Diurnal dynamics of the СО2 concentration in water of the coastal zone of lake Baikal in the ice period (testing of the DIEL - CO2 method for assessment of lake metabolic rate) / M. V. Panchenko [et al.]

Уровень набора: (RuTPU)RU\TPU\network\12028, Proceedings of SPIEАльтернативный автор-лицо: Panchenko, M. V., Mikhail Vasiljevich;Domysheva, V. M., Valentina Mikhaylovna;Pestunov, D. A., specialist in the field of electronics, Associate Professor of Tomsk Polytechnic University, Candidate of technical sciences, 1979-, Dmitry Aleksandrovich;Sakirko, M. V., Mariya Vladimirovna;Ivanov, V. G., Vyacheslav Gennadjevich;Shamrin, A. M., Artyom MikhaylovichКоллективный автор (вторичный): Национальный исследовательский Томский политехнический университет, Инженерная школа неразрушающего контроля и безопасности, Отделение электронной инженерииЯзык: английский.Резюме или реферат: Results of three long cycles of 24-hour measurements of the carbon dioxide content in the surface and bottom water in the ice period of 2014-2016 in the Baikal coastal zone are analyzed. The diurnal dynamics of the СО2 concentration in the subglacial water, in which photosynthesis plays the leading role, is described. It is found that, in comparison with the surface subglacial water (that is, directly adjacent to the ice bottom), the more pronounced diurnal rhythm of СО2 is observed in the bottom layer in all realizations. This rhythm is well correlated with pyranometer readings. The data on the diurnal dynamics of СО2 are used to estimate the gross primary production in the bottom water with the DIEL method based on the analysis of temporal variability of the carbon dioxide concentration in water in situ..Аудитория: .Тематика: электронный ресурс | труды учёных ТПУ | Байкал | ледниковый период | углекислый газ | фотосинтез | чистая продукция Ресурсы он-лайн:Щелкните здесь для доступа в онлайн
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Results of three long cycles of 24-hour measurements of the carbon dioxide content in the surface and bottom water in the ice period of 2014-2016 in the Baikal coastal zone are analyzed. The diurnal dynamics of the СО2 concentration in the subglacial water, in which photosynthesis plays the leading role, is described. It is found that, in comparison with the surface subglacial water (that is, directly adjacent to the ice bottom), the more pronounced diurnal rhythm of СО2 is observed in the bottom layer in all realizations. This rhythm is well correlated with pyranometer readings. The data on the diurnal dynamics of СО2 are used to estimate the gross primary production in the bottom water with the DIEL method based on the analysis of temporal variability of the carbon dioxide concentration in water in situ.

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