KINETICS OF THE REACTIONS OF THE SO4- RADICAL WITH SO4-, S2O82-, H2O AND FE2+
KINETICS OF THE REACTIONS OF THE SO4- RADICAL WITH SO4-, S2O82-, H2O AND FE2+
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DOI:
10.1039/ft9908602557
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发表时间:
1990-07-21
期刊:
影响因子:
--
通讯作者:
WAYGOOD, SJ
中科院分区:
文献类型:
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作者:
MCELROY, WJ;WAYGOOD, SJ
The sulphate radical anion, SO4-, is known to be a key intermediate in the aqueous aerobic oxidation of SO2 initiate by free radicals. The absorption spectrum of SO4- has been obtained following photolysis of K2S2O8 soltuions at 248 nm. Kinetic spectrophotometric techniques have been employed to investigate the decay of SO4- in the presence of S2O82- and Fe11. Several rate constants have been determined at 293 K: 2k(SO4- + SO4-) = (8.9 .+-. 0.3) .times. 108 dm3 mol-1 s-1 (at infinite dilution), k(SO4- + S2O82-) = (6.1 .+-. 0.6) .times. 105 dm3 mol-1 s-1 (at infinite dilution) and k(SO4- + H2O) = (500 .+-. 60) s-1. The reaction of SO4- with Fe11 proceeds via a rapid equilibration step followed by electron transfer which is rate-determining. Values of k1, k-1 and k2 at 293 K are (3.0 .+-. 1.9) .times. 108 dm3 mol-1 s-1 (4.8 .+-. 3.0) .times. 104 s-1 (6.5 .+-. 2.1) .times. 103 s-1 respectively. The implications of these results for current cloud and precipitation chemistry models are discussed.