Dynamics of Certain Macroelements During the Decomposition of Fallen Trees in an Old-Growth Middle-Taiga Spruce Forest of Kivach Nature Reserve
- Authors: Romashkin I.V.1, Kapitsa E.A.2, Nikerova K.M.1, Shorokhova E.V.1
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Affiliations:
- Forest Research Institute of the Karelian Research Centre of the Russian Academy of Sciences
- Kirov Saint Petersburg State Forest Technical University
- Issue: No 5 (2024)
- Pages: 553-574
- Section: RESEARCH
- URL: https://modernonco.orscience.ru/0024-1148/article/view/677396
- DOI: https://doi.org/10.31857/S0024114824050104
- EDN: https://elibrary.ru/OWGKRT
- ID: 677396
Cite item
Abstract
The dynamics of certain macroelements’ content (P, K, Ca, Mg and S) during the decomposition of bark and wood of fallen trees of the main forest-forming tree species the middle-taiga blueberry spruce forest (Kivach Nature Reserve, Republic of Karelia) was estimated. The initial content of most macroelements was higher in bark compared to that in wood. The direction and intensity of the element content dynamics in deadwood during the decomposition depended on the tree species identity and the log fraction. Depending on tree species, the content of P, and S increased in both bark and wood. The Mg content decreased in bark of deciduous species’ deadwood and did not change significantly in the bark of conifers, whereas it decreased in wood of all studied tree species. The K content decreased in both bark and wood of all studied tree species. The models of the macroelements stocks dynamics on the log scale were presented. In the bark, the stock of all macroelements decreased in direct proportion to the intensity of bark fragmentation: the loss rates varied from –0.08 to –0.69 year–1, depending on the tree species. In wood, the P amount increased in spruce logs and changed only slightly in logs of the other tree species. The stock of other macroelements decreased at a rate not exceeding –0.08 year–1. The loss intensity of those macroelements was higher in the logs of deciduous tree species compared to that in coniferous ones. The results obtained highlight the significant role of coarse woody debris, primarily coniferous tree species, as a long-term pool of macroelements within the biogeochemical cycle in the forest ecosystems.
Keywords
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About the authors
I. V. Romashkin
Forest Research Institute of the Karelian Research Centre of the Russian Academy of Sciences
Author for correspondence.
Email: romashkin@krc.karelia.ru
Russian Federation, 11, Pushkinskaya St., Petrozavodsk, 185910
E. A. Kapitsa
Kirov Saint Petersburg State Forest Technical University
Email: romashkin@krc.karelia.ru
Russian Federation, 5, Institutsky All., Saint Petersburg, 194021
K. M. Nikerova
Forest Research Institute of the Karelian Research Centre of the Russian Academy of Sciences
Email: romashkin@krc.karelia.ru
Russian Federation, 11, Pushkinskaya St., Petrozavodsk, 185910
E. V. Shorokhova
Forest Research Institute of the Karelian Research Centre of the Russian Academy of Sciences
Email: romashkin@krc.karelia.ru
Russian Federation, 11, Pushkinskaya St., Petrozavodsk, 185910
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