4.8 Article

Magnetically-mediated regeneration and reuse of core-shell Fe0@FeIII granules for in-situ hydrogen sulfide control in the river sediments

期刊

WATER RESEARCH
卷 157, 期 -, 页码 621-629

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.watres.2019.03.066

关键词

Sediment; Hydrogen sulfide; Fe-0@Fe-III granules; Microbial iron reduction; Magnetic separation; Indirect electron transfer

资金

  1. National Natural Science Foundation of China [51808231, 51638005]
  2. Guangdong Provincial Science and Technology Planning Project [20178050504003]

向作者/读者索取更多资源

A novel iron-cycling process based on core-shell iron granules, which contained zero-valent iron (Fe) in the core and maghemite (gamma-Fe2O3) on the shell (Fe-0@Fe-III granules), was proposed to in-situ control hydrogen sulfide in the sediments of the polluted urban rivers. The Fe-0@Fe-III granules added in the top sediment layer removed 97% of sulfide generated by sulfate-reducing bacteria in the sediments, and the sulfide removal capacity of virgin granules was 163 mg S/g Fe (114 mg S/g granule). The Fe-0@FeIII granules removed the formed sulfide through the abiotic sulfide oxidation and precipitation, and they also stimulated the microbial iron reduction, which competitively consumed wastewater-derived organics and partially inhibited the sulfate reduction in the sediments. The used Fe-0@Fe-III granules were easily regenerated through magnetic separation from sediments and air exposure for 12 h, which enhanced the sulfide removal capacities of the regenerated granules by 12%-22%, compared to the virgin granules. During the air exposure, ferrous products (i.e., iron sulfide and surface-associated Fe-II) on the granule shell were completely oxidized to poorly ordered Fe-III hydroxides (gamma-FeOOH and amorphous FeOOH) having larger specific surface areas and higher reactivity to sulfide than gamma-Fe2O3 on the virgin granules. Meanwhile, the Fe-0 in the core was also partially oxidized through the indirect electron transfer, which was facilitated by the electrically conductive iron oxide minerals (Fe3O4 and Fe2O3) and the microbial electron carriers (e.g., Geobacter). The oxidation of Fe core contributed additional Fe-III hydroxides to the sulfide control. The Fe-0@Fe-III granules were reused for four times in a 293-day trial, and their overall sulfide removal capacity was at least 920 mg S/g Fe. The proposed iron-cycling process can be a chemical saving, energy-saving and cost-effective approach for the hydrogen sulfide control in the sediments of polluted urban rivers, as well as lakes, aquaculture ponds and marine. (C) 2019 Elsevier Ltd. All rights reserved.

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