Wilkinson H L, Sullivan L P, Welling D J, Welling L W
Am J Physiol. 1983 Dec;245(6):F801-12. doi: 10.1152/ajprenal.1983.245.6.F801.
Techniques were developed to determine the location of exchangeable K pools that had been identified previously in kinetic studies of the intact perfused bullfrog kidney. Following perfusion of the kidneys with 42K, a washout of the isotope was begun and interrupted at various times; the kidneys were removed, frozen, dried at low pressure and temperature, and then microdissected. Glomerular capillary tufts, small segments of tissue containing early distal tubules (diluting segment), and other segments containing proximal tubular convolutions were removed and analyzed for total content of K and 42K. In the intact kidney 77% of tissue K exchanged in 60 min. The exchangeable K concentration was 95 mu eq/ml cell water. Correction for the K activity coefficient in Ringer solution yielded an activity of 72 mu eq/ml. Thirty-two percent of glomerular capillary K exchanged in 60 min; 7% exchanged with a half time of 3.5 min; and the remainder exchanged at a rate too slow to measure. The data from tissue containing proximal tubular segments were too scattered to permit analysis. In segments containing early distal tubules, 67% of tissue K was contained in two exchangeable pools: one pool exchanged at a rate 10-fold greater than did the other. The data for these two distal pools were analyzed in terms of a parallel model (two cell types?) and a nested model (cytoplasm and subcellular organelles?). Pool size and exchange rates were calculated for both models. Electron microscopic analysis revealed that early distal tubular segments contain only one cell type which has a large population of mitochondria. This suggests that the nested model is more plausible. The fast distal pool exchanged at the same rate as the fast-exchanging pool identified in kinetic studies of the intact functioning kidney and is considered to be the K secretory pool.
已开发出一些技术来确定先前在完整灌注牛蛙肾脏的动力学研究中所识别出的可交换钾池的位置。在用(^{42}K)灌注肾脏后,开始对同位素进行洗脱,并在不同时间中断;将肾脏取出、冷冻、在低压和低温下干燥,然后进行显微解剖。去除肾小球毛细血管丛、含有早期远端小管(稀释段)的小组织片段以及含有近端肾小管卷曲的其他片段,并分析其钾和(^{42}K)的总含量。在完整的肾脏中,(77%)的组织钾在(60)分钟内进行了交换。可交换钾浓度为(95)微当量/毫升细胞内液。校正林格氏溶液中的钾活度系数后,活度为(72)微当量/毫升。肾小球毛细血管钾的(32%)在(60)分钟内进行了交换;(7%)以(3.5)分钟的半衰期进行交换;其余部分的交换速率太慢无法测量。来自含有近端肾小管段的组织的数据过于分散,无法进行分析。在含有早期远端小管的片段中,(67%)的组织钾存在于两个可交换池中:一个池的交换速率比另一个池快(10)倍。根据平行模型(两种细胞类型?)和嵌套模型(细胞质和亚细胞细胞器?)对这两个远端池的数据进行了分析。计算了两种模型的池大小和交换速率。电子显微镜分析显示,早期远端小管段仅包含一种细胞类型,该细胞类型含有大量线粒体。这表明嵌套模型更合理。快速远端池的交换速率与完整功能肾脏的动力学研究中所识别出的快速交换池相同,被认为是钾分泌池。