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持续性水利尿对人体前列腺素E2排泄的影响。

Effect of sustained water diuresis on prostaglandin E2 excretion in humans.

作者信息

Roberts D G, Strife R J, Gerber J G, Murphy R C, Nies A S

出版信息

Am J Physiol. 1985 Jun;248(6 Pt 2):F830-4. doi: 10.1152/ajprenal.1985.248.6.F830.

Abstract

The relationship of the renal excretion of prostaglandin E2 (PGE2) to urine flow during a water diuresis was examined using radioimmunoassay (RIA) and gas chromatography-mass spectrometry (GC-MS). Seven normal women fasted overnight were water loaded with 20 ml/kg orally, and each hour for 3 h they drank water to replace the urine volume plus 20 ml. The osmolality of the collected urines ranged from 49 to 1,073 mosmol/kg. Assay of urinary PGE2 concentrations by both RIA and GC-MS gave a correlation coefficient of 0.94. Eight normal women were then studied with a water diuresis sustained for 6 h. The excretion of PGE2 (measured with the validated RIA) increased for the 1st 2-3 h (from 1.8 +/- 0.5 to 25.8 +/- 16.6 pg X kg-1 X min-1), but then fell to base-line level by the 5th h (to 2.9 +/- 0.8 pg X kg-1 X min-1) even though the water diuresis was sustained. The urinary concentration vs. time curves for PGE2 and for the freely diffusible solute urea were compared. PGE2 concentration remained elevated for 3 h before falling (from the 100 pg/ml range to 15 pg/ml) while urea concentration decreased steadily from the 1st h. This finding suggests that the early urinary PGE2 excretion was not a washout phenomenon and is consistent with a transient increase in PGE2 synthesis. We conclude that urinary excretion of PGE2 is not a simple function of urine flow after a water load. There is a transient initial increase in urinary PGE2 excretion at the start of a water load that probably reflects an increase in renal PGE2 synthesis. However, with a sustained water diuresis, PGE2 excretion falls, indicating that an enhanced PGE2 synthesis rate is not required to sustain a water diuresis.

摘要

采用放射免疫分析法(RIA)和气相色谱 - 质谱联用技术(GC - MS)研究了水利尿过程中前列腺素E2(PGE2)的肾排泄与尿量之间的关系。7名正常女性隔夜禁食后,口服20 ml/kg水进行水负荷试验,之后3小时内每小时饮水以补充尿量加20 ml。收集尿液的渗透压范围为49至1,073 mosmol/kg。通过RIA和GC - MS检测尿中PGE2浓度,二者的相关系数为0.94。随后对8名正常女性进行了为期6小时的水利尿研究。PGE2排泄量(用经过验证的RIA测量)在最初2 - 3小时增加(从1.8±0.5增至25.8±16.6 pg·kg-1·min-1),但到第5小时降至基线水平(降至2.9±0.8 pg·kg-1·min-1),尽管水利尿仍在持续。比较了PGE2和可自由扩散溶质尿素的尿浓度随时间变化曲线。PGE2浓度在下降前(从100 pg/ml范围降至15 pg/ml)持续升高3小时,而尿素浓度从第1小时起稳步下降。这一发现表明,早期尿中PGE2排泄并非冲洗现象,与PGE2合成的短暂增加一致。我们得出结论,水负荷后尿中PGE2排泄并非尿量的简单函数。水负荷开始时尿中PGE2排泄有短暂的初始增加,这可能反映了肾PGE2合成增加。然而,在持续水利尿时,PGE2排泄量下降,表明维持水利尿并不需要提高PGE2合成速率。

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