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Heterotrophic and rhizospheric respiration in coniferous forest soils along a latitudinal gradient

Mäki, Mari (författare)
University of Helsinki
Ryhti, Kira (författare)
University of Helsinki,Finnish Meteorological Institute
Fer, Istem (författare)
Finnish Meteorological Institute
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Ťupek, Boris (författare)
Natural Resources Institute Finland (Luke)
Vestin, Patrik (författare)
Lund University,Lunds universitet,Institutionen för naturgeografi och ekosystemvetenskap,Naturvetenskapliga fakulteten,Dept of Physical Geography and Ecosystem Science,Faculty of Science
Roland, Marilyn (författare)
University of Antwerp
Lehner, Irene (författare)
Lund University,Lunds universitet,ICOS Sweden,Centrum för miljö- och klimatvetenskap (CEC),Naturvetenskapliga fakulteten,Centre for Environmental and Climate Science (CEC),Faculty of Science
Köster, Egle (författare)
University of Eastern Finland
Lehtonen, Aleksi (författare)
Natural Resources Institute Finland (Luke)
Bäck, Jaana (författare)
University of Helsinki
Heinonsalo, Jussi (författare)
University of Helsinki
Pumpanen, Jukka (författare)
University of Eastern Finland
Kulmala, Liisa (författare)
University of Helsinki,Finnish Meteorological Institute
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 (creator_code:org_t)
Elsevier BV, 2022
2022
Engelska.
Ingår i: Agricultural and Forest Meteorology. - : Elsevier BV. - 1873-2240 .- 0168-1923. ; 317
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Northern forest soils are a major carbon (C) reservoir of global importance. To estimate how the C balance in these soils will change, the roles of tree roots and soil microbes in C balance should first be decoupled. This study determined how the activity of heterotrophs and tree roots together with root-associated microbes in the rhizosphere varies in coniferous forest soils in boreal, hemiboreal, and temperate climates along a latitudinal gradient using a trenching approach. We created experimental plots without living tree roots, measured soil respiration (CO2 efflux) from these and from unmanipulated plots using the chamber technique, and partitioned the efflux into root-rhizosphere (RR) and heterotrophic (RH) respiration. The share of RR in ecosystem gross primary production (GPP) decreased from north to south in the Scots pine (Pinus sylvestris L.) and the Norway spruce (Picea abies (L.) Karst.) forests, with the exception of a mixed site, where the share of RR in GPP varied strongly between the years. RR per ground area and per root biomass were mainly independent of climate within the gradient. RH per ground area increased from north to south with temperature, while RH per soil C did not change with temperature. Soil moisture did not significantly affect the respiration components in the northernmost site, whereas soil moisture was positively connected with RH and negatively with RR in other Scots pine sites and positively connected with RR in pure Norway spruce stands. The dynamic ecosystem model LPJ-GUESS was able to capture the seasonal dynamics of RH and RR at the sites, but overall accuracy varied markedly between the sites, as the model underestimated RH in the southern site and RR elsewhere. Our study provides knowledge about the nature of soil respiration components. The valuable insights can be used in more accurate land-ecosystem modelling of forest ecosystems.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Meteorologi och atmosfärforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Meteorology and Atmospheric Sciences (hsv//eng)

Nyckelord

Chamber measurements
Land-surface modelling
Soil carbon
Soil respiration
Trenching
CO2 efflux
Scots pine
Norway spruce
Forest soil
Carbon cycle

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art (ämneskategori)
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