Williamson G L, Edwards B R
Ren Physiol. 1984;7(1):54-64. doi: 10.1159/000172924.
Despite the absence of vasopressin, Brattleboro homozygous (DI) rats concentrate their urine to hypertonic levels when deprived of drinking water. Ultimately this rise in urine osmolality must follow from increased osmolality of the corticopapillary gradient and/or increased osmotic equilibration across the collecting ducts. In this study we examined the concentrations and contents of total solute, urea, and nonurea solute in tissue from cortex to papillary tip of DI rats before and after dehydration for 12, 24, and 48 h. The greatest increase in osmolality occurred during the first 12 h; both urea and nonurea solute concentrations increased, but urea preferentially. From 12 to 48 h there were only small further increases in these concentrations, largely as a result of decreased tissue water content. Osmotic equilibration (reflected by urine/papillary tip osmolality) increased dramatically during dehydration, presumably because of decreased flow rate, attaining full equilibration by 48 h. The rise in urine osmolality during the first 12 h of dehydration was due to increased osmotic equilibration and to the enhanced corticopapillary gradient; urine became more concentrated from 12 to 48 h largely as a result of increased osmotic equilibration.
尽管缺乏抗利尿激素,但布拉特洛维纯合子(尿崩症)大鼠在禁水时仍能将尿液浓缩至高渗水平。最终,尿液渗透压的升高必然源于皮质-髓质梯度渗透压的增加和/或集合管跨膜渗透平衡的增强。在本研究中,我们检测了脱水12、24和48小时前后,尿崩症大鼠从皮质到乳头尖端组织中总溶质、尿素和非尿素溶质的浓度及含量。渗透压最大的升高发生在最初的12小时内;尿素和非尿素溶质浓度均升高,但尿素升高更明显。从12小时到48小时,这些浓度仅有小幅进一步升高,这主要是由于组织含水量降低所致。脱水过程中渗透平衡(以尿液/乳头尖端渗透压反映)显著增加,推测是由于流速降低,到48小时达到完全平衡。脱水最初12小时内尿液渗透压的升高是由于渗透平衡增加和皮质-髓质梯度增强;从12小时到48小时尿液变得更浓缩,主要是由于渗透平衡增加。