Publikasjoner
NIBIOs ansatte publiserer flere hundre vitenskapelige artikler og forskningsrapporter hvert år. Her finner du referanser og lenker til publikasjoner og andre forsknings- og formidlingsaktiviteter. Samlingen oppdateres løpende med både nytt og historisk materiale. For mer informasjon om NIBIOs publikasjoner, besøk NIBIOs bibliotek.
2024
Sammendrag
Denne rapporten gir en oversikt over klimatiltak i planteproduksjoner som enten kan redusere utslipp av klimagasser eller øke karboninnholdet i jord. Den gir oversikt over tiltak som bla. drenering, gjødsling, kalking, husdyrgjødseltiltak, åkerbelgvekster, kløver i eng, presisjonsjordbruk, fangvekster, biokull. I prosjektet- finansiert fra Forskningmidler for jordbruk og matindustri- er det også utarbeidet en delrapport om klimatiltak i husdyrproduksjonen (Aass mfl., 2024) og en delrapport om sammenheng ellom klimatiltak, klimatilpasning, klimarisiko og matsikkerhet (Bardalen, 2024). De utgjør til sammen et oppdatert kunnskapsgrunnlag om klimatiltak i plante og husdyrproduksjoner. Se utvidet sammendrag i rapporten.
Sammendrag
Effekten av skogbruk på eutrofibelastningen i Oslofjorden er anslått basert på tilførsler av løst uorganisk nitrogen (DIN). Dette anslaget er beheftet med en rekke usikkerheter som kan forbedres ved å bl.a. samle inn flere data om effekten av skogsdrift på vann, samt forbedre anslag over årlig hogstareal. Våre anslag antyder at tap av nitrogen fra skogsdrift til Oslofjorden ligger på nivå med tapet fra spredt avløp og bebyggelse. På side 6 finnes et utvidet sammendrag. The effect of forestry on the eutrophic pressure of the Oslo Fjord has been estimated based on fluxes of DIN (dissolved inorganic nitrogen). This estimate is subject to many uncertainties that can be improved by, among other things, collecting more data on the effect of forestry on water, as well as improving estimates of annual logging area. Our estimate suggests that losses of nitrogen to the Oslo Fjord from forestry are in the same range as losses from households not connected to sewage treatment plants and from settlements.
Sammendrag
Black soils, which play an important role in agricultural production and food security, are well known for their relatively high content of soil organic matter (SOM). SOM has a significant impact on the sustainability of farmland and provides nutrients for plants. Hyperspectral imaging (HSI) in the visible and near-infrared region has shown the potential to detect soil nutrient levels in the laboratory. However, using portable spectrometers directly in the field remains challenging due to variations in soil moisture (SM). The current study used spectral data captured by a handheld spectrometer outdoors to predict SOM, available nitrogen (AN), available phosphorus (AP) and available potassium (AK) with different SM levels. Partial least squares regression (PLSR) models were established to compare the predictive performance of air-dried soil samples with SMs around 20%, 30% and 40%. The results showed that the model established using dry sample data had the best performance (RMSE = 4.47 g/kg) for the prediction of SOM, followed by AN (RMSE = 20.92 mg/kg) and AK (RMSE = 22.67 mg/kg). The AP was better predicted by the model based on 30% SM (RMSE = 8.04 mg/kg). In general, model performance deteriorated with an increase in SM, except for the case of AP. Feature wavelengths for predicting four kinds of soil properties were recommended based on variable importance in the projection (VIP), which offered useful guidance for the development of portable hyperspectral sensors based on discrete wavebands to reduce cost and save time for on-site data collection.
Forfattere
Teresa Gómez de la Bárcena Dorothee Kolberg Nora Hua Ly Kok Roar Lågbu Siri Svendgård-Stokke Geir-Harald Strand Anne B. Nilsen Shivesh Karan Anders Aas Marit Almvik Robert Barneveld Claire Coutris Erik J. Joner Till SeehusenSammendrag
Denne rapporten beskriver alle prosesser som er utarbeidet innenfor datafangst, dataforvaltning, bearbeiding og analyse samt formidling i implementeringsfasen av et nytt jordovervåkingsprogram for jordbruksjord i Norge. Rapporten inneholder detaljerte planer for hvordan jordinformasjon fra ulike indikatorer skal innhentes, analyseres og bearbeides slik at tilstand og endring i jordsmonnet kan overvåkes. Programmet vil danne grunnlaget for landsdekkende jordinformasjon som muliggjør en vurdering av jordsmonnets status og endring for de fem truslene man har identifisert for norsk jordbruksjord: erosjon, jordpakking, tap av organisk materiale, tap av jordbiodiversitet og forurensning.
Sammendrag
Biochar is a recalcitrant carbon-rich solid produced by pyrolysis of organic residues, and its application to soil is considered a promising approach to mitigate climate change, as biochar resists decomposition to readily contributes to soil carbon (C) sequestration. The IPCC provides a basis for future national-scale accounting of the changes in soil C stocks following biochar application to cropland soils. The IPCC Tier 1 approach for biochar is based on fixed emission factors to estimate biochar C sequestration. In contrast, the Tier 2 approach allows countries to use local emission factors and climate data to calculate the contribution of biochar to soil C sequestration. Accurate accounting of biochar C sequestration is essential for ensuring the credibility of C offsetting projects, as well as providing incentives for implementing biochar in C credit schemes, calling for comparative analyses of the different biochar Tier approaches. Here we retrieved biochar samples from local producers and measured their H/Corg to estimate the persistence of biochar in Norwegian croplands post application. Various feedstocks were considered, including forest residues, woody wastes, manure, sludge, and straw. For all biochar samples, the 100-year stable C fraction was calculated at ≥ 0.945, thus exceeding the default Tier 1 value (0.8). Biochar sourced from woody- and forestry residues had a Corg content above the default Tier 1 value (0.77). Based on this and data about national feedstock supplies, we compared the theoretical potential of biochar soil C sequestration to mitigate climate change in Norway, using the IPCC Tier 1 and Tier 2 approaches. Biochar C sequestration in soil was calculated at 0.79 Tg CO2-eq yr−1 and 0.92 to 0.96 Tg CO2-eq yr−1, respectively for the Tier 1 and Tier 2 approaches, thus, underlining that the choice of IPCC Tier approach can have a large impact on the estimated mitigation potential of biochar.
Forfattere
Marte Ragnhild Owren Ingvild Byskov Britta Maria Hoem Julien Jabot Hans H. Kolshus Kathrine Loe Bjønness Jakob Sandven Trude Melby Bothner Mona Irene Andersen Engedal Eirik Knutsen Lene Skyrudsmoen Berit Storbråten Kristina Vikesund Hart Evan Christian Wilhelm Mohr Gry Alfredsen Ana Aza Johannes Breidenbach Lise Dalsgaard Rune Eriksen Katharina Hobrak Christophe Moni Gunnhild SøgaardRedaktører
Ingeborg RønningSammendrag
Det er ikke registrert sammendrag
Sammendrag
Det er ikke registrert sammendrag
2023
Forfattere
Junbin Zhao Simon Weldon Alexandra Barthelmes Erin Swails Kristell Hergoualc’h Ülo Mander Chunjing Qiu John Connolly Whendee L. Silver David CampbellSammendrag
Greenhouse gas (GHGs) emissions from peatlands contribute significantly to ongoing climate change because of human land use. To develop reliable and comprehensive estimates and predictions of GHG emissions from peatlands, it is necessary to have GHG observations, including carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O), that cover different peatland types globally. We synthesize published peatland studies with field GHG flux measurements to identify gaps in observations and suggest directions for future research. Although GHG flux measurements have been conducted at numerous sites globally, substantial gaps remain in current observations, encompassing various peatland types, regions and GHGs. Generally, there is a pressing need for additional GHG observations in Africa, Latin America and the Caribbean regions. Despite widespread measurements of CO2 and CH4, studies quantifying N2O emissions from peatlands are scarce, particularly in natural ecosystems. To expand the global coverage of peatland data, it is crucial to conduct more eddy covariance observations for long-term monitoring. Automated chambers are preferable for plot-scale observations to produce high temporal resolution data; however, traditional field campaigns with manual chamber measurements remain necessary, particularly in remote areas. To ensure that the data can be further used for modeling purposes, we suggest that chamber campaigns should be conducted at least monthly for a minimum duration of one year with no fewer than three replicates and measure key environmental variables. In addition, further studies are needed in restored peatlands, focusing on identifying the most effective restoration approaches for different ecosystem types, conditions, climates, and land use histories.
Sammendrag
Det er ikke registrert sammendrag
Forfattere
Liang Wang Alba Dieguez-Alonso Maria Nicte Polanco Olsen Julie Cathrine Guldahl Øyvind Skreiberg Alice Budai Daniel RasseSammendrag
Det er ikke registrert sammendrag