1986
DOI: 10.1016/0045-6535(86)90037-8
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Steady state concentrations of the phototransient hydrated electron in natural waters

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Cited by 13 publications
(10 citation statements)
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“…Thermal deactivation was a dominant process (97%-99%), and only 1%-3% of energy would be transferred to an excited triplet state, most of which was involved in formation of '0 2 , In an aqueous solution of HA, Takahashi et al (1988) confirmed the formation of OH', 02H·, and '0 2 in the presence of O 2 by ESR measurements using spin-trapping reagents. Photoinduced generation of e~q from natural waters also has been confirmed by its conversion to OH· with N 20 (Thomas -Smith and Blough 2001) , and the steady-state concentration of e~q was estimated to be approximately 1.1 x 10-17 M (Breugem et al 1986). Photoinduced generation of e~q from natural waters also has been confirmed by its conversion to OH· with N 20 (Thomas -Smith and Blough 2001) , and the steady-state concentration of e~q was estimated to be approximately 1.1 x 10-17 M (Breugem et al 1986).…”
Section: F Photophysical and Photochemical Processes Of Soil Componentsmentioning
confidence: 88%
“…Thermal deactivation was a dominant process (97%-99%), and only 1%-3% of energy would be transferred to an excited triplet state, most of which was involved in formation of '0 2 , In an aqueous solution of HA, Takahashi et al (1988) confirmed the formation of OH', 02H·, and '0 2 in the presence of O 2 by ESR measurements using spin-trapping reagents. Photoinduced generation of e~q from natural waters also has been confirmed by its conversion to OH· with N 20 (Thomas -Smith and Blough 2001) , and the steady-state concentration of e~q was estimated to be approximately 1.1 x 10-17 M (Breugem et al 1986). Photoinduced generation of e~q from natural waters also has been confirmed by its conversion to OH· with N 20 (Thomas -Smith and Blough 2001) , and the steady-state concentration of e~q was estimated to be approximately 1.1 x 10-17 M (Breugem et al 1986).…”
Section: F Photophysical and Photochemical Processes Of Soil Componentsmentioning
confidence: 88%
“…While e -(aq) has been a known product of water radiolysis for more than 50 years (Herbert and Coons, 2017), it can also be produced in surface waters by the interaction of sunlight with constituents of DOM (Thomas- Smith and Blough, 2001). It appears that the lifetime of the e -(aq) in the DOM phase is sufficient for its reaction with hydrophobic compounds sorbed into the DOM phase (Breugem et al, 1986). Due to the hydrophobic nature of SCCPs, with estimated octanol-water partition coefficients (Kow) between 9×10 4 and 3×10 7 (Glüge et al, 2013), these compounds have the potential to be degraded by this mechanism.…”
Section: Introductionmentioning
confidence: 99%
“…48 It appears that the lifetime of the e -(aq) in the DOM phase is sufficient for its reaction with hydrophobic compounds sorbed by DOM. 49 Due to the hydrophobic nature of SCCPs, with estimated octanol-water partition coefficients (Kow) between 9x10 4 and 3x10 7 , these compounds have the potential to be degraded by this mechanism. 50 However, the reactivity of e -(aq) towards SCCPs has not yet been systematically investigated.…”
Section: Introductionmentioning
confidence: 99%
“…M 49,71 have been reported. However, since the lifetime of e -(aq) has been estimated to be much longer in a DOM microenvironment with different characteristics (e.g., lower O2) than the bulk aqueous solution, 91,92 DOM is expected to facilitate SCCP photodegradation in the environment.…”
mentioning
confidence: 99%