Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016)
| Parent link: | Atmospheric and Oceanic Optics: Scientific Journal Vol. 30, iss. 3.— 2017.— [P. 277-283] |
|---|---|
| Corporate Author: | |
| Other Authors: | , , , , |
| Summary: | Title screen Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elementsin 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 partialpressure of carbon dioxide in water (to 240–350 [mi]atm) as compared to the partial pressure of CO2 in theatmosphere (about 385 [mi]atm) by the end of ice cover season. Hence, the CO2 flux can be directed only fromthe atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. Режим доступа: по договору с организацией-держателем ресурса |
| Language: | English |
| Published: |
2017
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| Subjects: | |
| Online Access: | https://doi.org/10.1134/S1024856017030058 |
| Format: | Electronic Book Chapter |
| KOHA link: | https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=655960 |
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| 200 | 1 | |a Carbon dioxide, oxygen, and biogenic elements in subglacial water in the littoral zone of Southern Baikal (2004–2016) |f V. M. Domysheva [et al.] | |
| 203 | |a Text |c electronic | ||
| 300 | |a Title screen | ||
| 320 | |a [References.: p. 282-283 (23 tit.)] | ||
| 330 | |a Results of the annual series of complex measurements of carbon dioxide, oxygen, and biogenic elementsin 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 partialpressure of carbon dioxide in water (to 240–350 [mi]atm) as compared to the partial pressure of CO2 in theatmosphere (about 385 [mi]atm) by the end of ice cover season. Hence, the CO2 flux can be directed only fromthe atmosphere to the water surface during the ice breakup in the littoral zone of Southern Baikal. | ||
| 333 | |a Режим доступа: по договору с организацией-держателем ресурса | ||
| 461 | |t Atmospheric and Oceanic Optics |o Scientific Journal | ||
| 463 | |t Vol. 30, iss. 3 |v [P. 277-283] |d 2017 | ||
| 610 | 1 | |a электронный ресурс | |
| 610 | 1 | |a труды учёных ТПУ | |
| 610 | 1 | |a Baikal | |
| 610 | 1 | |a carbon | |
| 610 | 1 | |a dioxide | |
| 610 | 1 | |a oxygen | |
| 610 | 1 | |a nitrates | |
| 610 | 1 | |a phosphates | |
| 610 | 1 | |a silicon | |
| 610 | 1 | |a ice period | |
| 610 | 1 | |a diurnal variation | |
| 610 | 1 | |a photosynthesis | |
| 610 | 1 | |a photosynthesis | |
| 610 | 1 | |a optical characteristics of the ice | |
| 610 | 1 | |a озеро Байкал | |
| 610 | 1 | |a углекислый газ | |
| 610 | 1 | |a кислород | |
| 610 | 1 | |a нитраты | |
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| 610 | 1 | |a суточные вариации | |
| 610 | 1 | |a фотосинтез | |
| 610 | 1 | |a оптические характеристики | |
| 610 | 1 | |a льды | |
| 701 | 1 | |a Domysheva |b V. M. |g Valentina Mikhaylovna | |
| 701 | 1 | |a Pestunov |b D. A. |c specialist in the field of electronics |c Associate Professor of Tomsk Polytechnic University, Candidate of technical sciences |f 1979- |g Dmitry Aleksandrovich |3 (RuTPU)RU\TPU\pers\32321 | |
| 701 | 1 | |a Sakirko |b M. V. |g Mariya Vladimirovna | |
| 701 | 1 | |a Shamrin |b A. M. |g Artyom Mikhaylovich | |
| 701 | 1 | |a Panchenko |b M. V. |g Mikhail Vasiljevich | |
| 712 | 0 | 2 | |a Национальный исследовательский Томский политехнический университет (ТПУ) |b Институт неразрушающего контроля (ИНК) |b Кафедра промышленной и медицинской электроники (ПМЭ) |3 (RuTPU)RU\TPU\col\18719 |
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