A. Duker et al., ADSORPTION OF ZINC ON COLLOIDAL (HYDR)OXIDES OF SI, AL AND FE IN THE PRESENCE OF A FULVIC-ACID, Applied geochemistry, 10(2), 1995, pp. 197-205
The adsorption of Zn (total concentration 10(-6) M) to colloidal quart
z, hydrargillite and goethite (50, 300 and 70 mg/l, respectively) was
studied by a batch technique at a constant ionic strength (0.01 M) but
with variation of pH (3-10) and fulvic acid (FA) concentration (0, 2
or 20 mg/l). The adsorption had similar pH-dependence in all systems i
n the absence of FA giving a pH(50) (PH of 50% adsorption) of 7.6 unde
r these conditions. The presence of the FA reduced the overall adsorpt
ion to quartz (pH(50) Of 7.9 at 2 mg FA/I and 9.3 at 20 mg/l) and shif
ted the adsorption curves downwards (pH(50) Of 6.8) in the hydrargilli
te and goethite systems at 2 mg FA/I. At 20 mg FA/I, the adsorption in
the two latter systems was increased at pH <6.5 and reduced at pH >6.
5. The results reflect the affinity of the surfaces for FA as well as
the formation of Zn-FA complexes (in solution and on solid surfaces).