Olsen N V
Department of Anaesthesia, Rigshospitalet, University of Copenhagen, Denmark.
Acta Anaesthesiol Scand Suppl. 1995;107:165-70. doi: 10.1111/j.1399-6576.1995.tb04352.x.
Changes in body fluid homeostasis during acute hypoxaemia suggest a crucial role of renal function in acclimatization processes. Hypoxaemia stimulates sympathetic nervous activity, and also the cardiovascular system is affected with increases in heart rate and cardiac output. In most subjects, a hypoxic ventilatory response produces hypocapnia and respiratory alkalosis. Acute hypoxaemia depresses aldosterone secretion secondary to a direct effect on adrenal cells. Also plasma renin is decreased in resting hypoxaemic conditions, but the mechanism remains unknown. These hormonal changes may have the advantage of opposing excessive sodium and water retention, which characterizes acute mountain sickness. Short-term isocapnic or hypocapnic hypoxaemia in spontaneously breathing humans causes moderate if any increases in renal blood flow and only minor changes in GFR. In contrast, renal blood flow and GFR decreases during hypercapnic hypoxaemia. Renal clearance studies in humans after 24-48 hours in altitude hypoxia (4,350 m) demonstrate that glomerular and tubular function is only slightly changed in spite of marked depression of the renin-aldosterone system and increased plasma levels of norepinephrine. However, renal vascular tone may increase most probably secondary to the increased adrenosympathetic activity. In the first hours, acute hypoxaemia may induce an increased excretion of sodium and water. Previous studies suggest that the natriuretic response is caused by decreased reabsorption of sodium and bicarbonate in the proximal tubules secondary to the associated hyperventilation and hypocapnia. After 6 hours, sodium and water excretion is normalized or even depressed, dependent on the severity of acute mountain sickness. In view of the prompt increase in sodium and water excretion found during short-term hypoxaemia, the absence of such a response to more prolonged hypoxaemia suggests an adaptive time-dependent course of renal functional changes in hypoxaemia. Taken together, previous studies suggest that effects of acute hypoxaemia on renal haemodynamics are minor compared with effects on cerebral and coronary circulation. This might be the result of an appropriate resetting of autoregulatory mechanisms that would maintain the role of the kidney as a major sense organ to hypoxaemia and, subsequently, as a mediator of plasma volume regulation and erythropoietin synthesis.
急性低氧血症期间体液稳态的变化表明肾功能在适应过程中起着关键作用。低氧血症刺激交感神经活动,心血管系统也会受到影响,心率和心输出量增加。在大多数受试者中,低氧通气反应会导致低碳酸血症和呼吸性碱中毒。急性低氧血症由于对肾上腺细胞的直接作用而抑制醛固酮分泌。在静息低氧血症状态下,血浆肾素也会降低,但其机制尚不清楚。这些激素变化可能具有对抗过度钠和水潴留的优势,而过度钠和水潴留是急性高山病的特征。在自主呼吸的人体中,短期等碳酸血症或低碳酸血症性低氧血症会导致肾血流量适度增加(如果有增加的话),而肾小球滤过率(GFR)仅有轻微变化。相比之下,高碳酸血症性低氧血症期间肾血流量和GFR会降低。对在海拔4350米的高原低氧环境中停留24 - 48小时后的人体进行的肾清除率研究表明,尽管肾素 - 醛固酮系统明显受抑制且去甲肾上腺素血浆水平升高,但肾小球和肾小管功能仅有轻微变化。然而,肾血管张力很可能因肾上腺交感神经活动增加而升高。在最初几个小时,急性低氧血症可能会导致钠和水排泄增加。先前的研究表明,利钠反应是由于相关的过度通气和低碳酸血症导致近端小管中钠和碳酸氢盐重吸收减少所致。6小时后,钠和水排泄恢复正常甚至减少,这取决于急性高山病的严重程度。鉴于在短期低氧血症期间发现钠和水排泄迅速增加,而对更长时间低氧血症缺乏这种反应表明低氧血症时肾功能变化存在适应性的时间依赖性过程。综上所述,先前的研究表明,与对脑循环和冠状动脉循环的影响相比,急性低氧血症对肾血流动力学的影响较小。这可能是由于自身调节机制进行了适当的重新设定,从而维持了肾脏作为对低氧血症的主要传感器官以及随后作为血浆容量调节和促红细胞生成素合成介质的作用。