Zobrazeno 1 - 5
of 5
pro vyhledávání: '"D M Kuzmina"'
Autor:
T. V. Raudina, S. V. Loiko, A. G. Lim, I. V. Krickov, L. S. Shirokova, G. I. Istigechev, D. M. Kuzmina, S. P. Kulizhsky, S. N. Vorobyev, O. S. Pokrovsky
Publikováno v:
Biogeosciences, Vol 14, Pp 3561-3584 (2017)
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 active layer thickness (ALT) deepening in high-l
Externí odkaz:
https://doaj.org/article/02384a456cfb4aa7b638eccc30f2efee
Publikováno v:
IOP Conference Series: Earth and Environmental Science. 862:012062
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::60a16dae509b5f1d9c47da4eebff906c
https://doi.org/10.1088/1755-1315/862/1/012062
https://doi.org/10.1088/1755-1315/862/1/012062
Publikováno v:
Ukrainian Journal of Ecology. 7:414-423
In the article, the main results of the study of dissolved greenhouse gases (CO2, CH4), dissolved organic carbon (DOC) and colloidal trace elements-metals in surface and soil waters of hollows, depressions, permafrost subsidences are considered. Thes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae55ba89e68278c01df1e552be5cd4cf
https://doi.org/10.15421/2017_136
https://doi.org/10.15421/2017_136
Publikováno v:
Ukrainian Journal of Ecology, Vol 7, Iss 4, Pp 414-423 (2017)
In the article, the main results of the study of dissolved greenhouse gases (CO2, CH4), dissolved organic carbon (DOC) and colloidal trace elements-metals in surface and soil waters of hollows, depressions, permafrost subsidences are considered. Thes
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doajarticles::cdf4b130a00f64098ed31a13859d1005
http://ojs.mdpu.org.ua/index.php/biol/article/view/2073
http://ojs.mdpu.org.ua/index.php/biol/article/view/2073
Autor:
T V, Raudina, S V, Loiko, A, Lim, R M, Manasypov, L S, Shirokova, G I, Istigechev, D M, Kuzmina, S P, Kulizhsky, S N, Vorobyev, O S, Pokrovsky
Publikováno v:
The Science of the total environment. 634
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=pmid________::75efa3384395a6a9f1a58bc4f523a102
https://pubmed.ncbi.nlm.nih.gov/29660859
https://pubmed.ncbi.nlm.nih.gov/29660859