| Literature DB >> 24550712 |
Marcella Nebbioso1, Stefano Fazio1, Dario Di Blasio2, Nicola Pescosolido3.
Abstract
OBJECTIVE: The purpose of this study focused on understanding the mechanisms underlying ocular hydrodynamics and the changes which occur in the eyes of subjects exposed to hypobaric hypoxia (HH) to permit the achievement of more detailed knowledge in glaucomatous disease.Entities:
Mesh:
Year: 2014 PMID: 24550712 PMCID: PMC3914587 DOI: 10.1155/2014/585218
Source DB: PubMed Journal: ScientificWorldJournal ISSN: 1537-744X
Figure 1Values of tonometry measurements recorded at T1 (baseline phase to sea level), T2 (18,000 feet, phase of ascent), T3 (18,000 feet, phase of descent), and T4 (return phase to sea level). IOP: intraocular pressure (in mmHg); *statistically significant (P < 0.05); NS: not statistically significant; SD: standard deviation.
Values of mean intraocular pressure (IOP) recorded at T1 (baseline phase to sea level), T2 (ascent phase to 18,000 feet), T3 (descent phase to 18,000 feet), and T4 (return phase to sea level).
| Altitude (in feet) | IOP mean ± SD (in mmHg) |
|
|---|---|---|
| 0 | 16 ± 2.23 | / |
| 18,000 ↑ | 13.7 ± 4.17 | T1/T2 NS |
| 18,000 ↓ | 14.5 ± 2.74 | T1/T3 NS |
| 0 | 12.8 ± 2.57 | T1/T4 * |
SD: standard deviation; NS: not statistically significant; *statistically significant (P < 0.05).
Figure 2Pachymetry values related to corneal thickness in conditions of hypobarism revealed a statistically significant increase (P < 0.05). The average normobaric value was 555.14 ± 14.7 (SD) μm versus 564.64 ± 16.5 (SD) μm in hypobaric conditions, at 25,000 feet.