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자료유형
학술저널
저자정보
Kwon, Man Jae (한국과학기술연구원) Yang, Jung-Seok (한국과학기술연구원) Shim, Moo Joon (한국과학기술연구원) Lee, Seunghak (한국과학기술연구원) Boyanov, Maxim (알곤국립연구소) Kemner, Kenneth (알곤국립연구소) O'Loughlin, Edward (알곤국립연구소)
저널정보
한국지하수토양환경학회 지하수토양환경 지하수토양환경 제19권 제1호
발행연도
2014.1
수록면
54 - 62 (9page)

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To better understand dissimilatory iron and sulfate reduction (DIR and DSR) by subsurface microorganisms, we investigated the effects of sulfate and electron donors on the microbial goethite (${\alpha}$-FeOOH) reduction. Batch systems were created 1) with acetate or glucose (donor), 2) with goethite and sulfate (acceptor), and 3) with aquifer sediment (microbial source). With 0.2 mM sulfate, goethite reduction coupled with acetate oxidation was limited. However, with 10 mM sulfate, 8 mM goethite reduction occurred with complete sulfate reduction and x-ray absorption fine-structure analysis indicated the formation of iron sulfide. This suggests that goethite reduction was due to the sulfide species produced by DSR bacteria rather than direct microbial reaction by DIR bacteria. Both acetate and glucose promoted goethite reduction. The rate of goethite reduction was faster with glucose, while the extent of goethite reduction was higher with acetate. Sulfate reduction (10 mM) occurred only with acetate. The results suggest that glucose-fermenting bacteria rapidly stimulated goethite reduction, but acetate-oxidizing DSR bacteria reduced goethite indirectly by producing sulfides. This study suggests that the availability of specific electron donor and sulfate significantly influence microbial community activities as well as goethite transformation, which should be considered for the bioremediation of contaminated environments.

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