Above- and below-ground N stocks in coniferous boreal forests in Finland: Implications for sustainability of more intensive biomass utilization

Abstract Nitrogen (N) is typically the growth-limiting factor in boreal forest ecosystems. Therefore, knowledge on forest N stocks and fluxes is crucial in order to predict and evaluate the effects of different anthropogenic factors (e.g. climate change, air pollutant deposition, forest management practices) on the condition, development and sustainability of boreal forests. In this study, we evaluated the amount and distribution of N and biomass in different compartments of forest ecosystem, including not only tree stand and soil, but also such rarely reported N stocks as litter layer, ground vegetation and fine and small roots. We also calculated the theoretical export of N in three forest harvest regimes of different intensity (stem-only harvest, whole-tree harvest, whole-tree harvest and stump uplifting) and assessed the time required for N deposition to compensate the N losses occurring in them. The study included seven Scots pine and eight Norway spruce dominated stands belonging to the UN-ECE ICP Forests Level II programme in Finland. The average effective temperature sum and stand age of the sites ranged 658–1351 d.d. and 55–200 yrs, respectively. Among the study sites, the total biomass (needles, living and dead branches, stems, bark, stumps, coarse roots, fine and small roots, understory, litter, humus and mineral soil layers) ranged from 178 Mg ha −1 to 541 Mg ha −1 , the respective range for N stock being 1890–7530 kg ha −1 . The two largest pools of N in forest ecosystem were mineral soil (depth 0–40 cm; mean = 70%) and humus layer (mean = 16%). The largest living biomass N stock was in stems in pine stands (88 kg ha −1 ) and in needles in spruce stands (134 kg ha −1 ). Nstored in tree biomass accounted for 7–19% of the total ecosystem N stock. The proportion of N stored in potential logging residues or biofuel (needles, living and dead branches, stumps and coarse roots) was 67 ± 4% and 53 ± 5% of the tree N stock in northern spruce stands and in southern pine stands, respectively. The understory vegetation N stock was the largest in northern spruce stands, and the lowest in southern spruce stands. Our results supported the hypothesis that in boreal coniferous forests, inputs of N by deposition accumulating during the following rotation period will be able to replenish the export of N caused by conventional stem-only-harvest in final cutting, but the sustainability of the site productivity will be challenged when more intense whole tree harvest regimes are practiced, especially in Norway spruce stands.

[1]  J. Repola Biomass equations for Scots pine and Norway spruce in Finland , 2009 .

[2]  P. Hakkila,et al.  Bioenergy from Sustainable Forestry , 2002, Forestry Sciences.

[3]  H. Tuomenvirta,et al.  climatological characteristics of summer precipitation in helsinki during the period 1951 – 2000 , 2008 .

[4]  H. Helmisaari,et al.  Variation in Nutrient Concentrations of Pinus Sylvestris Roots , 1989 .

[5]  Pekka Nöjd,et al.  Fluxes of dissolved organic and inorganic nitrogen in relation to stand characteristics and latitude in Scots pine and Norway spruce stands in Finland , 2008 .

[6]  P. Tamminen,et al.  Effects of logging residue harvest in thinnings on amounts of soil carbon and nutrients in Scots pine and Norway spruce stands , 2012 .

[7]  A. Costantini Soil sampling bulk density in the coastal lowlands of south-east Queensland , 1995 .

[8]  Helmut Haberl,et al.  Large‐scale bioenergy from additional harvest of forest biomass is neither sustainable nor greenhouse gas neutral , 2012 .

[9]  Dominik Röser,et al.  Sustainable use of forest biomass for energy : a synthesis with focus on the Baltic and Nordic region , 2008 .

[10]  Deutsche Ausgabe World Reference Base for Soil Resources 2006 , 2007 .

[11]  E. Beuker,et al.  Heterotrophic respiration and nitrogen mineralisation in soils of Norway spruce, Scots pine and silver birch stands in contrasting climates , 2012 .

[12]  D. Berggren,et al.  Retention of deposited NH+ 4‐N and NO− 3‐N in coniferous forest ecosystems in Southern Sweden , 1998 .

[13]  P. Nöjd,et al.  Forest condition monitoring under the UN/ECE and EC programmes in Finland. , 2000 .

[14]  Pekka Tamminen,et al.  Logging residue removal after thinning in Nordic boreal forests: Long-term impact on tree growth , 2011 .

[15]  Anita Sellstedt,et al.  Quantifying nitrogen-fixation in feather moss carpets of boreal forests , 2002, Nature.

[16]  P. Curtis,et al.  Effects of Forest Management on Soil C and N Storage: Meta Analysis , 2001 .

[17]  P. Hari,et al.  The human footprint in the carbon cycle of temperate and boreal forests , 2007, Nature.

[18]  P. Hari,et al.  Nitrogen balance of a boreal Scots pine forest , 2013 .

[19]  H. Persson,et al.  The distribution and productivity of fine roots in boreal forests , 1983 .

[20]  S. Kellomäki,et al.  Below- and above-ground biomass, production and nitrogen use in Scots pine stands in eastern Finland , 2002 .

[21]  R. Mäkipää,et al.  Nitrogen fixation and methanotrophy in forest mosses along a N deposition gradient , 2013 .

[22]  Prof. Dr. Carl Olof Tamm Nitrogen in Terrestrial Ecosystems , 1991, Ecological Studies.

[23]  J. Derome,et al.  Carbon Quality and Stocks in Organic Horizons in Boreal Forest Soils , 2008, Ecosystems.

[24]  Juan A. Blanco,et al.  Sustainability of forest management practices: Evaluation through a simulation model of nutrient cycling , 2005 .

[25]  T. Näsholm,et al.  The below-ground perspective of forest plants: soil provides mainly organic nitrogen for plants and mycorrhizal fungi. , 2012, The New phytologist.

[26]  Juha Heiskanen,et al.  Soil water-retention characteristics of Scots pine and Norway spruce forest sites in Finnish Lapland , 2002 .

[27]  S. Willför,et al.  What is the composition of AIR? Pyrolysis-GC–MS characterization of acid-insoluble residue from fresh litter and organic horizons under boreal forests in southern Finland , 2012 .

[28]  Mark A. Sutton,et al.  Dry deposition of reactive nitrogen to European ecosystems: a comparison of inferential models across the NitroEurope network , 2010 .

[29]  Paul Hazlett,et al.  Logging impacts on the biogeochemistry of boreal forest soils and nutrient export to aquatic systems: A review , 2008 .

[30]  Risto Ojansuu,et al.  Biomass functions for Scots pine, Norway spruce and birch in Finland , 2007 .

[31]  L. Finér,et al.  Carbon and nitrogen pools in an old-growth, Norway spruce mixed forest in eastern Finland and changes associated with clear-cutting , 2003 .

[32]  B. McMichael,et al.  Plant Roots and Their Environment , 1992 .

[33]  T. Ahti,et al.  Vegetation zones and their sections in northwestern Europe , 1968 .

[34]  M. Starr,et al.  Levels and Characteristics of TOC in Throughfall, Forest Floor Leachate and Soil Solution in Undisturbed Boreal Forest Ecosystems , 2004 .

[35]  M. Kukkola,et al.  Impact of whole-tree harvesting and compensatory fertilization on growth of coniferous thinning stands , 2000 .

[36]  E. Malkonen Annual primary production and nutrient cycle in some Scots pine stands , 1974 .

[37]  Jan Bengtsson,et al.  Carbon and nitrogen in coniferous forest soils after clear-felling and harvests of different intensity , 1996 .

[38]  P. Nöjd,et al.  Response of boreal forest vegetation to the fertility status of the organic layer along a climatic gradient , 2008 .

[39]  Pekka Nöjd,et al.  Fine root biomass in relation to site and stand characteristics in Norway spruce and Scots pine stands. , 2007, Tree physiology.

[40]  Leena Finér,et al.  Estimation of nutrient removals in stem-only and whole-tree harvesting of Scots pine, Norway spruce, and birch stands with generalized nutrient equations , 2011, European Journal of Forest Research.

[41]  Evelyne Thiffault,et al.  Effects of forest biomass harvesting on soil productivity in boreal and temperate forests - a review. , 2011 .

[42]  J. Derome,et al.  Qualitative and quantitative changes in water-extractable organic compounds in the organic horizon of boreal coniferous forests , 2008 .

[43]  J. Palutikof,et al.  Climate change 2007 : impacts, adaptation and vulnerability , 2001 .

[44]  A. Cajander,et al.  Forest types and their significance. , 1949 .

[45]  P. Nöjd,et al.  Fluxes of dissolved organic carbon in stand throughfall and percolation water in 12 boreal coniferous stands on mineral soils in Finland , 2008 .

[46]  N. Clarke,et al.  Effects Of Very Intensive Forest Biomass Harvesting On Short And Long Term Site Productivity , 2008 .

[47]  Dominik Röser,et al.  Sustainable Use of Forest Biomass for Energy , 2008 .

[48]  K. Vogt,et al.  Organic Matter and Nutrient Dynamics in Forest Floors of Young and Mature Abies amabilis Stands in Western Washington, as Affected by Fine‐Root Input , 1983 .

[49]  Jari Liski,et al.  Indirect carbon dioxide emissions from producing bioenergy from forest harvest residues , 2011 .

[50]  M. Starr,et al.  Bulk density of forested mineral soils. , 1994 .

[51]  J. P. Skovsgaard,et al.  Nutrient concentrations in stumps and coarse roots of Norway spruce, Scots pine and silver birch in Sweden, Finland and Denmark , 2013 .

[52]  G. Likens,et al.  Is chloride a conservative ion in forest ecosystems? , 2012, Biogeochemistry.