Zobrazeno 1 - 10
of 20
pro vyhledávání: '"D.M. Kuzmina"'
Climate warming and increased precipitation and permafrost thaw in the Arctic are accompanied by an increase in the frequency of a full or partial drainage of thermokarst (thaw) lakes. After lake drainage, abundant plant communities on nutrient-rich
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d2efa98e1fc8b01110cafd667403f851
https://doi.org/10.5194/egusphere-egu21-15986
https://doi.org/10.5194/egusphere-egu21-15986
Autor:
Jan Karlsson, M. Tesfa, D. Payandi-Rolland, D.M. Kuzmina, Reiner Giesler, Liudmila S. Shirokova, A. G. Lim, Oleg S. Pokrovsky, Pascale Bénézeth
Publikováno v:
Science of the Total Environment
Science of the Total Environment, Elsevier, 2020, 749, pp.141463. ⟨10.1016/j.scitotenv.2020.141463⟩
Science of the Total Environment, 2020, 749, pp.141463. ⟨10.1016/j.scitotenv.2020.141463⟩
Science of the Total Environment, Elsevier, 2020, 749, pp.141463. ⟨10.1016/j.scitotenv.2020.141463⟩
Science of the Total Environment, 2020, 749, pp.141463. ⟨10.1016/j.scitotenv.2020.141463⟩
Arctic regions contain large amounts of organic carbon (OC) trapped in soil and wetland permafrost. With climate warming, part of this OC is released to aquatic systems and degraded by microorganisms, thus resulting in positive feedback due to carbon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::556b5469a80bca243d8392ef93d75e49
https://hal.archives-ouvertes.fr/hal-03004367/document
https://hal.archives-ouvertes.fr/hal-03004367/document
Publikováno v:
Plants
Volume 9
Issue 7
Plants, Vol 9, Iss 867, p 867 (2020)
Volume 9
Issue 7
Plants, Vol 9, Iss 867, p 867 (2020)
Climate warming, increased precipitation, and permafrost thaw in the Arctic are accompanied by an increase in the frequency of full or partial drainage of thermokarst lakes. After lake drainage, highly productive plant communities on nutrient-rich se
Autor:
Liudmila S. Shirokova, S.P. Kulizhsky, G.I. Istigechev, Sergey V. Loiko, Sergey N. Vorobyev, Oleg S. Pokrovsky, A. G. Lim, D.M. Kuzmina, R. M. Manasypov, T. V. Raudina
Publikováno v:
Science of the total environment. 2018. Vol. 634. P. 1004-1023
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, maximal hydraulic connectivity and element transport
Publikováno v:
Ukrainian Journal of Ecology, Vol 8, Iss 1, Pp 72-78 (2018)
Soil-forming rocks rock of the territory being researched consists of layers of polymict sands which is distinctly visible in the soil profile of present-day soil. The prevalent components of the sandy rocks are minerals resistant to weathering, name
Autor:
M. Tesfa, Oleg S. Pokrovsky, Reiner Giesler, D.M. Kuzmina, Jon Karlsson, Liudmila S. Shirokova, Geoscience, D. Payandi-Rolland, P. Bnzeth, A. G. Lim
Publikováno v:
Limnology and Freshwater Biology. :874-875
In Arctic regions, water bodies are hot spots of dissolved organic carbon (DOC) biodegradation, and their well-known large heterogeneity in the permafrost affected area could lead to a misrepresentation of their importance in the carbon (C) cycle. In
Autor:
S.P. Kulizhsky, D.M. Kuzmina, I. V. Kritskov, Alexandr Konstantinov, Sergey V. Loiko, G.I. Istigechev, A. G. Lim
Publikováno v:
International journal of environmental studies. 2015. Vol. 72, № 6. P. 1037-1046
We have investigated the low terraces of the Ob and Tom rivers in the south of Tomsk Oblast, primarily the Ob–Tom interfluve area. This area is situated near Seversk and Tomsk suburbs, where 70% of the Tomsk Oblast population is concentrated. Rapid
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.