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Four forested, well drained surface horizons of soils representing the range of textures located in the Lake Erie Basin of Southern Ontario were sampled in 1 cm increments to a depth of 15 cm. Gamma emitting radionuclides of natural sources, super(40)K, super(214)Bi ( super(238)U daughter), and super(208)Tl ( super(232)Th daughter), are distributed as a function of texture over the 15 cm depth. Increasing clay content results in increased retention of these isotopes. The super(40)K distribution is a result of the amount of organic carbon present. Increased organic carbon results in increased weathering and lower super(40)K values. Differing earthworm activity results in distinct distributions of super(137)Cs, a gamma emitting radionuclide from bomb fallout, within the four soils. Larger numbers and biomass of anecic earthworms in finer textured soils result in a linear distribution of super(137)Cs with depth. Endogeous species in the coarsest textured soil result in little incorporation of super(137)Cs with depth.