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.
2007
Forfattere
Daniel RasseSammendrag
Dynamics of soil organic matter is an important factor of soil quality. A long-standing view is that recalcitrant molecules of plant residues contribute more to long-term storage of organic carbon than more soluble plant residues. This view is currently being questioned, and parts of our recent studies will be presented that support the need for reconsideration of the topic.
Forfattere
Marie Alexis Daniel Rasse C. Rumpel G. Bardoux N. Péchot P. Schmalzer B.G. Drake A. MariottiSammendrag
Fire profoundly modifies the terrestrial C cycle of about 40% of the Earth"s land surface. The immediate effect of fire is that of a net loss of C as CO2 gas and soot particles to the atmosphere. Nevertheless, a proportion of the ecosystem biomass is converted into charcoal, which contains highly recalcitrant molecular structures that contribute to long-term C storage. The present study aimed to assess simultaneously losses to the atmosphere and charcoal production rates of C and N compounds as a result of prescription fire in a Florida scrub-oak ecosystem. Pre-fire and post-fire charred and unburned organic matter stocks were determined for vegetation leaves and stems, litter and soil in 20 sub-plots installed in a 30-ha area that was subjected to prescribed fire. Concentrations of C and N were determined, and fluxes among pools and to the atmosphere were derived from these measurements. Soil C and N stocks were unchanged by the fire. Post-fire standing dead biomass contained 30% and 12% of pre-fire vegetation C and N stocks, respectively. In litter, post-fire stocks contained 64% and 83% of pre-fire C and N stocks, respectively. Most of the difference in relative losses between vegetation and litter could be attributed to substantial litter fall of charred and unburned leaves during the fire event. Indeed, an estimated 21% of pre-fire vegetation leaf C was found in the post-fire litter, while the remaining 79% was lost to the atmosphere. About 3/4 of the fire-induced leaf litter fall was in the form of unburned tissue and the remainder was charcoal, which amounted to 5% of pre-fire leaf C stocks. Charcoal production ranged between 4% and 6% of the fireaffected biomass, i.e. the sum of charcoal production and atmospheric losses. This value is below the range of literature values for the transformation of plant tissue into stable soil organic matter through humification processes, which suggests that fire generates a smaller quantity of stable organic C than humification processes over decades and potentially centuries.
Sammendrag
Ikke tilgjengelig
Forfattere
Marie-France Dignac Cornelia Rumpel Daniel Rasse Mercedes Mendez-Millan Haithem Bahri André MariottiSammendrag
Little is known on the relationship between the chemical composition and the dynamics of plant biomolecules in soils at the long-term scale. Chemical recalcitrance of specific molecules such as lignins has been proposed as a possible factor governing organic matter stabilization in soils. Other stabilization mechanisms, involving soil mineral constituents, may act differently on above- and belowground tissues of plants, leading to contrasting contributions of these tissues to soil organic matter (SOM). Cutins and suberins are present respectively in the aboveground and the belowground tissues of higher plants and can be used as biomarkers of the inputs of these plant tissues to soils. Using compound specific isotopic tracer techniques applied to agricultural lands converted from C3 plant to C4 plant cropping, we followed the molecular turnover of lignins, cutins and suberins in soils, in order to assess their specific residence times, and infer the contributions of above- and belowground tissues to SOM. We showed that lignin turnover in soil is faster than that of total organic carbon. We evidenced contrasting behaviour of lignin as well as cutin/suberin monomers on a molecular basis which may be related to their chemical nature, their position into the polymeric structure and to the plant tissue in which they are present. Therefore, we suggest that compound specific isotope measurements in combination with longterm field trials could lead is understanding of soil carbon stocks and fluxes on a molecular level.
Sammendrag
NA
Forfattere
Lillian ØygardenSammendrag
Det er ikke registrert sammendrag
Forfattere
Lillian ØygardenSammendrag
Det er ikke registrert sammendrag
Sammendrag
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Forfattere
Lillian ØygardenSammendrag
Det er ikke registrert sammendrag
Sammendrag
Det er ikke registrert sammendrag