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.
2015
Forfattere
Johannes BreidenbachSammendrag
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Forfattere
Jørgen Todnem Tor LunnanSammendrag
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Forfattere
Inger Sundheim FløistadSammendrag
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Forfattere
Lars Vesterdal Nicholas Clarke Bjarni D. Sigurdsson Helena M Stefánsdóttir O. Janne Kjønaas Per Gundersen Inge Stupak Teresa Gómez de la Bárcena Lars Pødenphant KiærSammendrag
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Forfattere
Daniela Sauer Isabelle Schülli-Maurer Stephen Wagner Fabio Scarciglia Ragnhild Sperstad Siri Svendgård-Stokke Rolf Sørensen Gerhard SchellmannSammendrag
This paper reports soil development over time in different climates, on time-scales ranging from a few thousand to several hundred thousand years. Changes in soil properties over time, underlying soil-forming processes and their rates are presented. The paper is based on six soil chronosequences, i.e. sequences of soils of different age that are supposed to have developed under the similar conditions with regard to climate, vegetation and other living organisms, relief and parent material. The six soil chronosequences are from humid-temperate, Mediterranean and semi-arid climates. They are compared with regard to soil thickness increase, changes in soil pH, formation of pedogenic iron oxides (expressed as Fed/Fet ratios), clay formation, dust influx (both reflected in clay/silt ratios), and silicate weathering and leaching of base cations (expressed as (Ca+Mg+K+Na)/Al molar ratios) over time. This comparison reveals that the increase of solum thickness with time can be best described by logarithmic equations in all three types of climates. Fed/Fet ratios (proportion of pedogenic iron Fed compared to total iron Fet) reflects the transformation of iron in primary minerals into pedogenic iron. This ratio usually increases with time, except for regions, where the influx of dust (having low Fed/Fet ratios) prevails over the process of pedogenic iron oxide formation, which is the case in the Patagonian chronosequences. Dust influx has also a substantial influence on the time courses of clay/silt ratios and on element indices of silicate weathering. Using the example of a 730 ka soil chronosequence from southern Italy, the fact that soils of long chronosequences inevitably experienced major environmental changes is demonstrated, and, consequentially a modified definition of requirements for soil chronosequences is suggested. Moreover, pedogenic thresholds, feedback systems and progressive versus regressive processes identified in the soil chronosequences are discussed.
Forfattere
Holger Lange Lise Dalsgaard Signe Kynding Borgen O. Janne Kjønaas Ingeborg Callesen Jari Liski Line Tau StrandSammendrag
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Forfattere
Inge Stupak Karin Hansen Eva Ring Karsten Raulund-Rasmussen Ingeborg Callesen Nicholas ClarkeSammendrag
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