How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools
Abstract In the context of global carbon cycle management, accurate knowledge of carbon content in forests is a relevant issue in contemporary forest ecology. We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated...
Ausführliche Beschreibung
Autor*in: |
Gavrikov, Vladimir L. [verfasserIn] Sharafutdinov, Ruslan A. [verfasserIn] Knorre, Anastasyia A. [verfasserIn] Pakharkova, Nina V. [verfasserIn] Shabalina, Olga M. [verfasserIn] Bezkorovaynaya, Irina N. [verfasserIn] Borisova, Irina V. [verfasserIn] Erunova, Marina G. [verfasserIn] Khlebopros, Rem G. [verfasserIn] |
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Format: |
E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2015 |
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Schlagwörter: |
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Übergeordnetes Werk: |
Enthalten in: Journal of forestry research - Harbin : Univ., 1990, 27(2015), 4 vom: 08. Dez., Seite 907-912 |
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Übergeordnetes Werk: |
volume:27 ; year:2015 ; number:4 ; day:08 ; month:12 ; pages:907-912 |
Links: |
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DOI / URN: |
10.1007/s11676-015-0189-7 |
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Katalog-ID: |
SPR022201513 |
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520 | |a Abstract In the context of global carbon cycle management, accurate knowledge of carbon content in forests is a relevant issue in contemporary forest ecology. We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated from the forest inventory records containing volume stock and species composition data. The inventory data heavily underestimated the pools in the study area (Stolby State Nature Reserve, central Krasnoyarsk Territory, Russian Federation). The carbon pool estimated from the forest inventory data varied from 25 (t $ ha^{−1} $) (low-density stands) to 73 (t $ ha^{−1} $) (highly stocked stands). Our estimates ranged from 59 (t $ ha^{−1} $) (low-density stands) to 147 (t $ ha^{−1} $) (highly stocked stands). Our values included living trees, standing deadwood, living cover, brushwood and litter. We found that the proportion of biomass carbon (living trees): soil carbon varied from 99:1 to 8:2 for fully stocked and low-density forest stands, respectively. This contradicts the common understanding that the biomass in the boreal forests represents only 16–20 % of the total carbon pool, with the balance being the soil carbon pool. | ||
650 | 4 | |a Boreal taiga |7 (dpeaa)DE-He213 | |
650 | 4 | |a Biomass |7 (dpeaa)DE-He213 | |
650 | 4 | |a Soil |7 (dpeaa)DE-He213 | |
650 | 4 | |a Carbon pool |7 (dpeaa)DE-He213 | |
700 | 1 | |a Sharafutdinov, Ruslan A. |e verfasserin |4 aut | |
700 | 1 | |a Knorre, Anastasyia A. |e verfasserin |4 aut | |
700 | 1 | |a Pakharkova, Nina V. |e verfasserin |4 aut | |
700 | 1 | |a Shabalina, Olga M. |e verfasserin |4 aut | |
700 | 1 | |a Bezkorovaynaya, Irina N. |e verfasserin |4 aut | |
700 | 1 | |a Borisova, Irina V. |e verfasserin |4 aut | |
700 | 1 | |a Erunova, Marina G. |e verfasserin |4 aut | |
700 | 1 | |a Khlebopros, Rem G. |e verfasserin |4 aut | |
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10.1007/s11676-015-0189-7 doi (DE-627)SPR022201513 (SPR)s11676-015-0189-7-e DE-627 ger DE-627 rakwb eng 630 640 ASE Gavrikov, Vladimir L. verfasserin aut How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In the context of global carbon cycle management, accurate knowledge of carbon content in forests is a relevant issue in contemporary forest ecology. We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated from the forest inventory records containing volume stock and species composition data. The inventory data heavily underestimated the pools in the study area (Stolby State Nature Reserve, central Krasnoyarsk Territory, Russian Federation). The carbon pool estimated from the forest inventory data varied from 25 (t $ ha^{−1} $) (low-density stands) to 73 (t $ ha^{−1} $) (highly stocked stands). Our estimates ranged from 59 (t $ ha^{−1} $) (low-density stands) to 147 (t $ ha^{−1} $) (highly stocked stands). Our values included living trees, standing deadwood, living cover, brushwood and litter. We found that the proportion of biomass carbon (living trees): soil carbon varied from 99:1 to 8:2 for fully stocked and low-density forest stands, respectively. This contradicts the common understanding that the biomass in the boreal forests represents only 16–20 % of the total carbon pool, with the balance being the soil carbon pool. Boreal taiga (dpeaa)DE-He213 Biomass (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Carbon pool (dpeaa)DE-He213 Sharafutdinov, Ruslan A. verfasserin aut Knorre, Anastasyia A. verfasserin aut Pakharkova, Nina V. verfasserin aut Shabalina, Olga M. verfasserin aut Bezkorovaynaya, Irina N. verfasserin aut Borisova, Irina V. verfasserin aut Erunova, Marina G. verfasserin aut Khlebopros, Rem G. verfasserin aut Enthalten in Journal of forestry research Harbin : Univ., 1990 27(2015), 4 vom: 08. Dez., Seite 907-912 (DE-627)529093545 (DE-600)2299615-1 1993-0607 nnns volume:27 year:2015 number:4 day:08 month:12 pages:907-912 https://dx.doi.org/10.1007/s11676-015-0189-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE 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_121 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_206 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_374 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 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_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2036 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_2056 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_2700 GBV_ILN_2817 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 AR 27 2015 4 08 12 907-912 |
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10.1007/s11676-015-0189-7 doi (DE-627)SPR022201513 (SPR)s11676-015-0189-7-e DE-627 ger DE-627 rakwb eng 630 640 ASE Gavrikov, Vladimir L. verfasserin aut How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In the context of global carbon cycle management, accurate knowledge of carbon content in forests is a relevant issue in contemporary forest ecology. We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated from the forest inventory records containing volume stock and species composition data. The inventory data heavily underestimated the pools in the study area (Stolby State Nature Reserve, central Krasnoyarsk Territory, Russian Federation). The carbon pool estimated from the forest inventory data varied from 25 (t $ ha^{−1} $) (low-density stands) to 73 (t $ ha^{−1} $) (highly stocked stands). Our estimates ranged from 59 (t $ ha^{−1} $) (low-density stands) to 147 (t $ ha^{−1} $) (highly stocked stands). Our values included living trees, standing deadwood, living cover, brushwood and litter. We found that the proportion of biomass carbon (living trees): soil carbon varied from 99:1 to 8:2 for fully stocked and low-density forest stands, respectively. This contradicts the common understanding that the biomass in the boreal forests represents only 16–20 % of the total carbon pool, with the balance being the soil carbon pool. Boreal taiga (dpeaa)DE-He213 Biomass (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Carbon pool (dpeaa)DE-He213 Sharafutdinov, Ruslan A. verfasserin aut Knorre, Anastasyia A. verfasserin aut Pakharkova, Nina V. verfasserin aut Shabalina, Olga M. verfasserin aut Bezkorovaynaya, Irina N. verfasserin aut Borisova, Irina V. verfasserin aut Erunova, Marina G. verfasserin aut Khlebopros, Rem G. verfasserin aut Enthalten in Journal of forestry research Harbin : Univ., 1990 27(2015), 4 vom: 08. Dez., Seite 907-912 (DE-627)529093545 (DE-600)2299615-1 1993-0607 nnns volume:27 year:2015 number:4 day:08 month:12 pages:907-912 https://dx.doi.org/10.1007/s11676-015-0189-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE 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_121 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_206 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_374 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 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_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2036 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_2056 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_2700 GBV_ILN_2817 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 AR 27 2015 4 08 12 907-912 |
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10.1007/s11676-015-0189-7 doi (DE-627)SPR022201513 (SPR)s11676-015-0189-7-e DE-627 ger DE-627 rakwb eng 630 640 ASE Gavrikov, Vladimir L. verfasserin aut How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In the context of global carbon cycle management, accurate knowledge of carbon content in forests is a relevant issue in contemporary forest ecology. We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated from the forest inventory records containing volume stock and species composition data. The inventory data heavily underestimated the pools in the study area (Stolby State Nature Reserve, central Krasnoyarsk Territory, Russian Federation). The carbon pool estimated from the forest inventory data varied from 25 (t $ ha^{−1} $) (low-density stands) to 73 (t $ ha^{−1} $) (highly stocked stands). Our estimates ranged from 59 (t $ ha^{−1} $) (low-density stands) to 147 (t $ ha^{−1} $) (highly stocked stands). Our values included living trees, standing deadwood, living cover, brushwood and litter. We found that the proportion of biomass carbon (living trees): soil carbon varied from 99:1 to 8:2 for fully stocked and low-density forest stands, respectively. This contradicts the common understanding that the biomass in the boreal forests represents only 16–20 % of the total carbon pool, with the balance being the soil carbon pool. Boreal taiga (dpeaa)DE-He213 Biomass (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Carbon pool (dpeaa)DE-He213 Sharafutdinov, Ruslan A. verfasserin aut Knorre, Anastasyia A. verfasserin aut Pakharkova, Nina V. verfasserin aut Shabalina, Olga M. verfasserin aut Bezkorovaynaya, Irina N. verfasserin aut Borisova, Irina V. verfasserin aut Erunova, Marina G. verfasserin aut Khlebopros, Rem G. verfasserin aut Enthalten in Journal of forestry research Harbin : Univ., 1990 27(2015), 4 vom: 08. Dez., Seite 907-912 (DE-627)529093545 (DE-600)2299615-1 1993-0607 nnns volume:27 year:2015 number:4 day:08 month:12 pages:907-912 https://dx.doi.org/10.1007/s11676-015-0189-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE 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_121 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_206 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_374 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 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_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2036 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_2056 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_2700 GBV_ILN_2817 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 AR 27 2015 4 08 12 907-912 |
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10.1007/s11676-015-0189-7 doi (DE-627)SPR022201513 (SPR)s11676-015-0189-7-e DE-627 ger DE-627 rakwb eng 630 640 ASE Gavrikov, Vladimir L. verfasserin aut How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In the context of global carbon cycle management, accurate knowledge of carbon content in forests is a relevant issue in contemporary forest ecology. We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated from the forest inventory records containing volume stock and species composition data. The inventory data heavily underestimated the pools in the study area (Stolby State Nature Reserve, central Krasnoyarsk Territory, Russian Federation). The carbon pool estimated from the forest inventory data varied from 25 (t $ ha^{−1} $) (low-density stands) to 73 (t $ ha^{−1} $) (highly stocked stands). Our estimates ranged from 59 (t $ ha^{−1} $) (low-density stands) to 147 (t $ ha^{−1} $) (highly stocked stands). Our values included living trees, standing deadwood, living cover, brushwood and litter. We found that the proportion of biomass carbon (living trees): soil carbon varied from 99:1 to 8:2 for fully stocked and low-density forest stands, respectively. This contradicts the common understanding that the biomass in the boreal forests represents only 16–20 % of the total carbon pool, with the balance being the soil carbon pool. Boreal taiga (dpeaa)DE-He213 Biomass (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Carbon pool (dpeaa)DE-He213 Sharafutdinov, Ruslan A. verfasserin aut Knorre, Anastasyia A. verfasserin aut Pakharkova, Nina V. verfasserin aut Shabalina, Olga M. verfasserin aut Bezkorovaynaya, Irina N. verfasserin aut Borisova, Irina V. verfasserin aut Erunova, Marina G. verfasserin aut Khlebopros, Rem G. verfasserin aut Enthalten in Journal of forestry research Harbin : Univ., 1990 27(2015), 4 vom: 08. Dez., Seite 907-912 (DE-627)529093545 (DE-600)2299615-1 1993-0607 nnns volume:27 year:2015 number:4 day:08 month:12 pages:907-912 https://dx.doi.org/10.1007/s11676-015-0189-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE 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_121 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_206 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_374 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 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_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2036 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_2056 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_2700 GBV_ILN_2817 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 AR 27 2015 4 08 12 907-912 |
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10.1007/s11676-015-0189-7 doi (DE-627)SPR022201513 (SPR)s11676-015-0189-7-e DE-627 ger DE-627 rakwb eng 630 640 ASE Gavrikov, Vladimir L. verfasserin aut How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools 2015 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract In the context of global carbon cycle management, accurate knowledge of carbon content in forests is a relevant issue in contemporary forest ecology. We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated from the forest inventory records containing volume stock and species composition data. The inventory data heavily underestimated the pools in the study area (Stolby State Nature Reserve, central Krasnoyarsk Territory, Russian Federation). The carbon pool estimated from the forest inventory data varied from 25 (t $ ha^{−1} $) (low-density stands) to 73 (t $ ha^{−1} $) (highly stocked stands). Our estimates ranged from 59 (t $ ha^{−1} $) (low-density stands) to 147 (t $ ha^{−1} $) (highly stocked stands). Our values included living trees, standing deadwood, living cover, brushwood and litter. We found that the proportion of biomass carbon (living trees): soil carbon varied from 99:1 to 8:2 for fully stocked and low-density forest stands, respectively. This contradicts the common understanding that the biomass in the boreal forests represents only 16–20 % of the total carbon pool, with the balance being the soil carbon pool. Boreal taiga (dpeaa)DE-He213 Biomass (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Carbon pool (dpeaa)DE-He213 Sharafutdinov, Ruslan A. verfasserin aut Knorre, Anastasyia A. verfasserin aut Pakharkova, Nina V. verfasserin aut Shabalina, Olga M. verfasserin aut Bezkorovaynaya, Irina N. verfasserin aut Borisova, Irina V. verfasserin aut Erunova, Marina G. verfasserin aut Khlebopros, Rem G. verfasserin aut Enthalten in Journal of forestry research Harbin : Univ., 1990 27(2015), 4 vom: 08. Dez., Seite 907-912 (DE-627)529093545 (DE-600)2299615-1 1993-0607 nnns volume:27 year:2015 number:4 day:08 month:12 pages:907-912 https://dx.doi.org/10.1007/s11676-015-0189-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE 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_121 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_206 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_374 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 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_2018 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2036 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_2056 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_2700 GBV_ILN_2817 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4346 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4393 GBV_ILN_4700 GBV_ILN_4753 AR 27 2015 4 08 12 907-912 |
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Enthalten in Journal of forestry research 27(2015), 4 vom: 08. Dez., Seite 907-912 volume:27 year:2015 number:4 day:08 month:12 pages:907-912 |
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Enthalten in Journal of forestry research 27(2015), 4 vom: 08. Dez., Seite 907-912 volume:27 year:2015 number:4 day:08 month:12 pages:907-912 |
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Gavrikov, Vladimir L. @@aut@@ Sharafutdinov, Ruslan A. @@aut@@ Knorre, Anastasyia A. @@aut@@ Pakharkova, Nina V. @@aut@@ Shabalina, Olga M. @@aut@@ Bezkorovaynaya, Irina N. @@aut@@ Borisova, Irina V. @@aut@@ Erunova, Marina G. @@aut@@ Khlebopros, Rem G. @@aut@@ |
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We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated from the forest inventory records containing volume stock and species composition data. The inventory data heavily underestimated the pools in the study area (Stolby State Nature Reserve, central Krasnoyarsk Territory, Russian Federation). The carbon pool estimated from the forest inventory data varied from 25 (t $ ha^{−1} $) (low-density stands) to 73 (t $ ha^{−1} $) (highly stocked stands). Our estimates ranged from 59 (t $ ha^{−1} $) (low-density stands) to 147 (t $ ha^{−1} $) (highly stocked stands). Our values included living trees, standing deadwood, living cover, brushwood and litter. We found that the proportion of biomass carbon (living trees): soil carbon varied from 99:1 to 8:2 for fully stocked and low-density forest stands, respectively. 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|
author |
Gavrikov, Vladimir L. |
spellingShingle |
Gavrikov, Vladimir L. ddc 630 misc Boreal taiga misc Biomass misc Soil misc Carbon pool How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools |
authorStr |
Gavrikov, Vladimir L. |
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630 - Agriculture & related technologies 640 - Home & family management |
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1993-0607 |
topic_title |
630 640 ASE How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools Boreal taiga (dpeaa)DE-He213 Biomass (dpeaa)DE-He213 Soil (dpeaa)DE-He213 Carbon pool (dpeaa)DE-He213 |
topic |
ddc 630 misc Boreal taiga misc Biomass misc Soil misc Carbon pool |
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ddc 630 misc Boreal taiga misc Biomass misc Soil misc Carbon pool |
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ddc 630 misc Boreal taiga misc Biomass misc Soil misc Carbon pool |
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Elektronische Aufsätze Aufsätze Elektronische Ressource |
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How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools |
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How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools |
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Gavrikov, Vladimir L. |
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Gavrikov, Vladimir L. Sharafutdinov, Ruslan A. Knorre, Anastasyia A. Pakharkova, Nina V. Shabalina, Olga M. Bezkorovaynaya, Irina N. Borisova, Irina V. Erunova, Marina G. Khlebopros, Rem G. |
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Gavrikov, Vladimir L. |
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how much carbon can the siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools |
title_auth |
How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools |
abstract |
Abstract In the context of global carbon cycle management, accurate knowledge of carbon content in forests is a relevant issue in contemporary forest ecology. We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated from the forest inventory records containing volume stock and species composition data. The inventory data heavily underestimated the pools in the study area (Stolby State Nature Reserve, central Krasnoyarsk Territory, Russian Federation). The carbon pool estimated from the forest inventory data varied from 25 (t $ ha^{−1} $) (low-density stands) to 73 (t $ ha^{−1} $) (highly stocked stands). Our estimates ranged from 59 (t $ ha^{−1} $) (low-density stands) to 147 (t $ ha^{−1} $) (highly stocked stands). Our values included living trees, standing deadwood, living cover, brushwood and litter. We found that the proportion of biomass carbon (living trees): soil carbon varied from 99:1 to 8:2 for fully stocked and low-density forest stands, respectively. This contradicts the common understanding that the biomass in the boreal forests represents only 16–20 % of the total carbon pool, with the balance being the soil carbon pool. |
abstractGer |
Abstract In the context of global carbon cycle management, accurate knowledge of carbon content in forests is a relevant issue in contemporary forest ecology. We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated from the forest inventory records containing volume stock and species composition data. The inventory data heavily underestimated the pools in the study area (Stolby State Nature Reserve, central Krasnoyarsk Territory, Russian Federation). The carbon pool estimated from the forest inventory data varied from 25 (t $ ha^{−1} $) (low-density stands) to 73 (t $ ha^{−1} $) (highly stocked stands). Our estimates ranged from 59 (t $ ha^{−1} $) (low-density stands) to 147 (t $ ha^{−1} $) (highly stocked stands). Our values included living trees, standing deadwood, living cover, brushwood and litter. We found that the proportion of biomass carbon (living trees): soil carbon varied from 99:1 to 8:2 for fully stocked and low-density forest stands, respectively. This contradicts the common understanding that the biomass in the boreal forests represents only 16–20 % of the total carbon pool, with the balance being the soil carbon pool. |
abstract_unstemmed |
Abstract In the context of global carbon cycle management, accurate knowledge of carbon content in forests is a relevant issue in contemporary forest ecology. We measured the above-ground and soil carbon pools in the dark-coniferous boreal taiga. We compared measured carbon pools to those calculated from the forest inventory records containing volume stock and species composition data. The inventory data heavily underestimated the pools in the study area (Stolby State Nature Reserve, central Krasnoyarsk Territory, Russian Federation). The carbon pool estimated from the forest inventory data varied from 25 (t $ ha^{−1} $) (low-density stands) to 73 (t $ ha^{−1} $) (highly stocked stands). Our estimates ranged from 59 (t $ ha^{−1} $) (low-density stands) to 147 (t $ ha^{−1} $) (highly stocked stands). Our values included living trees, standing deadwood, living cover, brushwood and litter. We found that the proportion of biomass carbon (living trees): soil carbon varied from 99:1 to 8:2 for fully stocked and low-density forest stands, respectively. This contradicts the common understanding that the biomass in the boreal forests represents only 16–20 % of the total carbon pool, with the balance being the soil carbon pool. |
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title_short |
How much carbon can the Siberian boreal taiga store: a case study of partitioning among the above-ground and soil pools |
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https://dx.doi.org/10.1007/s11676-015-0189-7 |
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Sharafutdinov, Ruslan A. Knorre, Anastasyia A. Pakharkova, Nina V. Shabalina, Olga M. Bezkorovaynaya, Irina N. Borisova, Irina V. Erunova, Marina G. Khlebopros, Rem G. |
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Sharafutdinov, Ruslan A. Knorre, Anastasyia A. Pakharkova, Nina V. Shabalina, Olga M. Bezkorovaynaya, Irina N. Borisova, Irina V. Erunova, Marina G. Khlebopros, Rem G. |
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score |
7.3984203 |