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.
2025
Sammendrag
Det er ikke registrert sammendrag
Sammendrag
Plants in raingardens are important for evapotranspiration and maintaining infiltration properties. Hydrological conditions, however, fluctuate between dry and saturated, strongly affecting plant performance and limiting plant selection in design. This study experimentally assessed whether fluctuating hydrology impacts growth, flowering, and root morphology in the drought-tolerant Knautia arvensis and the wet-tolerant Lythrum salicaria. The hydrological regimes included repeated cycles of dry and wet conditions: Drought regime with cycles of a drought period followed by a single watering; Flooding regime with cycles of 72-hour flooding and a 48-hour drained period; and a subsequent Drought+Flooding regime with cycles of 72-hour flooding followed by a drought period. Knautia reduced growth under flooding cycles, while Lythrum reduced growth and flowering under drought cycles. Repeated consecutive drought and flooding cycles negatively influenced the growth of both species in the same way, with flooding affecting Knautia and drought affecting Lythrum. Lythrum showed more plasticity than Knautia, allocating more biomass to roots during drought cycles. Flooding cycles reduced root length in Knautia, while the drought cycles and consecutive Drought+Flooding cycles increased root diameter and decreased root length in Lythrum. Both species had coarse roots (> 2 mm) to support infiltration through biopores. If we assume that raingardens have free drainage and only rarely flood, drought-tolerant traits are more important. However, wet-tolerant species can benefit the system, especially through higher water use. This research contributes to the ecological understanding of plant responses to fluctuating hydrology, enabling a better plant selection for effective raingardens.
Forfattere
Hans‐Peter Schmidt Samuel Abiven Annette Cowie Bruno Glaser Stephen Joseph Claudia Kammann Johannes Lehmann Jens Leifeld Genxing Pan Daniel Rasse Cornelia Rumpel Dominic Woolf Andrew R. Zimmerman Nikolas HagemannSammendrag
1. The application of biochar to soil is a highly durable nature‐based carbon dioxide removal (CDR) pathway. It provides certifiable climate‐change mitigation, with mean carbon residence times exceeding 1,000 years, and additional co‐benefits for soil health and fertility. 2. Biochar persistence in soil depends on both intrinsic material properties and environmental factors. Its longevity is determined not only by the polyaromatic structure of the biochar itself but also by soil mineralogy, biological activity, and climatic conditions. 3. Biochar aging involves both decomposition and stabilization processes. The complementary mechanisms of decomposition and stabilization include interactions of biochar with minerals and native organic matter, as well as aggregations with soil particles that maintain its long‐term persistence. 4. Biochars and inertinite‐ranked fossil coals cannot be equated. Inertinite has been protected from biotic and abiotic oxidation for millions of years through burial in sediments and inclusion in minerals under high pressure and temperature. Biochar produced today in modern pyrolysis facilities is a fundamentally different material. 5. No carbonaceous material is completely inert. Field and laboratory studies consistently show measurable, though small, mineralization across a wide range of biochar types. Declaring that soil‐applied biochar carbon persists at 100% over millennia is inconsistent with current scientific understanding. 6. Analytical proxies indicate relative, but not absolute, biochar persistence. 7. Policy definitions of biochar CDR should reflect climate‐relevant timescales. The degree of persistence should be estimated on the order of centuries rather than millennia, supported by registered material properties, traceable application data, conservative modeling, and continued long‐term field experiments for model validation.
Forfattere
Gerard Cornelissen Nathalie Briels Thomas D. Bucheli Nicolas Estoppey Andrea Gredelj Nikolas Hagemann Sylvain Lerch Simon Lotz Daniel Rasse Hans-Peter Schmidt Erlend Grenager Sørmo Hans Peter Heinrich ArpSammendrag
Det er ikke registrert sammendrag
Forfattere
Tibor Zsigmond Csilla Farkas Andor Bódi Zsófia Bakacsi Eszter Tóth Márton Dencső Ágota HorelSammendrag
The aim of the present study was to investigate stream turbidity and water chemical parameters under varying environmental conditions. We analyzed a three-year-long (2021-2023) daily and bi-weekly dataset collected at six points (P1-P6) along a small stream. We measured stream water turbidity (FNU), total dissolved inorganic nitrogen (TDIN) content, water pH, and specific conductivity (SPC). Meteorological data were collected at the catchment outlet. Daily data showed a moderate positive correlation between FNU and precipitation (r=0.42, p <0.001), while weak negative connections were observed between SPC and FNU values (r=-0.14, p =0.011, n=349). The FNU values at the groundwater spring-fed sampling point (P3) were significantly different from the other sampling points on most parameters ( p <0.05). The results of the cluster analysis revealed three main clusters based on daily turbidity data. These groups of daily precipitation totals were i) below 4.8 mm, ii) averaging 6.3 mm, and iii) averaging 23.7 mm. The clusters were most significantly separated along precipitation and FNU values. Turbidity values were strongly correlated with precipitation events for two days, after which stream water quality returned to baseline. Stream water quality was not significantly influenced by soil management or antecedent moisture content but rather by water origin (i.e., precipitation, groundwater).
Sammendrag
Public conversation at the library in Kirkenes, Pasvik.
Forfattere
Lillian ØygardenSammendrag
Presentasjon ved lansering av FAO : International network on soil erosion INSER
Forfattere
Lillian ØygardenSammendrag
Det er ikke registrert sammendrag
Forfattere
Lillian ØygardenSammendrag
Presentasjon på SEVU ( Senter for videre og etterutdanning) kurs; Innføringskurs i klimagasser fra landbruket.
Forfattere
Lillian ØygardenSammendrag
Foredrag på Teknologidagen 2025, Apelsvoll.