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  • The parameter Q10 is commonly used to express the relationship between soil CO2 efflux and soil temperature. One advantage of this parameter is its application in a model expression of respiration losses of different ecosystems. Correct specification of Q10 in these models is indispensable. Soil surface CO2 efflux and soil temperature at different depths were measured in a 21-year-old Norway spruce stand and a mountain grassland site located at the Experimental Ecological Study Site Bily Kriz, Beskydy Mts. (NE Czech Republic), using automated gasometric systems. A time-delay and goodness-of-fit between soil CO2 efflux and soil temperature at different measuring depths were determined. Wide ranges of values for the time-delay of CO2 efflux in response to temperature, Q10 and the determination coefficient (R2) between CO2 efflux and temperature were obtained at the both sites.
  • The parameter Q10 is commonly used to express the relationship between soil CO2 efflux and soil temperature. One advantage of this parameter is its application in a model expression of respiration losses of different ecosystems. Correct specification of Q10 in these models is indispensable. Soil surface CO2 efflux and soil temperature at different depths were measured in a 21-year-old Norway spruce stand and a mountain grassland site located at the Experimental Ecological Study Site Bily Kriz, Beskydy Mts. (NE Czech Republic), using automated gasometric systems. A time-delay and goodness-of-fit between soil CO2 efflux and soil temperature at different measuring depths were determined. Wide ranges of values for the time-delay of CO2 efflux in response to temperature, Q10 and the determination coefficient (R2) between CO2 efflux and temperature were obtained at the both sites. (en)
Title
  • Dependence of the Q10 values on the depth of the soil temperature measuring point
  • Dependence of the Q10 values on the depth of the soil temperature measuring point (en)
skos:prefLabel
  • Dependence of the Q10 values on the depth of the soil temperature measuring point
  • Dependence of the Q10 values on the depth of the soil temperature measuring point (en)
skos:notation
  • RIV/67179843:_____/07:00341967!RIV10-MZP-67179843
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GD526/03/H036), P(SM/640/18/03), Z(AV0Z60870520)
http://linked.open...iv/cisloPeriodika
  • -
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 416225
http://linked.open...ai/riv/idVysledku
  • RIV/67179843:_____/07:00341967
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • respiration; soil; temperature; Q10; Norway spruce; grassland (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [6E08CE1C2057]
http://linked.open...i/riv/nazevZdroje
  • Plant and Soil
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 292
http://linked.open...iv/tvurceVysledku
  • Acosta, Manuel
  • Janouš, Dalibor
  • Pavelka, Marian
  • Marek, Michal V.
  • Kutsch, W.
http://linked.open...n/vavai/riv/zamer
issn
  • 0032-079X
number of pages
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