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Decade-long soil changes after the clear felling in forests of the North-Western Caucasus mountains

SAINS TANAH - Journal of Soil Science and Agroclimatology · Vol. 20 No. 1 (2023) · hlm. 1–9

DOI
10.20961/stjssa.v20i1.63187
ISSN
2356-1424, 1412-3606
Terbit
2023-01-03
Penerbit
Universitas Sebelas Maret
Bahasa
en

Abstrak

Clear-fell harvesting significantly alters ecosystem attributes at multiple spatial scales. The results of a study of the dynamics of changes in Rendzik Leptosol and Greyic Phaeozem Vertic forests in the middle mountains of the North-Western Caucasus after clear-cutting in 2010-2020 are presented. Immediately after clearing the forest, areas with varying degrees of disturbance of the soil and vegetation cover were identified in the clearings, from maximum disturbance in the central part of the clearing to slight disturbance on their periphery at different elevations of 540-1600 meters above sea level (masl). The soil covering is represented with Rendzik Leptosol and Greyic Phaeozem Vertic. Among used metrics were temperature, humidity, texture density, penetration resistance, structural and aggregate composition, and other soil parameters. On felling areas, increased temperatures and decreased soil humidity were recorded. The temperature of Rendzik Leptosol at a depth of 10-30 cm changes within the range of 1-15°С in the period 2018-2020. The terrain elevation affects the soil due to the temperature gradient significantly. Rendzik Leptosol is much colder at an elevation 1640 meters above sea level than at 1200 meters above sea level. The temperature of Phaeozem (540 meters above sea level) reaches 20°С during the summer months at a depth of 10 cm. Soils in felling have differences in structural and aggregate composition and water resistance of aggregates. The study results can be used in assessing damage to ecosystems after deforestation and developing methods for accelerating the restoration of soil properties after deforestation. The result of the study can be applied to assess the change in the state of ecosystems after forest degradation. The most informative diagnostic indicators for assessing the state of ecosystems after forest degradation are discussed in the article.

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  • Southern Federal University
  • Maikop State Technological University
  • University of Kurdistan
  • Latakia University
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Rekan penulisOrganisasiArtikel bersama
Saglara MandzhievaAfiliasi tidak diketahui6
Tatiana MinkinaSouthern Federal University6
Vishnu Dayal RajputSouthern Federal University6
Svetlana SushkovaSouthern Federal University6
Tatiana V. MinnikovaSouthern Federal University4
Ðœikhail NizhelskiyAfiliasi tidak diketahui4
Olga Nikolaevna BykhalovaAfiliasi tidak diketahui4
Yana RudenokMaikop State Technological University4
Аlena TimoshenkoAfiliasi tidak diketahui2
Morteza FeiziUniversity of Kurdistan2
Elena FedorenkoSouthern Federal University2
Sergey KolesnikovSouthern Federal University1
Yulia AkimenkoAfiliasi tidak diketahui1
Tigran Ter-MicakyantsAfiliasi tidak diketahui1
Anna Andreevna KuzinaSouthern Federal University1
Elena NevedomayaSouthern Federal University1
Anna RusevaAfiliasi tidak diketahui1
Elizaveta KushnarevaSouthern Federal University1
Maxim DesyatnikovSouthern Federal University1
Rama DaoudLatakia University1

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Sumber metadata: OAI-PMH (metadata jurnal) https://jurnal.uns.ac.id/tanah/oai, pertama di-harvest 10 Nov 2026, terakhir terlihat 10 Nov 2026.
Metadata asli (oai_dc) 
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	<dc:title xml:lang="en">Decade-long soil changes after the clear felling in forests of the North-Western Caucasus mountains</dc:title>
	<dc:creator xml:lang="en">Shkhapatsev, Aslan</dc:creator>
	<dc:creator xml:lang="en">Vilkova, Valeria</dc:creator>
	<dc:creator xml:lang="en">Soldatov, Vasiliy</dc:creator>
	<dc:creator xml:lang="en">Kazeev, Kamil</dc:creator>
	<dc:creator xml:lang="en">Kolesnikov, Sergey</dc:creator>
	<dc:subject xml:lang="en">Ecological state</dc:subject>
	<dc:subject xml:lang="en">Hydrothermal conditions</dc:subject>
	<dc:subject xml:lang="en">Penetration resistance</dc:subject>
	<dc:subject xml:lang="en">Soil stability</dc:subject>
	<dc:description xml:lang="en">Clear-fell harvesting significantly alters ecosystem attributes at multiple spatial scales. The results of a study of the dynamics of changes in Rendzik Leptosol and Greyic Phaeozem Vertic forests in the middle mountains of the North-Western Caucasus after clear-cutting in 2010-2020 are presented. Immediately after clearing the forest, areas with varying degrees of disturbance of the soil and vegetation cover were identified in the clearings, from maximum disturbance in the central part of the clearing to slight disturbance on their periphery at different elevations of 540-1600 meters above sea level (masl). The soil covering is represented with Rendzik Leptosol and Greyic Phaeozem Vertic. Among used metrics were temperature, humidity, texture density, penetration resistance, structural and aggregate composition, and other soil parameters. On felling areas, increased temperatures and decreased soil humidity were recorded. The temperature of Rendzik Leptosol at a depth of 10-30 cm changes within the range of 1-15°С in the period 2018-2020. The terrain elevation affects the soil due to the temperature gradient significantly. Rendzik Leptosol is much colder at an elevation 1640 meters above sea level than at 1200 meters above sea level. The temperature of Phaeozem (540 meters above sea level) reaches 20°С during the summer months at a depth of 10 cm. Soils in felling have differences in structural and aggregate composition and water resistance of aggregates. The study results can be used in assessing damage to ecosystems after deforestation and developing methods for accelerating the restoration of soil properties after deforestation. The result of the study can be applied to assess the change in the state of ecosystems after forest degradation. The most informative diagnostic indicators for assessing the state of ecosystems after forest degradation are discussed in the article.</dc:description>
	<dc:publisher xml:lang="en">Universitas Sebelas Maret</dc:publisher>
	<dc:date>2023-01-03</dc:date>
	<dc:type>info:eu-repo/semantics/article</dc:type>
	<dc:type>info:eu-repo/semantics/publishedVersion</dc:type>
	<dc:format>application/pdf</dc:format>
	<dc:format>application/pdf</dc:format>
	<dc:identifier>https://jurnal.uns.ac.id/tanah/article/view/63187</dc:identifier>
	<dc:identifier>10.20961/stjssa.v20i1.63187</dc:identifier>
	<dc:source xml:lang="en">SAINS TANAH - Journal of Soil Science and Agroclimatology; Vol. 20 No. 1 (2023): June; 1-9</dc:source>
	<dc:source>2356-1424</dc:source>
	<dc:source>1412-3606</dc:source>
	<dc:source>10.20961/stjssa.v20i1</dc:source>
	<dc:language>en</dc:language>
	<dc:relation>https://jurnal.uns.ac.id/tanah/article/view/63187/55818</dc:relation>
	<dc:relation>https://jurnal.uns.ac.id/tanah/article/view/63187/38819</dc:relation>
	<dc:rights xml:lang="en">Copyright (c) 2023 Shkhapatsev Aslan Kaplanovich, Vilkova Valeria Valerievna, Soldatov Vasiliy Petrovich, Kazeev Kamil Shagidullovich, Kolesnikov Sergey Ilyich</dc:rights>
</oai_dc:dc>