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原发性高血压中的钠代谢。对急性高渗盐水负荷的利钠反应。

Sodium metabolism in essential hypertension. Natriuretic response to acute hypertonic saline load.

作者信息

Kubo S, Nishioka A, Takatsu T

出版信息

Jpn Heart J. 1978 Nov;19(6):852-64. doi: 10.1536/ihj.19.852.

Abstract

In order to investigate the mechanism of the "exaggerated natriuresis" in hypertension, 300 ml of 3% saline was infused for 1 hour during hydropenia in 13 patients with normal renin essential hypertension and 5 normotensive subjects on a daily ingestion of 4 Gm and 16 Gm of NaCl. At the end of the infusion, the circulating blood volume indicated by the change in serum total protein concentration and the glomerular filtered load were increased in a similar manner in both groups. Prompt the enhanced natriuresis and diuresis were seen within 1--2 hours after starting the infusion in the hypertensives on a daily ingestion of 16 Gm of NaCl. Significant positive correlations were found between the change in mean arterial blood pressure (deltaMAP) and UV, and between deltaMAP and UNa V in the hypertensives either on a daily 4 Gm or 16 Gm ingestion of NaCl. Free water reabsorption (Tc H2O) was lower in the hypertensives than that in the controls at high levels of osmolar clearance (Cosm). Plasma renin activity (PRA) did not differ in either group on either NaCl ingestion and was equally suppressed on a daily ingestion of 4 Gm of NaCl, while little changed on a high salt intake. Plasma aldosterone levels changed in parallel with PRA. It is suggested that the "exaggerated natriuresis" is due to the decreased tubular sodium reabsorption, which may be the result of intrarenal hemodynamic changes related to the elevated renal perfusion pressure. The decreased medullary osmolar gradient probably induced by an increase in the medullary blood flow is a possible contributing factor in the enhanced sodium and water excretion, and the renin-aldosterone system does not seem to play an important role.

摘要

为了研究高血压患者“排钠增加”的机制,对13例正常肾素型原发性高血压患者和5例血压正常受试者进行了研究,这些受试者每日分别摄入4克和16克氯化钠,在禁水期间静脉输注300毫升3%的盐水1小时。输注结束时,两组血清总蛋白浓度变化所提示的循环血容量和肾小球滤过负荷均以相似的方式增加。在每日摄入16克氯化钠的高血压患者中,输注开始后1 - 2小时内出现了迅速增强的排钠和利尿现象。在每日摄入4克或16克氯化钠的高血压患者中,平均动脉血压变化(deltaMAP)与尿钠排泄量(UV)之间以及deltaMAP与尿钠排泄分数(UNa V)之间均存在显著正相关。在高渗清除率(Cosm)水平时,高血压患者的自由水重吸收(Tc H2O)低于对照组。无论氯化钠摄入量如何,两组的血浆肾素活性(PRA)均无差异,且在每日摄入4克氯化钠时均受到同等程度的抑制,而在高盐摄入时变化不大。血浆醛固酮水平与PRA平行变化。提示“排钠增加”是由于肾小管钠重吸收减少所致,这可能是肾灌注压升高引起肾内血流动力学变化的结果。髓质血流增加可能导致的髓质渗透压梯度降低是钠和水排泄增加的一个可能因素,而肾素 - 醛固酮系统似乎不起重要作用。

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