the major driver for the CEC in rocks and soil is the smectite content. With this in mind high smectite contents will also yield high CEC. This is a correlativ relationship it does not compensate for a precise determination of the CEC as shown in
Meier, L.P., Kahr, G., 1999. Determination of the cation exchange capacity (CEC) of clay
minerals using the complexes of Copper (II) ion with triethylenetetramine and
Thank you for your answer for my question, Yes exactly, semectite group characterize by high CEC, but in my country located in arid Environment and there is relative similarity in clay minerals distribution, and in my question I was wondering if we can put an equation for estimation CEC from Clay content and /or organic matter..
I would not go beyond that line which I drew in my answer. Using the smectite content as a direct correlation with the CEC would go a bit too far because of the complexity of the smectite-group minerals and the tendency to share mixed-layer structures, predominantly with illite. The organic part does not play such a role in arid climatic zones whereas the content of smectite- and hormite-group phyllosilicates may be rather high.
see:
DILL, H.G. (2017) Residual clay deposits on basement rocks: The impact of climate and the geological setting on supergene argillitization in the Bohemian
Massif (Central Europe) and across the globe.- Earth Sciences Reviews 165: 1-58.
DILL, H.G. (2016) Kaolin: soil, rock and ore From the mineral to the magmatic, sedimentary, and metamorphic environments.- Earth Sciences Reviews 161: 16-129