4.5 Article

Boreal tree species change as a climate mitigation strategy: impact on ecosystem C and N stocks and soil nutrient levels

期刊

ECOSPHERE
卷 12, 期 11, 页码 -

出版社

WILEY
DOI: 10.1002/ecs2.3826

关键词

Betula pubescens; boreal forest; carbon; dead wood; downy birch; ecosystem stocks; nitrogen; Norway spruce; Picea abies; soil organic carbon; soil chemistry; understory vegetation

类别

资金

  1. Research Council of Norway [255307]
  2. Nordic Forest Research, CAR-ES III

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By comparing native birch forests with planted Norway spruce forests in Norway, it was found that the spruce forests had significantly higher C and N stocks, while the birch forests had advantages in terms of understory vegetation cover and C/N stocks. However, the impact of tree species change on soil was not significant, and there were large differences in total ecosystem C stock and C accumulation between the two forest types.
To increase the annual uptake of CO2 as well as the long-term storage of carbon (C) in forests, the Norwegian government consider large-scale replacements of native, deciduous forests with faster-growing species like Norway spruce. To assess the effects of tree species change on ecosystem C and nitrogen (N) stocks and soil chemistry, we used a paired plot approach including stands of native downy birch and planted 45- to 60-yr-old Norway spruce. The birch stands were used as reference for the assessment of differences following the tree species change. We found significantly higher C and N stocks in living tree biomass in the spruce stands, whereas no significant differences were found for dead wood. The cover of understory species groups, and the C and N stocks of the aboveground understory vegetation were significantly higher in the birch stands. The tree species change did not affect the soil organic carbon (SOC) stock down to 1 m soil depth; however, the significantly higher stock in the forest floor of the spruce stands suggested a re-distribution of SOC within the profile. There was a significant positive correlation between the SOC stock down to 30 cm soil depth and the total ecosystem C stock for the birch stands, and a negative correlation for the spruce stands. Significant effects of tree species change were found for C and N concentrations, C/N, exchangeable acidity, base saturation, and exchangeable Ca, K, Mg, Na, S, and Fe in the organic horizon or the upper mineral soil layer. The total ecosystem C stock ranged between 197 and 277 Mg/ha for the birch stands, and 297 and 387 Mg/ha for the spruce stands. The ecosystem C accumulation varied between 32 and 142 Mg/ha over the past 45-60 yr, whereas the net ecosystem C capture was considerably lower and potentially negative. Our results suggest that the potential to meet the governments' targets to increase C sequestration depend on the C debt incurred from the removed birch stands, the rotation length, and potentially also the susceptibility of the different stand types to future risk factors related to climate change.

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