The sorption of metal ions (Pb2+, Zn2+ and Cu2+) and soil humic acids (HA)
from aqueous solutions onto mineral particles (sand, calcite and clay) was
investigated using a batch equilibrium system. The sorption reactions in tw
o-component systems (heavy metals-mineral particles and humic acids-mineral
particles), as well as interactions in three-component system (heavy metal
s-humic acids-mineral particles) were examined. Results showed that the pre
sence of humic acids, dissolved or bound onto mineral surfaces, considerabl
y influenced the fixation of heavy metals. The various effects, depending o
n mineral type, humic concentration and specific metal-ion, were observed i
n three-component system. Sorption of Cu2+-ions on all minerals studied rap
idly increased as the concentration of dissolved HA increased. The amount o
f pb(2+)-ions sorbed on sand slightly decreased, while on kaolin increased
between 15 and 20%. Sorption of Zn2+-ions on all minerals studied decreased
at pH 4. At pH 5.5 the sorption of Zn2+-ions onto calcite decreased, while
on kaolin and sand increased as a function of the humic acid concentration
giving the curve with maximum at c(HA) = 2.5 mmol C L-1. At pH 6.5 sorptio
n onto kaolin and sand increased. This effect occurs as a result of the con
ditional stability constant of Zn-HA complexes increasing at higher pH whic
h in rum promotes the chelation of Zn2+-ions to mineral-bound humic substan
ces. The enhanced sorption of metal ions from the aqueous phase in three-co
mponent systems is not only the result of mineral sorption of free metals b
ut also the result of chelation with HA sorbed on the mineral surface.