Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest
Abstract The analysis of daily, seasonal, and annual dynamics of $ CO_{2} $ emission from soils under different stands of monsoon tropical tall-tree forest was performed on the basis of field observations conducted at the Russian-Vietnamese Tropical Research and Technology Center of the Russian Acad...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Lopes de Gerenyu, V. O. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2011 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2011 |
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| Übergeordnetes Werk: |
Enthalten in: Eurasian soil science - Moscow : MAIK Nauka/Interperiodica Publ., 1996, 44(2011), 9 vom: 17. Sept. |
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| Übergeordnetes Werk: |
volume:44 ; year:2011 ; number:9 ; day:17 ; month:09 |
| Links: |
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| DOI / URN: |
10.1134/S1064229311090067 |
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SPR01995428X |
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| 100 | 1 | |a Lopes de Gerenyu, V. O. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest |
| 264 | 1 | |c 2011 | |
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| 520 | |a Abstract The analysis of daily, seasonal, and annual dynamics of $ CO_{2} $ emission from soils under different stands of monsoon tropical tall-tree forest was performed on the basis of field observations conducted at the Russian-Vietnamese Tropical Research and Technology Center of the Russian Academy of Sciences. Under a tropical climate, the main factors responsible for the rate of carbon dioxide emission from the soils are shown to be the soil type and the topographic position of the area studied along with the type of vegetation. Depending on these factors, the rate of $ CO_{2} $ emission from the soils was 65–178 mg C/($ m^{2} $ h) during the dry season and 123–259 mg C/($ m^{2} $ h) during the wet season. The daily dynamics of $ CO_{2} $ emissions from the soils of the tropical zone was weakly pronounced in both the wet and the dry season owing to the insignificant diurnal fluctuations of soil temperature. The investigations carried out allowed making an expert evaluation of the annual $ CO_{2} $ fluxes from the soils under different stands of monsoon tropical tall-tree forest in southern Vietnam. They amounted to 900–2000 g C/($ m^{2} $ yr) depending on the forest type. | ||
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| 700 | 1 | |a Anichkin, A. Ye. |4 aut | |
| 700 | 1 | |a Myakshina, T. N. |4 aut | |
| 700 | 1 | |a Kuznetsov, A. N. |4 aut | |
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10.1134/S1064229311090067 doi (DE-627)SPR01995428X (SPR)S1064229311090067-e DE-627 ger DE-627 rakwb eng Lopes de Gerenyu, V. O. verfasserin aut Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract The analysis of daily, seasonal, and annual dynamics of $ CO_{2} $ emission from soils under different stands of monsoon tropical tall-tree forest was performed on the basis of field observations conducted at the Russian-Vietnamese Tropical Research and Technology Center of the Russian Academy of Sciences. Under a tropical climate, the main factors responsible for the rate of carbon dioxide emission from the soils are shown to be the soil type and the topographic position of the area studied along with the type of vegetation. Depending on these factors, the rate of $ CO_{2} $ emission from the soils was 65–178 mg C/($ m^{2} $ h) during the dry season and 123–259 mg C/($ m^{2} $ h) during the wet season. The daily dynamics of $ CO_{2} $ emissions from the soils of the tropical zone was weakly pronounced in both the wet and the dry season owing to the insignificant diurnal fluctuations of soil temperature. The investigations carried out allowed making an expert evaluation of the annual $ CO_{2} $ fluxes from the soils under different stands of monsoon tropical tall-tree forest in southern Vietnam. They amounted to 900–2000 g C/($ m^{2} $ yr) depending on the forest type. Soil Temperature (dpeaa)DE-He213 Soil Respiration (dpeaa)DE-He213 Tropical Forest (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Alluvial Soil (dpeaa)DE-He213 Kurbatova, Yu. A. aut Kurganova, I. N. aut Tiunov, A. V. aut Anichkin, A. Ye. aut Myakshina, T. N. aut Kuznetsov, A. N. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 9 vom: 17. Sept. (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:9 day:17 month:09 https://dx.doi.org/10.1134/S1064229311090067 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2011 9 17 09 |
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10.1134/S1064229311090067 doi (DE-627)SPR01995428X (SPR)S1064229311090067-e DE-627 ger DE-627 rakwb eng Lopes de Gerenyu, V. O. verfasserin aut Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract The analysis of daily, seasonal, and annual dynamics of $ CO_{2} $ emission from soils under different stands of monsoon tropical tall-tree forest was performed on the basis of field observations conducted at the Russian-Vietnamese Tropical Research and Technology Center of the Russian Academy of Sciences. Under a tropical climate, the main factors responsible for the rate of carbon dioxide emission from the soils are shown to be the soil type and the topographic position of the area studied along with the type of vegetation. Depending on these factors, the rate of $ CO_{2} $ emission from the soils was 65–178 mg C/($ m^{2} $ h) during the dry season and 123–259 mg C/($ m^{2} $ h) during the wet season. The daily dynamics of $ CO_{2} $ emissions from the soils of the tropical zone was weakly pronounced in both the wet and the dry season owing to the insignificant diurnal fluctuations of soil temperature. The investigations carried out allowed making an expert evaluation of the annual $ CO_{2} $ fluxes from the soils under different stands of monsoon tropical tall-tree forest in southern Vietnam. They amounted to 900–2000 g C/($ m^{2} $ yr) depending on the forest type. Soil Temperature (dpeaa)DE-He213 Soil Respiration (dpeaa)DE-He213 Tropical Forest (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Alluvial Soil (dpeaa)DE-He213 Kurbatova, Yu. A. aut Kurganova, I. N. aut Tiunov, A. V. aut Anichkin, A. Ye. aut Myakshina, T. N. aut Kuznetsov, A. N. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 9 vom: 17. Sept. (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:9 day:17 month:09 https://dx.doi.org/10.1134/S1064229311090067 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2011 9 17 09 |
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10.1134/S1064229311090067 doi (DE-627)SPR01995428X (SPR)S1064229311090067-e DE-627 ger DE-627 rakwb eng Lopes de Gerenyu, V. O. verfasserin aut Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract The analysis of daily, seasonal, and annual dynamics of $ CO_{2} $ emission from soils under different stands of monsoon tropical tall-tree forest was performed on the basis of field observations conducted at the Russian-Vietnamese Tropical Research and Technology Center of the Russian Academy of Sciences. Under a tropical climate, the main factors responsible for the rate of carbon dioxide emission from the soils are shown to be the soil type and the topographic position of the area studied along with the type of vegetation. Depending on these factors, the rate of $ CO_{2} $ emission from the soils was 65–178 mg C/($ m^{2} $ h) during the dry season and 123–259 mg C/($ m^{2} $ h) during the wet season. The daily dynamics of $ CO_{2} $ emissions from the soils of the tropical zone was weakly pronounced in both the wet and the dry season owing to the insignificant diurnal fluctuations of soil temperature. The investigations carried out allowed making an expert evaluation of the annual $ CO_{2} $ fluxes from the soils under different stands of monsoon tropical tall-tree forest in southern Vietnam. They amounted to 900–2000 g C/($ m^{2} $ yr) depending on the forest type. Soil Temperature (dpeaa)DE-He213 Soil Respiration (dpeaa)DE-He213 Tropical Forest (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Alluvial Soil (dpeaa)DE-He213 Kurbatova, Yu. A. aut Kurganova, I. N. aut Tiunov, A. V. aut Anichkin, A. Ye. aut Myakshina, T. N. aut Kuznetsov, A. N. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 9 vom: 17. Sept. (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:9 day:17 month:09 https://dx.doi.org/10.1134/S1064229311090067 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2011 9 17 09 |
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10.1134/S1064229311090067 doi (DE-627)SPR01995428X (SPR)S1064229311090067-e DE-627 ger DE-627 rakwb eng Lopes de Gerenyu, V. O. verfasserin aut Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract The analysis of daily, seasonal, and annual dynamics of $ CO_{2} $ emission from soils under different stands of monsoon tropical tall-tree forest was performed on the basis of field observations conducted at the Russian-Vietnamese Tropical Research and Technology Center of the Russian Academy of Sciences. Under a tropical climate, the main factors responsible for the rate of carbon dioxide emission from the soils are shown to be the soil type and the topographic position of the area studied along with the type of vegetation. Depending on these factors, the rate of $ CO_{2} $ emission from the soils was 65–178 mg C/($ m^{2} $ h) during the dry season and 123–259 mg C/($ m^{2} $ h) during the wet season. The daily dynamics of $ CO_{2} $ emissions from the soils of the tropical zone was weakly pronounced in both the wet and the dry season owing to the insignificant diurnal fluctuations of soil temperature. The investigations carried out allowed making an expert evaluation of the annual $ CO_{2} $ fluxes from the soils under different stands of monsoon tropical tall-tree forest in southern Vietnam. They amounted to 900–2000 g C/($ m^{2} $ yr) depending on the forest type. Soil Temperature (dpeaa)DE-He213 Soil Respiration (dpeaa)DE-He213 Tropical Forest (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Alluvial Soil (dpeaa)DE-He213 Kurbatova, Yu. A. aut Kurganova, I. N. aut Tiunov, A. V. aut Anichkin, A. Ye. aut Myakshina, T. N. aut Kuznetsov, A. N. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 9 vom: 17. Sept. (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:9 day:17 month:09 https://dx.doi.org/10.1134/S1064229311090067 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2011 9 17 09 |
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10.1134/S1064229311090067 doi (DE-627)SPR01995428X (SPR)S1064229311090067-e DE-627 ger DE-627 rakwb eng Lopes de Gerenyu, V. O. verfasserin aut Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract The analysis of daily, seasonal, and annual dynamics of $ CO_{2} $ emission from soils under different stands of monsoon tropical tall-tree forest was performed on the basis of field observations conducted at the Russian-Vietnamese Tropical Research and Technology Center of the Russian Academy of Sciences. Under a tropical climate, the main factors responsible for the rate of carbon dioxide emission from the soils are shown to be the soil type and the topographic position of the area studied along with the type of vegetation. Depending on these factors, the rate of $ CO_{2} $ emission from the soils was 65–178 mg C/($ m^{2} $ h) during the dry season and 123–259 mg C/($ m^{2} $ h) during the wet season. The daily dynamics of $ CO_{2} $ emissions from the soils of the tropical zone was weakly pronounced in both the wet and the dry season owing to the insignificant diurnal fluctuations of soil temperature. The investigations carried out allowed making an expert evaluation of the annual $ CO_{2} $ fluxes from the soils under different stands of monsoon tropical tall-tree forest in southern Vietnam. They amounted to 900–2000 g C/($ m^{2} $ yr) depending on the forest type. Soil Temperature (dpeaa)DE-He213 Soil Respiration (dpeaa)DE-He213 Tropical Forest (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Alluvial Soil (dpeaa)DE-He213 Kurbatova, Yu. A. aut Kurganova, I. N. aut Tiunov, A. V. aut Anichkin, A. Ye. aut Myakshina, T. N. aut Kuznetsov, A. N. aut Enthalten in Eurasian soil science Moscow : MAIK Nauka/Interperiodica Publ., 1996 44(2011), 9 vom: 17. Sept. (DE-627)341913227 (DE-600)2071129-3 1556-195X nnns volume:44 year:2011 number:9 day:17 month:09 https://dx.doi.org/10.1134/S1064229311090067 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 44 2011 9 17 09 |
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Lopes de Gerenyu, V. O. @@aut@@ Kurbatova, Yu. A. @@aut@@ Kurganova, I. N. @@aut@@ Tiunov, A. V. @@aut@@ Anichkin, A. Ye. @@aut@@ Myakshina, T. N. @@aut@@ Kuznetsov, A. N. @@aut@@ |
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Under a tropical climate, the main factors responsible for the rate of carbon dioxide emission from the soils are shown to be the soil type and the topographic position of the area studied along with the type of vegetation. Depending on these factors, the rate of $ CO_{2} $ emission from the soils was 65–178 mg C/($ m^{2} $ h) during the dry season and 123–259 mg C/($ m^{2} $ h) during the wet season. The daily dynamics of $ CO_{2} $ emissions from the soils of the tropical zone was weakly pronounced in both the wet and the dry season owing to the insignificant diurnal fluctuations of soil temperature. The investigations carried out allowed making an expert evaluation of the annual $ CO_{2} $ fluxes from the soils under different stands of monsoon tropical tall-tree forest in southern Vietnam. 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Lopes de Gerenyu, V. O. |
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Lopes de Gerenyu, V. O. misc Soil Temperature misc Soil Respiration misc Tropical Forest misc EURASIAN Soil Science misc Alluvial Soil Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest |
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Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest Soil Temperature (dpeaa)DE-He213 Soil Respiration (dpeaa)DE-He213 Tropical Forest (dpeaa)DE-He213 EURASIAN Soil Science (dpeaa)DE-He213 Alluvial Soil (dpeaa)DE-He213 |
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Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest |
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Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest |
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Lopes de Gerenyu, V. O. Kurbatova, Yu. A. Kurganova, I. N. Tiunov, A. V. Anichkin, A. Ye. Myakshina, T. N. Kuznetsov, A. N. |
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daily and seasonal dynamics of $ co_{2} $ fluxes from soils under different stands of monsoon tropical forest |
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Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest |
| abstract |
Abstract The analysis of daily, seasonal, and annual dynamics of $ CO_{2} $ emission from soils under different stands of monsoon tropical tall-tree forest was performed on the basis of field observations conducted at the Russian-Vietnamese Tropical Research and Technology Center of the Russian Academy of Sciences. Under a tropical climate, the main factors responsible for the rate of carbon dioxide emission from the soils are shown to be the soil type and the topographic position of the area studied along with the type of vegetation. Depending on these factors, the rate of $ CO_{2} $ emission from the soils was 65–178 mg C/($ m^{2} $ h) during the dry season and 123–259 mg C/($ m^{2} $ h) during the wet season. The daily dynamics of $ CO_{2} $ emissions from the soils of the tropical zone was weakly pronounced in both the wet and the dry season owing to the insignificant diurnal fluctuations of soil temperature. The investigations carried out allowed making an expert evaluation of the annual $ CO_{2} $ fluxes from the soils under different stands of monsoon tropical tall-tree forest in southern Vietnam. They amounted to 900–2000 g C/($ m^{2} $ yr) depending on the forest type. © Pleiades Publishing, Ltd. 2011 |
| abstractGer |
Abstract The analysis of daily, seasonal, and annual dynamics of $ CO_{2} $ emission from soils under different stands of monsoon tropical tall-tree forest was performed on the basis of field observations conducted at the Russian-Vietnamese Tropical Research and Technology Center of the Russian Academy of Sciences. Under a tropical climate, the main factors responsible for the rate of carbon dioxide emission from the soils are shown to be the soil type and the topographic position of the area studied along with the type of vegetation. Depending on these factors, the rate of $ CO_{2} $ emission from the soils was 65–178 mg C/($ m^{2} $ h) during the dry season and 123–259 mg C/($ m^{2} $ h) during the wet season. The daily dynamics of $ CO_{2} $ emissions from the soils of the tropical zone was weakly pronounced in both the wet and the dry season owing to the insignificant diurnal fluctuations of soil temperature. The investigations carried out allowed making an expert evaluation of the annual $ CO_{2} $ fluxes from the soils under different stands of monsoon tropical tall-tree forest in southern Vietnam. They amounted to 900–2000 g C/($ m^{2} $ yr) depending on the forest type. © Pleiades Publishing, Ltd. 2011 |
| abstract_unstemmed |
Abstract The analysis of daily, seasonal, and annual dynamics of $ CO_{2} $ emission from soils under different stands of monsoon tropical tall-tree forest was performed on the basis of field observations conducted at the Russian-Vietnamese Tropical Research and Technology Center of the Russian Academy of Sciences. Under a tropical climate, the main factors responsible for the rate of carbon dioxide emission from the soils are shown to be the soil type and the topographic position of the area studied along with the type of vegetation. Depending on these factors, the rate of $ CO_{2} $ emission from the soils was 65–178 mg C/($ m^{2} $ h) during the dry season and 123–259 mg C/($ m^{2} $ h) during the wet season. The daily dynamics of $ CO_{2} $ emissions from the soils of the tropical zone was weakly pronounced in both the wet and the dry season owing to the insignificant diurnal fluctuations of soil temperature. The investigations carried out allowed making an expert evaluation of the annual $ CO_{2} $ fluxes from the soils under different stands of monsoon tropical tall-tree forest in southern Vietnam. They amounted to 900–2000 g C/($ m^{2} $ yr) depending on the forest type. © Pleiades Publishing, Ltd. 2011 |
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Daily and seasonal dynamics of $ CO_{2} $ fluxes from soils under different stands of monsoon tropical forest |
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Kurbatova, Yu. A. Kurganova, I. N. Tiunov, A. V. Anichkin, A. Ye Myakshina, T. N. Kuznetsov, A. N. |
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Kurbatova, Yu. A. Kurganova, I. N. Tiunov, A. V. Anichkin, A. Ye Myakshina, T. N. Kuznetsov, A. N. |
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| score |
7.3982687 |