FETAL-MATERNAL FLUID AND ELECTROLYTE RELATIONS DURING CHRONIC FETAL URINE LOSS IN SHEEP

被引:29
作者
WLODEK, ME
HARDING, R
THORBURN, GD
机构
来源
AMERICAN JOURNAL OF PHYSIOLOGY | 1992年 / 263卷 / 04期
关键词
FETUS; PLACENTA; AMNIOTIC FLUID; ALLANTOIC FLUID; OSMOLALITY; PLACENTAL TRANSFER;
D O I
10.1152/ajprenal.1992.263.4.F671
中图分类号
Q4 [生理学];
学科分类号
071003 ;
摘要
Our aim was to determine the effects of prolonged removal of fetal urine during late gestation on fetal-maternal fluid and electrolyte relationships. We measured the volume and composition of fetal urine and amniotic and allantoic fluids and the composition of fetal and maternal plasma in sheep before and during continuous urine drainage, which began at 130 days of gestation and continued until the onset of labor; a control group was also studied. The response to fetal urine drainage occurred in two phases. In the 'acute" phase (I -3 days), amniotic and allantoic fluid volumes decreased significantly, presumably due to their reabsorption into the fetal chorionic circulation or swallowing of amniotic fluid by the fetus. During the "chronic" phase, starting 3-5 days after urine drainage, a significant reversal in the transplacental osmotic gradient occurred due to a decrease in maternal plasma osmolality. During the entire drainage period (14.1 +/- 1.1 days, mean +/- SE, n = 5) at least 542 ml/day of water and 24 mmol/day of electrolytes passed from the mother into the fetal circulation and fetal plasma osmolality was unchanged. We conclude that, despite the loss of substantial water and electrolytes, the fetus is able to maintain its growth and fluid and electrolyte homeostasis by obtaining water and electrolytes initially from the amniotic and allantoic fluids and subsequently from its mother. The movement of water and electrolytes to the fetus would have been facilitated by the reversed transplacental osmotic gradient.
引用
收藏
页码:F671 / F679
页数:9
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