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天然有机物对微生物还原针铁矿过程中镉形态变化的影响

Effect of Natural Organic Matter on the Fate of Cadmium During Microbial Ferrihydrite Reduction.

机构信息

Geomicrobiology, Center for Applied Geosciences, University of Tuebingen, 72076 Tuebingen, Germany.

Delaware Environmental Institute, University of Delaware, Newark, Delaware 19716, United States.

出版信息

Environ Sci Technol. 2020 Aug 4;54(15):9445-9453. doi: 10.1021/acs.est.0c03062. Epub 2020 Jul 16.

DOI:10.1021/acs.est.0c03062
PMID:32633952
Abstract

Natural organic matter (NOM) is known to affect the microbial reduction and transformation of ferrihydrite, but its implication toward cadmium (Cd) associated with ferrihydrite is not well-known. Here, we investigated how Cd is redistributed when ferrihydrite undergoes microbial reduction in the presence of NOM. Incubation with showed that both the rate and the extent of reduction of Cd-loaded ferrihydrite were enhanced by increasing concentrations of NOM (i.e., C/Fe ratio). Without NOM, only 3-4% of Fe(III) was reduced, but around 61% of preadsorbed Cd was released into solution due to ferrihydrite transformation to lepidocrocite. At high C/Fe ratio (1.6), more than 35% of Fe(III) was reduced, as NOM can facilitate bioreduction by working as an electron shuttle and decreased aggregate size, but only a negligible amount of Cd was released into solution, thus decreasing Cd toxicity and prolonging microbial Fe(III) reduction. No ferrihydrite transformation was observed at high C/Fe ratios using Mössbauer spectroscopy and X-ray diffraction, and X-ray absorption spectroscopy indicated the proportion of Cd-OM bond increased after microbial reduction. This study shows that the presence of NOM leads to less mobilization of Cd under reducing condition possibly by inhibiting ferrihydrite transformation and recapturing Cd through Cd-OM bond.

摘要

天然有机物(NOM)已知会影响铁水铁矿的微生物还原和转化,但它对与铁水铁矿相关的镉(Cd)的影响尚不清楚。在这里,我们研究了当 NOM 存在时,铁水铁矿发生微生物还原时 Cd 是如何重新分配的。用 进行孵育表明,随着 NOM(即 C/Fe 比)浓度的增加,负载 Cd 的铁水铁矿的还原速率和程度都得到了增强。没有 NOM 时,只有 3-4%的 Fe(III)被还原,但由于铁水铁矿转化为纤铁矿,约 61%的预吸附 Cd 被释放到溶液中。在高 C/Fe 比(1.6)下,超过 35%的 Fe(III)被还原,因为 NOM 可以作为电子穿梭体并减小聚集体尺寸,从而促进生物还原,但只有极少量的 Cd 被释放到溶液中,从而降低了 Cd 的毒性并延长了微生物 Fe(III)还原。高 C/Fe 比下用穆斯堡尔光谱和 X 射线衍射观察到没有铁水铁矿转化,X 射线吸收光谱表明,微生物还原后 Cd-OM 键的比例增加。这项研究表明,在还原条件下,NOM 的存在可能通过抑制铁水铁矿转化和通过 Cd-OM 键重新捕获 Cd,导致 Cd 的迁移性降低。

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