Stromal lactate accumulation can account for corneal oedema osmotically following epithelial hypoxia in the rabbit.
- 1 December 1981
- journal article
- research article
- Published by Wiley in The Journal of Physiology
- Vol. 321 (1), 49-64
- https://doi.org/10.1113/jphysiol.1981.sp013971
Abstract
The mechanism underlying stromal edema subsequent to epithelial hypoxia was investigated in isolated rabbit corneas. Stromas swelled about 20 .mu.m following a 1-h period of tear side hypoxia in both whole corneal isolates and in preparations in which fluid movement across the endothelium was blocked with silicone oil. In the experiments using whole corneas, stromal thickness was independent of tear side O2 tension as long as aqueous humor P[partial pressure]O2 was > 40 mm Hg. Neither epithelial thickness nor epithelial electrical resistance, a measure of total ion permeability, was significantly affected by blocking respiration. A 10.degree. C reduction in corneal temperature markedly reduced the rate of hypoxic swelling, suggesting the involvement of a metabolism-dependent hydrating process and implicating the stromal accumulation of a catabolyte. When CN- was used to mimic the hypoxic effect in isolated whole corneas, the passive 36Cl unidirectional flux was unaffected, but lactate production rate and stromal [lactate] more than doubled. These measurements were used with a mathematical model for corneal hydration dynamics to examine the causes of hypoxic edema. Epithelial hypoxia enhances epithelial lactate production and release to the stroma. This process causes an increase in stromal lactate concentration and a decrease in stromal NaCl concentration (primarily through dilution). Stromal lactate accumulation exceeds in osmotic load the dilutional effect on [NaCl], producing stromal edema. Whereas hypoxia produces corneal metabolic acidosis, effects on endothelial permeability of HCO3- transport need not be postulated to explain the stromal edema that results from hypoxia.This publication has 27 references indexed in Scilit:
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