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ABSTRACT
Humic substances interfered with the ion-selective electrode determination of Cl- by complexing Ag+ and thereby reducing the activity of the potential determining ion. Binding of Ag+ was proven with a technique that involved equilibrium dialysis and Ag+ determination by atomic absorption spectroscopy. Competition between Ag+ and H+ for binding sites was evident from an increase in millivolt response of the Cl- ion-selective electrode with addition of HNO3 and release of protons upon Ag+ binding in the dialysis experiment. Selectivity coefficients (kCl,HA) for 11 humic and fulvic acids ranged from 0.59 x 10–4 to 1.3 x 10–4 mol g–1 at pH 6.5. Interference is negligible in solutions containing <0.1 g L–1 humic substances, but is serious in samples with low concentrations of Cl- (< 10–4.5 M) and high amounts of organic matter (>0.1 g L–1).
1 Contribution from the Dep. of Agronomy, Univ. of Illinois, Urbana, IL 61801. Supported in part by a grant from the United States-Israel Agricultural Research and Development Fund (BARD I-500-82).
2 Research Assistant and Professor of Soil Chemistry, respectively. The senior author is now Research Chemist, F242 NFDC, Tennessee Valley Authority, Muscle Shoals, AL 35660.
Received for publication November 17, 1986.
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