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Carbon and nutrient pools and fluxes in unmanaged mountain Norway spruce forests, and losses after natural tree dieback

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60077344%3A_____%2F23%3A00583771" target="_blank" >RIV/60077344:_____/23:00583771 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/60460709:41320/23:97146 RIV/60076658:12310/23:43907140

  • Výsledek na webu

    <a href="https://doi.org/10.1016/j.scitotenv.2023.166233" target="_blank" >https://doi.org/10.1016/j.scitotenv.2023.166233</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.scitotenv.2023.166233" target="_blank" >10.1016/j.scitotenv.2023.166233</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Carbon and nutrient pools and fluxes in unmanaged mountain Norway spruce forests, and losses after natural tree dieback

  • Popis výsledku v původním jazyce

    Forest areas infected by insects are increasing in Europe and North America due to accelerating climate change. A 2000-2020 mass budget study on major elements (C, N, P, Ca, Mg, K) in the atmosphere-plant-soil-water systems of two unmanaged catchments enabled us to evaluate changes in pools and fluxes related to tree dieback and long-term accumulation/losses during the post-glacial period. A bark-beetle outbreak killed >75% of all trees in a mature mountain spruce forest in one catchment and all dead biomass was left on site. A similar forest in a nearby catchment was only marginally affected. We observed that: (1) the long-term (millennial) C and N accumulation in soils averaged 10-22 and 0.5-1.1kgha(-1)yr(-1), respectively, while losses of Ca, Mg, and K from soils ranged from 0.1 to 2.6kgha(-1)yr(-1). (2) Only <0.8% and <1.5% of the respective total C and N fluxes entering the soil annually from vegetation were permanently stored in soils. (3) The post-disturbance decomposition of dead tree biomass reduced vegetation element pools from 27% (C) to 73% (P) between 2004 and 2019. (4) Tree dieback decreased net atmospheric element inputs to the impacted catchment, and increased theleachingof all elements and gaseous losses of C (similar to 2.3tha(-1)yr(-1)) and N (similar to 14kgha(-1)yr(-1)). The disturbed catchment became a net C source, but similar to 50% of the N released from dead biomass accumulated in soils. (5) Despite the severe forest disturbance, the dissolved losses of Ca and Mg represented 52-58% of their leaching from intact stands during the peaking atmospheric acidification from 1970 to 1990. (6) Disturbance-related net leaching of P, Ca, Mg, and K were 4, 69, 16, and 114kgha(-1), respectively, which represented 7-38% of the losses potentially related to sanitary logging and subsequent removal of the aboveground tree biomass.

  • Název v anglickém jazyce

    Carbon and nutrient pools and fluxes in unmanaged mountain Norway spruce forests, and losses after natural tree dieback

  • Popis výsledku anglicky

    Forest areas infected by insects are increasing in Europe and North America due to accelerating climate change. A 2000-2020 mass budget study on major elements (C, N, P, Ca, Mg, K) in the atmosphere-plant-soil-water systems of two unmanaged catchments enabled us to evaluate changes in pools and fluxes related to tree dieback and long-term accumulation/losses during the post-glacial period. A bark-beetle outbreak killed >75% of all trees in a mature mountain spruce forest in one catchment and all dead biomass was left on site. A similar forest in a nearby catchment was only marginally affected. We observed that: (1) the long-term (millennial) C and N accumulation in soils averaged 10-22 and 0.5-1.1kgha(-1)yr(-1), respectively, while losses of Ca, Mg, and K from soils ranged from 0.1 to 2.6kgha(-1)yr(-1). (2) Only <0.8% and <1.5% of the respective total C and N fluxes entering the soil annually from vegetation were permanently stored in soils. (3) The post-disturbance decomposition of dead tree biomass reduced vegetation element pools from 27% (C) to 73% (P) between 2004 and 2019. (4) Tree dieback decreased net atmospheric element inputs to the impacted catchment, and increased theleachingof all elements and gaseous losses of C (similar to 2.3tha(-1)yr(-1)) and N (similar to 14kgha(-1)yr(-1)). The disturbed catchment became a net C source, but similar to 50% of the N released from dead biomass accumulated in soils. (5) Despite the severe forest disturbance, the dissolved losses of Ca and Mg represented 52-58% of their leaching from intact stands during the peaking atmospheric acidification from 1970 to 1990. (6) Disturbance-related net leaching of P, Ca, Mg, and K were 4, 69, 16, and 114kgha(-1), respectively, which represented 7-38% of the losses potentially related to sanitary logging and subsequent removal of the aboveground tree biomass.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10617 - Marine biology, freshwater biology, limnology

Návaznosti výsledku

  • Projekt

    Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

  • Návaznosti

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Ostatní

  • Rok uplatnění

    2023

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Science of the Total Environment

  • ISSN

    0048-9697

  • e-ISSN

    1879-1026

  • Svazek periodika

    903

  • Číslo periodika v rámci svazku

    Aug

  • Stát vydavatele periodika

    NL - Nizozemsko

  • Počet stran výsledku

    13

  • Strana od-do

    166233

  • Kód UT WoS článku

    001066827300001

  • EID výsledku v databázi Scopus

    2-s2.0-85167790545