We have used in situ dialysis to measure the solubility of CdS(s) in sulfid
ic solutions. The solubility product for the reaction CdS(s) + H+ reversibl
e arrow r Cd2+ + HS- at 25 degrees C and 1 atm was found to be 10(-14.82+/-
0.03) for a crystalline product and to be 10(-14.15+/-0.06) and 10(-14.40+/
-0.06) for two precipitates, respectively. We show that the solubility of t
hese three solids at various pH values (4.2- 8.6) and sulfide concentration
s (10(-4.3)-10(-1.3) M) can be reproduced adequately by the following four
bisulfide complexes: CdHS+, Cd(HS)(2) Cd(HS)(3)(-), and Cd(HS)(4)(2-); the
log K-n Values for the general equation Cd2+ + nHS(-) reversible arrow Cd(H
S)(n)(2-n) are 7.38 +/- 0.68, 14.43 +/- 0.01, 1.6.26 +/- 0.58, and 18.43 +/
- 0.05, respectively. The species CdOHS-, which has been reported previousl
y, does not explain our experimental results. Calculations using estimated
concentrations of organic ligands (humic substances and organic thiols) kno
wn to be present in natural waters indicate that sulfide complexes largely
dominate Cd speciation in natural waters at Sigma S(-11) greater than or eq
ual to 10(-6) M.