REFERENCE SOILS OF THE FENNOSCANDIAN GREEN BELT
<p class="Style5">The core elements of the Green Belt of Fennoscandia are protected areas of various ranks. Such cores in the Republic of Karelia are the operating national parks Paanajarvi, Kalevalsky, Ladoga Skerries, strict nature reserve Kostomukshsky. The article describes the s...
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| Format: | Article |
| Language: | English |
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Karelian Research Centre of the Russian Academy of Sciences
2019-04-01
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| Series: | Transactions of the Karelian Research Centre of the Russian Academy of Sciences |
| Subjects: | |
| Online Access: | http://journals.krc.karelia.ru/index.php/thematic/article/view/1033 |
| _version_ | 1818307302920290304 |
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| author | Ol'ga Bakhmet Mariya Medvedeva |
| author_facet | Ol'ga Bakhmet Mariya Medvedeva |
| author_sort | Ol'ga Bakhmet |
| collection | DOAJ |
| description | <p class="Style5">The core elements of the Green Belt of Fennoscandia are protected areas of various ranks. Such cores in the Republic of Karelia are the operating national parks Paanajarvi, Kalevalsky, Ladoga Skerries, strict nature reserve Kostomukshsky. The article describes the soil cover in the protected areas of Karelia situated within the Green Belt of Fennoscandia. Reference soils have been identified for areas of similar natural conditions, their spatial shares have been determined. A distinguishing feature of soils in the north-taiga subzone of the Fennoscandian Green Belt is the prevalence of the podzol formation process, as opposed to soils of the Karelian Ladoga coast, where podburs and brown earths are widespread. Distinctive morphological and physical-chemical properties have been noted for the podzolic soils in the northern and middle taiga of the Green Belt of Fennoscandia. The classification positions of the reference soils of the Fennoscandian Green Belt were determined according to the regional, national and international soil classifications. The resultant data can be used for soil monitoring in natural and disturbed ecosystems, and serve as a basis for protected area planning and designation in Karelia.</p> |
| first_indexed | 2024-12-13T06:56:14Z |
| format | Article |
| id | doaj.art-746cf73279c7431a8adef0c7a809f2d8 |
| institution | Directory Open Access Journal |
| issn | 1997-3217 2312-4504 |
| language | English |
| last_indexed | 2024-12-13T06:56:14Z |
| publishDate | 2019-04-01 |
| publisher | Karelian Research Centre of the Russian Academy of Sciences |
| record_format | Article |
| series | Transactions of the Karelian Research Centre of the Russian Academy of Sciences |
| spelling | doaj.art-746cf73279c7431a8adef0c7a809f2d82022-12-21T23:56:02ZengKarelian Research Centre of the Russian Academy of SciencesTransactions of the Karelian Research Centre of the Russian Academy of Sciences1997-32172312-45042019-04-01410.17076/them1033704REFERENCE SOILS OF THE FENNOSCANDIAN GREEN BELTOl'ga Bakhmet0Mariya Medvedeva1Department of Multidisciplinary Scientific Research, Karelian Research Centre, Russian Academy of SciencesForest Research Institute, Karelian Research Centre, Russian Academy of Sciences<p class="Style5">The core elements of the Green Belt of Fennoscandia are protected areas of various ranks. Such cores in the Republic of Karelia are the operating national parks Paanajarvi, Kalevalsky, Ladoga Skerries, strict nature reserve Kostomukshsky. The article describes the soil cover in the protected areas of Karelia situated within the Green Belt of Fennoscandia. Reference soils have been identified for areas of similar natural conditions, their spatial shares have been determined. A distinguishing feature of soils in the north-taiga subzone of the Fennoscandian Green Belt is the prevalence of the podzol formation process, as opposed to soils of the Karelian Ladoga coast, where podburs and brown earths are widespread. Distinctive morphological and physical-chemical properties have been noted for the podzolic soils in the northern and middle taiga of the Green Belt of Fennoscandia. The classification positions of the reference soils of the Fennoscandian Green Belt were determined according to the regional, national and international soil classifications. The resultant data can be used for soil monitoring in natural and disturbed ecosystems, and serve as a basis for protected area planning and designation in Karelia.</p>http://journals.krc.karelia.ru/index.php/thematic/article/view/1033зеленый пояс фенноскандииэталонные почвыпочвенный покровклассификация почв |
| spellingShingle | Ol'ga Bakhmet Mariya Medvedeva REFERENCE SOILS OF THE FENNOSCANDIAN GREEN BELT Transactions of the Karelian Research Centre of the Russian Academy of Sciences зеленый пояс фенноскандии эталонные почвы почвенный покров классификация почв |
| title | REFERENCE SOILS OF THE FENNOSCANDIAN GREEN BELT |
| title_full | REFERENCE SOILS OF THE FENNOSCANDIAN GREEN BELT |
| title_fullStr | REFERENCE SOILS OF THE FENNOSCANDIAN GREEN BELT |
| title_full_unstemmed | REFERENCE SOILS OF THE FENNOSCANDIAN GREEN BELT |
| title_short | REFERENCE SOILS OF THE FENNOSCANDIAN GREEN BELT |
| title_sort | reference soils of the fennoscandian green belt |
| topic | зеленый пояс фенноскандии эталонные почвы почвенный покров классификация почв |
| url | http://journals.krc.karelia.ru/index.php/thematic/article/view/1033 |
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