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a Soil Science Program, Dep. of Agronomy, Pennsylvania State Univ., University Park, PA 16802 USA
b Dep. of Civil and Environmental Engineering, Pennsylvania State Univ., University Park, PA 16802 USA
c Dep. of Chemistry, Ohio State Univ., Columbus, OH 43210 USA
jdc7{at}psu.edu
Adsorption of quinoline
and background electrolyte (LiCl) onto specimen kaolinite was measured as a function of surface-bound humic acid (HA) concentration
, pH (310), and ionic strength (110 mM). Complexation of HA on the kaolinite surface (4.5 mg C kg-1) reduced the point of zero net charge (pznc) for kaolinite by more than one pH unit and resulted in a significant increase in negative surface charge. Maximum sorption of quinoline occurred near its pKa for all sorbents. Below the pKa, quinoline sorption increases with increasing pH and decreasing proton competition. Above the pKa, sorption is reduced in parallel with (but offset to a higher pH from) the ionized fraction. Competition with Li+ for surface sites is apparent from diminished quinoline adsorption with increasing ionic strength, but sorption of the ionized form of quinoline is always favored and kaolinite exhibits selectivity for cationic quinoline over
. However, increasing fOC diminishes quinoline sorption and selectivity
and increases sorption reversibility relative to uncoated kaolinite. Humic acid alone exhibits lower selectivity for quinoline
. The results indicate that mineral-sorbed humic substances can diminish retention of cationic quinoline despite an increase in overall cation-exchange capacity.
Abbreviations: BET, BrunauerEmmettTeller CPMAS-NMR, cross-polarization magic angle spinning nuclear magnetic resonance spectroscopy DOC, dissolved organic C EGME, ethylene glycol monoethyl ether fOC, mass fraction of soil organic C HA, humic acid NHC, N heterocyclic compound PAC, polycyclic aromatic compound pznc, point of zero net charge TOC, total organic C
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