Abstract
In the course of a study of the response of the guinea pig uterus to pituitrin when the ionic environment of the uterus was varied, the carbonate ion was found to be of importance in determining the magnitude of the response. The carbonate ion seems to exert its influence of itself, and not to be merely reflecting a change in calcium or hydrogen ion activity. This is shown by the following experimental results.
Whenever the carbonate ion activity was increased there was a diminished response of the uterus to pituitrin. This was true whether the carbonate ion activity was increased (a) by increasing the bicarbonate activity and CO2 tension proportionately so that there was no change in pH; (b) by increasing the bicarbonate activity alone with an increase in pH; or (c) by decreasing the CO2 tension alone, which also resulted in an increased pH.
Whenever the carbonate ion activity was decreased there was an increased response of the uterus to pituitrin. This occurred whether the carbonate ion activity was decreased (a) by decreasing the bicarbonate ion activity and CO2, tension proportionately without change in pH; (b) by decreasing the bicarbonate without change in CO2, tension thereby lowering the pH; or (c) by increasing only the CO2, tension which also resulted in a decreased pH.
When the carbonate ion activity was kept as CO2nstant as experimental technique permitted, there was either no change in response or a slight change which might at times be positive and at other times negative. This occurred regardless of whether the bicarbonate was doubled, the CO2, tension quadrupled and the resulting pH decreased, or the bicarbonate was halved, the CO2, tension quartered and the resulting pH increased
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