Determination of the cation exchange capacity of clays with copper complexes revisited
Determination of the cation exchange capacity of clays with copper complexes revisited
Clay Minerals (December 2005) 40 (4): 441-453
The determination of the cation exchange capacity (CEC) of clays by exchange with the cationic copper complexes [Cu(en) (sub 2) ] (super 2+) and [Cu(trien)] (super 2+) is revisited. The procedures reported by Bergaya & Vayer (1997) and Meier & Kahr (1999) are modified slightly. The concentration of the copper complexes in the equilibrium solutions is measured by spectral photometry. Correct CEC values of the [Cu(en) (sub 2) ] (super 2+) exchange are only obtained when a buffer ("tris", tris (hydroxymethyl) aminomethane, pH = 8) is added to the equilibrium solution after separation of the clay, because the molar extinction coefficient of this complex depends on the pH of the solution. A standard procedure is recommended as a reference method. In most cases, tris addition is not needed for the determination with [Cu(trien)] (super 2+) cations. Nevertheless, tris addition is recommended in the standard procedure. Determination of CEC for 40 samples (kaolins, "common clays", bentonites, montmorillonites and beidellite) shows a good agreement between measurements using [Cu(en) (sub 2) ] (super 2+) and [Cu(trien)] (super 2+) cations and with results by the ammonium acetate method.