Longo L D, Power G G, Forster R E
J Clin Invest. 1967 May;46(5):812-28. doi: 10.1172/JCI105581.
A technique is described for studying the respiratory function of the placenta using carbon monoxide, a gas whose exchange across the placenta between the maternal and fetal circulations is limited by diffusion rather than blood flow. During the steady state before the introduction of CO, the normal concentration of carboxyhemoglobin in the ewe, COHb, is approximately 0.90%, and that in the fetus is 2.9%, the ratio COHb/COHb being 3.2. In dogs the corresponding values are 1.9%, 4.8%, and 2.4%. After the introduction of CO into the mother animal, CO diffused across the placenta slowly with an equilibration half-time of approximately 2 hours. The average carbon monoxide diffusing capacity (D(Pco)) of the placenta during maternal to fetal exchange was 0.54 ml per (minute x mm Hg x kg fetal weight) (SD +/- 0.13) in sheep and 0.57 ml per (minute x mm Hg x kg) (SD +/- 0.18) in dogs. The fetal to maternal placental diffusing capacity in two sheep was 0.54 ml per (minute x mm Hg x kg). Calculations considering the relative rates of reaction of O(2) and CO with red cell hemoglobin and the relative rates of diffusion of the two gases suggest that the true D(Po2) should be about 1.2 to 2 times greater than the D(Pco) or 0.65 to 1.1 per (minute x mm Hg x kg). This is about 5 times greater than the reported value of D(Po2) calculated from measurements of P(O2) in the mixed uterine and umbilical venous blood. With a diffusing capacity of this magnitude the maternal and fetal placental end capillary P(O2) would approach equilibrium, becoming too small to measure, and the calculation of D(Po2) would be unreliable. We suggest that the apparent end capillary P(o2) gradients of 15 to 20 mm Hg, obtained from sampling uterine and umbilical venous blood, result from a combination of uneven distribution of maternal and fetal placental blood flow and from placental oxygen consumption.
本文描述了一种利用一氧化碳研究胎盘呼吸功能的技术,一氧化碳是一种气体,其在母胎循环之间跨胎盘的交换受扩散而非血流限制。在引入一氧化碳之前的稳定状态下,母羊中碳氧血红蛋白的正常浓度COHb约为0.90%,胎儿中的浓度为2.9%,COHb/COHb的比值为3.2。在狗中,相应的值分别为1.9%、4.8%和2.4%。将一氧化碳引入母体动物后,一氧化碳缓慢地跨胎盘扩散,平衡半衰期约为2小时。在母胎交换过程中,绵羊胎盘的平均一氧化碳扩散容量(D(Pco))为每(分钟×毫米汞柱×千克胎儿体重)0.54毫升(标准差±0.13),狗为每(分钟×毫米汞柱×千克)0.57毫升(标准差±0.18)。两只绵羊中从胎儿到母体的胎盘扩散容量为每(分钟×毫米汞柱×千克)0.54毫升。考虑到氧气和一氧化碳与红细胞血红蛋白反应的相对速率以及两种气体的相对扩散速率进行的计算表明,真正的D(Po2)应该比D(Pco)大约高1.2至2倍,即每(分钟×毫米汞柱×千克)0.65至1.1。这大约是根据子宫和脐静脉混合血中P(O2)测量值计算出的D(Po2)报告值的5倍。具有这种大小的扩散容量时,母胎胎盘终末毛细血管的P(O2)将接近平衡,变得太小而无法测量,并且D(Po2)的计算将不可靠。我们认为,从子宫和脐静脉血采样获得的15至20毫米汞柱的表观终末毛细血管P(o2)梯度是由母胎胎盘血流分布不均和胎盘氧消耗共同导致的。