School of Civil and Environmental Engineering, The University of New South Wales , Sydney, NSW 2052, Australia.
Environ Sci Technol. 2017 Mar 21;51(6):3287-3297. doi: 10.1021/acs.est.7b00396. Epub 2017 Mar 9.
Interaction of the exudate secreted by a toxic strain of the cyanobacterium Microcystis aeruginosa with Fe(II) and Fe(III) was investigated here under both acidic (pH 4) and alkaline (pH 8) conditions. At the concentrations of iron and exudate used, iron was present as dissolved iron (<0.025 μm) at pH 4 but principally as small (<0.45 μm) iron oxyhydroxide particles at pH 8 with only ∼3-27% present in the dissolved form as a result of iron binding by the organic exudate. The formation of strong Fe(III) exudate and relatively weak Fe(II) exudate complexes alters the reduction potential of the Fe(III)-Fe(II) redox couple, facilitating more-rapid oxidation of Fe(II) at pH 4 and 8 than was the case in the absence of exudate. Our results further show that the organic exudate contains Fe(III)-reducing moieties, resulting in the production of measurable concentrations of Fe(II). However, these reducing moieties are short-lived (with a half-life of 1.9 h) and easily oxidized in air-saturated environments. A kinetic model was developed that adequately describes the redox transformation of Fe in the presence of exudate both at pH 4 and pH 8.
在这里,研究了在酸性(pH4)和碱性(pH8)条件下,铜绿微囊藻有毒菌株分泌的渗出物与 Fe(II) 和 Fe(III) 的相互作用。在使用的铁和渗出物浓度下,铁在 pH4 时以溶解态铁(<0.025μm)存在,但在 pH8 时主要以小颗粒(<0.45μm)形式存在铁氧氢氧化物,只有约 3-27%以溶解态存在,这是由于有机渗出物与铁结合。强 Fe(III)渗出物和相对较弱的 Fe(II)渗出物复合物的形成改变了 Fe(III)-Fe(II)氧化还原对的还原电位,促进了在 pH4 和 8 时比没有渗出物时更快地氧化 Fe(II)。我们的结果进一步表明,有机渗出物含有 Fe(III)还原部分,导致可测量浓度的 Fe(II)的产生。然而,这些还原部分的寿命很短(半衰期为 1.9 小时),并且在空气饱和的环境中很容易被氧化。开发了一个动力学模型,该模型可以充分描述在存在渗出物的情况下,Fe 在 pH4 和 pH8 时的氧化还原转化。