| Literature DB >> 22211016 |
Gustavo Zubieta-Calleja, Gustavo Zubieta-Castillo, Luis Zubieta-Calleja, Gustavo Ardaya-Zubieta, Poul-Erik Paulev.
Abstract
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.Entities:
Keywords: Acidbase equilibrium; Base deficit; Base excess; High altitude; Hypoxia; Titratable hydrogen ion difference
Year: 2010 PMID: 22211016 PMCID: PMC3068777 DOI: 10.1007/s12291-010-0088-9
Source DB: PubMed Journal: Indian J Clin Biochem ISSN: 0970-1915