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Cr(VI) reduction by Fe(II)-dissolved organic matter complexes and the characterization of pore water dissolved organic matter from a coastal wetland in the Laurentian Great Lakes

Agrawal, Sheela G.

Abstract Details

2008, Doctor of Philosophy, Ohio State University, Environmental Science.

This study examines the chemical nature and reactivity of dissolved organic matter (DOM) in the anoxic, sedimentary, fresh water, pore waters of Old Woman Creek (OWC), located in Huron, OH.

Chapter 1 offers an introduction to DOM, and describes it general chemical makeup with respect to its source materials (terrestrial vs. microbial, allochthonous vs. autochthonous). More importantly, Chapter 1 explains the enormous role DOM plays in an ecosystem, with particular emphasis on DOM’s potential application in the realm of environmental remediation and rehabilitation. Chapter 2 examines pore water DOM reactivity in the context of Cr(VI) remediation by Fe(II)-DOM complexes. Model and natural systems are used to examine differences in DOM reactivity and the feasibility of Cr(VI) in a wetland environment. Generally, DOM complexed to Fe(II) increased Cr(VI) reduction dramatically as compared to Fe(II)-only and microbially-mediated reduction. Additionally, microbially-derived vs. terrestrially-derived DOM exhibited differential reactivities as a function chemical make-up. We also observed a non-3:1 Fe(II): Cr(VI) reduction stoichiometry cyclical reduction of oxidized Fe(III) back to Fe(II) by DOM. Chapter 3 employs a relatively new diagnostic tool known as Parallel Factor analysis (PARAFAC) to characterize pore water DOM in terms of mathematically modeled fluorescing constituents. In turn, these components represent chemically meaningful entities which may be used to explain pore water DOM reactivity. We identified three such components which are described as “humic-like”, “fulvic-like” and “protein”, “tryptophan”, “quinone-like” based upon comparison to existing PARAFAC models.

Chapter 4 characterizes pore water DOM using UV-VIS and fluorescence spectroscopy and existing correlations with 13C-NMR-determined aromaticity and the McKnight fluorescence index (a source material index). As a result OWC pore water DOM is identified as being both terrestrial and microbial in origin – which in turn explains its reactivity observed in Chapter 1. Chapter 5 presents a summary of the conclusions of Chapters 2-4.

Overall, the goal of this study is to supplement existing pore water studies to better understand the reactivity of DOM in natural systems, such as wetlands, especially in the context of contaminant remediation.

Yu-Ping Chin, PhD (Advisor)
David Culver, PhD (Committee Member)
Steven Lower, PhD (Committee Member)
Earl Epstein, PhD, JD (Committee Member)
111 p.

Recommended Citations

Citations

  • Agrawal, S. G. (2008). Cr(VI) reduction by Fe(II)-dissolved organic matter complexes and the characterization of pore water dissolved organic matter from a coastal wetland in the Laurentian Great Lakes [Doctoral dissertation, Ohio State University]. OhioLINK Electronic Theses and Dissertations Center. http://rave.ohiolink.edu/etdc/view?acc_num=osu1230735368

    APA Style (7th edition)

  • Agrawal, Sheela. Cr(VI) reduction by Fe(II)-dissolved organic matter complexes and the characterization of pore water dissolved organic matter from a coastal wetland in the Laurentian Great Lakes. 2008. Ohio State University, Doctoral dissertation. OhioLINK Electronic Theses and Dissertations Center, http://rave.ohiolink.edu/etdc/view?acc_num=osu1230735368.

    MLA Style (8th edition)

  • Agrawal, Sheela. "Cr(VI) reduction by Fe(II)-dissolved organic matter complexes and the characterization of pore water dissolved organic matter from a coastal wetland in the Laurentian Great Lakes." Doctoral dissertation, Ohio State University, 2008. http://rave.ohiolink.edu/etdc/view?acc_num=osu1230735368

    Chicago Manual of Style (17th edition)