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Association Between Arterial Blood Gas Variation and Intraocular Pressure in Healthy Subjects Exposed to Acute Short-Term Hypobaric Hypoxia

PURPOSE: To investigate the association between changes in arterial blood gases and intraocular pressure (IOP) after acute, short-term exposure to simulated elevation of 4000 m above sea level. METHODS: Twenty-five healthy young lowlanders participated in this prospective study. IOP was measured in...

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Detalles Bibliográficos
Autores principales: Xie, Yuan, Yang, Yiquan, Han, Ying, Yang, Diya, Sun, Yunxiao, Wang, Xinmao, Nguyen, Anh Hong, Chen, Yihan, Tian, Jiaxin, Zhang, Qing, Xin, Chen, Cao, Kai, Wang, Huaizhou, Liu, Xiaofang, Wang, Guozhong, Wang, Ningli
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Association for Research in Vision and Ophthalmology 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6871546/
https://www.ncbi.nlm.nih.gov/pubmed/31788351
http://dx.doi.org/10.1167/tvst.8.6.22
Descripción
Sumario:PURPOSE: To investigate the association between changes in arterial blood gases and intraocular pressure (IOP) after acute, short-term exposure to simulated elevation of 4000 m above sea level. METHODS: Twenty-five healthy young lowlanders participated in this prospective study. IOP was measured in both eyes with an Accupen tonometer. Arterial blood gas parameters (partial oxygen pressure [PaO(2)], partial carbon dioxide pressure [PaCO(2)], pH, and bicarbonate ion [HCO(3)(−)]) were checked using a blood gas analyzer. Measurements were taken at sea level (T1), at 15-minute (T2) and at 2-hour (T3) exposure times to simulated 4000 m above sea level in a hypobaric chamber, and upon return to sea level (T4). Associations between arterial blood gas parameters and IOP were evaluated using multivariate linear regression. RESULTS: PaO(2) significantly decreased at T2 and T3, resolving at T4 (P < 0.001). pH significantly increased at T2 and returned to baseline at T3 (P = 0.004). Actual and standard bicarbonate ion both dropped with IOP at T3 and T4. IOP significantly decreased from 16.4 ± 3.4 mm Hg at T1 to 15.1 ± 2.1 mm Hg (P = 0.041) at T3 and remained lower (14.9 ± 2.4 mm Hg; P = 0.029) at T4. IOP was not correlated with pH. Multivariate linear regression showed that lower IOP was associated with lower standard bicarbonate ion (beta = −1.061; 95% confidence interval, −0.049 to −2.074; P = 0.04) when adjusted for actual bicarbonate and diastolic blood pressure. CONCLUSIONS: Hypobaric hypoxia triggers plasma bicarbonate ion reduction which, rather than pH, may decrease aqueous humor formation and subsequently cause IOP reduction. These findings may shed light on the mechanism of IOP regulation at high altitude. TRANSLATIONAL RELEVANCE: Hypoxia-triggered reduction in plasma bicarbonate ion may decrease aqueous humor production, leading to IOP reduction at high altitude. These findings may provide new insight into a potential mechanism of IOP regulation. Hypobaric hypoxia at high altitude is an environmental factor that can reduce IOP and, therefore, deserves further study.