Zubieta-Calleja Gustavo, Zubieta-Castillo Gustavo, Zubieta-Calleja Luis, Ardaya-Zubieta Gustavo, Paulev Poul-Erik
Indian J Clin Biochem. 2011 Jan;26(1):62-5. doi: 10.1007/s12291-010-0088-9. Epub 2010 Nov 16.
As the oxygen tension of inspired air falls with increasing altitude in normal subjects, hyperventilation ensues. This acute respiratory alkalosis, induces increased renal excretion of bicarbonate, returning the pH back to normal, giving rise to compensated respiratory alkalosis or chronic hypocapnia. It seems a contradiction that so many normal people at high altitude should permanently live as chronic acid-base patients. Blood gas analyses of 1,865 subjects at 3,510 m, reported a P(a)CO(2) (arterial carbon dioxide tension ± SEM) = 29.4 ± 0.16 mmHg and pH = 7.40 ± 0.005. Base excess, calculated with the Van Slyke sea level equation, is -5 mM (milliMolar or mmol/l) as an average, suggesting chronic hypocapnia. THID, a new term replacing "Base Excess" is determined by titration to a pH of 7.40 at a P(a)CO(2) of 5.33 kPa (40 mmHg) at sea level, oxygen saturated and at 37°C blood temperature. Since our new modified Van Slyke equations operate with normal values for P(a)CO(2) at the actual altitude, a calculation of THID will always result in normal values-that is, zero.
在正常受试者中,随着海拔升高,吸入空气中的氧分压下降,继而出现过度通气。这种急性呼吸性碱中毒会导致肾脏对碳酸氢盐的排泄增加,使pH值恢复正常,从而产生代偿性呼吸性碱中毒或慢性低碳酸血症。许多正常人在高海拔地区竟会像慢性酸碱失衡患者一样长期生活,这似乎自相矛盾。对3510米海拔处的1865名受试者进行的血气分析报告显示,动脉二氧化碳分压(P(a)CO(2) ± 标准误)= 29.4 ± 0.16 mmHg,pH值 = 7.40 ± 0.005。用范斯莱克海平面方程计算得出的碱剩余平均为 -5 mM(毫摩尔或mmol/l),表明存在慢性低碳酸血症。THID是一个取代“碱剩余”的新术语,它是在海平面、氧饱和且血液温度为37°C的条件下,将样本滴定至pH值为7.40、P(a)CO(2)为5.33 kPa(40 mmHg)时所确定的值。由于我们新修改的范斯莱克方程使用的是实际海拔下P(a)CO(2)的正常值,所以THID的计算结果将始终为正常值,即零。