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  • Morphometric changes of the River Bodrog from the late 18th century to 2006
    28-40
    Views:
    30

    The river regulations of the 19th century have affected each of our rivers to a different degree. In the
    case of the River Bodrog it was stronger than the average. In our paper a section of the river between
    Bodroghalász and Szegi was examined, the extent and intensity of river channel changes was
    intended to be determined. The applied series of maps and aerial photos was georeferred and the river
    channel was vectorized. The morphometric parameters of the channel were measured and the changes
    were evaluated using the created database. From methodological aspect we concluded that the 9
    variables can be grouped into 3 factors therefore most of the indexes can be substituted. We measured
    the changes of length and lateral shift of the channel using GIS methods. Three development periods
    were identified based on our results. In the first period the development of the river was characterized
    by natural processes. Then, the development of the river altered owing to the antropogenic impacts. In
    this transient phase the average shifting of the channel was 7.43 m/y. In the third term this value
    reduces to 0.2 m/y as the river is getting to reach the equilibrium stage.

  • Morphology, sedimentology and origin of an anomalous cut-off along the Pravara river, deccan trap region, India
    23-43
    Views:
    256

    River meanders have always been an intriguing subject in fluvial geomorphology because of their ubiquity, dynamism, remarkable forms and practical consequences of their movement. Sometimes a relatively straight channel flowing over bedrock may develop a lone meander bend cut-off which is very out of the place from the surrounding area. The occurrence of a sudden bend along a river may not be a meandering bend but may be manifestation of sudden change in the river dynamism due to many reasons, such as, lithology, change in rainfall regime, tectonics etc. The formation of such features highlights the behavior of river in the past. One such striking feature has been observed along the River Pravara in the Deccan Trap Region, Maharashtra, India. Rivers in Deccan Trap Region do not meander and form cut-offs by rule. It is rocky country where rivers flow in deeply incised bedrock. Hence, the observed feature displays a striking anomaly in this region. Hence, an attempt has been made in the present paper to evaluate the mode of formation of this single cut-off along this channel. Morphological and sedimentological data were generated and analyzed for the channel loop and the link channel to understand the competence of the river in the past and present which were directly or indirectly responsible for the development of this channel anomaly in this reach. Based on the results of the analysis and intensive field observations, it has been inferred that this is a classic example of natural morphological adjustment of a river when a set of events occurred, first retardation of vertical erosion encountering bedrock followed by series of floods to induce the channel to divert from the original path to resume the present course. Presence of a tributary further aided to the process of the loop development. The study can provide additional knowledge to the studies involving anomalous channel cut-offs at any part of the world.

  • Morphological alteration of the Dráva as the result of human impact
    58-75
    Views:
    87

    The Croatian-Hungarian border section of the Dráva River has been undisturbed for almost a century, and it is characterised by unique fluvial morphology (braided pattern and islands) supporting rich habitats and wildlife. However, during the last decades human impact became more and more intensive. Between 1975 and 1989 three water reservoirs were built on the Croatian section of the river, just 16 km from the beginning of the border-section, altering the hydrology and the sediment characteristics of the river. On a local scale cut-offs, revetments and groynes were built. The aim of the study was to evaluate the effect of these human interventions. As the result of the alteration of the hydrology the channel pattern of the Dráva has been changing from braided to meandering, though on the upstream meandering part the territory and number of islands increased due to the drop of water stages. A cut-off and a groyne influenced only the morphology of a short section. As the result of the cut-off braided pattern became more pronounced, and the groyne caused intensive channel aggradation and gave way to lateral island development.

  • Active point bar development and river bank erosion in the incising channel of the lower Tisza river, Hungary
    13-28
    Views:
    205

    The development of point-bars and bank erosion are critical near-bank processes, as they indicate
    the sediment and hydraulic regime of a river system, thus, they refer to the equilibrium conditions of
    a channel. However, throughout history, rivers have been modified for various benefits which change
    the development of point-bars and the rate of bank erosion. In the Lower Tisza River (Hungary), river
    regulations influenced the channel and floodplain development, altering the natural fluvial processes.
    The aim of the research was to determine the rate of near-bank processes and to make trajectory for
    future river evolution to support future engineering works. The bank erosion and point-bar development
    at human-influenced and freely meandering sections of the Tisza River were monitored since 2011.
    Behind a collapsed revetment, the bank erosion rate was 0.6 m/y, while at a freely meandering section it
    was 2.3 m/y. The studied point-bars are located in revetted and freely meandering sections. Their surface
    eroded within the period. These intensive erosional processes refer to an incising meandering channel,
    which must be considered during future planning of in-channel structures (e.g. revetments, bridges),
    thus, geomorphic methods must be considered in any river engineering scheme.