Stephenson J L
Biophys J. 1976 Nov;16(11):1273-86. doi: 10.1016/S0006-3495(76)85773-6.
The canonical mass balance relation derived for the central core model of the renal medulla is extended to medullary models in which an arbitrary assemblage of renal tubules and vascular capillaries exchange with each other both directly and via the medullary interstitium and in which not all of the vascular loops or loops of Henle extend to the papilla. It is shown that if descending limbs of Henle and descending vasa recta enter the medulla at approximately plasma osmolality, the concentration ratio is given by: r = 1/[1 - ft(1 - fu)(1 - fw)], where ft is fractional solute transport out of ascending Henle's limb, fu is fractional urine flow, and fw is fractional dissipation; fw is a measure of the solute returned to the systemic circulation without its isotonic complement of water. A modified equation that applies to the diluting as well as the concentrating kidney is also derived. By allowing concentrations in interstitium and vascular capillaries to become identical at a given medullary level, conservation relations are derived for a multinephron central core model of the renal medulla.
为肾髓质中央核心模型推导的标准质量平衡关系被扩展到髓质模型,在该模型中,任意组合的肾小管和血管毛细血管既直接又通过髓质间质相互交换,并且并非所有的血管袢或亨氏袢都延伸至乳头。结果表明,如果亨氏袢降支和直小血管降支以近似血浆渗透压进入髓质,则浓度比由下式给出:r = 1/[1 - ft(1 - fu)(1 - fw)],其中ft是从亨氏袢升支输出的溶质分数,fu是尿流分数,fw是耗散分数;fw是溶质返回体循环但无水的等渗补充的量度。还推导了一个适用于稀释性和浓缩性肾脏的修正方程。通过使给定髓质水平处间质和血管毛细血管中的浓度相同,为肾髓质的多肾单位中央核心模型推导了守恒关系。