TY - JOUR
T1 - Cadmium and nickel distribution coefficients for sandy aquifer materials
AU - Christensen, T.H.
AU - Lehmann, N.
AU - Jackson, T.
AU - Holm, P.E.
PY - 1996
Y1 - 1996
N2 - Distribution coefficients (K(d)) were measured for cadmium (Cd) and nickel (Ni) in laboratory batch experiments for 18 sandy aquifer materials at environmentally relevant solute concentrations (Cd: 0.1-15 μg/l; Ni: 4-200 μg/l). The K(d)-values ranged three orders of magnitude: Cd: 2-1770 l/kg and Ni: 3-7250 l/kg. Correlating observed K(d)-values to characteristics of the aquifer materials (particle size fractions, organic-C content, surface area, pH) revealed very good correlation with pH in the pH range 4.9 to 8.9 (Cd: r2 = 0.942; Ni: r2 = 0.929). Including any other of the measured aquifer material characteristics did not improve the correlation significantly. The results indicate that at the same pH-values, the K(d)-values for aquifer materials are 4-10 times lower than K(d)-values for soils reported in the literature. However, the mobility of Cd and Ni, as reflected in the K(d)-values, is still very limited in sandy aquifers, unless the pH is very low. The results indicate that at pH 6 the relative mobility of both Cd and Ni is of the order of 1%.
AB - Distribution coefficients (K(d)) were measured for cadmium (Cd) and nickel (Ni) in laboratory batch experiments for 18 sandy aquifer materials at environmentally relevant solute concentrations (Cd: 0.1-15 μg/l; Ni: 4-200 μg/l). The K(d)-values ranged three orders of magnitude: Cd: 2-1770 l/kg and Ni: 3-7250 l/kg. Correlating observed K(d)-values to characteristics of the aquifer materials (particle size fractions, organic-C content, surface area, pH) revealed very good correlation with pH in the pH range 4.9 to 8.9 (Cd: r2 = 0.942; Ni: r2 = 0.929). Including any other of the measured aquifer material characteristics did not improve the correlation significantly. The results indicate that at the same pH-values, the K(d)-values for aquifer materials are 4-10 times lower than K(d)-values for soils reported in the literature. However, the mobility of Cd and Ni, as reflected in the K(d)-values, is still very limited in sandy aquifers, unless the pH is very low. The results indicate that at pH 6 the relative mobility of both Cd and Ni is of the order of 1%.
U2 - 10.1016/0169-7722(96)00012-5
DO - 10.1016/0169-7722(96)00012-5
M3 - Journal article
SN - 0169-7722
VL - 24
SP - 75
EP - 84
JO - Journal of Contaminant Hydrology
JF - Journal of Contaminant Hydrology
IS - 1
ER -