Long-term effects of site preparation on growth in Scots pine
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How does management affect soil C sequestration and greenhouse gas fluxes in boreal and temperate forests? – A review
2023, Forest Ecology and ManagementIntensive site preparation for reforestation wastes multi-trophic biodiversity potential in commercial oak woodlands
2021, Journal of Environmental ManagementMultiple stressors in small streams in the forestry context of Fennoscandia: The effects in time and space
2021, Science of the Total EnvironmentCitation Excerpt :To increase the chances of seedling survival, mechanized site preparation by disk trenching or mounding is typically done in Fennoscandian forests (Esseen et al., 1997). During site preparation, soils are scarified and the top humus layer turned over, exposing mineral layers, increasing nutrient availability, soil aeration, and drainage (Hallsby, 2007; Örlander et al., 1996). Since this practice causes physical soil disturbance, it is not allowed close to surface waters or on wet soils, especially in riparian areas (Skogsstyrelsen, 2019).
Ungulate-adapted forestry shows promise for alleviating pine browsing damage
2021, Forest Ecology and ManagementLong-term effects of mechanical site preparation on understorey plant communities in lowland floodplain forests
2021, Forest Ecology and ManagementInfluence of forest management activities on soil organic carbon stocks: A knowledge synthesis
2020, Forest Ecology and ManagementCitation Excerpt :Restricting sampling to the uppermost soil layer may exaggerate the effects of disturbance as they are usually most pronounced in the forest floor (Piirainen et al., 2015); soil C can moreover be translocated, buried and stabilized with depth as found by Swain et al. (2010). Significant reductions in total soil C contents were reported 60–70 years after mechanical site preparation (Örlander et al., 1996), but the changes were small when soil C was measured to a depth of 1 m and so would have included the buried organic matter (Prescott et al., 2017). Schmidt et al. (1996) found lower soil C in site-prepared, but the difference was significant only in microsites such as the trench bottom from which the organic layer had been displaced.