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身体水分状态与急性高原病的关系。

Association between body water status and acute mountain sickness.

机构信息

Department of Sport Science, Medical Section, University Innsbruck, Innsbruck, Austria.

出版信息

PLoS One. 2013 Aug 27;8(8):e73185. doi: 10.1371/journal.pone.0073185. eCollection 2013.

DOI:10.1371/journal.pone.0073185
PMID:24013267
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3754926/
Abstract

PURPOSE

The present study determined the association between body fluid variation and the development of acute mountain sickness (AMS) in adults.

METHODS

Forty-three healthy participants (26 males and 17 females, age: 26 ± 6 yr, height: 174 ± 9 cm, weight: 68 ± 12 kg) were passively exposed at a FiO2 of 12.6% (simulated altitude hypoxia of 4500 m, PiO2 = 83.9 mmHg) for 12-h. AMS severity was assessed using the Lake Louise Score (LLS). Food and drink intakes were consumed ad libitum and measured; all urine was collected. Before and after the 12-h exposure, body weight and plasma osmolality were measured and whole-body bioimpedance analysis was performed.

RESULTS

The overall AMS incidence was 43% (38% males, 50% females). Participants who developed AMS showed lower fluid losses (3.0 ± 0.9 vs. 4.5 ± 2.0 ml/kg/h, p = 0.002), a higher fluid retention (1.9 ± 1.5 vs. 0.6 ± 0.8 ml/kg/h, p = 0.022), greater plasma osmolality decreases (-7 ± 7 vs. -2 ± 5 mOsm/kg, p = 0.028) and a larger plasma volume expansion (11 ± 10 vs. 1 ± 15%, p = 0.041) compared to participants not developing AMS. Net water balance (fluid intake--fluid loss) and the amount of fluid loss were strong predictors whether getting sick or not (Nagelkerkes r(2) = 0.532). The LLS score was related to net water balance (r = 0.358, p = 0.018), changes in plasma osmolality (r = -0.325, p = 0.033) and sodium concentration (r = -0.305, p = 0.047). Changes in the impedance vector length were related to weight changes (r = -0.550, p<0.001), fluid intake (r = -0.533, p<0.001) and net water balance (r = -0.590, p<0.001).

CONCLUSIONS

Participants developing AMS within 12 hours showed a positive net water balance due to low fluid loss. Thus measures to avoid excess fluid retention are likely to reduce AMS symptoms.

摘要

目的

本研究旨在确定体液变化与成年人高原反应(AMS)发展之间的关系。

方法

43 名健康参与者(26 名男性和 17 名女性,年龄:26±6 岁,身高:174±9cm,体重:68±12kg)在 FiO2 为 12.6%(模拟海拔 4500 米的缺氧,PiO2=83.9mmHg)的条件下被动暴露 12 小时。使用路易湖评分(LLS)评估 AMS 严重程度。随意摄入食物和饮料并进行测量;收集所有尿液。在 12 小时暴露前后,测量体重和血浆渗透压,并进行全身生物阻抗分析。

结果

AMS 的总体发生率为 43%(男性 38%,女性 50%)。发生 AMS 的参与者表现出较低的液体流失(3.0±0.9 与 4.5±2.0ml/kg/h,p=0.002),更高的液体潴留(1.9±1.5 与 0.6±0.8ml/kg/h,p=0.022),更大的血浆渗透压下降(-7±7 与 -2±5mOsm/kg,p=0.028)和更大的血浆容量扩张(11±10 与 1±15%,p=0.041),与未发生 AMS 的参与者相比。净水平衡(液体摄入-液体流失)和液体流失量是判断是否生病的重要预测因素(Nagelkerkes r(2)=0.532)。LS 评分与净水平衡(r=0.358,p=0.018)、血浆渗透压变化(r=-0.325,p=0.033)和钠浓度变化(r=-0.305,p=0.047)相关。阻抗向量长度的变化与体重变化(r=-0.550,p<0.001)、液体摄入(r=-0.533,p<0.001)和净水平衡(r=-0.590,p<0.001)相关。

结论

在 12 小时内发生 AMS 的参与者由于液体流失较少,表现出正的净水平衡。因此,避免过度液体潴留的措施可能会减轻 AMS 症状。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8d13/3754926/214b312345a9/pone.0073185.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8d13/3754926/5f38112f95f5/pone.0073185.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8d13/3754926/214b312345a9/pone.0073185.g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8d13/3754926/5f38112f95f5/pone.0073185.g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/8d13/3754926/214b312345a9/pone.0073185.g002.jpg

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