2018
DOI: 10.3832/ifor2658-011
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Soil CO2 efflux in uneven-aged and even-aged Norway spruce stands in southern Finland

Abstract: Even-aged forests usually act as carbon sinks during most of their rotation. However, after clearcut they become sources of carbon for a period of several years. Applying uneven-aged forest management with selective cuttings will maintain tree cover and reduce the environmental impact on forest floor. The aim of this study was to compare the soil CO2 efflux between uneven-aged and even-aged Norway spruce stands with similar site properties, to investigate the effect of management practices on soil CO2 efflux a… Show more

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Cited by 8 publications
(2 citation statements)
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“…The inclusion of soil water potential in the model is consistent with previous findings. Soil temperature, relative to soil moisture, generally exerts a more consistent control on R s during the growing season in temperate and boreal forests (Maier and Kress, 2000;Gough et al, 2005;Kumpu et al, 2018). However, soil moisture can become an important control of R s during dry periods, namely by affecting the decomposition of leaf litter and thus R h (Epron et al, 1999;Fang and Moncrieff, 2001;Cisneros-Dozal et al, 2007;Vogel et al, 2013;Santonja et al, 2015).…”
Section: Influence Of Soil Water and Magnesium On R Smentioning
confidence: 99%
“…The inclusion of soil water potential in the model is consistent with previous findings. Soil temperature, relative to soil moisture, generally exerts a more consistent control on R s during the growing season in temperate and boreal forests (Maier and Kress, 2000;Gough et al, 2005;Kumpu et al, 2018). However, soil moisture can become an important control of R s during dry periods, namely by affecting the decomposition of leaf litter and thus R h (Epron et al, 1999;Fang and Moncrieff, 2001;Cisneros-Dozal et al, 2007;Vogel et al, 2013;Santonja et al, 2015).…”
Section: Influence Of Soil Water and Magnesium On R Smentioning
confidence: 99%
“…However, older stands may ensure higher carbon storage in living tree biomass and soil (Pregitzer and Euskirchen 2004, Badalamenti et al 2019, Kun et al 2020. The carbon stocks of old-growth stands are largely defined by multiple of factors such as vegetation type, soil properties, tree species, forest floor production, management and deadwood formation (Kumpu et al 2018, Jandl et al 2019, Mayer et al 2020, Clarke et al 2021, which have different influences on the carbon storage of old-growth, compared to younger, stands (Pregitzer and Euskirchen 2004, Ruel and Gardiner 2019, Molina-Valero et al 2020. Old-growth forest is defined as an ecosystem with overgrown old trees, large amounts of over-sized deadwood, multiple canopy layers which contain rich species composition, and with broad variation in tree size and spacing (Buchwald 2005).…”
Section: Introductionmentioning
confidence: 99%