The role of agroecological systems in cation interaction and aggregate formation in drylands of northeastern Brazil

Agroecological production systems are used in dryland agroecosystems. Therefore, it is necessary to verify their contributions, especially with regard to the functionality of soil attributes. From this perspective, this study aimed to evaluate the influence of soil use and management on the structural, hydraulic, and chemical attributes of a Haplic Cambisol in the Apodi Plateau, RN, Brazil. The experimental design adopted was completely randomized, with treatments distributed in a 5×3 factorial arrangement corresponding to five sampling locations (fruit farming, horticulture, agroecological, intercropping of Zea mays and Vigna unguiculata (L.) Walp), and three soil layers (0.00-0.10, 0.10-0.20, and 0.20-0.30 m), in addition to the correlation matrix and principal component analysis as multivariate statistical techniques. The parameters evaluated included soil pH, nutrient levels (available P, K+, Ca2+, and Mg2+), total organic carbon, soil density, total porosity, field capacity, permanent wilting point, available water, aggregation, aggregate stability, weighted mean diameter of aggregates, and the content of organic matter, Ca2+, and Mg2+ in different soil aggregate classes. The study concluded that continuous soil use practices such as intercropping Z. mays and V. unguiculata and horticulture significantly reduce nutrient availability, organic carbon content, moisture, and soil aggregation. However, areas under agroecological management and fruit cultivation, which involve minimal soil disturbance, promote the improvement of these properties.