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肾脏钾转运:各个肾单位节段及群体的作用

Renal potassium transport: contributions of individual nephron segments and populations.

作者信息

Wright F S, Giebisch G

出版信息

Am J Physiol. 1978 Dec;235(6):F515-27. doi: 10.1152/ajprenal.1978.235.6.F515.

Abstract

General features of the processes that contribute to renal potassium excretion are understood from clearance, stop-flow, micropuncture, and in vitro microperfusion experiments. However, the complex architecture of the kidney has made it difficult to examine individual nephron segments in all parts of the kidney. Accordingly, the extent to which distinguishable nephron populations, such as superficial and deep, may differ in their contributions to overall potassium excretion are not known. Also, the nature of transport processes across the successive segments of the nephrons (including not only the underlying cellular mechanisms, but even the direction of transport) is not known for all segments in any one nephron population. Excreted potassium is derived both from filtered potassium that escapes reabsorption and from secreted potassium. The filtered portion is large in amphibians and may be larger than generally recognized in mammals. The remainder is secreted primarily by distal nephron segments (distal tubule and cortical collecting duct). Potassium is also secreted into descending limbs of Henle loops; apparently this fraction is recycled from collecting ducts, and so does not represent an additional quantity of potassium transferred from blood to tubule fluid. Systemic factors that affect potassium excretion (potassium intake, sodium chloride intake, mineralocorticoid hormone levels, acid-base balance, and diuretic treatments) do so by modifying the net uptake of potassium from blood to cell and by altering the rate of fluid flow through the distal nephron. Under most circumstances, the distal nephron in the cortex appears to secrete potassium and the medullary collecting duct reabsorbs potassium. Although it is clear that successive nephron segments transport potassium in different ways, evidence to date does not indicate that potassium is handled differently by superficial nephrons compared to nephrons whose glomeruli lie in the deeper levels of the cortex.

摘要

通过清除率、停流、微穿刺和体外微灌注实验,人们了解了导致肾脏排钾过程的一般特征。然而,肾脏复杂的结构使得难以对肾脏所有部位的单个肾单位节段进行研究。因此,不同类型的可区分肾单位群体,如浅表肾单位和深部肾单位,对总体钾排泄的贡献程度尚不清楚。此外,对于任何一个肾单位群体中的所有节段,肾单位连续节段的转运过程的本质(不仅包括潜在的细胞机制,甚至包括转运方向)也不清楚。排泄的钾既来自未被重吸收的滤过钾,也来自分泌的钾。在两栖动物中,滤过部分占比很大,在哺乳动物中可能比普遍认为的还要大。其余部分主要由远端肾单位节段(远曲小管和皮质集合管)分泌。钾也分泌到髓袢降支中;显然这部分钾是从集合管循环而来的,因此并不代表从血液转移到小管液中的额外钾量。影响钾排泄的全身因素(钾摄入、氯化钠摄入、盐皮质激素水平、酸碱平衡和利尿剂治疗)是通过改变从血液到细胞的钾净摄取以及改变通过远端肾单位的液流速率来实现的。在大多数情况下,皮质中的远端肾单位似乎分泌钾,而髓质集合管重吸收钾。虽然很明显肾单位的连续节段以不同方式转运钾,但迄今为止的证据并未表明浅表肾单位与肾小球位于皮质较深层的肾单位在处理钾方面存在差异。

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