Soils of the northern part of the Subpolar Urals: Morphology, physicochemical properties, and carbon and nitrogen pools
The morphology and physicochemical properties of mountain-tundra and mountain-forest soils of the Subpolar Urals are analyzed. Gleyic humus-illuvial podburs, in combination with humus-illuvial podburs and raw-humus gleyzems, predominate in the mountain-tundra zone; permafrost-affected gleyzems and p...
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| Veröffentlicht in: | Eurasian soil science 2013-05, Vol.46 (5), p.459-467 |
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| creator | Dymov, A. A. Zhangurov, E. V. Startsev, V. V. |
| description | The morphology and physicochemical properties of mountain-tundra and mountain-forest soils of the Subpolar Urals are analyzed. Gleyic humus-illuvial podburs, in combination with humus-illuvial podburs and raw-humus gleyzems, predominate in the mountain-tundra zone; permafrost-affected gleyzems and peat gleyzems with a shallow (30–50 cm) permafrost table are developed on colluvial fans at the foots-lopes. Iron-illuvial podzols, iron-illuvial svetlozems, eluviated burozems, texture-differentiated podzolic soils with a microprofile of a podzol, and gleyed peat-podzolic soils occur in the mountain-forest zone. The organic carbon and nitrogen pools in the soils considerably vary depending on the soil type and local landscape conditions. The organic carbon pool stored in the upper 50 cm of the soil profile varies from 7.7 to 39.3 kg/m
2
in the mountain-tundra soils and from 6.5 to 11.8 kg/m
2
in the mountain-forest soils. The corresponding values for the nitrogen pool are 0.4–2.4 and 0.4–0.8 kg/m
2
, respectively. |
| doi_str_mv | 10.1134/S1064229313050025 |
| format | Article |
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2
in the mountain-tundra soils and from 6.5 to 11.8 kg/m
2
in the mountain-forest soils. The corresponding values for the nitrogen pool are 0.4–2.4 and 0.4–0.8 kg/m
2
, respectively.</description><identifier>ISSN: 1064-2293</identifier><identifier>EISSN: 1556-195X</identifier><identifier>DOI: 10.1134/S1064229313050025</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Analysis ; Carbon ; Carbon content ; Decomposing organic matter ; Earth and Environmental Science ; Earth Sciences ; Forest soils ; Genesis and Geography of Soils ; Geotechnical Engineering & Applied Earth Sciences ; Humus ; Morphology ; Mountains ; Nitrogen ; Organic carbon ; Peat ; Permafrost ; Physicochemical properties ; Podzols ; Soil profiles ; Soil sciences ; Soil types ; Soils ; Taiga & tundra ; Tundra ; Tundra ecology</subject><ispartof>Eurasian soil science, 2013-05, Vol.46 (5), p.459-467</ispartof><rights>Pleiades Publishing, Ltd. 2013</rights><rights>COPYRIGHT 2013 Springer</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a411t-57fecec7a1fdc075fcabbe284c59a1ef72210c0d650b14ce0140f1e93868c0f93</citedby><cites>FETCH-LOGICAL-a411t-57fecec7a1fdc075fcabbe284c59a1ef72210c0d650b14ce0140f1e93868c0f93</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1134/S1064229313050025$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1134/S1064229313050025$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Dymov, A. A.</creatorcontrib><creatorcontrib>Zhangurov, E. V.</creatorcontrib><creatorcontrib>Startsev, V. V.</creatorcontrib><title>Soils of the northern part of the Subpolar Urals: Morphology, physicochemical properties, and carbon and nitrogen pools</title><title>Eurasian soil science</title><addtitle>Eurasian Soil Sc</addtitle><description>The morphology and physicochemical properties of mountain-tundra and mountain-forest soils of the Subpolar Urals are analyzed. Gleyic humus-illuvial podburs, in combination with humus-illuvial podburs and raw-humus gleyzems, predominate in the mountain-tundra zone; permafrost-affected gleyzems and peat gleyzems with a shallow (30–50 cm) permafrost table are developed on colluvial fans at the foots-lopes. Iron-illuvial podzols, iron-illuvial svetlozems, eluviated burozems, texture-differentiated podzolic soils with a microprofile of a podzol, and gleyed peat-podzolic soils occur in the mountain-forest zone. The organic carbon and nitrogen pools in the soils considerably vary depending on the soil type and local landscape conditions. The organic carbon pool stored in the upper 50 cm of the soil profile varies from 7.7 to 39.3 kg/m
2
in the mountain-tundra soils and from 6.5 to 11.8 kg/m
2
in the mountain-forest soils. The corresponding values for the nitrogen pool are 0.4–2.4 and 0.4–0.8 kg/m
2
, respectively.</description><subject>Analysis</subject><subject>Carbon</subject><subject>Carbon content</subject><subject>Decomposing organic matter</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Forest soils</subject><subject>Genesis and Geography of Soils</subject><subject>Geotechnical Engineering & Applied Earth Sciences</subject><subject>Humus</subject><subject>Morphology</subject><subject>Mountains</subject><subject>Nitrogen</subject><subject>Organic carbon</subject><subject>Peat</subject><subject>Permafrost</subject><subject>Physicochemical properties</subject><subject>Podzols</subject><subject>Soil profiles</subject><subject>Soil sciences</subject><subject>Soil types</subject><subject>Soils</subject><subject>Taiga & tundra</subject><subject>Tundra</subject><subject>Tundra ecology</subject><issn>1064-2293</issn><issn>1556-195X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp1UcFuFDEMHSGQKIUP4BaJC4dOsWeSmQy3qioUqYjDUonbKJN1dlNl4yGZVbV_T5YFCYGwD7bs956e7Kp6jXCJ2Mp3K4RONs3QYgsKoFFPqjNUqqtxUN-elr6s6-P-efUi5weAVmupz6rHFfuQBTuxbElETqWkKGaTlt_D1X6aOZgk7pMJ-b34zGnecuDN4ULM20P2lu2Wdt6aIObEM6XFU74QJq6FNWni-LONfkm8oaLNHPLL6pkravTqVz2v7j_cfL2-re--fPx0fXVXG4m41Kp3ZMn2Bt3aQq-cNdNEjZZWDQbJ9U2DYGHdKZhQWgKU4JCGVnfaghva8-rtSbc4-76nvIw7ny2FYCLxPo8olVbNoAdZoG_-gj7wPsXibsRWSRigREFdnlAbE2j00fGSjC25Pp6AIzlf5ld9gxqg010h4IlgE-ecyI1z8juTDiPCePzd-M_vCqc5cXLBxg2lP6z8l_QDOiibyQ</recordid><startdate>20130501</startdate><enddate>20130501</enddate><creator>Dymov, A. 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V.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a411t-57fecec7a1fdc075fcabbe284c59a1ef72210c0d650b14ce0140f1e93868c0f93</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>Analysis</topic><topic>Carbon</topic><topic>Carbon content</topic><topic>Decomposing organic matter</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Forest soils</topic><topic>Genesis and Geography of Soils</topic><topic>Geotechnical Engineering & Applied Earth Sciences</topic><topic>Humus</topic><topic>Morphology</topic><topic>Mountains</topic><topic>Nitrogen</topic><topic>Organic carbon</topic><topic>Peat</topic><topic>Permafrost</topic><topic>Physicochemical properties</topic><topic>Podzols</topic><topic>Soil profiles</topic><topic>Soil sciences</topic><topic>Soil types</topic><topic>Soils</topic><topic>Taiga & tundra</topic><topic>Tundra</topic><topic>Tundra ecology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Dymov, A. 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A.</au><au>Zhangurov, E. V.</au><au>Startsev, V. V.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Soils of the northern part of the Subpolar Urals: Morphology, physicochemical properties, and carbon and nitrogen pools</atitle><jtitle>Eurasian soil science</jtitle><stitle>Eurasian Soil Sc</stitle><date>2013-05-01</date><risdate>2013</risdate><volume>46</volume><issue>5</issue><spage>459</spage><epage>467</epage><pages>459-467</pages><issn>1064-2293</issn><eissn>1556-195X</eissn><abstract>The morphology and physicochemical properties of mountain-tundra and mountain-forest soils of the Subpolar Urals are analyzed. Gleyic humus-illuvial podburs, in combination with humus-illuvial podburs and raw-humus gleyzems, predominate in the mountain-tundra zone; permafrost-affected gleyzems and peat gleyzems with a shallow (30–50 cm) permafrost table are developed on colluvial fans at the foots-lopes. Iron-illuvial podzols, iron-illuvial svetlozems, eluviated burozems, texture-differentiated podzolic soils with a microprofile of a podzol, and gleyed peat-podzolic soils occur in the mountain-forest zone. The organic carbon and nitrogen pools in the soils considerably vary depending on the soil type and local landscape conditions. The organic carbon pool stored in the upper 50 cm of the soil profile varies from 7.7 to 39.3 kg/m
2
in the mountain-tundra soils and from 6.5 to 11.8 kg/m
2
in the mountain-forest soils. The corresponding values for the nitrogen pool are 0.4–2.4 and 0.4–0.8 kg/m
2
, respectively.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S1064229313050025</doi><tpages>9</tpages></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 1064-2293 |
| ispartof | Eurasian soil science, 2013-05, Vol.46 (5), p.459-467 |
| issn | 1064-2293 1556-195X |
| language | eng |
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| source | Springer Online Journals |
| subjects | Analysis Carbon Carbon content Decomposing organic matter Earth and Environmental Science Earth Sciences Forest soils Genesis and Geography of Soils Geotechnical Engineering & Applied Earth Sciences Humus Morphology Mountains Nitrogen Organic carbon Peat Permafrost Physicochemical properties Podzols Soil profiles Soil sciences Soil types Soils Taiga & tundra Tundra Tundra ecology |
| title | Soils of the northern part of the Subpolar Urals: Morphology, physicochemical properties, and carbon and nitrogen pools |
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