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高压性心动过缓的机制。

Mechanisms of hyperbaric bradycardia.

作者信息

Lin Y C, Shida K K

机构信息

Department of Physiology, University of Hawaii, John A. Burns School of Medicine, Honolulu 96822.

出版信息

Chin J Physiol. 1988;31(1):1-22.

PMID:3067986
Abstract

Relative bradycardias have been reported to occur in humans both at rest and during exercise under a variety of hyperbaric conditions. Review of existing data reveals that there are two major mechanisms operating: one depends on hyperoxia and the other does not. While it is clear that hyperoxia produces bradycardia by a variety of well understood mechanisms, the non-oxygen-dependent causes of hyperbaric bradycardia have not been defined. Experimental results from animals studies have eliminated the involvement of increased ambient pressure and gas density in the development of hyperbaric bradycardia, in all normoxic conditions. This review considers two other possibilities, the altered respiratory pattern which may modify the HR secondarily, and circulatory deconditioning under hyperbaric environments, which masks the hyperbaric bradycardia. We propose that the return of a normal sea level HR following the initial bradycardia represents, in effect, bradycardia which would be seen if cardiovascular deconditioning were not present. It is concluded that hyperoxia is the major factor responsible for initiating and maintaining hyperbaric bradycardia, whereas non-oxygen dependent hyperbaric factors may alter respiratory patterns and secondarily cause a reduction in HR.

摘要

据报道,在各种高压环境下,人类在静息和运动时都会出现相对心动过缓。对现有数据的回顾表明,有两种主要机制在起作用:一种取决于高氧,另一种则不依赖高氧。虽然很明显高氧通过多种已被充分理解的机制导致心动过缓,但高压性心动过缓的非氧依赖性原因尚未明确。动物研究的实验结果排除了在所有常氧条件下环境压力和气体密度增加与高压性心动过缓发生有关。本综述考虑了另外两种可能性,即改变的呼吸模式可能继发改变心率,以及高压环境下的循环适应不良掩盖了高压性心动过缓。我们认为,初始心动过缓后恢复到正常海平面心率实际上代表了如果不存在心血管适应不良时会出现的心动过缓。得出的结论是,高氧是引发和维持高压性心动过缓的主要因素,而非氧依赖性高压因素可能改变呼吸模式并继发导致心率降低。

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