THE RELATIONSHIP BETWEEN STRUCTURAL STABILITY AND CHEMICAL CRITERIA OF SOME SOLONETZIC SOILS OF NORTHWESTERN ALBERTA
The Solonetzic soils of this study included three profiles at each of two widely separated sites that had a range in morphological characteristics from Solonetz to Solod soils. The soils had developed under similar conditions and were as identical between sites as could be determined by field methods.Clay mineral properties, particle size distribution, and total chemical composition of the soils revealed the uniformity of materials within and between sites.Differences in the soils, within and between sites, were disclosed by exchange analysis, soluble salt analysis, pH's and water stability of aggregates.The results of this study indicate that pH as well as Al3+ and exchange acidity content play a role in determining aggregate stability in these soils. Some hypotheses of the formation of stable structure in the B horizons of these soils are discussed in the light of the evidence presented.