Microbial responses to nitrogen additions in alpine tundra soil
1996
Fisk, M.C. | Schmidt, S.K.
Soil nitrogen transformations were measured the year following nitrogen fertilization of alpine Kobresia myosuroides meadows to determine the influence of greater plant production and N content on net N mineralization and the microbial N pool. Previously fertilized soils contained substantially greater amounts of organic N than control soils. The average increase in soil organic N accounted for 75% of total added N and, although variable, this quantity suggests a large capacity for retention of added N in these soils. Nitrogen transformations and more active pools also responded to fertilization. Net N mineralization, nitrification and soil inorganic N concentrations clearly were higher in fertilized than in control plots throughout the snow-free season. The most pronounced increase in mineralization in fertilized relative to control soils occurred during the second half of the snow-free period (mid-July-October), primarily after the short alpine growing season (June mid-August). Although the soil microbial N pool was not affected by fertilization during the growing season, microbial N did increase in the fall in fertilized compared to control soil, coinciding with the time of greatest N mineralization. The late season net uptake of N into the microbial pool exceeded by several times present rates of anthropogenic N inputs to these soils, and the microbial biomass may act as an increasingly important short-term sink for available N if N deposition to these areas continues to increase.
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