Literature DB >> 32157881

Role of in Situ Natural Organic Matter in Mobilizing As during Microbial Reduction of FeIII-Mineral-Bearing Aquifer Sediments from Hanoi (Vietnam).

M Glodowska1,2, E Stopelli3, M Schneider4, A Lightfoot3, B Rathi5, D Straub2,6, M Patzner1, V T Duyen7, M Berg3, S Kleindienst2, A Kappler1.   

Abstract

Natural organic matter (NOM) can contribute to arsenic (As) mobilization as an electron donor for microbially-mediated reductive dissolution of As-bearing Fe(III) (oxyhydr)oxides. However, to investigate this process, instead of using NOM, most laboratory studies used simple fatty acids or sugars, often at relatively high concentrations. To investigate the role of relevant C sources, we therefore extracted in situ NOM from the upper aquitard (clayey silt) and lower sandy aquifer sediments in Van Phuc (Hanoi area, Vietnam), characterized its composition, and used 100-day microcosm experiments to determine the effect of in situ OM on Fe(III) mineral reduction, As mobilization, and microbial community composition. We found that OM extracted from the clayey silt (OMC) aquitard resembles young, not fully degraded plant-related material, while OM from the sandy sediments (OMS) is more bioavailable and related to microbial biomass. Although all microcosms were amended with the same amount of C (12 mg C/L), the extent of Fe(III) reduction after 100 days was the highest with acetate/lactate (43 ± 3.5% of total Fe present in the sediments) followed by OMS (28 ± 0.3%) and OMC (19 ± 0.8%). Initial Fe(III) reduction rates were also higher with acetate/lactate (0.53 mg Fe(II) in 6 days) than with OMS and OMC (0.18 and 0.08 mg Fe(II) in 6 days, respectively). Although initially more dissolved As was detected in the acetate/lactate setups, after 100 days, higher concentrations of As (8.3 ± 0.3 and 8.8 ± 0.8 μg As/L) were reached in OMC and OMS, respectively, compared to acetate/lactate-amended setups (6.3 ± 0.7 μg As/L). 16S rRNA amplicon sequence analyses revealed that acetate/lactate mainly enriched Geobacter, while in situ OM supported growth and activity of a more diverse microbial community. Our results suggest that although the in situ NOM is less efficient in stimulating microbial Fe(III) reduction than highly bioavailable acetate/lactate, it ultimately has the potential to mobilize the same amount or even more As.

Entities:  

Year:  2020        PMID: 32157881     DOI: 10.1021/acs.est.9b07183

Source DB:  PubMed          Journal:  Environ Sci Technol        ISSN: 0013-936X            Impact factor:   9.028


  3 in total

Review 1.  An evolving view on biogeochemical cycling of iron.

Authors:  Andreas Kappler; Casey Bryce; Muammar Mansor; Ulf Lueder; James M Byrne; Elizabeth D Swanner
Journal:  Nat Rev Microbiol       Date:  2021-02-01       Impact factor: 60.633

Review 2.  Autotrophic Fe-Driven Biological Nitrogen Removal Technologies for Sustainable Wastewater Treatment.

Authors:  Suyan Pang; Ning Li; Huan Luo; Xiaonan Luo; Tong Shen; Yanan Yang; Jin Jiang
Journal:  Front Microbiol       Date:  2022-04-29       Impact factor: 6.064

3.  Reduction of iron (hydr)oxide-bound arsenate: Evidence from high depth resolution sampling of a reducing aquifer in Yinchuan Plain, China.

Authors:  Yuqin Sun; Jing Sun; Athena A Nghiem; Benjamin C Bostick; Tyler Ellis; Long Han; Zengyi Li; Songlin Liu; Shuangbao Han; Miao Zhang; Yu Xia; Yan Zheng
Journal:  J Hazard Mater       Date:  2020-11-18       Impact factor: 10.588

  3 in total

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