Jamison R L, Work J, Schafer J A
Am J Physiol. 1982 Apr;242(4):F297-312. doi: 10.1152/ajprenal.1982.242.4.F297.
This review focuses on the hypothesis that potassium is recycled in the medulla by secretion into the pars recta or descending limb of long-looped nephrons and reabsorption from the ascending limb and/or medullary collecting duct. Evidence supporting the recycling hypothesis is summarized and the process is analyzed quantitatively by an examination of the mass flow of potassium reaching different sites along superficial and juxtamedullary nephrons and collecting tubules. From differences in potassium mass flow between sites, we have estimated the amount of potassium that must be secreted or absorbed by individual segments of the renal tubule. These rates of secretion and absorption are compared with the potassium transport characteristics of the respective segments, as assessed by isolated tubule perfusion in vitro and micropuncture in vivo. It is apparent that potassium secretion can occur passively in the pars recta and descending limb of long-looped nephrons as a consequence of the elevated potassium concentration in the medullary interstitium. At present, no active potassium absorptive mechanism has been demonstrated in any segment of the ascending limb. Due to the very high ionic permeability of the thin ascending segment and the lumen-positive transepithelial voltage in the thick ascending segment, however, considerable passive absorption likely occurs, although net potassium secretion has also been demonstrated in the cortical thick ascending limb. The high potassium concentration in the inner medullary interstitium and the difference in mass flow of potassium between the end of superficial nephrons in the cortex and the collecting ducts in the papilla, at least under certain circumstances, are best accounted for by net potassium reabsorption in the medullary collecting duct.
钾在髓质中通过分泌到长襻肾单位的直部或降支,并从升支和/或髓质集合管重吸收来进行再循环。总结了支持再循环假说的证据,并通过检查沿浅表肾单位和近髓肾单位以及集合小管到达不同部位的钾质量流,对该过程进行了定量分析。根据不同部位之间钾质量流的差异,我们估算了肾小管各段必须分泌或吸收的钾量。将这些分泌和吸收速率与通过体外分离肾小管灌注和体内微穿刺评估的各段钾转运特性进行比较。显然,由于髓质间质中钾浓度升高,钾分泌可在长襻肾单位的直部和降支中被动发生。目前,在升支的任何段均未证实存在主动钾吸收机制。然而,由于细段升支的离子通透性非常高,且厚段升支存在管腔正跨上皮电压,尽管在皮质厚段升支也已证实存在钾净分泌,但仍可能发生大量被动吸收。至少在某些情况下,皮质浅表肾单位末端与乳头集合管之间钾质量流的差异以及髓质间质中高钾浓度,最好用髓质集合管中的钾净重吸收来解释。