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


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详细

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.

作者简介

A. Prokushkin

Sukachev Institute of Forestry, Siberian Branch; Siberian Federal University

编辑信件的主要联系方式.
Email: prokushkin@ksc.krasn.ru
俄罗斯联邦, Krasnoyarsk, 660036; Krasnoyarsk, 660041

O. Pokrovsky

Géosciences Environment Toulouse, Centre national de la recherché scientifique

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

M. Korets

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
俄罗斯联邦, Krasnoyarsk, 660036

A. Rubtsov

Sukachev Institute of Forestry, Siberian Branch; Siberian Federal University

Email: prokushkin@ksc.krasn.ru
俄罗斯联邦, Krasnoyarsk, 660036; Krasnoyarsk, 660041

S. Titov

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
俄罗斯联邦, Krasnoyarsk, 660036

I. Tokareva

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
俄罗斯联邦, Krasnoyarsk, 660036

R. Kolosov

Sukachev Institute of Forestry, Siberian Branch

Email: prokushkin@ksc.krasn.ru
俄罗斯联邦, Krasnoyarsk, 660036

R. Amon

Texas Agriculture and Mechanical University at Galveston

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

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