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正常受试者在海拔6000米处的体液分布、肾血流量及激素情况。

Body fluid compartments, renal blood flow, and hormones at 6,000 m in normal subjects.

作者信息

Anand I S, Chandrashekhar Y, Rao S K, Malhotra R M, Ferrari R, Chandana J, Ramesh B, Shetty K J, Boparai M S

机构信息

Department of Cardiology, Postgraduate Institute of Medical Education and Research, Chandigarh, India.

出版信息

J Appl Physiol (1985). 1993 Mar;74(3):1234-9. doi: 10.1152/jappl.1993.74.3.1234.

DOI:10.1152/jappl.1993.74.3.1234
PMID:8482663
Abstract

We previously described a syndrome of congestive heart failure occurring in healthy young men at extreme altitude (Anand et al. Lancet 335: 561-565, 1990). The pathogenesis of this condition is unclear. We therefore measured body fluid compartments, renal blood flow, and a variety of plasma hormones in 10 asymptomatic young men staying above 6,000 m for > 10 wk and compared the results with controls at sea level. Body compartments were measured with isotope dilution techniques and renal blood flow with o-[125I]iodohippurate sodium. There was a marked expansion of all the fluid spaces: total body sodium was 14% above normal (P < 0.05), total body water was 18% above normal (P < 0.05), plasma volume was 33% above normal (P < 0.05), and blood volume was 84.5% above normal (P < 0.001). The effective renal plasma flow was lower than normal by 55% (P < 0.001), but the reduction in the effective renal blood flow was 37% below normal (P < 0.001) because the hematocrit was high (41.6% above normal). Plasma norepinephrine was nearly 3 times normal (P < 0.01), cortisol 3 times normal (P < 0.001), and growth hormone 18 times normal (P < 0.01). Aldosterone was twice normal (P < 0.03). Plasma epinephrine, atrial natriuretic peptide, and plasma renin activity were unchanged. The degree of fluid retention in these normal subjects was similar to that in patients with severe untreated congestive heart failure (Anand et al. Circulation 80: 299-305, 1989), whereas sodium retention and reduction in effective renal blood flow were less.(ABSTRACT TRUNCATED AT 250 WORDS)

摘要

我们之前描述过一种发生在健康年轻男性身上的高原性充血性心力衰竭综合征(阿南德等人,《柳叶刀》335: 561 - 565, 1990)。这种病症的发病机制尚不清楚。因此,我们对10名在海拔6000米以上停留超过10周的无症状年轻男性的体液成分、肾血流量及多种血浆激素进行了测量,并将结果与海平面的对照组进行比较。体液成分采用同位素稀释技术测量,肾血流量采用邻 - [¹²⁵I]碘马尿酸钠测量。所有体液间隙均有显著扩张:总体钠比正常水平高14%(P < 0.05),总体水比正常水平高18%(P < 0.05),血浆容量比正常水平高33%(P < 0.05),血容量比正常水平高84.5%(P < 0.001)。有效肾血浆流量比正常水平低55%(P < 0.001),但有效肾血流量减少比正常水平低37%(P < 0.001),因为血细胞比容较高(比正常水平高41.6%)。血浆去甲肾上腺素接近正常水平的3倍(P < 0.01),皮质醇为正常水平的3倍(P < 0.001),生长激素为正常水平的18倍(P < 0.01)。醛固酮为正常水平的2倍(P < 0.03)。血浆肾上腺素、心钠素及血浆肾素活性未发生变化。这些正常受试者的液体潴留程度与未经治疗的严重充血性心力衰竭患者相似(阿南德等人,《循环》80: 299 - 305, 1989),而钠潴留和有效肾血流量减少程度较轻。(摘要截于250字)

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