Isothermal ternary diffusion coefficients for the system lysozyme chloride (1)+NH 4Cl (2)+H 2O at 25°C and pH 4.5 have been measured interferometrically for five mean NH 4Cl concentrations, C 2=0.25, 0.5, 0.9, 1.2 and 1.5 M, with C 1=0.6 mM. The main-term diffusion coefficient ( D 11) v varies slowly with C 2. The main-term ( D 22) v increases with increasing NH 4Cl concentration, as does the binary D v in aqueous NH 4Cl, but the ( D 22) v values are lower in the ternary system. The cross-term ( D 21) v, which relates the coupled flow of NH 4Cl to the protein concentration gradient, increases sharply with increasing salt concentration, and is 19 times larger than ( D 22) v at the highest concentration. The values of ( D 12) v are smaller than the corresponding values previously obtained for the lysozyme chloride+NaCl+H 2O system over the whole range of salt concentration studied. Using equations based on the Onsager Reciprocal Relations, we have calculated the derivative of the chemical potential of lysozyme chloride with respect to the NH 4Cl concentration, and have estimated the protein cation charge. Integration with respect to the NH 4Cl concentration gives the dependence of the chemical potential of lysozyme chloride on NH 4Cl concentration, providing information about the driving force for nucleation and crystal growth of lysozyme chloride.