Elevated levels of heavy metals in soils are a result of industrial activit
ies, atmospheric deposition, and the land application of sewage sludges and
industrial by-products. Their persistence in the soil environment has crea
ted interest in the possible changes in solubility. In this study, total di
ssolved concentrations of Pb, Zn, and Cu were monitored in seven metal-amen
ded soils (a calcareous and six acid mineral soils). Single metal solutions
were added to soils and equilibrated (aged) for 40 days. During the 40 day
s the soil was allowed to air-dry and was rewetted in cycles of about 5 day
s. At the end of this reaction period, metal solubility was measured (by at
omic absorption spectrometry and direct current plasma spectrometry) at the
initial soil pH and at decreased pH values which were induced by addition
of small aliquots of acid. As expected, solubility of added Pb, Zn, and Cu
increased with a decrease in pH. Furthermore, the results showed that the s
olubility relationship with pH was similar in all non-calcareous soils. Thi
s suggests that metal solubility may be controlled by similar soil componen
ts, presumably involving soil characteristics such as pH, organic matter co
ntent, and soil mineralogy. For each metal, an approximate pH value was fou
nd at which solubility deviated from the solubility of metals when they occ
ur in soils at typical (natural) values. This pH was about (pH +/- 0.2): 5.
2 for Pb, 6.2 for Zn, and 5.5 for Cu. Thus, pH values below these threshold
s may enhance metal mobility, biological availability and toxicity in soils
. Metals dissolved at higher pH in the calcareous soil (18.8 g kg(-1) inorg
anic carbon, initial pH 8.2). In a calcareous soil, a significant fraction
of these metals react with carbonates, and decreased pH results in much hig
her metal dissolution. Yet, metal solubility in soils is not determined by
the formation and dissolution of single metal compounds. (C) 1999 Elsevier
Science Ltd. All rights reserved.