Difference between revisions of "Holbina-Dunavat"

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(New page: =Holbina-Dunavat= <googlemap version="0.9" lat="44.8933364790133" lon="29.1226959228516" zoom="13" width="100%" height="400" scale="yes" overview="yes" toc="no" controls="large"> (A) 44.8...)
 
(Site description)
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==Site description==
 
==Site description==
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The Dunavat - Dranov region is a large depression, filled with peat, between two minor Danube distributaries. Both distributaries, presently the Dranov and Dunavat canals, flow from the Sf. Gheorghe Danube branch to the former Razim lagoon.
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The region was profoundly influenced by human activity in the 20th century. The Razim lagoon was cut off from the Black Sea and was changed into a fresh water reservoir with a raised water level. The isolated central peat area in the Dunavat - Dranov region was opened up to boats and to river water by an artificial canal system. The incoming river water from the Danube underwent a strong increase in nutrient contents, causing eutrophication of valuable mesotrophic water systems. Fish farm basins were constructed with ring dikes and pumping stations, a high-tension electric power line and some fish collection platforms with management buildings. The reed beds and peat soil in the fish farm basins were destroyed, causing a.o. a land subsidence with 0.5 - 1.0 meter.
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==Measures selection==
 
==Measures selection==
  

Revision as of 06:25, 26 May 2010

Holbina-Dunavat


Factsheet:

General
Country
River Name
Site Name
River Characterisation
    River typology
    Location (Lat Lon) ,
    Altitude
    Catchment area
    Geology
    National code/
    River type name

    Biological quality elements
    Ecosystem Services
    EU Directives
    Pressures
    Measures
    Other
    Project size
    Approximate costs
    Synergy
    Status
    Period of realization
    Evaluation


    Key features of the case study

    Site description

    The Dunavat - Dranov region is a large depression, filled with peat, between two minor Danube distributaries. Both distributaries, presently the Dranov and Dunavat canals, flow from the Sf. Gheorghe Danube branch to the former Razim lagoon. The region was profoundly influenced by human activity in the 20th century. The Razim lagoon was cut off from the Black Sea and was changed into a fresh water reservoir with a raised water level. The isolated central peat area in the Dunavat - Dranov region was opened up to boats and to river water by an artificial canal system. The incoming river water from the Danube underwent a strong increase in nutrient contents, causing eutrophication of valuable mesotrophic water systems. Fish farm basins were constructed with ring dikes and pumping stations, a high-tension electric power line and some fish collection platforms with management buildings. The reed beds and peat soil in the fish farm basins were destroyed, causing a.o. a land subsidence with 0.5 - 1.0 meter.

    Measures selection

    Success criteria

    Ecological response

    Hydromorphological response

    Monitoring before and after implementation of the project

    Socio-economic aspects

    Contact person within the organization

    Marian Tudor

    Extra background information

    References


    Related Measures

      No measures have been assigned to this project.

    Related Pressures