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