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早期液体潴留与重度急性高原病

Early fluid retention and severe acute mountain sickness.

作者信息

Loeppky Jack A, Icenogle Milton V, Maes Damon, Riboni Katrina, Hinghofer-Szalkay Helmut, Roach Robert C

机构信息

Lovelace Respiratory Research Institute, University of New Mexico, Albuquerque, NM 87108, USA.

出版信息

J Appl Physiol (1985). 2005 Feb;98(2):591-7. doi: 10.1152/japplphysiol.00527.2004. Epub 2004 Oct 22.

Abstract

Field studies of acute mountain sickness (AMS) usually include variations in exercise, diet, and environmental conditions over days and development of clinically apparent edemas. The purpose of this study was to clarify fluid status in persons developing AMS vs. those remaining without symptoms during simulated altitude with controlled fluid intake, diet, temperature, and without exercise. Ninety-nine exposures of 51 men and women to reduced barometric pressure (426 mmHg = 16,000 ft. = 4,880 m) were carried out for 8-12 h. AMS was evaluated by Lake Louise (LL) and AMS-C scores near the end of exposure. Serial measurements included fluid balance, electrolyte excretions, and plasma concentrations, regulating hormones, and free water clearance. Comparison between 16 subjects with the lowest AMS scores near the end of exposure ("non-AMS": mean LL = 1.0, range = 0-2.5) and 16 others with the highest AMS scores ("AMS": mean LL = 7.4, range = 5-11) demonstrated significant fluid retention in AMS beginning within the first 3 h, resulting from reduced urine flow. Plasma Na+ decreased significantly after 6 h, indicating dilution throughout the total body water. Excretion of Na+ and K+ trended downward with time in both groups, being lower in AMS after 6 h, and the urine Na+-to-K+ ratio was significantly higher for AMS after 6 h. Renal compensation for respiratory alkalosis, plasma renin activity, aldosterone, and atrial natriuretic peptide were not different between groups, with the latter tending to rise and aldosterone falling with time of exposure. Antidiuretic hormone fell in non-AMS and rose in AMS within 90 min of exposure and continued to rise in AMS, closely associated with severity of symptoms and fluid retention.

摘要

急性高原病(AMS)的实地研究通常包括数天内运动、饮食和环境条件的变化以及临床明显水肿的发展情况。本研究的目的是在模拟高原环境下,控制液体摄入量、饮食、温度且不进行运动的条件下,阐明发生AMS的人与无症状者的液体状态。对51名男性和女性进行了99次暴露于低气压环境(426 mmHg = 16,000英尺 = 4,880米)的实验,持续8 - 12小时。在暴露接近尾声时,通过路易斯湖(LL)评分和AMS - C评分评估AMS。连续测量包括液体平衡、电解质排泄、血浆浓度、调节激素和自由水清除率。比较暴露接近尾声时AMS评分最低的16名受试者(“非AMS”:平均LL = 1.0,范围 = 0 - 2.5)和另外16名AMS评分最高的受试者(“AMS”:平均LL = 7.4,范围 = 5 - 11),结果显示AMS患者在最初3小时内就开始出现明显的液体潴留,这是由于尿量减少所致。6小时后血浆Na⁺显著下降,表明全身水分稀释。两组中Na⁺和K⁺的排泄量均随时间呈下降趋势,6小时后AMS组更低,且6小时后AMS组的尿Na⁺/K⁺比值显著更高。两组间肾脏对呼吸性碱中毒的代偿、血浆肾素活性、醛固酮和心钠素无差异,后者随暴露时间有上升趋势,醛固酮则下降。抗利尿激素在非AMS组暴露后90分钟内下降,在AMS组上升,并在AMS组持续上升,与症状严重程度和液体潴留密切相关。

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