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胎儿羊水对长期输注5M氯化钠的反应:所有的盐分都去哪儿了?

Fetal fluid responses to long-term 5 M NaCl infusion: where does all the salt go?

作者信息

Powell T L, Brace R A

机构信息

Department of Reproductive Medicine, University of California, San Diego, La Jolla 92093-0802.

出版信息

Am J Physiol. 1991 Aug;261(2 Pt 2):R412-9. doi: 10.1152/ajpregu.1991.261.2.R412.

Abstract

The fetus must obtain Na and Cl ions in order to grow. However, the regulation of electrolyte acquisition by the fetus is not well understood. To explore fetal electrolyte balance, we intravenously infused 5 M NaCl at a rate equal to 80% of the total fetal body Na+ and Cl- content per day (240 mM/day) for 3 days into late-gestation fetal sheep. We hypothesized that the increase in fetal osmolality resulting from the infusion would cause a transplacental water movement into the fetal compartment, leading to hydrops fetalis and/or polyhydramnios. The fetal-to-maternal osmotic gradient was initially -2.8 +/- 0.9 (SE) mosmol/kgH2O and rose by 4.8 +/- 1.8 mosmol/kgH2O during the infusion. Fetal plasma [Na+] and [Cl-] increased (3.0 +/- 0.4 and 5.5 +/- 0.5 meq/l, respectively), but the normal maternal-to-fetal transplacental concentration gradients for these ions were not reversed. Most of the infused Na+ (92 +/- 14%) and Cl- (82 +/- 12%) was excreted by the fetus in large volumes of hypotonic urine. Amniotic fluid osmolality and [Na+] were unchanged, but amniotic [Cl-] increased 5.7 +/- 2.4 meq/l. The amniotic plus allantoic fluid volume, as estimated by ultrasonography, was increased (43.5 +/- 14.5%) at day 2 and returned to control by day 3 of infusion. There was no fetal edema during the study or at autopsy. In light of these results, we propose a novel and somewhat complex mechanism for transplacental fluid and electrolyte movement in which placental capillary permeability increases along the length of the capillary.(ABSTRACT TRUNCATED AT 250 WORDS)

摘要

胎儿必须获取钠和氯离子才能生长。然而,胎儿获取电解质的调节机制尚未完全明确。为了探究胎儿的电解质平衡,我们以每天等于胎儿体内总钠和氯含量的80%(240毫摩尔/天)的速率,向妊娠晚期的胎羊静脉输注5摩尔/升的氯化钠,持续3天。我们假设输注导致的胎儿渗透压升高会引起经胎盘的水向胎儿腔室移动,从而导致胎儿水肿和/或羊水过多。胎儿与母体的渗透梯度最初为-2.8±0.9(标准误)毫摩尔/千克水,输注期间上升了4.8±1.8毫摩尔/千克水。胎儿血浆中的[Na⁺]和[Cl⁻]升高(分别为3.0±0.4和5.5±0.5毫当量/升),但这些离子正常的母体到胎儿的经胎盘浓度梯度并未逆转。大部分输注的Na⁺(92±14%)和Cl⁻(82±12%)通过胎儿以大量低渗尿液排出。羊水渗透压和[Na⁺]未改变,但羊水[Cl⁻]升高了5.7±2.4毫当量/升。超声估计,羊膜腔加尿囊液体积在第2天增加(43.5±14.5%),输注第3天恢复至对照水平。研究期间及尸检时均未发现胎儿水肿。鉴于这些结果,我们提出了一种新的且 somewhat complex 的经胎盘液体和电解质移动机制,即胎盘毛细血管通透性沿毛细血管长度增加。(摘要截短至250字)

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