Permafrost thaw and climate warming may decrease the CO2, carbon, and metal concentration in peat soil waters of the Western Siberia Lowland

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 from soils to rivers and lakes occurs via supra-p...

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Bibliographic Details

Published in:	Science of the total environment Vol. 634. P. 1004-1023
Other Authors:	Loiko, Sergey V., Lim, Artem G., Manasypov, Rinat M., Shirokova, Liudmila S., Istigechev, Georgy I., Kuzmina, Daria M., Kulizhsky, Sergey P., Vorobyev, Sergey N. биолог, Pokrovsky, Oleg S., Raudina, Tatiana V.
Format:	Article
Language:	English
Subjects:	углекислый газ метан вечная мерзлота потепление климата Западно-Сибирская низменность торфяные воды торфяные почвы статьи в журналах
Online Access:	http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000657607 Перейти в каталог НБ ТГУ