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Evaluation of the IPCC model for N mineralization: An overview on N2O emissions, N mineralization and C:N ratios from projects recently conducted at SLU and from other Swedish sites
Utförare miljöövervakning, Universitet, Sveriges lantbruksuniversitet, SLU.
Utförare miljöövervakning, Universitet, Sveriges lantbruksuniversitet, SLU.
Ansvarlig organisasjon
2017 (engelsk)Rapport (Annet vitenskapelig)
Abstract [en]

A smaller literature study and a data retrieval on N2O emissions, N mineralization and C:N ratios from projects recently conducted at SLU and from other Swedish sites have been performed to evaluate whether the current IPCC Tier 1 approach with a default emission factor of 1% (EF1) for N2O emissions from agricultural soils and other land use categories should be changed to a higher Tier with more specific EFs.

The study showed that the use of a default N2O EF of 1% of the N applied to soils would either under- or overestimate N2O emissions. It was also concluded that there is no relationship between total N input and N2O emissions, i.e. high fertilizer input must not be related to high N2O emissions and low fertilizer input can result in high N2O emissions. Even though N2O emissions from different Swedish land use categories were lower as the default EF1 in 8 of the 21 reported data sets, there is clear evidence to change from the IPCC Tier 1 approach for N2O emissions to more adjusted EFs related to a country-specific methodology. The strong relationship between C:N ratios and N2O emissions from drained forested histosols may be used to improve our ability to predict N2O emissions from other land use categories such as grassland and cropland.

sted, utgiver, år, opplag, sider
2017. , s. 19
Serie
SMED Rapport, ISSN 1653-8102 ; 2017:15
Emneord [en]
C:N ratio, emission factor, greenhouse gas, IPCC Tier 1, land use category, N mineralization, nitrous oxide, production areas
HSV kategori
Forskningsprogram
SMED (Svenska MiljöEmissionsData), Luft och klimat
Identifikatorer
URN: urn:nbn:se:naturvardsverket:diva-8918OAI: oai:DiVA.org:naturvardsverket-8918DiVA, id: diva2:1579519
Tilgjengelig fra: 2021-07-09 Laget: 2021-07-09 Sist oppdatert: 2023-11-22bibliografisk kontrollert

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