Poyart C F, Fréminet A, Bursaux E
Respir Physiol. 1975 Oct;25(1):101-7. doi: 10.1016/0034-5687(75)90054-7.
Bone 14CO2 specific activities have been measured in 10 male rats perfused for 30, 60 or 120 minutes with [14C]bicarbonate. A steady blood 14CO2 specific activity is observed from the 30th minute, whereas bone 14CO2 specific activity increased linearly with time. About 7-10% of the total activity infused may be recovered in the skeleton at any given time. Bone samples heated to constant weight lost 15% of their total CO2 content and more than 50% of the 14CO2 activity. This indicates that 14CO2 present in bone is almost exclusively located in a bicarbonate pool which may be considered as the rapidly exchangeable bone CO2 fraction. The rate of exchange between bone and blood CO2 is estimated at a maximum of 15% of the total CO2 production. It is postulated that blood flow to the skeleton is the limiting factor for bone CO2 exchange. These results lead to the conclusion that the large bone CO2 store cannot play a significant role in the buffering of extracellular fluids in acute acid-base abnormalities.
对10只雄性大鼠进行了实验,用[¹⁴C]碳酸氢盐灌注30、60或120分钟,随后测定了骨骼¹⁴CO₂的比活度。从第30分钟开始观察到血液¹⁴CO₂比活度稳定,而骨骼¹⁴CO₂比活度随时间呈线性增加。在任何给定时间,注入的总活度中约7 - 10%可在骨骼中回收。加热至恒重的骨骼样品损失了其总CO₂含量的15%以及超过50%的¹⁴CO₂活度。这表明骨骼中存在的¹⁴CO₂几乎完全位于一个碳酸氢盐池中,该池可被视为骨骼中可快速交换的CO₂部分。骨骼与血液CO₂之间的交换速率估计最高为总CO₂产生量的15%。据推测,流向骨骼的血流量是骨骼CO₂交换的限制因素。这些结果得出结论,在急性酸碱异常情况下,大量的骨骼CO₂储备在细胞外液缓冲中不能发挥重要作用。