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力竭性次最大强度静态握力收缩期间及之后的钾稳态

Potassium homeostasis during and following exhaustive submaximal static handgrip contractions.

作者信息

Byström S, Sjøgaard G

机构信息

Division of Applied Work Physiology, National Institute of Occupational Health, Solna, Sweden.

出版信息

Acta Physiol Scand. 1991 May;142(1):59-66. doi: 10.1111/j.1748-1716.1991.tb09128.x.

Abstract

The aim of the present study was to follow local potassium homeostasis during and after exhaustive contractions. Eight subjects performed static handgrip with their right forearm at 10%, 25% and 40% maximal voluntary contraction. Blood flow (venous occlusion plethysmography) and the venous effluent plasma potassium concentration were followed during the contractions and during a 60-min recovery period. Electromyography was registered during exercise (frequency analysis). With all three protocols the blood flow increased significantly during the contractions and the same was true of the effluent plasma potassium concentrations. In the recovery period blood flow and the venous effluent plasma potassium concentration returned to base values within 30 min following 40% maximal voluntary contraction while following 10% and 25% maximal voluntary contraction, venous effluent plasma potassium concentration was still significantly below resting values one hour after the exercise had ceased, indicating a long-lasting uptake of potassium from the blood into the muscles. In line with this a significant potassium deficit was still seen after 1 hour of recovery following 10% and 25% maximal voluntary contraction. It is concluded that the recovery of potassium homeostasis following prolonged low-intensity contractions is a slow process. This may be due to either sequestration of potassium in other tissues with a subsequent slow release and/or insufficient sodium/potassium pump activation. The contraction induced potassium loss may play a major role in muscle performance since it may impair mechanical force production, and it is hypothesized that this may be the origin of low-frequency fatigue.

摘要

本研究的目的是追踪力竭性收缩期间及之后局部钾离子的稳态。八名受试者用其右前臂进行静态握力试验,分别达到最大自主收缩力的10%、25%和40%。在收缩过程中以及60分钟的恢复期内,监测血流量(静脉阻断体积描记法)和静脉流出血浆钾离子浓度。运动期间记录肌电图(频率分析)。在所有三种方案中,收缩期间血流量显著增加,流出血浆钾离子浓度也是如此。在恢复期,40%最大自主收缩后,血流量和静脉流出血浆钾离子浓度在30分钟内恢复至基线值,而10%和25%最大自主收缩后,运动停止一小时后,静脉流出血浆钾离子浓度仍显著低于静息值,表明钾离子从血液持续摄取到肌肉中。与此一致的是,10%和25%最大自主收缩后1小时的恢复期后,仍可见明显的钾离子缺乏。得出的结论是,长时间低强度收缩后钾离子稳态的恢复是一个缓慢的过程。这可能是由于钾离子在其他组织中螯合,随后缓慢释放和/或钠/钾泵激活不足。收缩诱导的钾离子流失可能在肌肉性能中起主要作用,因为它可能损害机械力的产生,并且据推测这可能是低频疲劳的根源。

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