Nanoparticle-enhanced Breakdown of Penicillin Antibiotic in Water: Implications for Fate of Drugs in the Environment
Faculty Mentor(s)
Dr. Jonathan Peterson, Hope College
Dr. Michael Seymour, Hope College
Document Type
Poster
Publication Date
4-15-2011
Abstract
Extensive use of pharmaceuticals in human and animal medicine has resulted in antibiotic contamination of natural waters. Nanoparticles (10-9 m) are found in natural soil-water environments and have the ability to adsorb contaminants due to the large surface to volume ratio. Though adsorption to nanosurfaces likely plays a significant role in reducing aqueous concentrations of drugs, nanoparticle-mediated degradation of organic compounds may also be a significant mechanism. This was investigated by exposing ampicillin (AMP), a common penicillin antibiotic, to nanoparticles of Fe2O3, TiO2, Al2O3, and SiO2 in separate timed batch experiments. AMP adsorption and degradation were measured by HPLC analysis of solutions and breakdown products were identified by LC/MS analysis.
Degradation of zwitterionic AMP (pKa1 = 2.5, pKa2 = 7.3) was observed in timed mixing experiments with 25nm- TiO2 (anatase) at pH 6.2 over 48 hours. TiO2 has a net positive surface charge at pH < 7.2 (pzc). Significant degradation of AMP (m/z = 350) was measured in mixed samples relative to controls, with initial parent AMP of 553 μmol/L dropping to 1 μmol/L within 48 hours. Decrease in AMP concentration was accompanied by an increase in the concentrations of two products, isomers of penicilloic acid (P1 and P2, at m/z = 368-369), likely formed by the hydrolysis of the beta-lactam ring of AMP. Formation of the P2 penicilloic acid isomer can be described by a logarithmic function of ln [P2] = 0.965 (ln(time)) + 5.02 (R2 > 0.98). Comparison of adsorption isotherm and timed experiment data are in progress to quantify the actual extent of, and relationships between adsorption and degradation mechanisms. Similar trends were observed in experiments with nano-Fe2O3 and Al2O3, but no significant enhancement was observed in SiO2 data experiments.
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Comments
The research was funded in part by the NASA-Michigan Space Grant Consortium Seed Grant Program, Howard Hughes Medical Institute, the Hope College Department of Geological & Environmental Sciences, and the Hope College Chemistry Department. Many thanks to team members Nicholas Powers, Emily Van Wieren and Jeffrey Wilcox. Conversations with Kenneth Brown and Jason Gilmore were very helpful.