COS 17-6 - Nitrogen fertilization differentiates carbon and nitrogen sequestrations in terrestrial ecosystem: A meta-analysis

Tuesday, August 5, 2008: 9:50 AM
102 E, Midwest Airlines Center
Meng Lu, Smithsonian Environmental Research Center, Edgewater, MD, Yiqi Luo, Department of Microbiology and Plant Biology, University of Oklahoma, Norman, OK and Bo Li, Ministry of Education Key Lab for Biodiversity Science and Ecological Engineering, The Institute of Biodiversity Science, Fudan University, Shanghai, China
Background/Question/Methods Nitrogen (N), a key element in biological systems, is one of the most important factors to carbon (C) and N processes in terrestrial ecosystem. N limitation theory indicates that N is a limited factor for plant. However, how the N fertilization influences terrestrial ecosystem C storage is still uncertain. In this study, we extracted data from 151 independently published papers that study the effects of long-term manipulative N fertilization on terrestrial ecosystem C and N sequestrations. The database contains C and N pools of plant and soil, microbial biomass C and N, soil available N, and C:N ratios of plant, soil and microbe.Results/Conclusions Overall, our results show that N fertilization has different effects on plant, soil and microbe. Compared to the control group, averaged C and N pool sizes of plant (including aboveground plant and belowground plant) significantly increase in N fertilization group, ranging from a 24% increase in aboveground C pool to a 67% increase in aboveground N pool. The C and N contents in litter pools are consistently higher in N fertilization group than control group. N fertilization does not change the soil C pool but significantly increases the soil N pool and soil available N, ranging from a 11% increase in soil N pool to a 110% increase in soil available N. The microbial biomass C and N decrease by 12% and 6% respectively. Averaged C:N ratios of plant, soil, litter and microbe all significantly decrease. Different ecosystems (Cropland, Forest, Grassland, Wetland, Tundra etc.) and soil properties of different soil depths (0-15cm, 15-30cm and 30-55cm) have variant responses to long-term N fertilization. Our results also show that the effect of N fertilization on soil C pool is not influenced by latitude variation, N fertilizer rate or experiment duration. To some degree, even the N fertilization does not change the soil C pool, the net C accumulation in plant caused by N fertilization could help to sequestrate C in terrestrial ecosystem and prevent the rising of atmospheric CO2.
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