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The role of polysaccharides and diatom exudates in the redox cycling of Fe and the photoproduction of hydrogen peroxide in coastal seawaters

机译:多糖和硅藻渗出物在沿海海水中铁的氧化还原循环和过氧化氢的光生产中的作用

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The effect of artificial acidic polysaccharides (PS) and exudates ofPhaeodactylum tricornutum on the half-life of Fe(II) in seawater was investigated in laboratoryexperiments. Strong photochemical hydrogen peroxide (H2O2)production of 5.2 to 10.9 nM (mg C)−1 h−1 was found in thepresence of PS and diatom exudates. Furthermore when illuminated with UVlight the presence of algal exudates had a net stabilising effect on ferrousiron in seawater (initial value 100 nmol L−1) above that expected fromoxidation kinetics. In the dark the PS gum xanthan showed no stabilisingeffect on Fe(II). The photochemical formation of superoxide (O2−)in the presence of diatom exudates and its reducing effect on Fe(III)appears to result in greater than expected concentrations of Fe(II). A modelof the photochemical redox cycle of iron incorporating these processessupported the observed data well. Diatom exudates seem to have the potentialto play an important role for the photochemistry of iron in coastal waters.
机译:在实验室实验中,研究了人工酸性多糖(PS)和三角藻(Phaeodylum tricornutum)的渗出物对海水中Fe(II)半衰期的影响。强光化学过氧化氢(H 2 O 2 )产生5.2至10.9 nM(mg C) -1 h -1 < / sup>存在于PS和硅藻渗出液中。此外,当用紫外线照射时,藻类渗出液对海水中亚铁的净稳定作用(初始值100 nmol L -1 )高于氧化动力学所预期的稳定作用。在黑暗中,PS胶黄原胶对Fe(II)没有显示稳定作用。在硅藻渗出液存在下,超氧化物(O 2 -)的光化学形成及其对Fe(III)的还原作用似乎导致Fe(III)的浓度高于预期。 II)。结合这些过程的铁的光化学氧化还原循环模型很好地支持了观察到的数据。硅藻渗出物似乎对沿海水域铁的光化学起着重要作用。

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