Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China

Abstract Subtropical evergreen broad-leaved forest is the most widely distributed land-cover type in eastern China. As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground...
Ausführliche Beschreibung

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Autor*in:	Zhang, Kai [verfasserIn] Xu, Xiaoniu [verfasserIn] Wang, Qin [verfasserIn] Liu, Bo [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2009

Schlagwörter:	Above and below-ground biomass Coarse root Nutrient storage Subtropical secondary forest

Übergeordnetes Werk:	Enthalten in: Journal of forest research - Tokyo : Springer, 1996, 15(2009), 4 vom: 29. Dez., Seite 274-282
Übergeordnetes Werk:	volume:15 ; year:2009 ; number:4 ; day:29 ; month:12 ; pages:274-282

Links:	Volltext

DOI / URN:	10.1007/s10310-009-0175-z

Katalog-ID:	SPR009422293

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520			\|a Abstract Subtropical evergreen broad-leaved forest is the most widely distributed land-cover type in eastern China. As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground biomass and ecosystem pools of N and C in a subtropical secondary forest were investigated at Laoshan Mountain Natural Reserve, eastern China. Total biomass was 142.9 Mg $ ha^{−1} $ for a young stand (18 years) and 421.9 Mg $ ha^{−1} $ for a premature stand (ca. 60 years); of this, root biomass was from 26.9 (18.8% of the total) to 100.3 Mg $ ha^{−1} $ (23.8%). Total biomass C and N pools were, respectively, 71.4 Mg $ ha^{−1} $ and 641.6 kg $ ha^{−1} $ in the young stand, and 217.0 Mg $ ha^{−1} $ and 1387.4 kg $ ha^{−1} $ in the premature stand. The tree layer comprised 91.8 and 89.4% of the total biomass C and N pools in the young stand, and 98.0 and 95.6% in the premature stand. Total ecosystem C and N pools were, respectively, 101.4 and 4.6 Mg $ ha^{−1} $ for the young stand, and 260.2 and 6.6 Mg $ ha^{−1} $ for the premature stand. Soil C comprised 23.8–29.6% of total ecosystem C whereas soil N comprised 76.9–84.4% of the total. Our results suggest that a very high percentage of N in this subtropical forest ecosystem is stored in the mineral soil, whereas the proportion of organic C in the soil pool is more variable. The subtropical forest in eastern China seems to rapidly accumulate biomass during secondary succession, which makes it a potentially rapid accumulator of, and large sink for, atmospheric C.
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700	1		\|a Liu, Bo \|e verfasserin \|4 aut
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allfields	10.1007/s10310-009-0175-z doi (DE-627)SPR009422293 (SPR)s10310-009-0175-z-e DE-627 ger DE-627 rakwb eng 630 ASE 630 640 ASE 48.40 bkl Zhang, Kai verfasserin aut Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Subtropical evergreen broad-leaved forest is the most widely distributed land-cover type in eastern China. As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground biomass and ecosystem pools of N and C in a subtropical secondary forest were investigated at Laoshan Mountain Natural Reserve, eastern China. Total biomass was 142.9 Mg $ ha^{−1} $ for a young stand (18 years) and 421.9 Mg $ ha^{−1} $ for a premature stand (ca. 60 years); of this, root biomass was from 26.9 (18.8% of the total) to 100.3 Mg $ ha^{−1} $ (23.8%). Total biomass C and N pools were, respectively, 71.4 Mg $ ha^{−1} $ and 641.6 kg $ ha^{−1} $ in the young stand, and 217.0 Mg $ ha^{−1} $ and 1387.4 kg $ ha^{−1} $ in the premature stand. The tree layer comprised 91.8 and 89.4% of the total biomass C and N pools in the young stand, and 98.0 and 95.6% in the premature stand. Total ecosystem C and N pools were, respectively, 101.4 and 4.6 Mg $ ha^{−1} $ for the young stand, and 260.2 and 6.6 Mg $ ha^{−1} $ for the premature stand. Soil C comprised 23.8–29.6% of total ecosystem C whereas soil N comprised 76.9–84.4% of the total. Our results suggest that a very high percentage of N in this subtropical forest ecosystem is stored in the mineral soil, whereas the proportion of organic C in the soil pool is more variable. The subtropical forest in eastern China seems to rapidly accumulate biomass during secondary succession, which makes it a potentially rapid accumulator of, and large sink for, atmospheric C. Above and below-ground biomass (dpeaa)DE-He213 Coarse root (dpeaa)DE-He213 Nutrient storage (dpeaa)DE-He213 Subtropical secondary forest (dpeaa)DE-He213 Xu, Xiaoniu verfasserin aut Wang, Qin verfasserin aut Liu, Bo verfasserin aut Enthalten in Journal of forest research Tokyo : Springer, 1996 15(2009), 4 vom: 29. Dez., Seite 274-282 (DE-627)363744819 (DE-600)2104467-3 1610-7403 nnns volume:15 year:2009 number:4 day:29 month:12 pages:274-282 https://dx.doi.org/10.1007/s10310-009-0175-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_95 GBV_ILN_100 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_224 GBV_ILN_266 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 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_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4313 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 48.40 ASE AR 15 2009 4 29 12 274-282
spelling	10.1007/s10310-009-0175-z doi (DE-627)SPR009422293 (SPR)s10310-009-0175-z-e DE-627 ger DE-627 rakwb eng 630 ASE 630 640 ASE 48.40 bkl Zhang, Kai verfasserin aut Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Subtropical evergreen broad-leaved forest is the most widely distributed land-cover type in eastern China. As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground biomass and ecosystem pools of N and C in a subtropical secondary forest were investigated at Laoshan Mountain Natural Reserve, eastern China. Total biomass was 142.9 Mg $ ha^{−1} $ for a young stand (18 years) and 421.9 Mg $ ha^{−1} $ for a premature stand (ca. 60 years); of this, root biomass was from 26.9 (18.8% of the total) to 100.3 Mg $ ha^{−1} $ (23.8%). Total biomass C and N pools were, respectively, 71.4 Mg $ ha^{−1} $ and 641.6 kg $ ha^{−1} $ in the young stand, and 217.0 Mg $ ha^{−1} $ and 1387.4 kg $ ha^{−1} $ in the premature stand. The tree layer comprised 91.8 and 89.4% of the total biomass C and N pools in the young stand, and 98.0 and 95.6% in the premature stand. Total ecosystem C and N pools were, respectively, 101.4 and 4.6 Mg $ ha^{−1} $ for the young stand, and 260.2 and 6.6 Mg $ ha^{−1} $ for the premature stand. Soil C comprised 23.8–29.6% of total ecosystem C whereas soil N comprised 76.9–84.4% of the total. Our results suggest that a very high percentage of N in this subtropical forest ecosystem is stored in the mineral soil, whereas the proportion of organic C in the soil pool is more variable. The subtropical forest in eastern China seems to rapidly accumulate biomass during secondary succession, which makes it a potentially rapid accumulator of, and large sink for, atmospheric C. Above and below-ground biomass (dpeaa)DE-He213 Coarse root (dpeaa)DE-He213 Nutrient storage (dpeaa)DE-He213 Subtropical secondary forest (dpeaa)DE-He213 Xu, Xiaoniu verfasserin aut Wang, Qin verfasserin aut Liu, Bo verfasserin aut Enthalten in Journal of forest research Tokyo : Springer, 1996 15(2009), 4 vom: 29. Dez., Seite 274-282 (DE-627)363744819 (DE-600)2104467-3 1610-7403 nnns volume:15 year:2009 number:4 day:29 month:12 pages:274-282 https://dx.doi.org/10.1007/s10310-009-0175-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_95 GBV_ILN_100 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_224 GBV_ILN_266 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 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_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4313 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 48.40 ASE AR 15 2009 4 29 12 274-282
allfields_unstemmed	10.1007/s10310-009-0175-z doi (DE-627)SPR009422293 (SPR)s10310-009-0175-z-e DE-627 ger DE-627 rakwb eng 630 ASE 630 640 ASE 48.40 bkl Zhang, Kai verfasserin aut Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Subtropical evergreen broad-leaved forest is the most widely distributed land-cover type in eastern China. As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground biomass and ecosystem pools of N and C in a subtropical secondary forest were investigated at Laoshan Mountain Natural Reserve, eastern China. Total biomass was 142.9 Mg $ ha^{−1} $ for a young stand (18 years) and 421.9 Mg $ ha^{−1} $ for a premature stand (ca. 60 years); of this, root biomass was from 26.9 (18.8% of the total) to 100.3 Mg $ ha^{−1} $ (23.8%). Total biomass C and N pools were, respectively, 71.4 Mg $ ha^{−1} $ and 641.6 kg $ ha^{−1} $ in the young stand, and 217.0 Mg $ ha^{−1} $ and 1387.4 kg $ ha^{−1} $ in the premature stand. The tree layer comprised 91.8 and 89.4% of the total biomass C and N pools in the young stand, and 98.0 and 95.6% in the premature stand. Total ecosystem C and N pools were, respectively, 101.4 and 4.6 Mg $ ha^{−1} $ for the young stand, and 260.2 and 6.6 Mg $ ha^{−1} $ for the premature stand. Soil C comprised 23.8–29.6% of total ecosystem C whereas soil N comprised 76.9–84.4% of the total. Our results suggest that a very high percentage of N in this subtropical forest ecosystem is stored in the mineral soil, whereas the proportion of organic C in the soil pool is more variable. The subtropical forest in eastern China seems to rapidly accumulate biomass during secondary succession, which makes it a potentially rapid accumulator of, and large sink for, atmospheric C. Above and below-ground biomass (dpeaa)DE-He213 Coarse root (dpeaa)DE-He213 Nutrient storage (dpeaa)DE-He213 Subtropical secondary forest (dpeaa)DE-He213 Xu, Xiaoniu verfasserin aut Wang, Qin verfasserin aut Liu, Bo verfasserin aut Enthalten in Journal of forest research Tokyo : Springer, 1996 15(2009), 4 vom: 29. Dez., Seite 274-282 (DE-627)363744819 (DE-600)2104467-3 1610-7403 nnns volume:15 year:2009 number:4 day:29 month:12 pages:274-282 https://dx.doi.org/10.1007/s10310-009-0175-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_95 GBV_ILN_100 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_224 GBV_ILN_266 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 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_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4313 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 48.40 ASE AR 15 2009 4 29 12 274-282
allfieldsGer	10.1007/s10310-009-0175-z doi (DE-627)SPR009422293 (SPR)s10310-009-0175-z-e DE-627 ger DE-627 rakwb eng 630 ASE 630 640 ASE 48.40 bkl Zhang, Kai verfasserin aut Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Subtropical evergreen broad-leaved forest is the most widely distributed land-cover type in eastern China. As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground biomass and ecosystem pools of N and C in a subtropical secondary forest were investigated at Laoshan Mountain Natural Reserve, eastern China. Total biomass was 142.9 Mg $ ha^{−1} $ for a young stand (18 years) and 421.9 Mg $ ha^{−1} $ for a premature stand (ca. 60 years); of this, root biomass was from 26.9 (18.8% of the total) to 100.3 Mg $ ha^{−1} $ (23.8%). Total biomass C and N pools were, respectively, 71.4 Mg $ ha^{−1} $ and 641.6 kg $ ha^{−1} $ in the young stand, and 217.0 Mg $ ha^{−1} $ and 1387.4 kg $ ha^{−1} $ in the premature stand. The tree layer comprised 91.8 and 89.4% of the total biomass C and N pools in the young stand, and 98.0 and 95.6% in the premature stand. Total ecosystem C and N pools were, respectively, 101.4 and 4.6 Mg $ ha^{−1} $ for the young stand, and 260.2 and 6.6 Mg $ ha^{−1} $ for the premature stand. Soil C comprised 23.8–29.6% of total ecosystem C whereas soil N comprised 76.9–84.4% of the total. Our results suggest that a very high percentage of N in this subtropical forest ecosystem is stored in the mineral soil, whereas the proportion of organic C in the soil pool is more variable. The subtropical forest in eastern China seems to rapidly accumulate biomass during secondary succession, which makes it a potentially rapid accumulator of, and large sink for, atmospheric C. Above and below-ground biomass (dpeaa)DE-He213 Coarse root (dpeaa)DE-He213 Nutrient storage (dpeaa)DE-He213 Subtropical secondary forest (dpeaa)DE-He213 Xu, Xiaoniu verfasserin aut Wang, Qin verfasserin aut Liu, Bo verfasserin aut Enthalten in Journal of forest research Tokyo : Springer, 1996 15(2009), 4 vom: 29. Dez., Seite 274-282 (DE-627)363744819 (DE-600)2104467-3 1610-7403 nnns volume:15 year:2009 number:4 day:29 month:12 pages:274-282 https://dx.doi.org/10.1007/s10310-009-0175-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_95 GBV_ILN_100 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_224 GBV_ILN_266 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 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_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4313 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 48.40 ASE AR 15 2009 4 29 12 274-282
allfieldsSound	10.1007/s10310-009-0175-z doi (DE-627)SPR009422293 (SPR)s10310-009-0175-z-e DE-627 ger DE-627 rakwb eng 630 ASE 630 640 ASE 48.40 bkl Zhang, Kai verfasserin aut Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China 2009 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Subtropical evergreen broad-leaved forest is the most widely distributed land-cover type in eastern China. As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground biomass and ecosystem pools of N and C in a subtropical secondary forest were investigated at Laoshan Mountain Natural Reserve, eastern China. Total biomass was 142.9 Mg $ ha^{−1} $ for a young stand (18 years) and 421.9 Mg $ ha^{−1} $ for a premature stand (ca. 60 years); of this, root biomass was from 26.9 (18.8% of the total) to 100.3 Mg $ ha^{−1} $ (23.8%). Total biomass C and N pools were, respectively, 71.4 Mg $ ha^{−1} $ and 641.6 kg $ ha^{−1} $ in the young stand, and 217.0 Mg $ ha^{−1} $ and 1387.4 kg $ ha^{−1} $ in the premature stand. The tree layer comprised 91.8 and 89.4% of the total biomass C and N pools in the young stand, and 98.0 and 95.6% in the premature stand. Total ecosystem C and N pools were, respectively, 101.4 and 4.6 Mg $ ha^{−1} $ for the young stand, and 260.2 and 6.6 Mg $ ha^{−1} $ for the premature stand. Soil C comprised 23.8–29.6% of total ecosystem C whereas soil N comprised 76.9–84.4% of the total. Our results suggest that a very high percentage of N in this subtropical forest ecosystem is stored in the mineral soil, whereas the proportion of organic C in the soil pool is more variable. The subtropical forest in eastern China seems to rapidly accumulate biomass during secondary succession, which makes it a potentially rapid accumulator of, and large sink for, atmospheric C. Above and below-ground biomass (dpeaa)DE-He213 Coarse root (dpeaa)DE-He213 Nutrient storage (dpeaa)DE-He213 Subtropical secondary forest (dpeaa)DE-He213 Xu, Xiaoniu verfasserin aut Wang, Qin verfasserin aut Liu, Bo verfasserin aut Enthalten in Journal of forest research Tokyo : Springer, 1996 15(2009), 4 vom: 29. Dez., Seite 274-282 (DE-627)363744819 (DE-600)2104467-3 1610-7403 nnns volume:15 year:2009 number:4 day:29 month:12 pages:274-282 https://dx.doi.org/10.1007/s10310-009-0175-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-FOR SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_63 GBV_ILN_70 GBV_ILN_95 GBV_ILN_100 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_224 GBV_ILN_266 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2055 GBV_ILN_2059 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2106 GBV_ILN_2108 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_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4313 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4700 48.40 ASE AR 15 2009 4 29 12 274-282
language	English
source	Enthalten in Journal of forest research 15(2009), 4 vom: 29. Dez., Seite 274-282 volume:15 year:2009 number:4 day:29 month:12 pages:274-282
sourceStr	Enthalten in Journal of forest research 15(2009), 4 vom: 29. Dez., Seite 274-282 volume:15 year:2009 number:4 day:29 month:12 pages:274-282
format_phy_str_mv	Article
institution	findex.gbv.de
topic_facet	Above and below-ground biomass Coarse root Nutrient storage Subtropical secondary forest
dewey-raw	630
isfreeaccess_bool	false
container_title	Journal of forest research
authorswithroles_txt_mv	Zhang, Kai @@aut@@ Xu, Xiaoniu @@aut@@ Wang, Qin @@aut@@ Liu, Bo @@aut@@
publishDateDaySort_date	2009-12-29T00:00:00Z
hierarchy_top_id	363744819
dewey-sort	3630
id	SPR009422293
language_de	englisch
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author	Zhang, Kai
spellingShingle	Zhang, Kai ddc 630 bkl 48.40 misc Above and below-ground biomass misc Coarse root misc Nutrient storage misc Subtropical secondary forest Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China
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topic_title	630 ASE 630 640 ASE 48.40 bkl Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China Above and below-ground biomass (dpeaa)DE-He213 Coarse root (dpeaa)DE-He213 Nutrient storage (dpeaa)DE-He213 Subtropical secondary forest (dpeaa)DE-He213
topic	ddc 630 bkl 48.40 misc Above and below-ground biomass misc Coarse root misc Nutrient storage misc Subtropical secondary forest
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title	Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China
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title_full	Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China
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author_browse	Zhang, Kai Xu, Xiaoniu Wang, Qin Liu, Bo
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title_sort	biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern china
title_auth	Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China
abstract	Abstract Subtropical evergreen broad-leaved forest is the most widely distributed land-cover type in eastern China. As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground biomass and ecosystem pools of N and C in a subtropical secondary forest were investigated at Laoshan Mountain Natural Reserve, eastern China. Total biomass was 142.9 Mg $ ha^{−1} $ for a young stand (18 years) and 421.9 Mg $ ha^{−1} $ for a premature stand (ca. 60 years); of this, root biomass was from 26.9 (18.8% of the total) to 100.3 Mg $ ha^{−1} $ (23.8%). Total biomass C and N pools were, respectively, 71.4 Mg $ ha^{−1} $ and 641.6 kg $ ha^{−1} $ in the young stand, and 217.0 Mg $ ha^{−1} $ and 1387.4 kg $ ha^{−1} $ in the premature stand. The tree layer comprised 91.8 and 89.4% of the total biomass C and N pools in the young stand, and 98.0 and 95.6% in the premature stand. Total ecosystem C and N pools were, respectively, 101.4 and 4.6 Mg $ ha^{−1} $ for the young stand, and 260.2 and 6.6 Mg $ ha^{−1} $ for the premature stand. Soil C comprised 23.8–29.6% of total ecosystem C whereas soil N comprised 76.9–84.4% of the total. Our results suggest that a very high percentage of N in this subtropical forest ecosystem is stored in the mineral soil, whereas the proportion of organic C in the soil pool is more variable. The subtropical forest in eastern China seems to rapidly accumulate biomass during secondary succession, which makes it a potentially rapid accumulator of, and large sink for, atmospheric C.
abstractGer	Abstract Subtropical evergreen broad-leaved forest is the most widely distributed land-cover type in eastern China. As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground biomass and ecosystem pools of N and C in a subtropical secondary forest were investigated at Laoshan Mountain Natural Reserve, eastern China. Total biomass was 142.9 Mg $ ha^{−1} $ for a young stand (18 years) and 421.9 Mg $ ha^{−1} $ for a premature stand (ca. 60 years); of this, root biomass was from 26.9 (18.8% of the total) to 100.3 Mg $ ha^{−1} $ (23.8%). Total biomass C and N pools were, respectively, 71.4 Mg $ ha^{−1} $ and 641.6 kg $ ha^{−1} $ in the young stand, and 217.0 Mg $ ha^{−1} $ and 1387.4 kg $ ha^{−1} $ in the premature stand. The tree layer comprised 91.8 and 89.4% of the total biomass C and N pools in the young stand, and 98.0 and 95.6% in the premature stand. Total ecosystem C and N pools were, respectively, 101.4 and 4.6 Mg $ ha^{−1} $ for the young stand, and 260.2 and 6.6 Mg $ ha^{−1} $ for the premature stand. Soil C comprised 23.8–29.6% of total ecosystem C whereas soil N comprised 76.9–84.4% of the total. Our results suggest that a very high percentage of N in this subtropical forest ecosystem is stored in the mineral soil, whereas the proportion of organic C in the soil pool is more variable. The subtropical forest in eastern China seems to rapidly accumulate biomass during secondary succession, which makes it a potentially rapid accumulator of, and large sink for, atmospheric C.
abstract_unstemmed	Abstract Subtropical evergreen broad-leaved forest is the most widely distributed land-cover type in eastern China. As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground biomass and ecosystem pools of N and C in a subtropical secondary forest were investigated at Laoshan Mountain Natural Reserve, eastern China. Total biomass was 142.9 Mg $ ha^{−1} $ for a young stand (18 years) and 421.9 Mg $ ha^{−1} $ for a premature stand (ca. 60 years); of this, root biomass was from 26.9 (18.8% of the total) to 100.3 Mg $ ha^{−1} $ (23.8%). Total biomass C and N pools were, respectively, 71.4 Mg $ ha^{−1} $ and 641.6 kg $ ha^{−1} $ in the young stand, and 217.0 Mg $ ha^{−1} $ and 1387.4 kg $ ha^{−1} $ in the premature stand. The tree layer comprised 91.8 and 89.4% of the total biomass C and N pools in the young stand, and 98.0 and 95.6% in the premature stand. Total ecosystem C and N pools were, respectively, 101.4 and 4.6 Mg $ ha^{−1} $ for the young stand, and 260.2 and 6.6 Mg $ ha^{−1} $ for the premature stand. Soil C comprised 23.8–29.6% of total ecosystem C whereas soil N comprised 76.9–84.4% of the total. Our results suggest that a very high percentage of N in this subtropical forest ecosystem is stored in the mineral soil, whereas the proportion of organic C in the soil pool is more variable. The subtropical forest in eastern China seems to rapidly accumulate biomass during secondary succession, which makes it a potentially rapid accumulator of, and large sink for, atmospheric C.
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container_issue	4
title_short	Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China
url	https://dx.doi.org/10.1007/s10310-009-0175-z
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author2	Xu, Xiaoniu Wang, Qin Liu, Bo
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up_date	2024-07-04T01:59:48.071Z
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As the rate of land-use change accelerates worldwide, it is becoming increasingly important to quantify ecosystem biomass and carbon (C) and nitrogen (N) pools. Above and below-ground biomass and ecosystem pools of N and C in a subtropical secondary forest were investigated at Laoshan Mountain Natural Reserve, eastern China. Total biomass was 142.9 Mg $ ha^{−1} $ for a young stand (18 years) and 421.9 Mg $ ha^{−1} $ for a premature stand (ca. 60 years); of this, root biomass was from 26.9 (18.8% of the total) to 100.3 Mg $ ha^{−1} $ (23.8%). Total biomass C and N pools were, respectively, 71.4 Mg $ ha^{−1} $ and 641.6 kg $ ha^{−1} $ in the young stand, and 217.0 Mg $ ha^{−1} $ and 1387.4 kg $ ha^{−1} $ in the premature stand. The tree layer comprised 91.8 and 89.4% of the total biomass C and N pools in the young stand, and 98.0 and 95.6% in the premature stand. Total ecosystem C and N pools were, respectively, 101.4 and 4.6 Mg $ ha^{−1} $ for the young stand, and 260.2 and 6.6 Mg $ ha^{−1} $ for the premature stand. Soil C comprised 23.8–29.6% of total ecosystem C whereas soil N comprised 76.9–84.4% of the total. Our results suggest that a very high percentage of N in this subtropical forest ecosystem is stored in the mineral soil, whereas the proportion of organic C in the soil pool is more variable. The subtropical forest in eastern China seems to rapidly accumulate biomass during secondary succession, which makes it a potentially rapid accumulator of, and large sink for, atmospheric C.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Above and below-ground biomass</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Coarse root</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Nutrient storage</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Subtropical secondary forest</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Xiaoniu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Qin</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Liu, Bo</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Journal of forest research</subfield><subfield code="d">Tokyo : Springer, 1996</subfield><subfield code="g">15(2009), 4 vom: 29. Dez., Seite 274-282</subfield><subfield code="w">(DE-627)363744819</subfield><subfield code="w">(DE-600)2104467-3</subfield><subfield code="x">1610-7403</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:15</subfield><subfield code="g">year:2009</subfield><subfield code="g">number:4</subfield><subfield code="g">day:29</subfield><subfield code="g">month:12</subfield><subfield code="g">pages:274-282</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://dx.doi.org/10.1007/s10310-009-0175-z</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_SPRINGER</subfield></datafield><datafield tag="912" 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Biomass, and carbon and nitrogen pools in a subtropical evergreen broad-leaved forest in eastern China

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