SwePub
Tyck till om SwePub Sök här!
Sök i SwePub databas

  Utökad sökning

Träfflista för sökning "WFRF:(Langvall O.) "

Sökning: WFRF:(Langvall O.)

  • Resultat 1-7 av 7
Sortera/gruppera träfflistan
   
NumreringReferensOmslagsbildHitta
1.
  •  
2.
  • Bergkvist, Bo, et al. (författare)
  • Pools and fluxes of carbon in three Norway spruce ecosystems along a climatic gradient in Sweden
  • 2008
  • Ingår i: Biogeochemistry. - : Springer Science and Business Media LLC. - 0168-2563 .- 1573-515X. ; 89:1, s. 7-25
  • Tidskriftsartikel (refereegranskat)abstract
    • This paper presents an integrated analysis of organic carbon (C) pools in soils and vegetation, within-ecosystem fluxes and net ecosystem exchange (NEE) in three 40-year old Norway spruce stands along a north-south climatic gradient in Sweden, measured 2001-2004. A process-orientated ecosystem model (CoupModel), previously parameterised on a regional dataset, was used for the analysis. Pools of soil organic carbon (SOC) and tree growth rates were highest at the southernmost site (1.6 and 2.0-fold, respectively). Tree litter production (litterfall and root litter) was also highest in the south, with about half coming from fine roots (< 1 mm) at all sites. However, when the litter input from the forest floor vegetation was included, the difference in total litter input rate between the sites almost disappeared (190-233 g C m(-2) year(-1)). We propose that a higher N deposition and N availability in the south result in a slower turnover of soil organic matter than in the north. This effect seems to overshadow the effect of temperature. At the southern site, 19% of the total litter input to the O horizon was leached to the mineral soil as dissolved organic carbon, while at the two northern sites the corresponding figure was approx. 9%. The CoupModel accurately described general C cycling behaviour in these ecosystems, reproducing the differences between north and south. The simulated changes in SOC pools during the measurement period were small, ranging from -8 g C m(-2) year(-1) in the north to +9 g C m(-2) year(-1) in the south. In contrast, NEE and tree growth measurements at the northernmost site suggest that the soil lost about 90 g C m(-2) year(-1).
  •  
3.
  • Dahl, Åslög, 1955, et al. (författare)
  • Se klimatförändringarna med egna ögon – gör fenologiska observationer.
  • 2008
  • Ingår i: Svensk Botanisk Tidskrift. - 0039-646X. ; 102:1, s. 19-26
  • Tidskriftsartikel (övrigt vetenskapligt/konstnärligt)abstract
    • Med den förestående klimatförändringen finns ett ökat behov av att veta hur arter och växtsamhällen påverkas, Svensk naturvård har genom åren haft stor nytta av alla de botanister som på fritiden inventerat den svenska floran. Författarna vill här uppmana till en ny angelägen insats. I dag finns tekniken att rapportera fenologiska observationer som datum för lövsprickning, blomning eller fruktmognad på ett enkelt sätt.
  •  
4.
  • Klemedtsson, Leif, 1953, et al. (författare)
  • Bayesian calibration method used to elucidate carbon turnover in forest on drained organic soil
  • 2008
  • Ingår i: Biogeochemistry. - : Springer Science and Business Media LLC. - 0168-2563 .- 1573-515X. ; 89:1, s. 61-79
  • Tidskriftsartikel (refereegranskat)abstract
    • Depending on the balance between sink and source processes for C, drained organic forest soil ecosystems can be in balance or act as net sinks or sources of CO2 to the atmosphere. In order to study the effect of groundwater level and soil temperature on C-flux, the CoupModel was calibrated (climate data, groundwater levels, soil CO2 flux, net ecosystem fluxes of CO2-exchange, sensible heat flux and latent heat flux, forest production etc.) for a drained forest in Sweden. Bayesian calibration techniques were used to elucidate how different parameters and variables were interlinked in C-circulation. The calibrated model reproduced abiotic and biotic variables reasonably well except for root respiration, which was largely underestimated. Bayesian calibration reduced the uncertainties in the model and highlighted the fact that calibrations should be performed with a high number of parameters instead of specific parameter values.
  •  
5.
  • Lindroth, Anders, et al. (författare)
  • Gudrun - en kolbomb
  • 2005
  • Ingår i: Miljöforskning : Formas tidning för ett uthålligt samhälle. - 1650-4925. ; 5-6, s. 22-24
  • Tidskriftsartikel (populärvet., debatt m.m.)
  •  
6.
  • Lindroth, Anders, et al. (författare)
  • Measurement of net ecosystem exchange, productivity and respiration in three spruce forests in Sweden shows unexpectedly large soil carbon losses
  • 2008
  • Ingår i: Biogeochemistry. - : Springer Science and Business Media LLC. - 0168-2563 .- 1573-515X. ; 89:1, s. 43-60
  • Tidskriftsartikel (refereegranskat)abstract
    • Measurement of net ecosystem exchange was made using the eddy covariance method above three forests along a north-south climatic gradient in Sweden: Flakaliden in the north, Knottasen in central and Asa in south Sweden. Data were obtained for 2 years at Flakaliden and Knottasen and for one year at Asa. The net fluxes (N-ep) were separated into their main components, total ecosystem respiration (R-t) and gross primary productivity (P-g). The maximum half-hourly net uptake during the heart of the growing season was highest in the southernmost site with -0.787 mg CO2 m(-2) s(-1) followed by Knottasen with -0.631 mg CO2 m(-2) s(-1) and Flakaliden with -0.429 mg CO2 m(-2) s(-1). The maximum respiration rates during the summer were highest in Knottasen with 0.245 mg CO2 m(-2) s(-1) while it was similar at the two other sites with 0.183 mg CO2 m(-2) s(-1). The annual N-ep ranged between uptake of -304 g C m(-2) year(-1) (Asa) and emission of 84 g C m(-2) year(-1) (Knottasen). The annual R-t and P-g ranged between 793 to 1253 g C m(-2)year(-1) and -875 to -1317 g C m(-2) year(-1), respectively. Biomass increment measurements in the footprint area of the towers in combination with the measured net ecosystem productivity were used to estimate the changes in soil carbon and it was found that the soils were losing on average 96-125 g C m(-2)year(-1). The most plausible explanation for these losses was that the studied years were much warmer than normal causing larger respiratory losses. The comparison of net primary productivity and P-g showed that ca 60% of P-g was utilized for autotrophic respiration.
  •  
7.
  •  
Skapa referenser, mejla, bekava och länka
  • Resultat 1-7 av 7

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy