溶解
化学
缺氧水域
鳞片岩
催化作用
无机化学
吸附
配体(生物化学)
金属
红外光谱学
环境化学
针铁矿
物理化学
生物化学
受体
有机化学
作者
Jagannath Biswakarma,Kyounglim Kang,Susan C. Borowski,Walter D. C. Schenkeveld,Stephan M. Kraemer,Janet G. Hering,Stephan J. Hug
标识
DOI:10.1021/acs.est.8b03910
摘要
Fe incorporation at the mineral surface. Infrared spectra indicated no change in the bulk, but changes in the spectra of adsorbed EDTA after addition of Fe(II) were observed. A kinetic model shows that the catalytic effect can be explained by electron transfer to surface Fe(III) sites and rapid detachment of Fe(III)EDTA due to the weaker bonds to reduced sites. We conclude that the catalytic effect of Fe(II) on dissolution of Fe(III)(hydr)oxides is likely important under circumneutral anoxic conditions and in sunlit environments.
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