Calorimetric and static techniques were employed to study the interaction of FeCl3 with sodium montmorillonite in dilute aqueous suspension. The results show that the amount adsorbed and the adsorption enthalpy are strong functions of the pH and temperature. The adsorption mechanism was discussed on the basis of the experimental data.
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References
1.
AdamsJ.M., DyerS., MartinK., MatearW.A. and McCabeR.W. (1994) J. Chem. Soc., Perkin Trans. 1761.
2.
EwinG.J., ErnoB.P. and HeplerL.G. (1981) Can. J. Chem. 59, 2927.
3.
HerrerraR. and PeechM. (1970) Soil Sci. Soc. Am., Proc. 34, 740.
4.
JamesR.O. and HealyT.H. (1972) J. Colloid Interface Sci. 40, 65.
5.
LaszloP., LucchettiJ. and de LiegeU. (1984) Tetrahedron Lett. 25, 2147.
6.
MurphyP.J., PosnerA.M. and QuirkJ.P. (1975) Aust. J. Soil Res. 13, 189.
7.
RaglandJ.L. (1962) Soil Sci. Soc. Am., Proc. 26, 133.
8.
RengasamyP. and OadesJ.M. (1977) Aust. J. Soil Res. 15, 221.
9.
RothC.B., JacksonM.L. and SyersJ.K. (1969) Clays Clay Miner. 17, 253.
10.
WhittigL.D. and PageA.L. (1961) Soil Sci. Soc. Am., Proc. 25, 278.
11.
YarivS. and CrossH. (1979) Geochemistry of Colloid Systems for Earth Scientists Springer-Verlag, New York.
12.
YuanG. and LavkulichL.M. (1994) Soil Sci. Soc. Am., J. 58, 343.