INTERACTION OF A FLUOROQUINOLONE ANTIBIOTIC WITH NANOMETER-SIZE SOIL OXIDE PARTICLES: ADSORPTION AND BREAKDOWN
OFX is an amphoteric fluoroquinolone (pKa1 = 5.97, pKa2 = 8.28). Al2O3 has a net (+) surface charge at pH < 8.7 (pzc), while the pzc values for the other particles are: SiO2 < 2.8, Fe2O3 < 6.5-7.0, and TiO2 < 7.2. OFX sorption to Al2O3 generates linear isotherms of mass sorbed/mass nano vs. liquid concentration (R2>.96). Maximum OFX sorbed was 16 mmol/kg, with a Kd of 441 L/kg (± 35). OFX sorption to SiO2, TiO2 and Fe2O3 is logarithmic, with the parameters: SiO2 Ln Kf=3.0 (± .52), n=.57 (± .10); TiO2. Ln Kf = 8.6 (±3.5), n= .82 (±.51); Fe2O3 Ln Kf = 5.5 (± 1.2), n=.89 (± .17). Maximum OFX sorbed was 10 mmol/kg to SiO2, 370 mmol/kg to TiO2, and 11 mmol/kg to Fe2O3. Substrates with sorbed OFX were rinsed with OFX-free solutions in successive desorption experiments to remove weakly attached molecules. Results show ~ 7% of the initially-adsorbed OFX could be removed from Al2O3, 89% from SiO2, < 1% from TiO2, and 27% from Fe2O3. Smaller percentages indicate stronger adsorption mechanisms.
Breakdown of zwitterionic OFX was observed in 80-hr timed mixing experiments with 25nm-TiO2 when samples analyzed at intervals were compared to OFX controls. Decrease in OFX was accompanied by an increase in at least 2 product compounds. Mass spectral data suggest these breakdown reactions may involve the N-methyl, carbonyl, and carboxyl groups. Concentrations of the two products (m/z = 336-337 and m/z = 348-349) increase at a linear rate of ~ 1.5%/hr. Comparison of data from isotherm and timed experiments will quantify the amount of sorption vs. breakdown. Preliminary results from SiO2, Fe2O3 and Al2O3 timed experiments indicate less breakdown of OFX compared to the effects of TiO2.