Sources of Dissolved Organic Carbon in Rivers of the Yenisei River Basin


Дәйексөз келтіру

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Рұқсат жабық Тек жазылушылар үшін

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.

Авторлар туралы

A. Prokushkin

Sukachev Institute of Forestry, Siberian Branch; Siberian Federal University

Хат алмасуға жауапты Автор.
Email: prokushkin@ksc.krasn.ru
Ресей, Krasnoyarsk, 660036; Krasnoyarsk, 660041

O. Pokrovsky

Géosciences Environment Toulouse, Centre national de la recherché scientifique

Email: prokushkin@ksc.krasn.ru
Франция, Toulouse, 31400

M. Korets

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
Ресей, Krasnoyarsk, 660036

A. Rubtsov

Sukachev Institute of Forestry, Siberian Branch; Siberian Federal University

Email: prokushkin@ksc.krasn.ru
Ресей, Krasnoyarsk, 660036; Krasnoyarsk, 660041

S. Titov

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
Ресей, Krasnoyarsk, 660036

I. Tokareva

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
Ресей, Krasnoyarsk, 660036

R. Kolosov

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
Ресей, Krasnoyarsk, 660036

R. Amon

Texas Agriculture and Mechanical University at Galveston

Email: prokushkin@ksc.krasn.ru
АҚШ, Galveston, Texas, 77553

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