Bärtsch P, Shaw S, Weidmann P, Oelz O
Medizinische Klinik und Poliklinik, Universität Heidelberg.
Schweiz Z Sportmed. 1993 Mar;41(1):7-13.
This paper summarizes the main findings of 3 publications of our group [2-4] examining fluid balance at high altitude. Of 57 mountaineers ascending from 1170 m to 4559 m within 22 to 77 hours, 24 developed acute mountain sickness (AMS) and 16 developed high altitude pulmonary edema (HAPE). In 14 cases HAPE was preceded by symptoms of AMS. Independently of the amount of fluid intake, which varied from 2 to 4 l/24 h in these studies, subjects developing AMS showed decreased diuresis and natriuresis compared to healthy controls with similar fluid intake. Higher fluid intake resulted in greater urine output but did not prevent AMS. Higher plasma levels of aldosterone at rest and greater exercise-induced rises of plasma aldosterone and vasopressine may explain the increased water and salt retention in subjects with AMS. Whether these hormonal changes are secondary to a more severe hypoxemic stress or present a primary cause of AMS remains to be determined.
本文总结了我们团队3篇关于高海拔地区液体平衡研究论文[2-4]的主要发现。在57名于22至77小时内从1170米攀升至4559米的登山者中,24人出现急性高山病(AMS),16人出现高原肺水肿(HAPE)。14例HAPE患者在发病前有AMS症状。在这些研究中,尽管液体摄入量有所不同,从2至4升/24小时不等,但与摄入相似液体量的健康对照组相比,出现AMS的受试者利尿和排钠减少。较高的液体摄入量导致尿量增加,但并不能预防AMS。静息时较高的血浆醛固酮水平以及运动引起的血浆醛固酮和血管加压素的更大升高,可能解释了AMS患者水盐潴留增加的原因。这些激素变化是更严重的低氧应激的继发结果还是AMS的主要原因,仍有待确定。