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Title: Impact of organic acids and sulfate on the biogeochemical properties of soil from urban subsurface environments

Abstract

Urban subsurface environments are often different from undisturbed subsurface environments due to the impacts of human activities. For example, deterioration of underground infrastructure can introduce elevated levels of Ca, Fe, and heavy metals into subsurface soils and groundwater. Likewise, leakage from sewer systems can lead to contamination by organic C, N, S, and P. However, the impact of these organic and inorganic compounds on biogeochemical processes including microbial redox reactions, mineral transformations, and microbial community transitions in urban subsurface environments is poorly understood. Here we conducted a microcosm experiment with soil samples from an urban construction site to investigate the possible biotic and abiotic processes impacted when sulfate and acetate or lactate were introduced into an urban subsurface environment. In the top-layer soil (0-0.3 m) microcosms, which were highly alkaline (pH > 10), the major impact was on abiotic processes such as secondary mineral precipitation. In the mid-layer (2-3 m) soil microcosms, the rate of Fe(III)-reduction and the amount of Fe(II) produced were greatly impacted by the specific organic acid added, and sulfate-reduction was not observed until after Fe(III)-reduction was complete. Near the end of the incubation, some genera related to syntrophic acetate oxidation and methanogenesis were observed in themore » lactateamended microcosms. In the bottom-layer (7-8 m) soil microcosms, the rate of Fe(III)-reduction and the amount of Fe(II) produced were affected by the concentration of amended sulfate. Sulfate-reduction was concurrent with Fe(III)-reduction, suggesting that Fe(II) production was likely due to abiotic reduction of Fe(III) by sulfide produced by microbial sulfate reduction. The slightly acidic initial pH (~5.8) of the mid-soil system was a major factor controlling sequential microbial Fe(III) and sulfate reduction versus parallel Fe(III) and sulfate reduction in the bottom soil system, which had a neutral initial pH (~7.2). Finally, 16S rRNA gene-based community analysis revealed a variety of indigenous microbial groups including alkaliphiles, dissimilatory iron and sulfate reducers, syntrophes, and methanogens tightly coupled with, and impacted by, these complex abiotic and biogeochemical processes occurring in urban subsurface environments.« less

Authors:
 [1];  [2];  [1]
+ Show Author Affiliations
  1. Korea Univ., Seoul, (Korea, Republic of)
  2. Argonne National Lab. (ANL), Argonne, IL (United States)
Publication Date:
Research Org.:
Argonne National Lab. (ANL), Argonne, IL (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER); National Research Foundation of Korea (NRF); Korea University
OSTI Identifier:
1826073
Grant/Contract Number:  
AC02-06CH11357; 2018R1A2B6001660
Resource Type:
Accepted Manuscript
Journal Name:
Journal of Environmental Management
Additional Journal Information:
Journal Volume: 292; Journal ID: ISSN 0301-4797
Publisher:
Elsevier
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; Alkaliphilic bacteria; Calcium sulfate minerals; Dissimilatory iron reduction; Dissimilatory sulfate reduction; Microbial community; Synthrophic acetate oxidation

Citation Formats

Lee, Sunhui, O'Loughlin, Edward J., and Kwon, Man Jae. Impact of organic acids and sulfate on the biogeochemical properties of soil from urban subsurface environments. United States: N. p., 2021. Web. doi:10.1016/j.jenvman.2021.112756.
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Lee, Sunhui, O'Loughlin, Edward J., & Kwon, Man Jae. Impact of organic acids and sulfate on the biogeochemical properties of soil from urban subsurface environments. United States. https://doi.org/10.1016/j.jenvman.2021.112756
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Lee, Sunhui, O'Loughlin, Edward J., and Kwon, Man Jae. Tue . "Impact of organic acids and sulfate on the biogeochemical properties of soil from urban subsurface environments". United States. https://doi.org/10.1016/j.jenvman.2021.112756. https://www.osti.gov/servlets/purl/1826073.
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@article{osti_1826073,
title = {Impact of organic acids and sulfate on the biogeochemical properties of soil from urban subsurface environments},
author = {Lee, Sunhui and O'Loughlin, Edward J. and Kwon, Man Jae},
abstractNote = {Urban subsurface environments are often different from undisturbed subsurface environments due to the impacts of human activities. For example, deterioration of underground infrastructure can introduce elevated levels of Ca, Fe, and heavy metals into subsurface soils and groundwater. Likewise, leakage from sewer systems can lead to contamination by organic C, N, S, and P. However, the impact of these organic and inorganic compounds on biogeochemical processes including microbial redox reactions, mineral transformations, and microbial community transitions in urban subsurface environments is poorly understood. Here we conducted a microcosm experiment with soil samples from an urban construction site to investigate the possible biotic and abiotic processes impacted when sulfate and acetate or lactate were introduced into an urban subsurface environment. In the top-layer soil (0-0.3 m) microcosms, which were highly alkaline (pH > 10), the major impact was on abiotic processes such as secondary mineral precipitation. In the mid-layer (2-3 m) soil microcosms, the rate of Fe(III)-reduction and the amount of Fe(II) produced were greatly impacted by the specific organic acid added, and sulfate-reduction was not observed until after Fe(III)-reduction was complete. Near the end of the incubation, some genera related to syntrophic acetate oxidation and methanogenesis were observed in the lactateamended microcosms. In the bottom-layer (7-8 m) soil microcosms, the rate of Fe(III)-reduction and the amount of Fe(II) produced were affected by the concentration of amended sulfate. Sulfate-reduction was concurrent with Fe(III)-reduction, suggesting that Fe(II) production was likely due to abiotic reduction of Fe(III) by sulfide produced by microbial sulfate reduction. The slightly acidic initial pH (~5.8) of the mid-soil system was a major factor controlling sequential microbial Fe(III) and sulfate reduction versus parallel Fe(III) and sulfate reduction in the bottom soil system, which had a neutral initial pH (~7.2). Finally, 16S rRNA gene-based community analysis revealed a variety of indigenous microbial groups including alkaliphiles, dissimilatory iron and sulfate reducers, syntrophes, and methanogens tightly coupled with, and impacted by, these complex abiotic and biogeochemical processes occurring in urban subsurface environments.},
doi = {10.1016/j.jenvman.2021.112756},
journal = {Journal of Environmental Management},
number = ,
volume = 292,
place = {United States},
year = {Tue May 25 00:00:00 EDT 2021},
month = {Tue May 25 00:00:00 EDT 2021}
}
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