THE RELATIONSHIP OF WATER-SOLUBLE CATIONS TO FIELD SEPARATIONS OF CHERNOZEMIC AND SOLONETZIC SOILS
It is suggested that cations present in extracts of water-saturated soil samples can be used to complement and substantiate the field classification of soils into the Solonetzic and Chernozemic Orders by the Canadian system, and that an evaluation of these cations together with pH can be used as substantiating criteria at the sub-group level.Two hundred and ninety-one profiles, sampled by the Saskatchewan Soil Survey during the 1959–61 seasons, have been separated into high, medium and low sodium profiles and on this basis correlated with the field classification. Most of the high sodium soils were in the Solonetzic Order, and the medium and low sodium in the Chernozemic Order.The proposed laboratory criteria gave over 80 per cent agreement with the field classification at the order level. This percentage was obtained from a range of 97 per cent for the Orthic Chernozem to 63 per cent for the Solonetz profile. The agreement at the lower level varied from 95 per cent for the Rego Chernozem to 38 for the Solonetz.