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In situ net nitrogen mineralization response to regional and interannual variation in precipitation across the Central Great Plains of North America. McCulley, Rebecca1, Burke, Ingrid1, Lauenroth, William1, Knapp, Alan2, 1 2 ABSTRACT- Regional analyses and biogeochemical models predict that ecosystem nitrogen (N) pools and N cycling rates increase from the semi-arid shortgrass steppe to the sub-humid tallgrass prairie of the Central Great Plains, yet few field data exist to evaluate these predictions. We hypothesized that in situ net N mineralization would increase with increasing N pool sizes across this grassland community gradient and track interannual and regional differences in precipitation and temperature. We measured in situ net N mineralization monthly during two growing seasons at five sites across a precipitation gradient in the Great Plains region. Growing season precipitation varied more than two-fold across the gradient and by >25% at each site between years. Respectively, soil N pools and the N content of aboveground net primary production (ANPP-N) increased significantly from the shortgrass steppe (208 and 1.76 g N m -2) to the tallgrass prairie (409 and 3.27 g N m -2), and ANPP-N at the shortgrass steppe sites tracked the differences in interannual precipitation (0.88 g N m -2 in a dry year to 2.12 g N m -2 in a wet year). However, measured in situ net N mineralization rates did not increase across the community gradient or reflect regional and/or interannual differences in precipitation and temperature. These data suggest that current methods of measuring in situ net N mineralization may not be effective for soils with large immobilization potentials. KEY WORDS: in situ net nitrogen mineralization, nitrogen pools, precipitation gradient, grasslands |