Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016)
Abstract Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elements in the subglacial water in the littoral zone of the southern area of Lake Baikal, carried out from 2004 to 2016, are analyzed. It was found that the plankton photosynthetic activity signifi...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Domysheva, V. M. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2017 |
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| Übergeordnetes Werk: |
Enthalten in: Atmospheric and oceanic optics - Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009, 30(2017), 3 vom: Mai, Seite 277-283 |
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| Übergeordnetes Werk: |
volume:30 ; year:2017 ; number:3 ; month:05 ; pages:277-283 |
| Links: |
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| DOI / URN: |
10.1134/S1024856017030058 |
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| Katalog-ID: |
SPR026323427 |
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| 100 | 1 | |a Domysheva, V. M. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) |
| 264 | 1 | |c 2017 | |
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| 520 | |a Abstract Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elements in the subglacial water in the littoral zone of the southern area of Lake Baikal, carried out from 2004 to 2016, are analyzed. It was found that the plankton photosynthetic activity significantly decreases the partial pressure of carbon dioxide in water (to 240–350 μatm) as compared to the partial pressure of $ CO_{2} $ in the atmosphere (about 385 μatm) by the end of ice cover season. Hence, the $ CO_{2} $ flux can be directed only from the atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. | ||
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| 650 | 4 | |a carbon dioxide |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a oxygen |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a nitrates |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a phosphates |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a silicon |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a ice period |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a diurnal variation |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a photosynthesis |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a optical characteristics of the ice |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Pestunov, D. A. |4 aut | |
| 700 | 1 | |a Sakirko, M. V. |4 aut | |
| 700 | 1 | |a Shamrin, A. M. |4 aut | |
| 700 | 1 | |a Panchenko, M. V. |4 aut | |
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10.1134/S1024856017030058 doi (DE-627)SPR026323427 (SPR)S1024856017030058-e DE-627 ger DE-627 rakwb eng Domysheva, V. M. verfasserin aut Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elements in the subglacial water in the littoral zone of the southern area of Lake Baikal, carried out from 2004 to 2016, are analyzed. It was found that the plankton photosynthetic activity significantly decreases the partial pressure of carbon dioxide in water (to 240–350 μatm) as compared to the partial pressure of $ CO_{2} $ in the atmosphere (about 385 μatm) by the end of ice cover season. Hence, the $ CO_{2} $ flux can be directed only from the atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. Baikal (dpeaa)DE-He213 carbon dioxide (dpeaa)DE-He213 oxygen (dpeaa)DE-He213 nitrates (dpeaa)DE-He213 phosphates (dpeaa)DE-He213 silicon (dpeaa)DE-He213 ice period (dpeaa)DE-He213 diurnal variation (dpeaa)DE-He213 photosynthesis (dpeaa)DE-He213 optical characteristics of the ice (dpeaa)DE-He213 Pestunov, D. A. aut Sakirko, M. V. aut Shamrin, A. M. aut Panchenko, M. V. aut Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 30(2017), 3 vom: Mai, Seite 277-283 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:30 year:2017 number:3 month:05 pages:277-283 https://dx.doi.org/10.1134/S1024856017030058 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_101 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 30 2017 3 05 277-283 |
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10.1134/S1024856017030058 doi (DE-627)SPR026323427 (SPR)S1024856017030058-e DE-627 ger DE-627 rakwb eng Domysheva, V. M. verfasserin aut Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elements in the subglacial water in the littoral zone of the southern area of Lake Baikal, carried out from 2004 to 2016, are analyzed. It was found that the plankton photosynthetic activity significantly decreases the partial pressure of carbon dioxide in water (to 240–350 μatm) as compared to the partial pressure of $ CO_{2} $ in the atmosphere (about 385 μatm) by the end of ice cover season. Hence, the $ CO_{2} $ flux can be directed only from the atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. Baikal (dpeaa)DE-He213 carbon dioxide (dpeaa)DE-He213 oxygen (dpeaa)DE-He213 nitrates (dpeaa)DE-He213 phosphates (dpeaa)DE-He213 silicon (dpeaa)DE-He213 ice period (dpeaa)DE-He213 diurnal variation (dpeaa)DE-He213 photosynthesis (dpeaa)DE-He213 optical characteristics of the ice (dpeaa)DE-He213 Pestunov, D. A. aut Sakirko, M. V. aut Shamrin, A. M. aut Panchenko, M. V. aut Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 30(2017), 3 vom: Mai, Seite 277-283 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:30 year:2017 number:3 month:05 pages:277-283 https://dx.doi.org/10.1134/S1024856017030058 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_101 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 30 2017 3 05 277-283 |
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10.1134/S1024856017030058 doi (DE-627)SPR026323427 (SPR)S1024856017030058-e DE-627 ger DE-627 rakwb eng Domysheva, V. M. verfasserin aut Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elements in the subglacial water in the littoral zone of the southern area of Lake Baikal, carried out from 2004 to 2016, are analyzed. It was found that the plankton photosynthetic activity significantly decreases the partial pressure of carbon dioxide in water (to 240–350 μatm) as compared to the partial pressure of $ CO_{2} $ in the atmosphere (about 385 μatm) by the end of ice cover season. Hence, the $ CO_{2} $ flux can be directed only from the atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. Baikal (dpeaa)DE-He213 carbon dioxide (dpeaa)DE-He213 oxygen (dpeaa)DE-He213 nitrates (dpeaa)DE-He213 phosphates (dpeaa)DE-He213 silicon (dpeaa)DE-He213 ice period (dpeaa)DE-He213 diurnal variation (dpeaa)DE-He213 photosynthesis (dpeaa)DE-He213 optical characteristics of the ice (dpeaa)DE-He213 Pestunov, D. A. aut Sakirko, M. V. aut Shamrin, A. M. aut Panchenko, M. V. aut Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 30(2017), 3 vom: Mai, Seite 277-283 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:30 year:2017 number:3 month:05 pages:277-283 https://dx.doi.org/10.1134/S1024856017030058 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_101 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 30 2017 3 05 277-283 |
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10.1134/S1024856017030058 doi (DE-627)SPR026323427 (SPR)S1024856017030058-e DE-627 ger DE-627 rakwb eng Domysheva, V. M. verfasserin aut Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elements in the subglacial water in the littoral zone of the southern area of Lake Baikal, carried out from 2004 to 2016, are analyzed. It was found that the plankton photosynthetic activity significantly decreases the partial pressure of carbon dioxide in water (to 240–350 μatm) as compared to the partial pressure of $ CO_{2} $ in the atmosphere (about 385 μatm) by the end of ice cover season. Hence, the $ CO_{2} $ flux can be directed only from the atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. Baikal (dpeaa)DE-He213 carbon dioxide (dpeaa)DE-He213 oxygen (dpeaa)DE-He213 nitrates (dpeaa)DE-He213 phosphates (dpeaa)DE-He213 silicon (dpeaa)DE-He213 ice period (dpeaa)DE-He213 diurnal variation (dpeaa)DE-He213 photosynthesis (dpeaa)DE-He213 optical characteristics of the ice (dpeaa)DE-He213 Pestunov, D. A. aut Sakirko, M. V. aut Shamrin, A. M. aut Panchenko, M. V. aut Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 30(2017), 3 vom: Mai, Seite 277-283 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:30 year:2017 number:3 month:05 pages:277-283 https://dx.doi.org/10.1134/S1024856017030058 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_101 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 30 2017 3 05 277-283 |
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10.1134/S1024856017030058 doi (DE-627)SPR026323427 (SPR)S1024856017030058-e DE-627 ger DE-627 rakwb eng Domysheva, V. M. verfasserin aut Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2017 Abstract Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elements in the subglacial water in the littoral zone of the southern area of Lake Baikal, carried out from 2004 to 2016, are analyzed. It was found that the plankton photosynthetic activity significantly decreases the partial pressure of carbon dioxide in water (to 240–350 μatm) as compared to the partial pressure of $ CO_{2} $ in the atmosphere (about 385 μatm) by the end of ice cover season. Hence, the $ CO_{2} $ flux can be directed only from the atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. Baikal (dpeaa)DE-He213 carbon dioxide (dpeaa)DE-He213 oxygen (dpeaa)DE-He213 nitrates (dpeaa)DE-He213 phosphates (dpeaa)DE-He213 silicon (dpeaa)DE-He213 ice period (dpeaa)DE-He213 diurnal variation (dpeaa)DE-He213 photosynthesis (dpeaa)DE-He213 optical characteristics of the ice (dpeaa)DE-He213 Pestunov, D. A. aut Sakirko, M. V. aut Shamrin, A. M. aut Panchenko, M. V. aut Enthalten in Atmospheric and oceanic optics Dordrecht [u.a.] : Springer Science + Business Media B.V, 2009 30(2017), 3 vom: Mai, Seite 277-283 (DE-627)599674695 (DE-600)2493873-7 2070-0393 nnns volume:30 year:2017 number:3 month:05 pages:277-283 https://dx.doi.org/10.1134/S1024856017030058 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_101 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 30 2017 3 05 277-283 |
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Enthalten in Atmospheric and oceanic optics 30(2017), 3 vom: Mai, Seite 277-283 volume:30 year:2017 number:3 month:05 pages:277-283 |
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Enthalten in Atmospheric and oceanic optics 30(2017), 3 vom: Mai, Seite 277-283 volume:30 year:2017 number:3 month:05 pages:277-283 |
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Baikal carbon dioxide oxygen nitrates phosphates silicon ice period diurnal variation photosynthesis optical characteristics of the ice |
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Atmospheric and oceanic optics |
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Domysheva, V. M. @@aut@@ Pestunov, D. A. @@aut@@ Sakirko, M. V. @@aut@@ Shamrin, A. M. @@aut@@ Panchenko, M. V. @@aut@@ |
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Domysheva, V. M. |
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Domysheva, V. M. misc Baikal misc carbon dioxide misc oxygen misc nitrates misc phosphates misc silicon misc ice period misc diurnal variation misc photosynthesis misc optical characteristics of the ice Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) |
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Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) Baikal (dpeaa)DE-He213 carbon dioxide (dpeaa)DE-He213 oxygen (dpeaa)DE-He213 nitrates (dpeaa)DE-He213 phosphates (dpeaa)DE-He213 silicon (dpeaa)DE-He213 ice period (dpeaa)DE-He213 diurnal variation (dpeaa)DE-He213 photosynthesis (dpeaa)DE-He213 optical characteristics of the ice (dpeaa)DE-He213 |
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Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) |
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Domysheva, V. M. Pestunov, D. A. Sakirko, M. V. Shamrin, A. M. Panchenko, M. V. |
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carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of southern baikal (2004–2016) |
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Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) |
| abstract |
Abstract Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elements in the subglacial water in the littoral zone of the southern area of Lake Baikal, carried out from 2004 to 2016, are analyzed. It was found that the plankton photosynthetic activity significantly decreases the partial pressure of carbon dioxide in water (to 240–350 μatm) as compared to the partial pressure of $ CO_{2} $ in the atmosphere (about 385 μatm) by the end of ice cover season. Hence, the $ CO_{2} $ flux can be directed only from the atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. © Pleiades Publishing, Ltd. 2017 |
| abstractGer |
Abstract Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elements in the subglacial water in the littoral zone of the southern area of Lake Baikal, carried out from 2004 to 2016, are analyzed. It was found that the plankton photosynthetic activity significantly decreases the partial pressure of carbon dioxide in water (to 240–350 μatm) as compared to the partial pressure of $ CO_{2} $ in the atmosphere (about 385 μatm) by the end of ice cover season. Hence, the $ CO_{2} $ flux can be directed only from the atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. © Pleiades Publishing, Ltd. 2017 |
| abstract_unstemmed |
Abstract Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elements in the subglacial water in the littoral zone of the southern area of Lake Baikal, carried out from 2004 to 2016, are analyzed. It was found that the plankton photosynthetic activity significantly decreases the partial pressure of carbon dioxide in water (to 240–350 μatm) as compared to the partial pressure of $ CO_{2} $ in the atmosphere (about 385 μatm) by the end of ice cover season. Hence, the $ CO_{2} $ flux can be directed only from the atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. © Pleiades Publishing, Ltd. 2017 |
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Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) |
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https://dx.doi.org/10.1134/S1024856017030058 |
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Pestunov, D. A. Sakirko, M. V. Shamrin, A. M. Panchenko, M. V. |
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|
| score |
7.4011316 |