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Active point bar development and river bank erosion in the incising channel of the lower Tisza river, Hungary
Published December 20, 2019

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 th...e 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.

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Morphological alteration of the Dráva as the result of human impact
Published October 20, 2011

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.

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Land use changes and their effect on floodplain aggradation along the Middle-Tisza River, Hungary
Published March 21, 2019

Land-use changes and their effect on overbank sediment accumulation were investigated on the
floodplain of Middle-Tisza River. Military survey maps (1783, 1860, 1883 and 1890) and aerial
photos (1950, 1965, 1980 and 2000) were used to evaluate land-use changes and to calculate the
vegetational roughness of the area. To determinate the ...rate of overbank sedimentation sediment
samples were collected from a pit, the grain-size, content of organic matter, heavy metal content (Pb,
Cu, Zn, Ni and Cd) and pH were measured. Until 1950 meadows and pastures were typical on the
floodplain, gallery-forest was along the river, the oxbow-lake and the artificial levee. Notable landuse changes were detected in the second half of the 20th century, as the aerial photo taken in 1965
shows extensive forestry in the area. These land-use changes affected the average vegetational
roughness, as it has been doubled since the disappearance of grasslands. Land-use changes highly
affect the aggradation, as the increased roughness decreases the flood velocity on the floodplain,
causing accelerated aggradation. Using Pb marker horizons and grain-size changes the studied
sediment profile was compared to dated profiles (Braun et al. 2003), thus, the sediment accumulation
rate could be determined for the periods of 1858-1965 and 1965-2005. According to our
measurements the accumulation rate was doubled since 1965, very likely in connection with the
doubled vegetational roughness.

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