Changes in the Ratio of Aggregate Fractions in Humus Horizons of Сhernozemsin Response to the Type of Their Use
Data on the aggregate-size distribution (dry sifting method) in humus horizons of chernozems were processed by the principal components analysis (PCA) with the centered logratio transformation of the initial data set. The analysis of the position of particular trials in the space of principal components coupled with the analysis of eigenvector magnitudes made it possible to identify several size fractions of aggregates, whose contents in the soils reflects soil degradation or progradation processes. These groups fitted well to the partial lognormal curves of aggregate sizes. In addition, the distribution of water-stable aggregates in coarse aggregate fractions (>10, 10–7, 7–5, and 5–3 mm) was analyzed. The integral analysis of the obtained data made it possible to propose the following conceptual model of the recovery of the structure of plowed Chernozems. In the course of tillage, soil particles <0.25 mm in size are formed due to comminution. These particles are unstable and may stick together to shape large (>10 mm) water-unstable aggregates (clods). With the removal of tillage loads, large aggregates interact with fresh organic matter, and the water stability of aggregates increases. At the same time, the largest aggregates (mainly >10 mm) tend to transform into aggregates of smaller sizes.