The rate of progression and stability of progressive nitrogen limitation at elevated atmospheric CO2 in a grazed grassland over 11 years of Free Air CO2 enrichment
| Autor: | Phil Theobald, Paul C. D. Newton, W. M. Saman D. Bowatte, Shona C. Brock, Des J. Ross, Mark Lieffering, Chris L. Hunt |
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| Rok vydání: | 2010 |
| Předmět: |
geography
geography.geographical_feature_category food and beverages Soil Science chemistry.chemical_element Plant physiology Plant Science Nitrogen Pasture Grassland Mesocosm chemistry.chemical_compound Animal science chemistry Carbon dioxide Botany Environmental science Ecosystem Terrestrial ecosystem |
| Zdroj: | Plant and Soil. 336:433-441 |
| ISSN: | 1573-5036 0032-079X |
| DOI: | 10.1007/s11104-010-0493-0 |
| Popis: | A decline in the availability of nitrogen (N) for plant growth (progressive nitrogen limitation or PNL) is a feedback that could constrain terrestrial ecosystem responses to elevated atmospheric CO2. Several long-term CO2 enrichment experiments have measured changes in plant and soil pools and fluxes consistent with PNL but evidence for PNL in grasslands is limited. In an 11 year Free Air CO2 Enrichment (FACE) experiment on grazed grassland we found the amount of N harvested in aboveground plant biomass was greater at elevated CO2 but declined over time to be indistinguishable from ambient after 5 years. Re-wetting after a major drought resulted in a large input of N from mineralisation and a return to a higher N harvested under elevated CO2 followed by a further decline. Over these two periods the amount of N in soil significantly increased at elevated CO2. Data from mesocosms introduced into the rings at intervals, and therefore having different lengths of exposure to CO2, showed plant N availability declined at elevated CO2 reaching a new equilibrium after 6 years of exposure. We conclude that the availability of N for plants in this grassland is dynamic but the underlying trend at elevated CO2 is for PNL. |
| Databáze: | OpenAIRE |
| Externí odkaz: |
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