Sökning: onr:"swepub:oai:gup.ub.gu.se/51784" > The likely impact o...
Fältnamn | Indikatorer | Metadata |
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000 | 06008naa a2200949 4500 | |
001 | oai:gup.ub.gu.se/51784 | |
003 | SwePub | |
008 | 240528s2007 | |||||||||||000 ||eng| | |
009 | oai:lup.lub.lu.se:801fb3c8-0f3e-40b9-8cd1-5056a4384ba0 | |
009 | oai:DiVA.org:oru-4240 | |
024 | 7 | a https://gup.ub.gu.se/publication/517842 URI |
024 | 7 | a https://doi.org/10.1111/j.1469-8137.2007.01967.x2 DOI |
024 | 7 | a https://lup.lub.lu.se/record/6371072 URI |
024 | 7 | a https://urn.kb.se/resolve?urn=urn:nbn:se:oru:diva-42402 URI |
040 | a (SwePub)gud (SwePub)lud (SwePub)oru | |
041 | a eng | |
042 | 9 SwePub | |
072 | 7 | a ref2 swepub-contenttype |
072 | 7 | a for2 swepub-publicationtype |
100 | 1 | a Hyvonen, R.4 aut |
245 | 1 0 | a The likely impact of elevated [CO2], nitrogen deposition, increased temperature and management on carbon sequestration in temperate and boreal forest ecosystems: a literature review |
264 | c 2007-01-16 | |
264 | 1 | a Cambridge :b Wiley,c 2007 |
520 | a Temperate and boreal forest ecosystems contain a large part of the carbon stored on land, in the form of both biomass and soil organic matter. Increasing atmospheric [CO2], increasing temperature, elevated nitrogen deposition and intensified management will change this C store. Well documented single-factor responses of net primary production are: higher photosynthetic rate (the main [CO2] response); increasing length of growing season (the main temperature response); and higher leaf-area index (the main N deposition and partly [CO2] response). Soil organic matter will increase with increasing litter input, although priming may decrease the soil C stock initially, but litter quality effects should be minimal (response to [CO2], N deposition, and temperature); will decrease because of increasing temperature; and will increase because of retardation of decomposition with N deposition, although the rate of decomposition of high-quality litter can be increased and that of low-quality litter decreased. Single-factor responses can be misleading because of interactions between factors, in particular those between N and other factors, and indirect effects such as increased N availability from temperature-induced decomposition. In the long term the strength of feedbacks, for example the increasing demand for N from increased growth, will dominate over short-term responses to single factors. However, management has considerable potential for controlling the C store. | |
650 | 7 | a NATURVETENSKAPx Biologix Ekologi0 (SwePub)106112 hsv//swe |
650 | 7 | a NATURAL SCIENCESx Biological Sciencesx Ecology0 (SwePub)106112 hsv//eng |
650 | 7 | a LANTBRUKSVETENSKAPERx Lantbruksvetenskap, skogsbruk och fiskex Jordbruksvetenskap0 (SwePub)401012 hsv//swe |
650 | 7 | a AGRICULTURAL SCIENCESx Agriculture, Forestry and Fisheriesx Agricultural Science0 (SwePub)401012 hsv//eng |
650 | 7 | a LANTBRUKSVETENSKAPERx Lantbruksvetenskap, skogsbruk och fiskex Markvetenskap0 (SwePub)401062 hsv//swe |
650 | 7 | a AGRICULTURAL SCIENCESx Agriculture, Forestry and Fisheriesx Soil Science0 (SwePub)401062 hsv//eng |
650 | 7 | a NATURVETENSKAPx Biologix Botanik0 (SwePub)106072 hsv//swe |
650 | 7 | a NATURAL SCIENCESx Biological Sciencesx Botany0 (SwePub)106072 hsv//eng |
650 | 7 | a NATURVETENSKAPx Geovetenskap och miljövetenskapx Naturgeografi0 (SwePub)105072 hsv//swe |
650 | 7 | a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Physical Geography0 (SwePub)105072 hsv//eng |
650 | 7 | a NATURVETENSKAPx Kemi0 (SwePub)1042 hsv//swe |
650 | 7 | a NATURAL SCIENCESx Chemical Sciences0 (SwePub)1042 hsv//eng |
653 | a carbon balance | |
653 | a carbon dioxide (CO2) | |
653 | a climate change | |
653 | a fertilization | |
653 | a global warming | |
653 | a SOIL ORGANIC-MATTER | |
653 | a LEAF-LITTER DECOMPOSITION | |
653 | a GROSS PRIMARY PRODUCTION | |
653 | a NET PRIMARY PRODUCTION | |
653 | a FOREST | |
653 | a FINE-ROOT PRODUCTION | |
653 | a ATMOSPHERIC CO2 | |
653 | a carbon balance | |
653 | a NATURAL SCIENCES | |
653 | a Chemistry | |
653 | a Chemistry | |
700 | 1 | a Agren, G. I.4 aut |
700 | 1 | a Linder, S.4 aut |
700 | 1 | a Persson, T.4 aut |
700 | 1 | a Cotrufo, M. F.4 aut |
700 | 1 | a Ekblad, Alfu Örebro universitet,Institutionen för naturvetenskap4 aut0 (Swepub:oru)afed |
700 | 1 | a Freeman, M.4 aut |
700 | 1 | a Grelle, A.4 aut |
700 | 1 | a Janssens, I. A.4 aut |
700 | 1 | a Jarvis, P. G.4 aut |
700 | 1 | a Kellomaki, S.4 aut |
700 | 1 | a Lindroth, Andersu Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science4 aut0 (Swepub:lu)ngeo-ali |
700 | 1 | a Loustau, D.4 aut |
700 | 1 | a Lundmark, T.4 aut |
700 | 1 | a Norby, R. J.4 aut |
700 | 1 | a Oren, R.4 aut |
700 | 1 | a Pilegaard, K.4 aut |
700 | 1 | a Ryan, M. G.4 aut |
700 | 1 | a Sigurdsson, B. D.4 aut |
700 | 1 | a Stromgren, M.4 aut |
700 | 1 | a van Oijen, M.4 aut |
700 | 1 | a Wallin, Göran,d 1955u Gothenburg University,Göteborgs universitet,Institutionen för växt- och miljövetenskaper,Department of Plant and Environmental Sciences4 aut0 (Swepub:gu)xwallg |
710 | 2 | a Örebro universitetb Institutionen för naturvetenskap4 org |
773 | 0 | t New Phytologistd Cambridge : Wileyg 173:3, s. 463-480q 173:3<463-480x 0028-646Xx 1469-8137 |
856 | 4 | u https://nph.onlinelibrary.wiley.com/doi/pdfdirect/10.1111/j.1469-8137.2007.01967.x |
856 | 4 | u http://dx.doi.org/10.1111/j.1469-8137.2007.01967.xy FULLTEXT |
856 | 4 | u https://doi.org/10.1111/j.1469-8137.2007.01967.xy Fulltext |
856 | 4 8 | u https://gup.ub.gu.se/publication/51784 |
856 | 4 8 | u https://doi.org/10.1111/j.1469-8137.2007.01967.x |
856 | 4 8 | u https://lup.lub.lu.se/record/637107 |
856 | 4 8 | u https://urn.kb.se/resolve?urn=urn:nbn:se:oru:diva-4240 |
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