Element budgets of pine stands on lignite and pyrite containing mine soils

摘要

To analyze the development of pine ecosystems on lignite and pyrite containing mine soils, four pine stands with ages of 3-35 years were investigated in a chronosequence approach, Bulk precipitation, throughfall and soil solution in depths of 20, 40, 70 and 100 cm were studied over a three-year period to determine element fluxes in these forest ecosystems on extreme acidic and saline soils. Element budgets are controlled by the processes induced by pyrite oxidation such as intensive weathering of primary minerals, precipitation and leaching of secondary phases. Despite low water fluxes, element outputs can reach extraordinary high values due to very high concentration in the soil solution. Although element outputs decrease drastically with stand age, respectively, site age, they exceed those of comparable pine stands on non-mine sites. Nitrogen release from the lignite fraction represents a special characteristic of the examined substrates. Nitrogen losses beneath the rooted zone can be 34 kg N ha~(-1) yr~(-1) in 100 cm depth. Element input and output in the examined ecosytems are far from balance. Closed cuycling of nutrients seems to be recognizable in the case of potassium.