Abstract
Solution ionic composition strongly affects ion sorption onto solid surfaces. This study evaluated the effect of competing ions on heavymetal sorption by soil. Investigations were conducted on Ca‐saturated soil in 0.5 mmol L−1 CaCl2 solution. Sorption of Ni2+, Co2+, and Cu2+ in binary metal‐Ca and ternary Ni‐Co‐Ca or Ni‐Cu‐Ca systems were evaluated. Sorption occurred in the order Cu > Ni ≈ Co, with the soil exhibiting selectivity to Cu2+, but not to Ni2+ or Co2+. Nickel sorption was equivalent to Ca2+ release, but neither Co2+ nor Cu2+ sorption was accompanied by an equivalent Ca2+ release. In the ternary systems, neither Co2+ nor 0.016 mmol L−1 Cu2+ caused a significant decrease in Ni2+ sorption. At 0.079 mmol L−1, Cu2+ did cause an observable decrease in Ni2+ sorption. Copper sorption was not affected by Ni2+, but Co2+ sorption decreased in direct proportion to Ni2+ sorption. Apparently, Ni2+ was retained by an exchange mechanism, but Co2+ and Cu2+ sorption was more complex. Nickel competed with Co2+ for sorption sites to a greater extent than did Co2+ for Ni2+ sites. Copper was selectively sorbed from the Ca2+ solution, while Co2+ and Ni2+ were able to compete with Ca2+ only in very dilute solutions. Maintaining a near‐neutral soil pH may not always be the best strategy for minimizing heavy‐metal mobility. Some ions appear unable to compete with Ca2+ for sorption sites at ionic strengths representative of near‐neutral pH. Thus, while absolute solubility may be controlled, mobility in solution may be enhanced by increased ionic strength as the soil pH approaches neutrality.

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