Труды сотрудников ИЛ им. В.Н. Сукачева СО РАН

/ A. S. Prokushkin [et al.] // Dokl. Earth Sci. - 2018. - Vol. 480, Is. 2. - P763-766, DOI 10.1134/S1028334X18060077. - Cited References:14. - This work was supported by the Russian Science Foundation, project no. 14-24-00113. . - ISSN 1028-334X. - ISSN 1531-8354РУБ Geosciences, Multidisciplinary

Аннотация: The spatial and temporal variations in concentrations of dissolved organic carbon in the Yenisei River and its major tributaries are analyzed. The results obtained suggest that the maximal contribution to the flows of dissolved organic carbon in the Yenisei River is made by cryohydromorphic forest landscapes of the Central Siberian Plateau.

WOS,
Смотреть статью,
Scopus

Держатели документа:
Russian Acad Sci, Siberian Branch, Sukachev Inst Forestry, Krasnoyarsk 660036, Russia.
Siberian Fed Univ, Krasnoyarsk 660041, Russia.
CNRS, Geosci Environm Toulouse, F-31400 Toulouse, France.
Texas A&M Univ, Galveston, TX 77553 USA.

Доп.точки доступа:
Prokushkin, A. S.; Pokrovsky, O. S.; Korets, M. A.; Rubtsov, A. V.; Titov, S. V.; Tokareva, I. V.; Kolosov, R. A.; Amon, R. M. W.; Russian Science Foundation [14-24-00113]