Oxygen regime of rivers in Volga,Ob, and Lena basins |
| |
Authors: | A V Goncharov V A Isaev E E Lobchenko I P Nichiporova |
| |
Institution: | 1.Moscow State University,Moscow,Russia;2.Hydrochemical Institute,Rostov-on-Don,Russia |
| |
Abstract: | A close negative correlation was found to exist between oxygen concentration in winter and the latitude in rivers in the basins
of the Ob and Volga. This can be explained by an increase in the duration of the freeze-up period (during which oxygen is
consumed for oxidation of organic matter (OM) in water and bottom sediments) in the direction from the south to the north,
while the input from oxygen from the atmosphere and photosynthesis is practically zero. No inverse relationship was found
to exist between dissolved oxygen and the latitude, because in rivers of mountain and semimountain types, typical of this
basin, organic matter (OM) does not accumulate in bottom sediments and the conditions of atmospheric circulation are better
than in lowland rivers. The magnitude of seasonal variations in oxygen in lowland rivers is greater than in mountain ones
because of an abrupt drop in oxygen concentration in slowly flowing rivers in winter and the saturation of their water by
oxygen from photosynthesis in summer. |
| |
Keywords: | |
本文献已被 SpringerLink 等数据库收录! |
|