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  • Investigation of the wind power potential of the Hernád valley
    93-107
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    43

    The University of Debrecen, Department of Meteorology has carried out research into the climatic and social-economic conditions of the Hernád valley in the scope of a scientific project (OTKA K 75794) between 2009 and 2012. The aim is to find out the optimal area for wind and solar energy, as well as biomass utilization. Our purpose is to work out a model wherein the complex evaluation of natural and social-economic conditions and effects can eventually result in a sustainable and conflictfree land use. The results of the research will be useful in working out a regional improvement based on the use of renewable energy sources to help the local decision-making process.

  • 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.