Taniguchi J, Tabei K, Imai M
Am J Physiol. 1987 Mar;252(3 Pt 2):F393-402. doi: 10.1152/ajprenal.1987.252.3.F393.
We simulated profiles of water and solute transport along the descending limb of the long-loop nephron by a mathematical model based on mass balance equations for water, sodium, potassium, and urea, using phenomenological coefficients reported for hamsters. We assumed that interstitial concentration of sodium, potassium, and urea increased linearly along the descending limb from 150 to 350, from 5 to 50, and from 5 to 300 mM, respectively. Under this condition an increase in osmolality at the end-descending limb was mainly accounted for by the absorption of water. Considerable amounts of potassium and urea were secreted along the descending limb. Sodium was reabsorbed rather than secreted along the descending limb by both diffusion and solvent drag. The secreted amounts of urea and potassium were comparable to those observed by micropuncture studies. The sodium concentration in the lumen was higher than in the interstitium, with the transmural sodium gradient being 15 meq/liter at the hairpin turn. The potassium mass flow rate at the end-descending limb increased by 2.4 times. Large variations in potassium concentration of the delivered fluid scarcely changed the potassium mass flow rate at the end-descending limb. The secretion of urea and potassium and the reabsorption of sodium were increased as a function of delivered flow rate. An increase in corticomedullary urea gradient decreased the net potassium secretion along the descending limb. When the transport parameters for rabbits were used, both reabsorption of sodium and addition of urea were decreased, but a similar amount of potassium was secreted. These analyses indicate that the mathematical model that takes the species difference and internephron heterogeneity into consideration is useful in illustrating the transport processes along the descending limb of Henle's loop under various physiological and pathophysiological conditions.
我们通过一个基于水、钠、钾和尿素质量平衡方程的数学模型,利用仓鼠的现象学系数,模拟了长襻肾单位降支中水和溶质的转运情况。我们假设钠、钾和尿素的间质浓度沿降支分别从150毫摩尔/升线性增加到350毫摩尔/升、从5毫摩尔/升增加到50毫摩尔/升、从5毫摩尔/升增加到300毫摩尔/升。在此条件下,降支末端渗透压的升高主要是由于水的重吸收。大量的钾和尿素沿降支分泌。钠通过扩散和溶剂拖曳在降支中被重吸收而非分泌。尿素和钾的分泌量与微穿刺研究观察到的相当。管腔内钠浓度高于间质,在U形转弯处跨壁钠梯度为15毫当量/升。降支末端钾的质量流速增加了2.4倍。输送液体中钾浓度的大幅变化几乎不会改变降支末端钾的质量流速。尿素和钾的分泌以及钠的重吸收随输送流速增加而增加。皮质髓质尿素梯度的增加会减少降支的净钾分泌。当使用兔子的转运参数时,钠的重吸收和尿素的添加均减少,但钾的分泌量相似。这些分析表明该数学模型考虑了物种差异和肾单位间的异质性,有助于阐明在各种生理和病理生理条件下亨氏袢降支的转运过程。