Titze Jens
Department of Nephrology and Hypertension, Friedrich-Alexander University, Glückstrasse 6, Erlangen-Nürnberg, Germany.
Semin Dial. 2009 May-Jun;22(3):253-5. doi: 10.1111/j.1525-139X.2009.00569.x.
The widely accepted concept of body fluid and electrolyte homeostasis is that Na(+) is restricted mainly to the extracellular fluid and K(+) to the intracellular space, where both ions act to hold water and thereby control the extracellular and intracellular fluid volume by their osmotic activity. Na(+) accumulation thus inevitably leads to water retention. The constancy of the extracellular volume is the task of the kidneys, which control the total body Na(+) content. More recent data have questioned this traditional view, suggesting that large amounts of Na(+) can be accumulated without accompanying water retention by osmotically inactive Na(+) retention, or by osmotically neutral Na(+)/K(+) exchange. Besides the control of the body Na(+) content by the kidneys, redistribution of body electrolytes hence provides an extrarenal regulatory alternative in the maintenance of body fluid volume and blood pressure control.
广泛接受的体液和电解质稳态概念是,Na⁺主要局限于细胞外液,K⁺主要存在于细胞内空间,这两种离子都通过保持水分,进而通过其渗透活性来控制细胞外液和细胞内液的容量。因此,Na⁺的蓄积不可避免地导致水潴留。细胞外液量的恒定是肾脏的任务,肾脏控制着全身Na⁺的含量。最近的数据对这一传统观点提出了质疑,表明大量的Na⁺可以通过无渗透活性的Na⁺潴留或渗透中性的Na⁺/K⁺交换而蓄积,而不会伴有水潴留。除了肾脏对体内Na⁺含量的控制外,体内电解质的重新分布因此为维持体液量和控制血压提供了一种肾外调节方式。