 Torr). VA/Q distributions were estimated using the multiple inert gas elimination technique. Dispersion of the distributions of blood flow and ventilation were evaluated by both loge standard deviations (derived from the VA/Q 50-compartment lung model) and three new indices of dispersion that are derived directly from inert gas data. Both methods indicated a broadening of the distributions of blood flow and ventilation with increasing exercise at sea level, but the trend was of borderline statistical significance. There was no change in the resting distributions with altitude. However, with exercise at high altitude (10,000 and 15,000 ft) there was a significant increase in dispersion of blood flow (P less than 0.05) which implies an increase in intraregional inhomogeneity that more than counteracts the more uniform topographical distribution that occurs. Since breathing 100% O2 at 15,000 ft abolished the increased dispersion, the greater VA/Q mismatching seen during exercise at altitude may be related to pulmonary hypertension.

摘要

为研究运动和急性暴露于高海拔对肺通气/灌注(VA/Q)关系的影响,对9名年轻男性在静息状态及在自行车测力计上进行的三种不同运动水平下进行了研究。在低压舱中模拟海拔高度,在海平面(平均气压 = 755托)以及模拟海拔5000英尺(632托)、10000英尺(523托)和15000英尺(429托)时进行测量。使用多惰性气体消除技术估算VA/Q分布。通过自然对数标准差(源自VA/Q 50分区肺模型)和直接从惰性气体数据得出的三个新的离散指数评估血流和通气分布的离散情况。两种方法均表明,在海平面随着运动增加,血流和通气分布变宽,但该趋势具有边缘统计学意义。静息分布随海拔高度无变化。然而,在高海拔(10000英尺和15000英尺)运动时,血流离散度显著增加(P小于0.05),这意味着区域内不均匀性增加,超过了所出现的更均匀的地形分布。由于在15000英尺呼吸100%氧气可消除增加的离散度,在高海拔运动期间出现的更大的VA/Q不匹配可能与肺动脉高压有关。

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