大鼠母体与19日龄胎儿间水分交换的单向性。

A Romeu, M Alemany, L Arola
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引用次数: 0

摘要

将氚化水注射到怀孕19天的大鼠体内,并估计其与胎儿的结合率。氚化水从母亲到胎儿再到周围子宫的转移是通过测量白蛋白盐水溶液的放射性来估计的,这种溶液浸泡在一个除去胎盘附着的子宫周围的孕妇的外部。氚水的转移非常显著,甚至在胎儿同位素平衡之前,估计超过1.5 ml/h。相反,氚从生理盐水中转移到母体中,只导致了这个数字的一小部分。结果提示母胎单位存在单向水循环:母体动脉血----胎盘----胎儿循环----羊水----羊膜----子宫内膜----母体静脉血。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Unidirectionality of the water exchange between mother and 19-day fetus in the rat.

Tritiated water was injected into 19-day pregnant rats and the rate of incorporation into their fetuses was estimated. The transfer of tritiated water from mother to fetus and then to the surrounding uterus was estimated by measuring the appearance of radioactivity in an albumin-saline solution that bathed externally one conceptus freed of its surrounding uterus except for the placental attachment. There was a very significant transfer of tritium water, even before isotopic equilibration of the fetus, estimated at more than 1.5 ml/h. The reverse, the transfer of tritium from the saline solution towards the mother, resulted in only a small fraction of that figure. The results suggest the existence of unidirectional water circulation in the materno-fetal unit: maternal arterial blood----placenta----fetal circulation----amniotic fluid----amniotic membranes----endometrium----maternal venous blood.

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