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Titel Influence of 13 different biochars on N2O production and its sources during rewetting-drying cycles
VerfasserIn Nicole Wrage-Mönnig, Sebastian Fiedler, Teresa Fuertes-Mendizábal, José-Maria Estavillo, Jim A. Ippolito, Nils Borchard, Maria Luz Cayuela, Kurt Spokas, Jeff Novak, Claudia Kammann
Konferenz EGU General Assembly 2017
Medientyp Artikel
Sprache en
Digitales Dokument PDF
Erschienen In: GRA - Volume 19 (2017)
Datensatznummer 250142021
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2017-5592.pdf
 
Zusammenfassung
Biochars have been found to have variable impacts on nitrous oxide (N2O) emissions. The variability has been attributed to differences in soil – biochar properties and microbial communities. While some information exists on biochar and soil properties, the effect of biochars on microbial sources of N2O is still a matter of speculation. In this study, we tested these effects for12 biochars prepared from cypress, loblolly pine and grape wood produced at four different controlled temperatures (350, 500, 700 and 900˚ C), respectively, plus a grapevine Kontiki biochar (600-700˚ C). The biochars were added (2%) to a loamy sand brought to pH 7.1 with CaO. The treatments plus one control were pre-incubated at 40% water holding capacity (WHC) for four days. Then, they were brought to 80% WHC and 15N-nitrate was added (50 mg NO3−-N kg−1 soil, 10% enriched in 15N). All treatments were set up with four replicates. In total, three cycles of (re)wetting – drying (80 to 40% WHC, total duration 20 days) were monitored. Samples for analyses of N2O concentrations and stable isotope signatures were taken daily (except for weekends) after closing the incubation vessels for 90 minutes. N2O emissions increased with each addition of water and decreased during drying to background values. Each rewetting led to larger emissions than measured in the previous cycle for all treatments including controls. All biochars decreased total N2O emissions compared to the control treatments. The higher the production temperature of the biochar, the larger usually the emission reduction. Largest effects were found for the grape wood and the Kontiki biochars. Interestingly, the addition of biochars also changed the isotopic signatures of the emitted N2O. Whereas emissions in the controls were enriched to about 5 atom% 15N excess at peak emissions, the enrichment was usually less after addition of biochars (1-5 atom% excess). Again, this effect tended to be larger at higher production temperatures of the biochars and was greatest for the grape wood and Kontiki biochars. The results indicate that NO3− was an important source for N2O emissions under the conditions of the study, probably by denitrification. The addition of biochars changed not only the amount of emissions, but also the N source of emissions. In this study, N2O production from labelled NO3− was a smaller source of emissions after addition of biochars (especially produced at high temperatures) than in control treatments. This indicates that the 15N-NO3− source was diluted by (accelerated) mineralization-nitrification or that microbial sources using other substrates but added NO3− contributed more to N2O production. Whether potential capture of NO3− by biochars could contribute to this, needs to be further investigated. Acknowledgements: This contribution was made possible by the ‘DesignChar4Food’ project (D4F) funded by the BLE and FACCE-JPI (German partners), by FACCE-CSA nº 276610/MIT04-DESIGN-UPVASC and IT-932-16 (Spanish partners), and the USDA-National Institute of Food and Agriculture (Project # 2014-35615-21971; US colleagues) plus USDA-ARS CHARnet and GRACENetprograms. CK gratefully acknowledges funding by DFG grant KA3442/1-1 and “OptiChar4EcoVin” (Hessian Ministry for Higher Education, Research and the Arts).