Slovenian Forestry Institute

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    1721 research outputs found

    Information on LULUCF actions Slovenia

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    Acta silvae et ligni

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    Opisna sortna lista za jajčevec 2015

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    Bazoljubno borovje v Sloveniji: združbe črnega in rdečega bora na karbonatni podlagi in rušja v alpskih dolinah

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    Opisna sortna lista za krompir 2015

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    Spremljanje nastajanja ksilema in floema ter kambijeve aktivnosti pri bukvi in smreki v Sloveniji

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    Temporal dynamics of cambial activity and wood and phloem formation was monitored in European beech (Fagus sylvatica L.) and Norway spruce (Picea abies (L.) Karst.) at the sites Panška reka near Ljubljana (400 m a.s.l.) and on Menina planina (1200 m a.s.l.) from 2006 until 2014. The monitoring is based on histometrical analysis of stem tissues of adult trees including cambial zone, xylem (wood) and phloem. Samples (micro cores) for analyses were taken from trees using a Trephor tool at weekly intervals during the growing seasons. Micro cores were embedded in paraffin in order to cut cross-sections and make permanent slides for observations under the light microscope. We always measured the width or counted the number of cells in the cambium, forming xylem and forming phloem increments. The measurements or counting were performed along three radial files of xylem and phloem growth rings and the cambial zone. We recorded the phases of xylem formation: PC – post-cambial extension growth, SW – deposition of secondary wall and lignification, MT – mature cells. In phloem we separately recorded the formation of early and late phloem. Research on beech was conducted in 2006 and from 2008 until 2014, and on spruce from 2009 until 2014. The monitoring and sampling continues. We present some main findings on the beginning, dynamics and cessation of processes which lead to formation of wood and phloem annual growth layers in beech and spruce from both sites. We show how the processes depend on climatic factors. We also present how the spruce data included in a global data set of conifers helps to predict how tree productivity (and survival) will change due to climatic change. The described processes and their variability are still poorly understood; it is therefore necessary to continue the research presented. The results provide basic knowledge to better understand productivity of trees and forest stands, wood quality, the impact of climate change on tree growth and survival, accumulation of carbon and other processes

    Fine root dynamics in Slovenian beech forests in relation to soil temperature and water availability

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    The ingrowth and mortality of European beech (Fagus sylvatica L.) fine roots (diameters <2 mm) were studied in relation to environmental variables describing temperature and water availability at four sites, covering a range in environmental conditions likely to be encountered in Slovenian beech forests. Minirhizotron images were used to determine fine root dynamics in a stand and gap in each of the sites for 12 periods during the 2007–2009 growing seasons. The environmental variables included air and soil temperatures, precipitation, forest floor precipitation, evapotranspiration and soil water contents. For data analysis, the daily mean values for each period for all variables were used. Fine root ingrowth and mortality were higher in the managed stand and gap compared to the old-growth stand and gap, but only significantly correlated with each other in the case of the managed stand. Forest floor precipitation and soil temperature were significant in explaining fine root ingrowth, whereas maximal evapotranspiration, soil temperature and soil water content were more important for fine root mortality. However, the correlations were weak and inconsistent among the four sites. By including site as predictor as well as environmental variables, R2 values of 0.49 and 0.55 for ingrowth and mortality, respectively, were achieved. Despite this, the relationships between the fine root dynamics and selected environmental factors appeared relatively weak and complex, especially for fine root ingrowth and might be partially related also to differences in successional stages of the forests under study

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