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Lateral Podzolization in a Granite Landscape

^a Inst. für Biomathematik und Biometrie, GSF-Forschungszentrum für Umwelt and Gesundheit, Ingolstädter Landstr. 1, 85764 Neuherberg, Germany
^b Inst. für Bodenk. und Standortslehre, Univ. Hohenheim, Emil-Wolfe Str. 27, 70593 Stuttgart, Germany

View larger version (14K): [in a new window]   Fig. 1 (a) Topographic position of the selected pedons and landscape segments and (b) illuvial/eluvial ratio of podzolization (IERpodzol). Boxplots with 5, 25, 50, 75, 95 percentiles and mean values (filled square); numbers in brackets = numbers of augering points in the landscape segments

View larger version (21K): [in a new window]   Fig. 2 X-ray diffraction patterns of the clay fraction (<2 mm) in three typical horizons: (a) E1 in G=1, (b) Bsh in G=4, and (c) 2 Cr in G=4

View larger version (36K): [in a new window]   Fig. 3 Results of mass balance calculations plotted as relative gains and losses of Fe, Al, and Mn (in percentage of initial mass)

View larger version (24K): [in a new window]   Fig. 4 The concepts of vertical (left) and lateral podzolization (right)