Soil Carbon in the Forests of Russia
Abstract The 50% variation in the estimates of carbon (C) content in the forest soils of Russia at present is caused by confusion of terms and ignorance of the soil geographical representativeness in forests. The GIS-based analysis closes the gap to the estimate published earlier by Alexeyev and Bir...
Ausführliche Beschreibung
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| Autor*in: |
Stolbovoi, Vladimir [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2006 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer Science + Business Media, Inc. 2006 |
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| Übergeordnetes Werk: |
Enthalten in: Mitigation and adaptation strategies for global change - Springer Netherlands, 1996, 11(2006), 1 vom: 01. Jan., Seite 203-222 |
|---|---|
| Übergeordnetes Werk: |
volume:11 ; year:2006 ; number:1 ; day:01 ; month:01 ; pages:203-222 |
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| DOI / URN: |
10.1007/s11027-006-1021-7 |
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OLC2047794021 |
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| 520 | |a Abstract The 50% variation in the estimates of carbon (C) content in the forest soils of Russia at present is caused by confusion of terms and ignorance of the soil geographical representativeness in forests. The GIS-based analysis closes the gap to the estimate published earlier by Alexeyev and Birdsey (1994, p. 170). The average soil carbon density (SCD) for the 0.3 meter (m) layer of the forest soils in Russia is about 8.1 kg C $ m^{−2} $; the 1 m layer captures some 11.4 kg C $ m^{−2} $; and the 2 m layer holds nearly 12.3 kg C $ m^{− 2} $. The mass of C is about 61.6 Pg C concentrated in the 0.3 m layer of forest soils; the 1 m layer accumulates 87.6 Pg C and the 2 m layer holds about 94.1 Pg C. The C content in soils of the forest zone is much higher for Russia. The SCD is 18.8 kg C $ m^{− 2} $ and the soil C pool (SCP) is 223.6 Pg C in 1 m layer. Peat soils contribute a considerable portion of C to the forest zone of the country. The cold climate, permafrost and vegetation residues that are rich in recalcitrant compounds support a high accumulation rate of organic matter and associated nutrients in soils. This conservation is a mechanism to keep the production potential of the boreal ecosystems high in spite of their relatively low actual productivity in present environments. | ||
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10.1007/s11027-006-1021-7 doi (DE-627)OLC2047794021 (DE-He213)s11027-006-1021-7-p DE-627 ger DE-627 rakwb eng 333.7 690 VZ Stolbovoi, Vladimir verfasserin aut Soil Carbon in the Forests of Russia 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science + Business Media, Inc. 2006 Abstract The 50% variation in the estimates of carbon (C) content in the forest soils of Russia at present is caused by confusion of terms and ignorance of the soil geographical representativeness in forests. The GIS-based analysis closes the gap to the estimate published earlier by Alexeyev and Birdsey (1994, p. 170). The average soil carbon density (SCD) for the 0.3 meter (m) layer of the forest soils in Russia is about 8.1 kg C $ m^{−2} $; the 1 m layer captures some 11.4 kg C $ m^{−2} $; and the 2 m layer holds nearly 12.3 kg C $ m^{− 2} $. The mass of C is about 61.6 Pg C concentrated in the 0.3 m layer of forest soils; the 1 m layer accumulates 87.6 Pg C and the 2 m layer holds about 94.1 Pg C. The C content in soils of the forest zone is much higher for Russia. The SCD is 18.8 kg C $ m^{− 2} $ and the soil C pool (SCP) is 223.6 Pg C in 1 m layer. Peat soils contribute a considerable portion of C to the forest zone of the country. The cold climate, permafrost and vegetation residues that are rich in recalcitrant compounds support a high accumulation rate of organic matter and associated nutrients in soils. This conservation is a mechanism to keep the production potential of the boreal ecosystems high in spite of their relatively low actual productivity in present environments. boreal forest carbon soil Enthalten in Mitigation and adaptation strategies for global change Springer Netherlands, 1996 11(2006), 1 vom: 01. Jan., Seite 203-222 (DE-627)216535506 (DE-600)1339119-7 (DE-576)252453298 1381-2386 nnns volume:11 year:2006 number:1 day:01 month:01 pages:203-222 https://doi.org/10.1007/s11027-006-1021-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-FOR SSG-OLC-WIW GBV_ILN_26 GBV_ILN_601 GBV_ILN_4012 AR 11 2006 1 01 01 203-222 |
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10.1007/s11027-006-1021-7 doi (DE-627)OLC2047794021 (DE-He213)s11027-006-1021-7-p DE-627 ger DE-627 rakwb eng 333.7 690 VZ Stolbovoi, Vladimir verfasserin aut Soil Carbon in the Forests of Russia 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science + Business Media, Inc. 2006 Abstract The 50% variation in the estimates of carbon (C) content in the forest soils of Russia at present is caused by confusion of terms and ignorance of the soil geographical representativeness in forests. The GIS-based analysis closes the gap to the estimate published earlier by Alexeyev and Birdsey (1994, p. 170). The average soil carbon density (SCD) for the 0.3 meter (m) layer of the forest soils in Russia is about 8.1 kg C $ m^{−2} $; the 1 m layer captures some 11.4 kg C $ m^{−2} $; and the 2 m layer holds nearly 12.3 kg C $ m^{− 2} $. The mass of C is about 61.6 Pg C concentrated in the 0.3 m layer of forest soils; the 1 m layer accumulates 87.6 Pg C and the 2 m layer holds about 94.1 Pg C. The C content in soils of the forest zone is much higher for Russia. The SCD is 18.8 kg C $ m^{− 2} $ and the soil C pool (SCP) is 223.6 Pg C in 1 m layer. Peat soils contribute a considerable portion of C to the forest zone of the country. The cold climate, permafrost and vegetation residues that are rich in recalcitrant compounds support a high accumulation rate of organic matter and associated nutrients in soils. This conservation is a mechanism to keep the production potential of the boreal ecosystems high in spite of their relatively low actual productivity in present environments. boreal forest carbon soil Enthalten in Mitigation and adaptation strategies for global change Springer Netherlands, 1996 11(2006), 1 vom: 01. Jan., Seite 203-222 (DE-627)216535506 (DE-600)1339119-7 (DE-576)252453298 1381-2386 nnns volume:11 year:2006 number:1 day:01 month:01 pages:203-222 https://doi.org/10.1007/s11027-006-1021-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-FOR SSG-OLC-WIW GBV_ILN_26 GBV_ILN_601 GBV_ILN_4012 AR 11 2006 1 01 01 203-222 |
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10.1007/s11027-006-1021-7 doi (DE-627)OLC2047794021 (DE-He213)s11027-006-1021-7-p DE-627 ger DE-627 rakwb eng 333.7 690 VZ Stolbovoi, Vladimir verfasserin aut Soil Carbon in the Forests of Russia 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science + Business Media, Inc. 2006 Abstract The 50% variation in the estimates of carbon (C) content in the forest soils of Russia at present is caused by confusion of terms and ignorance of the soil geographical representativeness in forests. The GIS-based analysis closes the gap to the estimate published earlier by Alexeyev and Birdsey (1994, p. 170). The average soil carbon density (SCD) for the 0.3 meter (m) layer of the forest soils in Russia is about 8.1 kg C $ m^{−2} $; the 1 m layer captures some 11.4 kg C $ m^{−2} $; and the 2 m layer holds nearly 12.3 kg C $ m^{− 2} $. The mass of C is about 61.6 Pg C concentrated in the 0.3 m layer of forest soils; the 1 m layer accumulates 87.6 Pg C and the 2 m layer holds about 94.1 Pg C. The C content in soils of the forest zone is much higher for Russia. The SCD is 18.8 kg C $ m^{− 2} $ and the soil C pool (SCP) is 223.6 Pg C in 1 m layer. Peat soils contribute a considerable portion of C to the forest zone of the country. The cold climate, permafrost and vegetation residues that are rich in recalcitrant compounds support a high accumulation rate of organic matter and associated nutrients in soils. This conservation is a mechanism to keep the production potential of the boreal ecosystems high in spite of their relatively low actual productivity in present environments. boreal forest carbon soil Enthalten in Mitigation and adaptation strategies for global change Springer Netherlands, 1996 11(2006), 1 vom: 01. Jan., Seite 203-222 (DE-627)216535506 (DE-600)1339119-7 (DE-576)252453298 1381-2386 nnns volume:11 year:2006 number:1 day:01 month:01 pages:203-222 https://doi.org/10.1007/s11027-006-1021-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-FOR SSG-OLC-WIW GBV_ILN_26 GBV_ILN_601 GBV_ILN_4012 AR 11 2006 1 01 01 203-222 |
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10.1007/s11027-006-1021-7 doi (DE-627)OLC2047794021 (DE-He213)s11027-006-1021-7-p DE-627 ger DE-627 rakwb eng 333.7 690 VZ Stolbovoi, Vladimir verfasserin aut Soil Carbon in the Forests of Russia 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science + Business Media, Inc. 2006 Abstract The 50% variation in the estimates of carbon (C) content in the forest soils of Russia at present is caused by confusion of terms and ignorance of the soil geographical representativeness in forests. The GIS-based analysis closes the gap to the estimate published earlier by Alexeyev and Birdsey (1994, p. 170). The average soil carbon density (SCD) for the 0.3 meter (m) layer of the forest soils in Russia is about 8.1 kg C $ m^{−2} $; the 1 m layer captures some 11.4 kg C $ m^{−2} $; and the 2 m layer holds nearly 12.3 kg C $ m^{− 2} $. The mass of C is about 61.6 Pg C concentrated in the 0.3 m layer of forest soils; the 1 m layer accumulates 87.6 Pg C and the 2 m layer holds about 94.1 Pg C. The C content in soils of the forest zone is much higher for Russia. The SCD is 18.8 kg C $ m^{− 2} $ and the soil C pool (SCP) is 223.6 Pg C in 1 m layer. Peat soils contribute a considerable portion of C to the forest zone of the country. The cold climate, permafrost and vegetation residues that are rich in recalcitrant compounds support a high accumulation rate of organic matter and associated nutrients in soils. This conservation is a mechanism to keep the production potential of the boreal ecosystems high in spite of their relatively low actual productivity in present environments. boreal forest carbon soil Enthalten in Mitigation and adaptation strategies for global change Springer Netherlands, 1996 11(2006), 1 vom: 01. Jan., Seite 203-222 (DE-627)216535506 (DE-600)1339119-7 (DE-576)252453298 1381-2386 nnns volume:11 year:2006 number:1 day:01 month:01 pages:203-222 https://doi.org/10.1007/s11027-006-1021-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-FOR SSG-OLC-WIW GBV_ILN_26 GBV_ILN_601 GBV_ILN_4012 AR 11 2006 1 01 01 203-222 |
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10.1007/s11027-006-1021-7 doi (DE-627)OLC2047794021 (DE-He213)s11027-006-1021-7-p DE-627 ger DE-627 rakwb eng 333.7 690 VZ Stolbovoi, Vladimir verfasserin aut Soil Carbon in the Forests of Russia 2006 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer Science + Business Media, Inc. 2006 Abstract The 50% variation in the estimates of carbon (C) content in the forest soils of Russia at present is caused by confusion of terms and ignorance of the soil geographical representativeness in forests. The GIS-based analysis closes the gap to the estimate published earlier by Alexeyev and Birdsey (1994, p. 170). The average soil carbon density (SCD) for the 0.3 meter (m) layer of the forest soils in Russia is about 8.1 kg C $ m^{−2} $; the 1 m layer captures some 11.4 kg C $ m^{−2} $; and the 2 m layer holds nearly 12.3 kg C $ m^{− 2} $. The mass of C is about 61.6 Pg C concentrated in the 0.3 m layer of forest soils; the 1 m layer accumulates 87.6 Pg C and the 2 m layer holds about 94.1 Pg C. The C content in soils of the forest zone is much higher for Russia. The SCD is 18.8 kg C $ m^{− 2} $ and the soil C pool (SCP) is 223.6 Pg C in 1 m layer. Peat soils contribute a considerable portion of C to the forest zone of the country. The cold climate, permafrost and vegetation residues that are rich in recalcitrant compounds support a high accumulation rate of organic matter and associated nutrients in soils. This conservation is a mechanism to keep the production potential of the boreal ecosystems high in spite of their relatively low actual productivity in present environments. boreal forest carbon soil Enthalten in Mitigation and adaptation strategies for global change Springer Netherlands, 1996 11(2006), 1 vom: 01. Jan., Seite 203-222 (DE-627)216535506 (DE-600)1339119-7 (DE-576)252453298 1381-2386 nnns volume:11 year:2006 number:1 day:01 month:01 pages:203-222 https://doi.org/10.1007/s11027-006-1021-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-FOR SSG-OLC-WIW GBV_ILN_26 GBV_ILN_601 GBV_ILN_4012 AR 11 2006 1 01 01 203-222 |
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Soil Carbon in the Forests of Russia |
| abstract |
Abstract The 50% variation in the estimates of carbon (C) content in the forest soils of Russia at present is caused by confusion of terms and ignorance of the soil geographical representativeness in forests. The GIS-based analysis closes the gap to the estimate published earlier by Alexeyev and Birdsey (1994, p. 170). The average soil carbon density (SCD) for the 0.3 meter (m) layer of the forest soils in Russia is about 8.1 kg C $ m^{−2} $; the 1 m layer captures some 11.4 kg C $ m^{−2} $; and the 2 m layer holds nearly 12.3 kg C $ m^{− 2} $. The mass of C is about 61.6 Pg C concentrated in the 0.3 m layer of forest soils; the 1 m layer accumulates 87.6 Pg C and the 2 m layer holds about 94.1 Pg C. The C content in soils of the forest zone is much higher for Russia. The SCD is 18.8 kg C $ m^{− 2} $ and the soil C pool (SCP) is 223.6 Pg C in 1 m layer. Peat soils contribute a considerable portion of C to the forest zone of the country. The cold climate, permafrost and vegetation residues that are rich in recalcitrant compounds support a high accumulation rate of organic matter and associated nutrients in soils. This conservation is a mechanism to keep the production potential of the boreal ecosystems high in spite of their relatively low actual productivity in present environments. © Springer Science + Business Media, Inc. 2006 |
| abstractGer |
Abstract The 50% variation in the estimates of carbon (C) content in the forest soils of Russia at present is caused by confusion of terms and ignorance of the soil geographical representativeness in forests. The GIS-based analysis closes the gap to the estimate published earlier by Alexeyev and Birdsey (1994, p. 170). The average soil carbon density (SCD) for the 0.3 meter (m) layer of the forest soils in Russia is about 8.1 kg C $ m^{−2} $; the 1 m layer captures some 11.4 kg C $ m^{−2} $; and the 2 m layer holds nearly 12.3 kg C $ m^{− 2} $. The mass of C is about 61.6 Pg C concentrated in the 0.3 m layer of forest soils; the 1 m layer accumulates 87.6 Pg C and the 2 m layer holds about 94.1 Pg C. The C content in soils of the forest zone is much higher for Russia. The SCD is 18.8 kg C $ m^{− 2} $ and the soil C pool (SCP) is 223.6 Pg C in 1 m layer. Peat soils contribute a considerable portion of C to the forest zone of the country. The cold climate, permafrost and vegetation residues that are rich in recalcitrant compounds support a high accumulation rate of organic matter and associated nutrients in soils. This conservation is a mechanism to keep the production potential of the boreal ecosystems high in spite of their relatively low actual productivity in present environments. © Springer Science + Business Media, Inc. 2006 |
| abstract_unstemmed |
Abstract The 50% variation in the estimates of carbon (C) content in the forest soils of Russia at present is caused by confusion of terms and ignorance of the soil geographical representativeness in forests. The GIS-based analysis closes the gap to the estimate published earlier by Alexeyev and Birdsey (1994, p. 170). The average soil carbon density (SCD) for the 0.3 meter (m) layer of the forest soils in Russia is about 8.1 kg C $ m^{−2} $; the 1 m layer captures some 11.4 kg C $ m^{−2} $; and the 2 m layer holds nearly 12.3 kg C $ m^{− 2} $. The mass of C is about 61.6 Pg C concentrated in the 0.3 m layer of forest soils; the 1 m layer accumulates 87.6 Pg C and the 2 m layer holds about 94.1 Pg C. The C content in soils of the forest zone is much higher for Russia. The SCD is 18.8 kg C $ m^{− 2} $ and the soil C pool (SCP) is 223.6 Pg C in 1 m layer. Peat soils contribute a considerable portion of C to the forest zone of the country. The cold climate, permafrost and vegetation residues that are rich in recalcitrant compounds support a high accumulation rate of organic matter and associated nutrients in soils. This conservation is a mechanism to keep the production potential of the boreal ecosystems high in spite of their relatively low actual productivity in present environments. © Springer Science + Business Media, Inc. 2006 |
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Soil Carbon in the Forests of Russia |
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https://doi.org/10.1007/s11027-006-1021-7 |
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10.1007/s11027-006-1021-7 |
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2024-07-03T16:20:14.969Z |
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