Rates of in situ microbial sulfate reduction in response to geochemical perturbations were determined using Native Organism Geochemical Experimentation Enclosures (NOGEEs), a new in situ technique developed to facilitate evaluation of controls on microbial reaction rates. NOGEEs function by first trapping a native microbial community in situ and then subjecting it to geochemical perturbations through the introduction of various test solutions. On three occasions, NOGEEs were used at the Norman Landfill research site in Norman, Oklahoma, to evaluate sulfate-reduction rates in wetland sediments impacted by landfill leachate. The initial experiment, in May 2007, consisted of five introductions of a sulfate test solution over 11 d. Each test stimulated sulfate reduction with rates increasing until an apparent maximum was achieved. Two subsequent experiments, conducted in October 2007 and February 2008, evaluated the effects of concentration on sulfate-reduction rates. Results from these experiments showed that faster sulfate-reduction rates were associated with increased sulfate concentrations. Understanding variability in sulfate-reduction rates in response to perturbations may be an important factor in predicting rates of natural attenuation and bioremediation of contaminants in systems not at biogeochemical equilibrium.
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http://dx.doi.org/10.1111/j.1745-6584.2010.00782.x | DOI Listing |
Environ Microbiol Rep
April 2025
School of Chemical and Metallurgical Engineering, University of the Witwatersrand, Johannesburg, South Africa.
This study investigated the suitability of readily available and naturally occurring sources of microorganisms (inoculum) to use for the cultivation of sulphate-reducing bacteria (SRB) for acid mine drainage (AMD) remediation. The selected inocula included AMD water (AMD), mud (MUD) and reed-bed mud (RM) from the AMD surrounds, mealworms (MW), cow dung (CD) and raw sewage sludge (RS). The suitability of the different inoculum sources was evaluated by comparing the SO reduction and sulfide (S) production rates at three different pHs.
View Article and Find Full Text PDFISME J
March 2025
Bigelow Laboratory for Ocean Sciences, East Boothbay, ME 04544, United States.
The chemical cycles carried out by bacteria and archaea living in coastal sediments are vital aspects of benthic ecology. These ecosystems are subject to physical disruption, which may allow for increased respiration and complex carbon consumption - impacting chemical cycling in this environment often thought to be a terminal place of deposition. We use the redox-enzyme sensitive probe RedoxSensor Green to measure rates of electron transfer physiology in individual sulfate reducer cells residing in anoxic sediment, subjected to transient exposure of oxygen and laminarin.
View Article and Find Full Text PDFWater Res
February 2025
State Key Laboratory of Advanced Environmental Technology and Guangdong-Hong Kong-Maco Joint Laboratory for Environmental Pollution and Control, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; Guangdong Key Laboratory of Environmental Protection and Resources and Utilization, Guangzhou 510640, China.
Microplastics have increasingly accumulated in sulfate- and organic matter-rich mangrove ecosystems, yet their effects on microbially mediated carbon and sulfur cycling in sediments remains poorly understood. In this study, we performed a 70-day anaerobic microcosm experiment to examine the effects of polylactic acid (PLA) microplastics with different sizes on sulfate reduction and dissolved organic carbon (DOC) degradation in mangrove sediments. Our results demonstrated that millimeter-scale PLA (mm-PLA) more effectively enhanced sulfate reduction, sulfur isotope fractionation, reduced sulfide production, and carbon dioxide (CO) emission compared to micrometer-scale PLA (m-PLA).
View Article and Find Full Text PDFWater Res
February 2025
Basin Water Environmental Research Department, Changjiang River Scientific Research Institute, Wuhan, PR China; Key Lab of Basin Water Resource and Eco-Environmental Science in Hubei Province, Wuhan, PR China.
Saltwater-freshwater mixing in mangrove wetlands drives complex biogeochemical processes that regulate the cycling and transformation of key elements. Yet, the detailed quantification of biogenic element cycling and transformations under saltwater-freshwater interactions remains insufficiently explored. This study developed a field-scale reactive transport model, constrained by multi-level monitoring and hydrochemical data, to investigate the migration, transformation, and fluxes of biogenic elements (C, N, S, Fe) in the Dongzhai Harbor mangrove wetland aquifer.
View Article and Find Full Text PDFBioresour Technol
February 2025
Laboratory for Research on Advanced Processes for Water Treatment, Engineering Institute, Campus Juriquilla, Universidad Nacional Autónoma de México (UNAM), Blvd. Juriquilla 2001, 76230 Querétaro, Mexico. Electronic address:
Bioreactors supplied with sulfate and Fe(III) oxides (hematite and goethite), as electron acceptors, were tested for their capacity to remove dissolved methane from a digestate from a methanogenic reactor treating synthetic wastewater. Negligible removal of dissolved methane occurred when no electron acceptor was provided. However, when hematite and goethite were supplied, methane removal rates of 6.
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