Abstract
Summary o 1. Simultaneous determinations of the rate of oxygen evolution, the rate of reduction of added oxidant, and the rate of hydrogen-ion production during the photolysis of water by illuminated chloroplast fragments were made continuously on the same system during the course of illumination. 2. The stoichiometry indicated in the following equation was found to hold within the experimental error throughout the course of the reaction: 3. None of the component reactions of the photolysis of water could be dissociated under the conditions employed in order to permit separate study. 4K3Fe(CN)6+4K++2H2O→4K4Fe(CN)6+4H++O2.
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