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Functionalization and Dispersion of Carbon Nanomaterials Using an Environmentally Friendly Ultrasonicated Ozonolysis Process
Published on: May 30, 2017
Implications of water chemistry on ozone nanobubble-based advanced oxidation processes
Andre Luna Magdaleno1, Kathleen Myers-Haeussler1, Kenneth Mensah2
1Nanosystems Engineering Research Center for Nanotechnology-Enabled Water Treatment, School of Sustainable Engineering and the Built Environment, Arizona State University, Tempe, AZ 85287-3005, USA.
Abstract:
Ozone nanobubbles (O3-NBs) are increasingly promoted to enhance advanced oxidation processes (AOPs) through improved gas dissolution and interfacial reactivity, yet their behavior in realistic waters remains poorly resolved. Here we evaluate O3-NBs generation, stability, and reactivity across ultra-pure water, synthetic and real freshwater, and synthetic and real seawater. The ζ-potential measurements showed strong matrix dependence, shifting from -25 mV in ultra-pure water to +30 mV in real freshwater due to ionic and organic species adsorption. Salt presence during bubble nucleation, combined with matrix-induced alterations in surface charge, governed interfacial properties and ultimately controlled O3 reactivity. Across all systems, NBs delivered mass-transfer coefficients more than an order of magnitude higher than macrobubbles (MBs), confirming superior O3 delivery (kLa= 1.12-1.90 min-1 vs. 0.13-0.22 min-1). However, O3 persistence varied sharply with matrix composition. Decay was minimal in ultra-pure water (kd = 0.003 min-1), but ionic and organic components in freshwater accelerated interfacial decomposition (kd up to 0.160 min-1), demonstrating that NBs do not inherently extend O3 lifetime. In seawater, high ionic strength intensified NBs-driven reactions, producing rapid O3 depletion (decay over the first minute, Δ01= 1.6 mg L-1 min-1) and near-complete bromide oxidation to bromate. MBs formed mostly hypobromous acid, which interfered with O3 measurements. These processes strongly influenced treatment performance. Despite higher O3 exposure, O3-NBs favored interface-driven and selective oxidation rather than sustained bulk mineralization, resulting in limited DOC removal in both real freshwater and seawater. Across matrices, O3-NBs preferentially oxidized humic- and fulvic-like fractions while largely preserving protein-like and microbial by-product-like components. These mechanistic insights highlight the importance of water chemistry and interfacial processes for optimizing O3-based treatment, particularly in saline environments.
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