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EN
The Ob River is one of the largest rivers in Russia and currently the most important traffic route in Western Siberia. The paper presents the history of water transport on the Ob River against the background of channel processes limiting the navigation on the river. The heterogeneity of the Ob River is determined by specific features of the channel processes and the stability of the riverbed, morphological types of the channel, the nature of deformations, long-term and seasonal changes of riffles and sections of the channel characterized by the presence of riffles. The main measures aimed at improving the navigational conditions of the Ob River include dredging of riffles, construction of dams and bypass channels.
EN
The paper presents the morphology and the long-term regime of riffles formed in the local widening of river channels: the Ob, the Northern Dvina, and the Ganges. Navigation maps for the last 120 years, detailed channel plans for the last 60 years as well as satellite images from 1977 and further were used to study the long-term regime of riffles. Five types of riffles are distinguished in the widening of river channels. Each type of riffles has a specific regime and a characteristic period of long-term reformations, with both the regime and the period being controlled by local surroundings of riffles. The presented study of the long-term regime of riffles and its relationship with local morphological conditions could be useful to optimize dredging works and, as a consequence, help to preserve optimal conditions of waterways.
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