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Effects of salvage logging on the soil microclimate of temperate European forests following Norway spruce dieback

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F62156489%3A43410%2F25%3A43927179" target="_blank" >RIV/62156489:43410/25:43927179 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://doi.org/10.1016/j.foreco.2025.122922" target="_blank" >https://doi.org/10.1016/j.foreco.2025.122922</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.foreco.2025.122922" target="_blank" >10.1016/j.foreco.2025.122922</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Effects of salvage logging on the soil microclimate of temperate European forests following Norway spruce dieback

  • Popis výsledku v původním jazyce

    In most managed forests, salvage logging is a common method of regaining forest natural and economic capital following disturbances. Nevertheless, trade-offs between management objectives and the ecological impacts of salvage logging can influence other forest restoration decisions. Following an episode of Norway spruce (Picea abies) dieback in 2018, we monitored soil temperature and soil water content, both key soil microclimate variables, to assess the impact of three commonly used post-disturbance treatments: immediate salvage logging (&lt; 2 years), delayed salvage logging (3-4 years), and no salvage logging. Immediate logging had the greatest negative impact on soil temperature variables, with maximum daytime soil temperatures increasing by up to 3.5oC in the topsoil (10 cm) and diurnal temperature variation rising by up to 1.9oC. Increases were also evident in the subsoil layers (30 and 60 cm). Prolonging the time between disturbance and logging, however, mitigated these negative effects on soil temperature stability, providing soil microclimate readings similar to those at sites with no salvage logging and/or pre-disturbance conditions. In addition, delaying salvage logging, or opting for no salvage logging, resulted in an 8-11 % increase in soil water content compared to the control. These findings suggest that postponing salvage logging by approximately 3-4 years significantly reduces negative ecological impacts on soil microclimate and enhances the resilience of temperate forests in the face of potential large-scale disturbances under climate change.

  • Název v anglickém jazyce

    Effects of salvage logging on the soil microclimate of temperate European forests following Norway spruce dieback

  • Popis výsledku anglicky

    In most managed forests, salvage logging is a common method of regaining forest natural and economic capital following disturbances. Nevertheless, trade-offs between management objectives and the ecological impacts of salvage logging can influence other forest restoration decisions. Following an episode of Norway spruce (Picea abies) dieback in 2018, we monitored soil temperature and soil water content, both key soil microclimate variables, to assess the impact of three commonly used post-disturbance treatments: immediate salvage logging (&lt; 2 years), delayed salvage logging (3-4 years), and no salvage logging. Immediate logging had the greatest negative impact on soil temperature variables, with maximum daytime soil temperatures increasing by up to 3.5oC in the topsoil (10 cm) and diurnal temperature variation rising by up to 1.9oC. Increases were also evident in the subsoil layers (30 and 60 cm). Prolonging the time between disturbance and logging, however, mitigated these negative effects on soil temperature stability, providing soil microclimate readings similar to those at sites with no salvage logging and/or pre-disturbance conditions. In addition, delaying salvage logging, or opting for no salvage logging, resulted in an 8-11 % increase in soil water content compared to the control. These findings suggest that postponing salvage logging by approximately 3-4 years significantly reduces negative ecological impacts on soil microclimate and enhances the resilience of temperate forests in the face of potential large-scale disturbances under climate change.

Klasifikace

  • Druh

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

  • CEP obor

  • OECD FORD obor

    40102 - Forestry

Návaznosti výsledku

  • Projekt

  • Návaznosti

    S - Specificky vyzkum na vysokych skolach

Ostatní

  • Rok uplatnění

    2025

  • Kód důvěrnosti údajů

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

Údaje specifické pro druh výsledku

  • Název periodika

    Forest Ecology and Management

  • ISSN

    0378-1127

  • e-ISSN

    1872-7042

  • Svazek periodika

    593

  • Číslo periodika v rámci svazku

    1 October

  • Stát vydavatele periodika

    NL - Nizozemsko

  • Počet stran výsledku

    14

  • Strana od-do

    122922

  • Kód UT WoS článku

    001517356400001

  • EID výsledku v databázi Scopus

    2-s2.0-105008517581