Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China
Abstract To control soil and water loss and environmental degradation, shelter/protective forests were established in the Loess Plateau as a component of the Three-North Shelter Forest Program (TNSFP). With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plat...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Sun, Yirong [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag Berlin Heidelberg 2016 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental earth sciences - Berlin : Springer, 2009, 75(2016), 4 vom: 11. Feb. |
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| Übergeordnetes Werk: |
volume:75 ; year:2016 ; number:4 ; day:11 ; month:02 |
| Links: |
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| DOI / URN: |
10.1007/s12665-015-5199-4 |
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| Katalog-ID: |
SPR026726335 |
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| 100 | 1 | |a Sun, Yirong |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China |
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| 520 | |a Abstract To control soil and water loss and environmental degradation, shelter/protective forests were established in the Loess Plateau as a component of the Three-North Shelter Forest Program (TNSFP). With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plateau on carbon (C) stock have been investigated. To assess the effects of shelter forests in the Loess Plateau on the C stock, we utilized the data obtained from field investigations and Landsat ETM+ images to assess the C stocks (aboveground and belowground carbon) of shelter forests in the central Loess Plateau in China (11.94 × $ 10^{6} $ ha) during the TNSFP construction period (from 1978 to 2007). We also performed an uncertainty analysis up-scaling from field plots to the study area. The total vegetation C stocks increased significantly from 144 Tg in 1978, to 269 Tg in 2007, and shelter forests accounted for 80 % of total C stocks. The annual mean C sink was 4.28 Tg $ year^{−1} $ for the vegetation. Shelter forests were estimated to have sequestered 2.55 Tg $ year^{−1} $ biomass C and conserved 3.35 Tg $ year^{−1} $ soil C. These results suggest that the shelter forests in the central Loess Plateau have acted as a C sink since the initiation of the TNSFP in 1978. Furthermore, afforestation and reforestation have a significant effect on C sequestration. | ||
| 650 | 4 | |a Carbon stocks |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a The Loess Plateau |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a The Three-North Shelter Forest Program |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Remote sensing |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Zhu, Jiaojun |4 aut | |
| 700 | 1 | |a Yan, Qiaoling |4 aut | |
| 700 | 1 | |a Hu, Zhibin |4 aut | |
| 700 | 1 | |a Zheng, Xiao |4 aut | |
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10.1007/s12665-015-5199-4 doi (DE-627)SPR026726335 (SPR)s12665-015-5199-4-e DE-627 ger DE-627 rakwb eng Sun, Yirong verfasserin aut Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract To control soil and water loss and environmental degradation, shelter/protective forests were established in the Loess Plateau as a component of the Three-North Shelter Forest Program (TNSFP). With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plateau on carbon (C) stock have been investigated. To assess the effects of shelter forests in the Loess Plateau on the C stock, we utilized the data obtained from field investigations and Landsat ETM+ images to assess the C stocks (aboveground and belowground carbon) of shelter forests in the central Loess Plateau in China (11.94 × $ 10^{6} $ ha) during the TNSFP construction period (from 1978 to 2007). We also performed an uncertainty analysis up-scaling from field plots to the study area. The total vegetation C stocks increased significantly from 144 Tg in 1978, to 269 Tg in 2007, and shelter forests accounted for 80 % of total C stocks. The annual mean C sink was 4.28 Tg $ year^{−1} $ for the vegetation. Shelter forests were estimated to have sequestered 2.55 Tg $ year^{−1} $ biomass C and conserved 3.35 Tg $ year^{−1} $ soil C. These results suggest that the shelter forests in the central Loess Plateau have acted as a C sink since the initiation of the TNSFP in 1978. Furthermore, afforestation and reforestation have a significant effect on C sequestration. Carbon stocks (dpeaa)DE-He213 The Loess Plateau (dpeaa)DE-He213 The Three-North Shelter Forest Program (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 Zhu, Jiaojun aut Yan, Qiaoling aut Hu, Zhibin aut Zheng, Xiao aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 4 vom: 11. Feb. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:4 day:11 month:02 https://dx.doi.org/10.1007/s12665-015-5199-4 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 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_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 75 2016 4 11 02 |
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10.1007/s12665-015-5199-4 doi (DE-627)SPR026726335 (SPR)s12665-015-5199-4-e DE-627 ger DE-627 rakwb eng Sun, Yirong verfasserin aut Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract To control soil and water loss and environmental degradation, shelter/protective forests were established in the Loess Plateau as a component of the Three-North Shelter Forest Program (TNSFP). With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plateau on carbon (C) stock have been investigated. To assess the effects of shelter forests in the Loess Plateau on the C stock, we utilized the data obtained from field investigations and Landsat ETM+ images to assess the C stocks (aboveground and belowground carbon) of shelter forests in the central Loess Plateau in China (11.94 × $ 10^{6} $ ha) during the TNSFP construction period (from 1978 to 2007). We also performed an uncertainty analysis up-scaling from field plots to the study area. The total vegetation C stocks increased significantly from 144 Tg in 1978, to 269 Tg in 2007, and shelter forests accounted for 80 % of total C stocks. The annual mean C sink was 4.28 Tg $ year^{−1} $ for the vegetation. Shelter forests were estimated to have sequestered 2.55 Tg $ year^{−1} $ biomass C and conserved 3.35 Tg $ year^{−1} $ soil C. These results suggest that the shelter forests in the central Loess Plateau have acted as a C sink since the initiation of the TNSFP in 1978. Furthermore, afforestation and reforestation have a significant effect on C sequestration. Carbon stocks (dpeaa)DE-He213 The Loess Plateau (dpeaa)DE-He213 The Three-North Shelter Forest Program (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 Zhu, Jiaojun aut Yan, Qiaoling aut Hu, Zhibin aut Zheng, Xiao aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 4 vom: 11. Feb. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:4 day:11 month:02 https://dx.doi.org/10.1007/s12665-015-5199-4 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 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_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 75 2016 4 11 02 |
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10.1007/s12665-015-5199-4 doi (DE-627)SPR026726335 (SPR)s12665-015-5199-4-e DE-627 ger DE-627 rakwb eng Sun, Yirong verfasserin aut Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract To control soil and water loss and environmental degradation, shelter/protective forests were established in the Loess Plateau as a component of the Three-North Shelter Forest Program (TNSFP). With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plateau on carbon (C) stock have been investigated. To assess the effects of shelter forests in the Loess Plateau on the C stock, we utilized the data obtained from field investigations and Landsat ETM+ images to assess the C stocks (aboveground and belowground carbon) of shelter forests in the central Loess Plateau in China (11.94 × $ 10^{6} $ ha) during the TNSFP construction period (from 1978 to 2007). We also performed an uncertainty analysis up-scaling from field plots to the study area. The total vegetation C stocks increased significantly from 144 Tg in 1978, to 269 Tg in 2007, and shelter forests accounted for 80 % of total C stocks. The annual mean C sink was 4.28 Tg $ year^{−1} $ for the vegetation. Shelter forests were estimated to have sequestered 2.55 Tg $ year^{−1} $ biomass C and conserved 3.35 Tg $ year^{−1} $ soil C. These results suggest that the shelter forests in the central Loess Plateau have acted as a C sink since the initiation of the TNSFP in 1978. Furthermore, afforestation and reforestation have a significant effect on C sequestration. Carbon stocks (dpeaa)DE-He213 The Loess Plateau (dpeaa)DE-He213 The Three-North Shelter Forest Program (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 Zhu, Jiaojun aut Yan, Qiaoling aut Hu, Zhibin aut Zheng, Xiao aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 4 vom: 11. Feb. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:4 day:11 month:02 https://dx.doi.org/10.1007/s12665-015-5199-4 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 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_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 75 2016 4 11 02 |
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10.1007/s12665-015-5199-4 doi (DE-627)SPR026726335 (SPR)s12665-015-5199-4-e DE-627 ger DE-627 rakwb eng Sun, Yirong verfasserin aut Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract To control soil and water loss and environmental degradation, shelter/protective forests were established in the Loess Plateau as a component of the Three-North Shelter Forest Program (TNSFP). With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plateau on carbon (C) stock have been investigated. To assess the effects of shelter forests in the Loess Plateau on the C stock, we utilized the data obtained from field investigations and Landsat ETM+ images to assess the C stocks (aboveground and belowground carbon) of shelter forests in the central Loess Plateau in China (11.94 × $ 10^{6} $ ha) during the TNSFP construction period (from 1978 to 2007). We also performed an uncertainty analysis up-scaling from field plots to the study area. The total vegetation C stocks increased significantly from 144 Tg in 1978, to 269 Tg in 2007, and shelter forests accounted for 80 % of total C stocks. The annual mean C sink was 4.28 Tg $ year^{−1} $ for the vegetation. Shelter forests were estimated to have sequestered 2.55 Tg $ year^{−1} $ biomass C and conserved 3.35 Tg $ year^{−1} $ soil C. These results suggest that the shelter forests in the central Loess Plateau have acted as a C sink since the initiation of the TNSFP in 1978. Furthermore, afforestation and reforestation have a significant effect on C sequestration. Carbon stocks (dpeaa)DE-He213 The Loess Plateau (dpeaa)DE-He213 The Three-North Shelter Forest Program (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 Zhu, Jiaojun aut Yan, Qiaoling aut Hu, Zhibin aut Zheng, Xiao aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 4 vom: 11. Feb. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:4 day:11 month:02 https://dx.doi.org/10.1007/s12665-015-5199-4 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 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_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 75 2016 4 11 02 |
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10.1007/s12665-015-5199-4 doi (DE-627)SPR026726335 (SPR)s12665-015-5199-4-e DE-627 ger DE-627 rakwb eng Sun, Yirong verfasserin aut Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract To control soil and water loss and environmental degradation, shelter/protective forests were established in the Loess Plateau as a component of the Three-North Shelter Forest Program (TNSFP). With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plateau on carbon (C) stock have been investigated. To assess the effects of shelter forests in the Loess Plateau on the C stock, we utilized the data obtained from field investigations and Landsat ETM+ images to assess the C stocks (aboveground and belowground carbon) of shelter forests in the central Loess Plateau in China (11.94 × $ 10^{6} $ ha) during the TNSFP construction period (from 1978 to 2007). We also performed an uncertainty analysis up-scaling from field plots to the study area. The total vegetation C stocks increased significantly from 144 Tg in 1978, to 269 Tg in 2007, and shelter forests accounted for 80 % of total C stocks. The annual mean C sink was 4.28 Tg $ year^{−1} $ for the vegetation. Shelter forests were estimated to have sequestered 2.55 Tg $ year^{−1} $ biomass C and conserved 3.35 Tg $ year^{−1} $ soil C. These results suggest that the shelter forests in the central Loess Plateau have acted as a C sink since the initiation of the TNSFP in 1978. Furthermore, afforestation and reforestation have a significant effect on C sequestration. Carbon stocks (dpeaa)DE-He213 The Loess Plateau (dpeaa)DE-He213 The Three-North Shelter Forest Program (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 Zhu, Jiaojun aut Yan, Qiaoling aut Hu, Zhibin aut Zheng, Xiao aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 4 vom: 11. Feb. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:4 day:11 month:02 https://dx.doi.org/10.1007/s12665-015-5199-4 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_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 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_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 75 2016 4 11 02 |
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With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plateau on carbon (C) stock have been investigated. To assess the effects of shelter forests in the Loess Plateau on the C stock, we utilized the data obtained from field investigations and Landsat ETM+ images to assess the C stocks (aboveground and belowground carbon) of shelter forests in the central Loess Plateau in China (11.94 × $ 10^{6} $ ha) during the TNSFP construction period (from 1978 to 2007). We also performed an uncertainty analysis up-scaling from field plots to the study area. The total vegetation C stocks increased significantly from 144 Tg in 1978, to 269 Tg in 2007, and shelter forests accounted for 80 % of total C stocks. The annual mean C sink was 4.28 Tg $ year^{−1} $ for the vegetation. Shelter forests were estimated to have sequestered 2.55 Tg $ year^{−1} $ biomass C and conserved 3.35 Tg $ year^{−1} $ soil C. 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| author |
Sun, Yirong |
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Sun, Yirong misc Carbon stocks misc The Loess Plateau misc The Three-North Shelter Forest Program misc Remote sensing Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China |
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Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China Carbon stocks (dpeaa)DE-He213 The Loess Plateau (dpeaa)DE-He213 The Three-North Shelter Forest Program (dpeaa)DE-He213 Remote sensing (dpeaa)DE-He213 |
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Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China |
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Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China |
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Sun, Yirong |
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Environmental earth sciences |
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Sun, Yirong Zhu, Jiaojun Yan, Qiaoling Hu, Zhibin Zheng, Xiao |
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changes in vegetation carbon stocks between 1978 and 2007 in central loess plateau, china |
| title_auth |
Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China |
| abstract |
Abstract To control soil and water loss and environmental degradation, shelter/protective forests were established in the Loess Plateau as a component of the Three-North Shelter Forest Program (TNSFP). With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plateau on carbon (C) stock have been investigated. To assess the effects of shelter forests in the Loess Plateau on the C stock, we utilized the data obtained from field investigations and Landsat ETM+ images to assess the C stocks (aboveground and belowground carbon) of shelter forests in the central Loess Plateau in China (11.94 × $ 10^{6} $ ha) during the TNSFP construction period (from 1978 to 2007). We also performed an uncertainty analysis up-scaling from field plots to the study area. The total vegetation C stocks increased significantly from 144 Tg in 1978, to 269 Tg in 2007, and shelter forests accounted for 80 % of total C stocks. The annual mean C sink was 4.28 Tg $ year^{−1} $ for the vegetation. Shelter forests were estimated to have sequestered 2.55 Tg $ year^{−1} $ biomass C and conserved 3.35 Tg $ year^{−1} $ soil C. These results suggest that the shelter forests in the central Loess Plateau have acted as a C sink since the initiation of the TNSFP in 1978. Furthermore, afforestation and reforestation have a significant effect on C sequestration. © Springer-Verlag Berlin Heidelberg 2016 |
| abstractGer |
Abstract To control soil and water loss and environmental degradation, shelter/protective forests were established in the Loess Plateau as a component of the Three-North Shelter Forest Program (TNSFP). With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plateau on carbon (C) stock have been investigated. To assess the effects of shelter forests in the Loess Plateau on the C stock, we utilized the data obtained from field investigations and Landsat ETM+ images to assess the C stocks (aboveground and belowground carbon) of shelter forests in the central Loess Plateau in China (11.94 × $ 10^{6} $ ha) during the TNSFP construction period (from 1978 to 2007). We also performed an uncertainty analysis up-scaling from field plots to the study area. The total vegetation C stocks increased significantly from 144 Tg in 1978, to 269 Tg in 2007, and shelter forests accounted for 80 % of total C stocks. The annual mean C sink was 4.28 Tg $ year^{−1} $ for the vegetation. Shelter forests were estimated to have sequestered 2.55 Tg $ year^{−1} $ biomass C and conserved 3.35 Tg $ year^{−1} $ soil C. These results suggest that the shelter forests in the central Loess Plateau have acted as a C sink since the initiation of the TNSFP in 1978. Furthermore, afforestation and reforestation have a significant effect on C sequestration. © Springer-Verlag Berlin Heidelberg 2016 |
| abstract_unstemmed |
Abstract To control soil and water loss and environmental degradation, shelter/protective forests were established in the Loess Plateau as a component of the Three-North Shelter Forest Program (TNSFP). With the development of the TNSFP in this region, the effects of shelter forests in the Loess Plateau on carbon (C) stock have been investigated. To assess the effects of shelter forests in the Loess Plateau on the C stock, we utilized the data obtained from field investigations and Landsat ETM+ images to assess the C stocks (aboveground and belowground carbon) of shelter forests in the central Loess Plateau in China (11.94 × $ 10^{6} $ ha) during the TNSFP construction period (from 1978 to 2007). We also performed an uncertainty analysis up-scaling from field plots to the study area. The total vegetation C stocks increased significantly from 144 Tg in 1978, to 269 Tg in 2007, and shelter forests accounted for 80 % of total C stocks. The annual mean C sink was 4.28 Tg $ year^{−1} $ for the vegetation. Shelter forests were estimated to have sequestered 2.55 Tg $ year^{−1} $ biomass C and conserved 3.35 Tg $ year^{−1} $ soil C. These results suggest that the shelter forests in the central Loess Plateau have acted as a C sink since the initiation of the TNSFP in 1978. Furthermore, afforestation and reforestation have a significant effect on C sequestration. © Springer-Verlag Berlin Heidelberg 2016 |
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| title_short |
Changes in vegetation carbon stocks between 1978 and 2007 in central Loess Plateau, China |
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https://dx.doi.org/10.1007/s12665-015-5199-4 |
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Zhu, Jiaojun Yan, Qiaoling Hu, Zhibin Zheng, Xiao |
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Zhu, Jiaojun Yan, Qiaoling Hu, Zhibin Zheng, Xiao |
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10.1007/s12665-015-5199-4 |
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2024-07-03T22:24:36.998Z |
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| score |
7.3976336 |