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    Soil Microbiome Dynamics During Pyritic Mine Tailing Phytostabilization

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    Author
    Hottenstein, John
    Issue Date
    2016
    Keywords
    Environmental reclamation
    Microbial bioindicators
    Microbial ecology
    Phytostabilization
    Pyrite dissolution
    Acid mine drainge
    Advisor
    Maier, Raina M.
    
    Metadata
    Show full item record
    Publisher
    The University of Arizona.
    Rights
    Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author.
    Embargo
    Release after 18-Jan-2018
    Abstract
    Challenges to the reclamation of pyritic mine tailings arise from in-situ acid generation that severely constrains natural revegetation. While microbial communities that participate in acid generation through iron and sulfur (FeS) oxidation in acidic aquatic environments are well studied, relatively little information is available concerning the initial dynamics of in-situ soil acidification due to microbial FeS oxidation that occur in moderately acidic conditions. This research characterizes the taxonomic composition and behavior of microbial FeS oxidizing communities across a pH gradient from moderately acidic to highly acidic environmental conditions. We combine results from a 7-year compost-assisted phytostabilization field study with a controlled microcosm enrichment experiment that was conducted in an artificial soil matrix to follow the influence of pH on development of the soil microbiome. Microcosm results show that biological activity significantly increases the acidification rate in moderately acidic pH conditions in comparison to abiotic controls. Taxonomic profiles of the microbial communities in the microcosms and from the field study reveal that populations associated with both heterotrophic and lithotrophic activity (Alicyclobacillaceae, Acetobacteraceae and Xanthomonadaceae) dominate during acidification in moderately acidic conditions. These results suggest that chemoheterotrophs are an important element of the microbial community that help enable, directly and indirectly, lithotrophic FeS oxidation across moderately acidic conditions. Taken together, this research suggests that shifts of microbial populations associated with pH transitions have the potential to be used as bioindicators of the present and future status of the phytostabilization process.
    Type
    text
    Electronic Thesis
    Degree Name
    M.S.
    Degree Level
    masters
    Degree Program
    Graduate College
    Soil, Water and Environmental Science
    Degree Grantor
    University of Arizona
    Collections
    Master's Theses

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