Morphological-genetic characterization of soils on the Enganepe Ridge

Abstract Specific features of the soil formation in the Polar Urals related to the slope aspects, parent rocks, and vegetation are considered using the example of the Enganepe Ridge. Soils of the same type (humus-illuvial podburs and podzolized podburs) are formed under the severe climatic condition...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Dymov, A. A. [verfasserIn] Zhangurov, E. V.

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2011

Schlagwörter:	Humus EURASIAN Soil Science Southern Slope Parent Rock Slope Aspect

Anmerkung:	© Pleiades Publishing, Ltd. 2011

Übergeordnetes Werk:	Enthalten in: Eurasian soil science - Moscow : MAIK Nauka/Interperiodica Publ., 1996, 44(2011), 5 vom: 20. Mai
Übergeordnetes Werk:	volume:44 ; year:2011 ; number:5 ; day:20 ; month:05

Links:	Volltext

DOI / URN:	10.1134/S1064229311050048

Katalog-ID:	SPR019953569

Internformat


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520			\|a Abstract Specific features of the soil formation in the Polar Urals related to the slope aspects, parent rocks, and vegetation are considered using the example of the Enganepe Ridge. Soils of the same type (humus-illuvial podburs and podzolized podburs) are formed under the severe climatic conditions of the mountain tundra belt irrespective of the slope aspect. The main differences in the prevalent soils are manifested in the mountain belt of sparse forests. Under the sparse larch forests on the southeast-facing slope, illuvial-humus-iron podzols predominate. On the south-facing slope under the sparse spruce forests, clay-illuviated illuvialhumus-iron podzols alternate with mucky-dark humus soddy lithozems. Burozems are formed in a few ecological niches. The richness of the parent rocks, along with the southern slope aspect and the transitional-accumulative nutrient transfer, is shown to promote the formation of sparse spruce forests under the climatic conditions of the Polar Urals.
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912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_152
912			\|a GBV_ILN_161
912			\|a GBV_ILN_170
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912			\|a GBV_ILN_187
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allfields	10.1134/S1064229311050048 doi (DE-627)SPR019953569 (SPR)S1064229311050048-e DE-627 ger DE-627 rakwb eng Dymov, A. A. verfasserin aut Morphological-genetic characterization of soils on the Enganepe Ridge 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract Specific features of the soil formation in the Polar Urals related to the slope aspects, parent rocks, and vegetation are considered using the example of the Enganepe Ridge. Soils of the same type (humus-illuvial podburs and podzolized podburs) are formed under the severe climatic conditions of the mountain tundra belt irrespective of the slope aspect. The main differences in the prevalent soils are manifested in the mountain belt of sparse forests. Under the sparse larch forests on the southeast-facing slope, illuvial-humus-iron podzols predominate. On the south-facing slope under the sparse spruce forests, clay-illuviated illuvialhumus-iron podzols alternate with mucky-dark humus soddy lithozems. Burozems are formed in a few ecological niches. The richness of the parent rocks, along with the southern slope aspect and the transitional-accumulative nutrient transfer, is shown to promote the formation of sparse spruce forests under the climatic conditions of the Polar Urals. Humus (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Southern Slope (dpeaa)DE-He213 Parent Rock (dpeaa)DE-He213 Slope Aspect (dpeaa)DE-He213 Zhangurov, E. V. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 5 vom: 20. Mai (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:5 day:20 month:05 https://dx.doi.org/10.1134/S1064229311050048 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2011 5 20 05
spelling	10.1134/S1064229311050048 doi (DE-627)SPR019953569 (SPR)S1064229311050048-e DE-627 ger DE-627 rakwb eng Dymov, A. A. verfasserin aut Morphological-genetic characterization of soils on the Enganepe Ridge 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract Specific features of the soil formation in the Polar Urals related to the slope aspects, parent rocks, and vegetation are considered using the example of the Enganepe Ridge. Soils of the same type (humus-illuvial podburs and podzolized podburs) are formed under the severe climatic conditions of the mountain tundra belt irrespective of the slope aspect. The main differences in the prevalent soils are manifested in the mountain belt of sparse forests. Under the sparse larch forests on the southeast-facing slope, illuvial-humus-iron podzols predominate. On the south-facing slope under the sparse spruce forests, clay-illuviated illuvialhumus-iron podzols alternate with mucky-dark humus soddy lithozems. Burozems are formed in a few ecological niches. The richness of the parent rocks, along with the southern slope aspect and the transitional-accumulative nutrient transfer, is shown to promote the formation of sparse spruce forests under the climatic conditions of the Polar Urals. Humus (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Southern Slope (dpeaa)DE-He213 Parent Rock (dpeaa)DE-He213 Slope Aspect (dpeaa)DE-He213 Zhangurov, E. V. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 5 vom: 20. Mai (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:5 day:20 month:05 https://dx.doi.org/10.1134/S1064229311050048 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2011 5 20 05
allfields_unstemmed	10.1134/S1064229311050048 doi (DE-627)SPR019953569 (SPR)S1064229311050048-e DE-627 ger DE-627 rakwb eng Dymov, A. A. verfasserin aut Morphological-genetic characterization of soils on the Enganepe Ridge 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract Specific features of the soil formation in the Polar Urals related to the slope aspects, parent rocks, and vegetation are considered using the example of the Enganepe Ridge. Soils of the same type (humus-illuvial podburs and podzolized podburs) are formed under the severe climatic conditions of the mountain tundra belt irrespective of the slope aspect. The main differences in the prevalent soils are manifested in the mountain belt of sparse forests. Under the sparse larch forests on the southeast-facing slope, illuvial-humus-iron podzols predominate. On the south-facing slope under the sparse spruce forests, clay-illuviated illuvialhumus-iron podzols alternate with mucky-dark humus soddy lithozems. Burozems are formed in a few ecological niches. The richness of the parent rocks, along with the southern slope aspect and the transitional-accumulative nutrient transfer, is shown to promote the formation of sparse spruce forests under the climatic conditions of the Polar Urals. Humus (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Southern Slope (dpeaa)DE-He213 Parent Rock (dpeaa)DE-He213 Slope Aspect (dpeaa)DE-He213 Zhangurov, E. V. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 5 vom: 20. Mai (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:5 day:20 month:05 https://dx.doi.org/10.1134/S1064229311050048 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2011 5 20 05
allfieldsGer	10.1134/S1064229311050048 doi (DE-627)SPR019953569 (SPR)S1064229311050048-e DE-627 ger DE-627 rakwb eng Dymov, A. A. verfasserin aut Morphological-genetic characterization of soils on the Enganepe Ridge 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract Specific features of the soil formation in the Polar Urals related to the slope aspects, parent rocks, and vegetation are considered using the example of the Enganepe Ridge. Soils of the same type (humus-illuvial podburs and podzolized podburs) are formed under the severe climatic conditions of the mountain tundra belt irrespective of the slope aspect. The main differences in the prevalent soils are manifested in the mountain belt of sparse forests. Under the sparse larch forests on the southeast-facing slope, illuvial-humus-iron podzols predominate. On the south-facing slope under the sparse spruce forests, clay-illuviated illuvialhumus-iron podzols alternate with mucky-dark humus soddy lithozems. Burozems are formed in a few ecological niches. The richness of the parent rocks, along with the southern slope aspect and the transitional-accumulative nutrient transfer, is shown to promote the formation of sparse spruce forests under the climatic conditions of the Polar Urals. Humus (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Southern Slope (dpeaa)DE-He213 Parent Rock (dpeaa)DE-He213 Slope Aspect (dpeaa)DE-He213 Zhangurov, E. V. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 5 vom: 20. Mai (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:5 day:20 month:05 https://dx.doi.org/10.1134/S1064229311050048 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2011 5 20 05
allfieldsSound	10.1134/S1064229311050048 doi (DE-627)SPR019953569 (SPR)S1064229311050048-e DE-627 ger DE-627 rakwb eng Dymov, A. A. verfasserin aut Morphological-genetic characterization of soils on the Enganepe Ridge 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract Specific features of the soil formation in the Polar Urals related to the slope aspects, parent rocks, and vegetation are considered using the example of the Enganepe Ridge. Soils of the same type (humus-illuvial podburs and podzolized podburs) are formed under the severe climatic conditions of the mountain tundra belt irrespective of the slope aspect. The main differences in the prevalent soils are manifested in the mountain belt of sparse forests. Under the sparse larch forests on the southeast-facing slope, illuvial-humus-iron podzols predominate. On the south-facing slope under the sparse spruce forests, clay-illuviated illuvialhumus-iron podzols alternate with mucky-dark humus soddy lithozems. Burozems are formed in a few ecological niches. The richness of the parent rocks, along with the southern slope aspect and the transitional-accumulative nutrient transfer, is shown to promote the formation of sparse spruce forests under the climatic conditions of the Polar Urals. Humus (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Southern Slope (dpeaa)DE-He213 Parent Rock (dpeaa)DE-He213 Slope Aspect (dpeaa)DE-He213 Zhangurov, E. V. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 5 vom: 20. Mai (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:5 day:20 month:05 https://dx.doi.org/10.1134/S1064229311050048 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2011 5 20 05
language	English
source	Enthalten in Eurasian soil science 44(2011), 5 vom: 20. Mai volume:44 year:2011 number:5 day:20 month:05
sourceStr	Enthalten in Eurasian soil science 44(2011), 5 vom: 20. Mai volume:44 year:2011 number:5 day:20 month:05
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Humus EURASIAN Soil Science Southern Slope Parent Rock Slope Aspect
isfreeaccess_bool	false
container_title	Eurasian soil science
authorswithroles_txt_mv	Dymov, A. A. @@aut@@ Zhangurov, E. V. @@aut@@
publishDateDaySort_date	2011-05-20T00:00:00Z
hierarchy_top_id	341913227
id	SPR019953569
language_de	englisch
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author	Dymov, A. A.
spellingShingle	Dymov, A. A. misc Humus misc EURASIAN Soil Science misc Southern Slope misc Parent Rock misc Slope Aspect Morphological-genetic characterization of soils on the Enganepe Ridge
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topic_title	Morphological-genetic characterization of soils on the Enganepe Ridge Humus (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Southern Slope (dpeaa)DE-He213 Parent Rock (dpeaa)DE-He213 Slope Aspect (dpeaa)DE-He213
topic	misc Humus misc EURASIAN Soil Science misc Southern Slope misc Parent Rock misc Slope Aspect
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title	Morphological-genetic characterization of soils on the Enganepe Ridge
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title_full	Morphological-genetic characterization of soils on the Enganepe Ridge
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author_browse	Dymov, A. A. Zhangurov, E. V.
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title_sort	morphological-genetic characterization of soils on the enganepe ridge
title_auth	Morphological-genetic characterization of soils on the Enganepe Ridge
abstract	Abstract Specific features of the soil formation in the Polar Urals related to the slope aspects, parent rocks, and vegetation are considered using the example of the Enganepe Ridge. Soils of the same type (humus-illuvial podburs and podzolized podburs) are formed under the severe climatic conditions of the mountain tundra belt irrespective of the slope aspect. The main differences in the prevalent soils are manifested in the mountain belt of sparse forests. Under the sparse larch forests on the southeast-facing slope, illuvial-humus-iron podzols predominate. On the south-facing slope under the sparse spruce forests, clay-illuviated illuvialhumus-iron podzols alternate with mucky-dark humus soddy lithozems. Burozems are formed in a few ecological niches. The richness of the parent rocks, along with the southern slope aspect and the transitional-accumulative nutrient transfer, is shown to promote the formation of sparse spruce forests under the climatic conditions of the Polar Urals. © Pleiades Publishing, Ltd. 2011
abstractGer	Abstract Specific features of the soil formation in the Polar Urals related to the slope aspects, parent rocks, and vegetation are considered using the example of the Enganepe Ridge. Soils of the same type (humus-illuvial podburs and podzolized podburs) are formed under the severe climatic conditions of the mountain tundra belt irrespective of the slope aspect. The main differences in the prevalent soils are manifested in the mountain belt of sparse forests. Under the sparse larch forests on the southeast-facing slope, illuvial-humus-iron podzols predominate. On the south-facing slope under the sparse spruce forests, clay-illuviated illuvialhumus-iron podzols alternate with mucky-dark humus soddy lithozems. Burozems are formed in a few ecological niches. The richness of the parent rocks, along with the southern slope aspect and the transitional-accumulative nutrient transfer, is shown to promote the formation of sparse spruce forests under the climatic conditions of the Polar Urals. © Pleiades Publishing, Ltd. 2011
abstract_unstemmed	Abstract Specific features of the soil formation in the Polar Urals related to the slope aspects, parent rocks, and vegetation are considered using the example of the Enganepe Ridge. Soils of the same type (humus-illuvial podburs and podzolized podburs) are formed under the severe climatic conditions of the mountain tundra belt irrespective of the slope aspect. The main differences in the prevalent soils are manifested in the mountain belt of sparse forests. Under the sparse larch forests on the southeast-facing slope, illuvial-humus-iron podzols predominate. On the south-facing slope under the sparse spruce forests, clay-illuviated illuvialhumus-iron podzols alternate with mucky-dark humus soddy lithozems. Burozems are formed in a few ecological niches. The richness of the parent rocks, along with the southern slope aspect and the transitional-accumulative nutrient transfer, is shown to promote the formation of sparse spruce forests under the climatic conditions of the Polar Urals. © Pleiades Publishing, Ltd. 2011
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title_short	Morphological-genetic characterization of soils on the Enganepe Ridge
url	https://dx.doi.org/10.1134/S1064229311050048
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up_date	2024-07-04T03:26:57.972Z
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Morphological-genetic characterization of soils on the Enganepe Ridge

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