PHOTOCHEMISTRY OF AQUEOUS IRON(III) POLYCARBOXYLATE COMPLEXES - ROLES IN THE CHEMISTRY OF ATMOSPHERIC AND SURFACE WATERS

被引:509
作者
FAUST, BC [1 ]
ZEPP, RG [1 ]
机构
[1] US EPA,ENVIRONM RES LAB,ATHENS,GA 30605
关键词
D O I
10.1021/es00048a032
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Photochemical redox reactions of Fe(III) complexes of polycarboxylates (e.g., citrate, malonate, oxalate) occur on time scales of minutes in sunlight and are potentially important sources of Fe(II), .O2-/HO2., H2O2, and .OH in atmospheric water drops and surface waters. Quantum yields for Fe(II) formation, determined from experiments and equilibrium speciation calculations, are (i) 0.28 for Fe(OH)(citrate)- at 436 nm, (ii) 0.027 for Fe(malonate)2- at 366 nm, and (iii) 1.0 for Fe(oxalate)2- and 0.6 for Fe(oxalate)3(3-) at 436 nm. Competitive reactions of O2 and Fe(III) with the polycarboxylate radicals and/or the carbon-centered radicals derived from decarboxylation, as well as the speciation of Fe(II) and Fe(III), affect the experimental quantum yields of Fe(II) formation.
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页码:2517 / 2522
页数:6
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