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" Influence of electrolyte chemistry on the structure and reactivity of Fe(III) precipitates generated by Fe(0) electrocoagulation: "
van Genuchten, Case Michael
Gadgil, Ashok JPeña, Jasquelin
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Latin Dissertation
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English
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897428
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TL8kk0b8h1
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Sieverding, Maia
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Influence of electrolyte chemistry on the structure and reactivity of Fe(III) precipitates generated by Fe(0) electrocoagulation:\ van Genuchten, Case MichaelGadgil, Ashok JPeña, Jasquelin
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2013
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2013
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| Abstract
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The formation of Fe(III) (oxyhydr)oxide precipitates from Fe(II) oxidation and/or Fe(III) hydrolysis is a key process that often governs the fate and bioavailability of contaminants and nutrients in natural and engineered systems. Electrocoagulation (EC) using Fe(0) electrodes is a low-cost water treatment technology that generates reactive Fe(III) precipitates in-situ via the electrolytic dissolution of an Fe(0) anode. EC-generated Fe(III) precipitates efficiently sorb contaminants, such as arsenic, and can then be separated from treated water by gravitational settling and/or filtration. The goal of this work is to determine the influence of electrolyte chemistry and EC operating parameters on the structure and reactivity of EC-generated Fe(III) precipitates. This dissertation begins with an investigation of the structure and arsenic removal mechanism of Fe(III) precipitates generated by EC at a range of current densities in synthetic Bangladesh groundwater (SBGW). Shell-by-shell fits of the Fe K-edge extended X-ray absorption fine structure (EXAFS) spectra indicate that EC precipitates consist of nanoscale chains (polymers) of edge-sharing FeO6 octahedra. Shell-by-shell fits of As K-edge EXAFS spectra show that arsenic binds to EC precipitates in the binuclear, 2C corner-sharing geometry. When bound in this specific configuration, arsenic prevents the formation of FeO6 corner-sharing linkages. Phosphate and silicate oxyanions, abundant in SBGW, likely bind to EC precipitates in a similar configuration and contribute to the absence corner-sharing Fe-Fe linkages. The high extent of As(III) oxidation indicated by the As K-edge spectra is likely due to the reactive intermediates generated during EC treatment by the oxidation of Fe(II) by dissolved oxygen (i.e., Fenton-type reactions). Fe and As K-edge EXAFS spectra were found to be similar among samples generated at a large range of current density (0.02, 1.1, 5.0, 100 mA/cm2), suggesting this operating parameter does not play a major role in the structure of EC precipitates. The next objective after characterizing EC precipitates generated in SBGW is to systematically investigate the individual and combined effects of major solutes (Ca2+, Mg2+, P, As(V), Si) on the structure and reactivity of EC-generated Fe(III) precipitates. Fe(II) oxidation in the presence of weakly adsorbing electrolytes (NaCl, CaCl2, MgCl2) produces pseudo-lepidocrocite (pseudo-Lp; γ-FeOOH), a poorly crystalline version of Lp with low sheet-stacking coherence. In the absence of bivalent cations, P and As(V) have similar uptake behavior, but different effects on the average Fe(III) precipitate structure: pseudo-Lp dominates in the presence of P, whereas a disordered ferrihydrite-like precipitate akin to hydrous ferric oxide (HFO) is the dominant phase that forms in the presence of As(V). Despite its lower affinity for Fe(III) precipitates, Si leads to Si-HFO under all conditions tested. The presence of 1 mM Ca2+ or Mg2+ enhances oxyanion uptake, destabilizes the colloidally stable oxyanion-bearing particle suspensions and, in some P and As(V) electrolytes, results in more crystalline precipitates. The trends in oxyanion uptake and Fe(III) precipitate structure in the presence of Ca2+/Mg2+ suggest a systematic decrease in the strength of bivalent cation:oxyanion interaction in the order of Ca2+>Mg2+ and P>As(V)>>Si. In the third research chapter, the effect of the interaction between cations and oxyanions on the structure of EC-generated Fe(III) precipitates is examined in greater detail. The sequential formation of Fe(III) precipitates from Fe(II) oxidation in the presence of oxyanions leads to multiple mineral phases: short-ranged oxyanion-rich Fe(III) polymers with a large sorption capacity form at the onset of electrolysis followed by pseudo-Lp after oxyanions are depleted from the electrolyte. The larger As:Fe and P:Fe solids ratios in the presence of Ca2+ leads to less Fe required to deplete oxyanions from solution, and thus pseudo-Lp forms earlier in the electrolysis stage in Ca2+-containing electrolytes. Shell-by-shell fits of the As K-edge EXAFS spectra of all samples indicate no significant change in As(V) coordination in the presence or absence of Ca2+ and that As(V) binds primarily in the 2C binuclear, corner-sharing geometry. Structural models for the oxyanion-bearing Fe(III) polymers that form at the onset of electrolysis are proposed using constraints derived from batch sorption experiments, mobilization data, and molecular scale characterization techniques. According to these structural models, the role of Ca2+ in increasing the As:Fe or P:Fe solids ratios is two-fold: 1) "structural" Ca2+ participates in direct bonding with sorbed As(V) or P and increases oxyanion uptake via specific bonding interactions and 2) "electrostatic" Ca2+ associates with the solid in weaker, non-specific interactions that increase oxyanion uptake by minimizing electrostatic repulsion between oxyanions and the negatively charged Fe(III) precipitate surface. The sustainable operation of EC systems in the field requires a rigorous understanding of the effects of EC operating parameters, such as current density, on EC system performance. Knowledge of the effects of individual and combined concentrations of major dissolved species on the local bonding environment, mineral phase, crystallinity, and mechanism of ion uptake of EC-generated Fe(III) precipitates will permit more accurate predictions of EC system performance across a diverse range of chemical matrices likely to be encountered in the field. This information also advances the understanding of contaminant and nutrient transport at natural redox boundaries such as hyporheic zones in soils and sediments.
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van Genuchten, Case Michael
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UC Berkeley
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