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Pulse Radiolysis of Liquids at High Pressures. II. Diffusion-Controlled Reactions of the Hydrated Electron
28
Citations
19
References
1972
Year
Chemical KineticsEngineeringAtmospheric PhotochemistryOrganic ChemistryChemistryIon ProcessSolution (Chemistry)Chemical EngineeringDiffusion CoefficientAnalytical ChemistryMolecular KineticsRadiation ChemistryChemical MeasurementPhysicsPulse RadiolysisPhysical ChemistryHydrogenHydrated ElectronAbsolute Specific RatesNatural SciencesActivation VolumeReaction ProcessHigh Pressures
For each of 11 presumably diffusion-controlled reactions of eaq−, absolute specific rates were determined by pulse radiolysis at four to seven pressures from atmospheric to 6.4 kbar. The ratio of specific rate at 6.4 kbar to that at 1 atm, followed by the corresponding activation volume in milliliters mole−1, is given in parentheses for each of the reactants: O2 (1.05, −0.2), H2O2 (0.88, 0.5), acrylamide (0.90, 0.4), benzamide (0.95, 0.2), p-nitrophenol (0.84, 0.7), NO3− (1.00, 0.0), S2O82− (1.07, −0.3), Cr(C2O4)33− (1.32, −1.1), Tl+ (0.74, 1.2), Cd2+ (0.75, 1.1), Sm3+ (0.86, 0.6). The Debye equation for specific rate of a diffusion-controlled reaction is used for analysis of the results. Such an analysis suggests that the diffusion coefficient of eaq− changes negligibly (compared to normal ions and molecules) and possibly increases with increase in pressure to 6.4 kbar. With the result for reaction of eaq− with NO3−, certain activation volumes obtained in previous γ-radiolysis studies (by assumption of an activation volume for the NO3− reaction) are corrected, and corrected values of 0 and 3 ml mole−1 are obtained for the partial molal volume and cavity volume, respectively, of an electron in water.
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