Linér M H, Linnarsson D
Department of Physiology and Pharmacology, Karolinska Institutet, Stockholm, Sweden.
J Appl Physiol (1985). 1994 Aug;77(2):542-7. doi: 10.1152/jappl.1994.77.2.542.
Alveolar gas exchange was studied in 11 submerged subjects during and after 75-s breath holds with or without a transient increase of ambient pressure to 3 ATA (20 msw). During surface breath holds (SBH), cardiac index fell to 73% of eupneic control but was partially restored at depth to 88% of control during breath-hold dives (BHD). O2 uptake fell to 84% of control during SBH and was restored to control level during BHD. The turnover of O2 stores was much slower during SBH than during the ensuing recovery. Carbon dioxide store dynamics were markedly slowed after BHD. We conclude that SBH and BHD are associated with large shifts in tissue O2 and CO2 stores and that much of these shifts can be explained by primary circulatory events. The changes in turnover rate for tissue O2 and CO2 stores could not be explained by the cardiac index changes alone but were compatible with peripheralization of venous blood volume and preferential peripheral vasoconstriction induced by apnea with elevated intrathoracic pressure during SBH. The transient compression during BHD reversed these central and peripheral circulatory changes by counteracting the increase in intrathoracic pressure.
在11名潜水者中,研究了在75秒屏气期间及之后,在环境压力瞬态增加至3ATA(20米海水深度)或不增加的情况下的肺泡气体交换。在水面屏气(SBH)期间,心指数降至平静呼吸对照值的73%,但在屏气潜水(BHD)时深度处部分恢复至对照值的88%。在SBH期间,氧气摄取量降至对照值的84%,并在BHD期间恢复至对照水平。在SBH期间,氧气储备的周转比随后的恢复过程要慢得多。BHD后二氧化碳储备动态明显减慢。我们得出结论,SBH和BHD与组织氧气和二氧化碳储备的大幅变化有关,并且这些变化中的大部分可以由主要的循环事件来解释。组织氧气和二氧化碳储备周转率的变化不能仅用心指数变化来解释,但与静脉血容量的外周化以及SBH期间因呼吸暂停伴胸腔内压力升高引起的外周血管优先收缩相一致。BHD期间的短暂加压通过抵消胸腔内压力的增加,逆转了这些中枢和外周循环变化。