Alluvial soil formation in the plains of northeastern Brazil

Abstract

Soils in alluvial plains of the lower course of the Acaraú River, Ceará State, Brazil, are weakly developed and have a complex distribution in the landscape. This study reports the pedogenic characterization of such soils in an effort to understand their formation. Soil pits were opened in four representative sites, profile morphology was described, and soil samples were collected for chemical, physical, mineralogical, and micromorphological analyses. All profiles had weak pedogenic development, as inferred from their morphological characteristics, lack of B horizon, and high silt/clay ratio. Organic carbon and particle size distributions were heterogeneous in Fluvisol, Planosol, and Solonchak, in agreement with their sedimentary nature. Intrinsic characteristics of each profile indicated variations in pedogenic processes related to depositional conditions, which, in turn, were determined by the alluvial nature of sediments and water table dynamics. Consequently, Fluvisols at higher elevations showed reduced pedogenic development. In adjacent areas, Planosols showed pores filled with clay minerals and a texture gradient, indicative of past lessivage. Vertisol was identified in small depressions and exhibited intense pedoturbation and high sodium concentration in deep layers. Solonchak had a high degree of hydromorphism, high sodium concentration, and high electrical conductivity. The distinct pedogenesis of alluvial plain soils in Northeastern Brazil is evidenced by their morphological, chemical, and physical properties.

Classification of alluvial soils - problematic issues on the examples from South Baltic Lakelands, north Poland

“…Leaching processes are also noticed in alluvial soils in many parts of the World (e.g. Cipriano-Silva et al, 2020;Suther and Leigh, 2020) and Poland (Terelak, 1967;Banaszuk, 1987). However, such processes were not recorded in the investigated soils.…”

“…The presence of alluvial material is expressed by using the fluvic qualifier on lower rank units (e.g. Cipriano-Silva et al, 2020;Kawałko et al, 2021). Fluvisols Reference Group was placed on the end of the classification key and refers to young alluvial soils weakly changed by pedogenesis only.…”