Search

Published After
Published Before

Search Results

  • Studying floodplain roughness in an Upper Tisza study area
    85-90
    Views:
    179

    Floods slowing down due to the significant decrease of the gradient have considerable sediment accumulation capacity in the floodplain. The grade of accumulation is further increased if the width of the floodplain is not uniform as water flowing out of the narrow sections diverge and its speed is decreased. Surface roughness in a study area of 492 hectares in the Upper Tisza region was analysed based on CIR (color-infrared) orthophotos from 2007. An NDVI index layer was created first on which object-based image segmentation and threshold-based image classification were performed. The study area is dominated by land cover / land use types (grassland-shrubs, forest) with high roughness values. It was concluded that vegetation activity based analyses on their own are not enough for determining floodplain roughness.

  • Land use changes and their effect on floodplain aggradation along the Middle-Tisza River, Hungary
    1-10
    Views:
    62

    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.

  • Accumulation studies at specific sampling areas of the active floodplain in the Upper-Tisza region
    14-22
    Views:
    170

    In this paper the rate of accumulation was studied along four VO floodplain cross sections of the UpperTisza region between 1974 and 2014. VO floodplain cross sections are based on a mapping base-point grid (established in 1890), and they are located a few kilometers from each other. Furthermore, the roughness changes of different surface types, crossed by the VO floodplain cross-sections, were also determined between 1965 and 2015. The accumulation studies were extended to include the accumulation rates of the cut off meanders located along and/or close to the VO cross-sections. The roughness values increased in all four floodplain VO cross-sections since 1965; in two of them it reached or approximated 100 %. The average accumulation along the VO cross-sections was between 28 and 47 cm (0.73–1.23 cm/year) during the 38-year period. However, its areal distribution showed large differences. The highest values (169–309 cm, i.e. 4.44–8.13 cm/year) were found at the lowest points of the cut off meanders and swales in every case. The accumulation rate of the examined three cut off meanders near the floodplain cross-sections (140 and 1570 meters from the river bed) was lower (0.84–2.5 cm/year), but the study period was significantly longer (154 and 161 years, respectively). Comparing the values of the two periods, it is obvious that the accumulation of the active floodplain accelerates, presumably due to the significant increase of surface roughness.