2000/07/01 by Michael Sommer, Dietrich Halm, Ulrich Weller +2 · 1 citation
Materials Science · Engineering · Agricultural and Biological Sciences · #Clay minerals and soil interactions #Soil and Unsaturated Flow #Soil Carbon and Nitrogen Dynamics
paper · pdf · doi:10.2136/sssaj2000.6441434x
openalex publication_date 2000/07/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/06/11
Analysis of soil pattern, especially the pattern of depletion and accumulation zones, is a powerful tool to decipher pedogenic processes at the landscape scale. To clarify the pedogenesis of a distinct pattern of podzolized soils in the cool, perhumid Black Forest (Germany) we performed a study in the forested upper part of a granitic catchment (B a ¨ rhalde). From detailed soil mapping we selected a typical catena of four pedons, which were analyzed for physical (bulk densities and particle‐size distribution), chemical (pH, organic C, pyrophosphate, oxalate, dithionite, and total Al, Mn, Fe), and mineralogical (clay minerals) properties. Standard mass balance calculations were modified to include a two‐component system with regard to parent material. Results showed a shift from two‐mica granite to granite–porphyry downslope. Soil pattern revealed podzolized soils with thick E horizons and thin spodic horizons developed in the upslope areas, whereas in downslope soils the reverse was found (thick spodic B and thin E horizons). Soil chemical and mineralogical properties were linked to soil morphology in that contents of organic C, pedogenic oxides, hydroxy‐interlayered vermiculites (HIV), and pH increased from eluvial to illuvial horizons as well as from up‐ to downslope soils. Mass balances of Fe and Al showed negative fluxes in upslope soils and positive fluxes in downslope soils during pedogenesis. We concluded from these results that a catenary eluvial–illuvial sequence (lateral podzolization) develops as a result of upslope mobilization followed by a (partially) lateral transport and subsequent immobilization in downslope zones, probably because the base‐richer parent material built up a geochemical barrier.