Long-term Nitrogen Addition Decreases Organic Matter Decomposition and Increases Forest Soil Carbon

Eastern North American forests receive anthropogenically elevated nitrogen (N) deposition that alters soil processes and forest productivity. We examined N deposition effects on soil carbon (C) and N in temperate, N-rich forest plots fertilized annually (100 kg N ha(-1) y(-1)) since 1993. After nearly two decades, soil C in O, A, and upper 50 cm of B horizons of N-addition plots was 17% greater (14.2 +/- 0.7 kg C m(-2)) than control plots. Aboveground tree biomass growth and litterfall were not affected by fertilization. Fine root mass (0-1 mm) was 34% greater in N-addition plots, but did not explain soil C increases. Rather, reduced decomposition of litter and soil organic matter drove C increases in N-addition plots. Decomposition rates of black cherry, sugar maple, and mixed leaf litter were 43, 67, and 36%, greater, respectively, in control than N-addition plots. Light fraction organic matter was greater in N-addition plots than in control plots, due to either enhanced root production or decreased decomposition of soil organic matter. Soil respiration was reduced, and microbial biomass in O, A, and upper-B horizons was lower in N-addition plots than controls. The soil microbial community composition was also altered dramatically with N additions. Recalcitrant organic matter enzyme activity (peroxidase) was reduced in the O-horizon by N addition. Available Ca, Mg, and K were reduced in O and A horizons by N fertilization. These results suggest that chronic elevated atmospheric N inputs can increase forest soil C storage by decreasing decomposition, however the long-term stability of this additional C sequestration is unknown.