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首页> 外文期刊>The Science of the Total Environment >Synthetic iron complexes as models for natural iron-humic compounds: Synthesis, characterization and algal growth experiments
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Synthetic iron complexes as models for natural iron-humic compounds: Synthesis, characterization and algal growth experiments

机译:合成铁络合物作为天然铁腐殖质化合物的模型:合成,表征和藻类生长实验

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摘要

A series of monomeric and dimeric Fe~Ⅲ complexes with O,O-; O,N-; O,S-coordination motifs has been prepared and characterized by standard analytical methods in order to elucidate their potential to act as model compounds for aquatic humic acids. Due to the postulated reduction of iron in humic acids and following uptake by microorganisms, the redox behavior of the models was investigated with cyclic voltammetry. Most of the investigated compounds showed iron reduction potentials accessible to biological reducing agents. Additionally, observed reduction processes were predominantly irreversible, suggesting that subsequent reactions can take place after reduction of the iron center. Also the stability of the synthesized complexes in pure water and artificial seawater was monitored from 24 h up to 21 days by means of UV-Vis spectrometry. Several complexes remained stable even after 21 days, showing only partially precipitation but some of them showed changes in UV-Vis spectra already after 24 h which were connected to protonation/deprotonation processes as well as redox processes and degradation of the complexes. The ability to act as an iron source for primary producers was tested in algal growth experiments with two marine algae species Chlorella salina and Prymnesium parvum. Some of the compounds showed effects on the algal cultures, which are comparable with natural humic acids and better as for the samples kept under ideal conditions. Those findings help to understand which functional groups of humic acids could be responsible for the reversible iron binding and transport in aquatic humic substances.
机译:一系列具有O,O-的单体和二聚Fe〜Ⅲ配合物;上-;为了阐明它们作为水生腐殖酸的模型化合物的潜力,已通过标准分析方法制备了O,S配位基序并进行了表征。由于假定腐殖酸中铁减少并被微生物吸收,因此使用循环伏安法研究了该模型的氧化还原行为。大多数被研究的化合物显示出生物还原剂可达到的铁还原潜力。另外,观察到的还原过程主要是不可逆的,表明随后的反应可在铁中心还原后发生。还通过UV-Vis光谱法监测合成的配合物在纯水和人造海水中的稳定性,从24小时到21天。甚至在21天后,一些配合物仍保持稳定,仅显示部分沉淀,但其中一些在24小时后就已经显示UV-Vis光谱变化,这与质子化/去质子化过程以及氧化还原过程和配合物的降解有关。在藻类生长实验中,用两种海藻小球藻小球藻和小白球藻测试了作为主要生产者的铁源的能力。一些化合物对藻类培养物具有影响,可与天然腐殖酸相媲美,并且比保存在理想条件下的样品更好。这些发现有助于了解哪些腐殖酸官能团可能负责水生腐殖质中可逆的铁结合和转运。

著录项

  • 来源
    《The Science of the Total Environment》 |2017年第15期|94-104|共11页
  • 作者单位

    Institute of Inorganic Chemistry, Faculty of Chemistry, University of Vienna, Waehringer Str. 42, A-1090 Vienna, Austria;

    Institute of Inorganic Chemistry, Faculty of Chemistry, University of Vienna, Waehringer Str. 42, A-1090 Vienna, Austria;

    Department of Nutritional and Physiological Chemistry, Faculty of Chemistry, University of Vienna, Althanstr. 14/UZA Ⅱ, A-1090 Vienna, Austria;

    Institute of Inorganic Chemistry, Faculty of Chemistry, University of Vienna, Waehringer Str. 42, A-1090 Vienna, Austria,Department of Zoology, University of Johannesburg, Auckland Park 2006, South Africa;

    Institute of Inorganic Chemistry, Faculty of Chemistry, University of Vienna, Waehringer Str. 42, A-1090 Vienna, Austria;

    Institute of Inorganic Chemistry, Faculty of Chemistry, University of Vienna, Waehringer Str. 42, A-1090 Vienna, Austria;

    Institute of Inorganic Chemistry, Faculty of Chemistry, University of Vienna, Waehringer Str. 42, A-1090 Vienna, Austria;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Humic acids models; Coordination compounds; Iron complexes; Iron uptake; Algal growth experiments;

    机译:腐殖酸模型;配位化合物;铁络合物;铁摄取;藻类生长实验;

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