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Authors:
Byzaakay, Arysia A. |
Kolesnichenko, Larisa G. |
Kolesnichenko, Yuri Y. |
Khovalyg, Aldynai O. |
Raudina, Tatiana V. |
Prokushkin, Anatoly S. |
Lushchaeva, Inna V. |
Kvasnikova, Zoya N. |
Vorobyev, Sergey N. (биолог) |
Pokrovsky, Oleg S. |
Kirpotin, Sergey N.
Source: Water. 2023. Vol. 15, № 19. P. 3411 (1-26)
Type: статьи в журналах
Date: 2023
Description:
The carbon (C) cycle in inland waters, including carbon concentrations in and carbon dioxide (CO2 ) emissions from water surfaces, are at the forefront of biogeochemical studies, especially in regions
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Authors:
Loiko, Sergey V. |
Lim, A. G. |
Manasypov, Rinat M. |
Shirokova, Liudmila S. |
Istigechev, G. I. |
Kuzmina, D. M. |
Kulizhsky, Sergey P. |
Vorobyev, Sergey N. (биолог) |
Pokrovsky, Oleg S. |
Raudina, Tatiana V.
Source: Science of the total environment. 2018. Vol. 634. P. 1004-1023
Type: статьи в журналах
Date: 2018
Description:
Soil pore waters are a vital component of the ecosystem as they are efficient tracers of mineral weathering, plant litter leaching, and nutrient uptake by vegetation. In the permafrost environment, ma
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Authors:
Lushchaeva, Inna V. |
Morgaleva, Tamara G. |
Kolesnichenko, Larisa G. |
Loiko, Sergey V. |
Kritskov, I. V. |
Lim, A. G. |
Raudina, Tatiana V. |
Volkova, Irina I. |
Shirokova, Liudmila S. |
Morgalev, Sergei Yu. |
Vorobyev, Sergey N. (биолог) |
Kirpotin, Sergey N. |
Pokrovsky, Oleg S. |
Morgalev, Yuri N.
Source: Polar biology. 2017. Vol. 40, № 8. P. 1645-1659
Type: статьи в журналах
Date: 2017
Description:
The microbial activity in the soils of the permafrost-affected zones is assumed to be one of the major factors that modify the organic carbon and nitrogen cycle under current climate change. In contra
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Authors:
Raudina, Tatiana V. |
Lim, A. G. |
Kritskov, I. V. |
Shirokova, Liudmila S. |
Istigechev, G. I. |
Kuzmina, D. M. |
Kulizhsky, Sergey P. |
Vorobyev, Sergey N. (биолог) |
Pokrovsky, Oleg S. |
Loiko, Sergey V.
Source: Biogeosciences. 2017. Vol. 14, № 14. P. 3561-3584
Type: статьи в журналах
Date: 2017
Description:
Mobilization of dissolved organic carbon (DOC) and related trace elements (TEs) from the frozen peat to surface waters in the permafrost zone is expected to enhance under ongoing permafrost thaw and a
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