Естественное лесовосстановление на вырубках в северо-таежном равнинном районе Западной Сибири
The indicators of undergrowth accumulation in the felling sites of the West Siberian north taiga lowland forest area have been analyzed. The undergrowth has been recorded on the plots measuring 2×2 m in the amount of 30 plots on each studied felling site. It is noted that reforestation in the study...
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| Vydáno v: | Izvestiâ vysših učebnyh zavedenij. Lesnoj žurnal číslo 1; s. 58 - 70 |
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| Hlavní autoři: | , , , , , |
| Médium: | Journal Article |
| Jazyk: | angličtina |
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01.02.2025
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| ISSN: | 0536-1036 |
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| Abstract | The indicators of undergrowth accumulation in the felling sites of the West Siberian north taiga lowland forest area have been analyzed. The undergrowth has been recorded on the plots measuring 2×2 m in the amount of 30 plots on each studied felling site. It is noted that reforestation in the study area is proceeding quite successfully. In the conditions of green moss-berry and wild rosemary-lingonberry forest types, the undergrowth includes Scots pine (Pinus sylvestris L.), silver (Betula pendula Roth.) and downy (B. рubescens Ehrh.) birch, Siberian stone pine (Pinus sibirica Rupr.), aspen (Populus tremula L.), Siberian spruce (Picea obovata Ledeb.) and Siberian larch (Larix sibirica Ledeb.) with the dominance of Scots pine and silver birch. The high proportion of birch is explained by the annual seed production of the species and the transfer of seeds by wind over long distances, as well as its ability to vegetatively renew. The regeneration of coniferous species is inhibited by the periodicity of seed years, the suspension of seeds in the forest litter and moss thalli. These problems can be solved by soil mineralization. It is better to combine mineralization with the clearing of felling sites from felling residues. The latter are bulldozed onto a skidding trail from 2 sides. As a result of mixing the felling residues with the forest litter and soil, wood destruction processes are activated and the fire hazard at the felling site is minimized, and ideal conditions for the accumulation of undergrowth are created. The main area between the skidding trails (65–70 %) remains without mineralization, since in this part of the felling site, the maximum amount of pre-generation undergrowth is preserved during logging operations. In the conditions of the northern taiga subzone of the Khanty-Mansy Autonomous Okrug – Yugra, where the average wood increment is 0.6 m3/ha, the raw material value of the stands gives way to the ecological value. Considering the important ecological role of silver and downy birch, it is advisable to establish them as the main tree species. This will speed up the transfer of felling sites to forested lands and reduce an unreasonably high proportion of the forest culture fund area. |
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| AbstractList | The indicators of undergrowth accumulation in the felling sites of the West Siberian north taiga lowland forest area have been analyzed. The undergrowth has been recorded on the plots measuring 2×2 m in the amount of 30 plots on each studied felling site. It is noted that reforestation in the study area is proceeding quite successfully. In the conditions of green moss-berry and wild rosemary-lingonberry forest types, the undergrowth includes Scots pine (Pinus sylvestris L.), silver (Betula pendula Roth.) and downy (B. рubescens Ehrh.) birch, Siberian stone pine (Pinus sibirica Rupr.), aspen (Populus tremula L.), Siberian spruce (Picea obovata Ledeb.) and Siberian larch (Larix sibirica Ledeb.) with the dominance of Scots pine and silver birch. The high proportion of birch is explained by the annual seed production of the species and the transfer of seeds by wind over long distances, as well as its ability to vegetatively renew. The regeneration of coniferous species is inhibited by the periodicity of seed years, the suspension of seeds in the forest litter and moss thalli. These problems can be solved by soil mineralization. It is better to combine mineralization with the clearing of felling sites from felling residues. The latter are bulldozed onto a skidding trail from 2 sides. As a result of mixing the felling residues with the forest litter and soil, wood destruction processes are activated and the fire hazard at the felling site is minimized, and ideal conditions for the accumulation of undergrowth are created. The main area between the skidding trails (65–70 %) remains without mineralization, since in this part of the felling site, the maximum amount of pre-generation undergrowth is preserved during logging operations. In the conditions of the northern taiga subzone of the Khanty-Mansy Autonomous Okrug – Yugra, where the average wood increment is 0.6 m3/ha, the raw material value of the stands gives way to the ecological value. Considering the important ecological role of silver and downy birch, it is advisable to establish them as the main tree species. This will speed up the transfer of felling sites to forested lands and reduce an unreasonably high proportion of the forest culture fund area. |
| Author | Predeina, Irina V. Bashegurov, Konstantin A. Rozinkina, Ekaterina P. Zalesov, Sergey V. Gavrilenko, Andrey N. Popov, Artem S. |
| Author_xml | – sequence: 1 givenname: Konstantin A. orcidid: 0000-0002-9050-8902 surname: Bashegurov fullname: Bashegurov, Konstantin A. – sequence: 2 givenname: Andrey N. orcidid: 0000-0003-3088-7020 surname: Gavrilenko fullname: Gavrilenko, Andrey N. – sequence: 3 givenname: Ekaterina P. orcidid: 0000-0002-8000-9122 surname: Rozinkina fullname: Rozinkina, Ekaterina P. – sequence: 4 givenname: Artem S. orcidid: 0000-0002-3060-9461 surname: Popov fullname: Popov, Artem S. – sequence: 5 givenname: Sergey V. orcidid: 0000-0003-3779-410X surname: Zalesov fullname: Zalesov, Sergey V. – sequence: 6 givenname: Irina V. orcidid: 0009-0003-6806-8968 surname: Predeina fullname: Predeina, Irina V. |
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