Water Reservoir Within the Karst Field Overburden: Gusić Polje, Croatia
<div>The Gusić reservoir is a compensation basin constructed in the karst</div><div>field. The reservoir lies on a Quaternary overburden free of ponors</div><div>(sinkholes) and suffosions. After the reservoir filling the water losses</div><div>were up to &a...
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Croatian Geological Survey
2002-06-01
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doaj-b42e885d319b4afb9511b946082fa51f2020-11-25T01:30:08ZengCroatian Geological SurveyGeologia Croatica1330-030X1333-48752002-06-015519310010.4154/GC.2002.09160Water Reservoir Within the Karst Field Overburden: Gusić Polje, CroatiaAnte Pavičić0Davor Benamatić1Damir Pešt2Marijan Marasović3Croatian Geological SurveyMOHOElektroprojektElektroprojekt<div>The Gusić reservoir is a compensation basin constructed in the karst</div><div>field. The reservoir lies on a Quaternary overburden free of ponors</div><div>(sinkholes) and suffosions. After the reservoir filling the water losses</div><div>were up to <6.4 m3/s. The bottom impermeability has been ensured</div><div>with a 0.4 m thick clay base blanket. During reservoir exploitation,</div><div>suffosions and ponors developed through which 2 m3/s water was</div><div>lost. Such conditions required reservoir repair within a short time</div><div>frame of approximately 10 days during which the power plant was</div><div>shut down. When the reservoir was emptied, a resistivity sounding</div><div>(Wenner electrodes arrangement at five depth levels) was conducted</div><div>on the reservoir bottom and clay blanket. An alternative concept has</div><div>also been considered - the construction of a new reservoir area that</div><div>has similar hydrogeological conditions. The solution for the possible</div><div>impact of groundwater (air) ÒpressureÓ could be the construction of a</div><div>horizontal ÒventÓ in the deepest part of the palaeodepression, where</div><div>the bedrock karstification is the most intensive and the interrelation</div><div>between groundwater and air pressure on the overburden is possible.</div><div>The reservoir bottom impermeability could be resolved with a clay</div><div>blanket or with synthetic materials.</div>http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/247Surface water reservoirKarstWater lossesGeophysical investigationGusić poljeCroatia |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Ante Pavičić Davor Benamatić Damir Pešt Marijan Marasović |
spellingShingle |
Ante Pavičić Davor Benamatić Damir Pešt Marijan Marasović Water Reservoir Within the Karst Field Overburden: Gusić Polje, Croatia Geologia Croatica Surface water reservoir Karst Water losses Geophysical investigation Gusić polje Croatia |
author_facet |
Ante Pavičić Davor Benamatić Damir Pešt Marijan Marasović |
author_sort |
Ante Pavičić |
title |
Water Reservoir Within the Karst Field Overburden: Gusić Polje, Croatia |
title_short |
Water Reservoir Within the Karst Field Overburden: Gusić Polje, Croatia |
title_full |
Water Reservoir Within the Karst Field Overburden: Gusić Polje, Croatia |
title_fullStr |
Water Reservoir Within the Karst Field Overburden: Gusić Polje, Croatia |
title_full_unstemmed |
Water Reservoir Within the Karst Field Overburden: Gusić Polje, Croatia |
title_sort |
water reservoir within the karst field overburden: gusić polje, croatia |
publisher |
Croatian Geological Survey |
series |
Geologia Croatica |
issn |
1330-030X 1333-4875 |
publishDate |
2002-06-01 |
description |
<div>The Gusić reservoir is a compensation basin constructed in the karst</div><div>field. The reservoir lies on a Quaternary overburden free of ponors</div><div>(sinkholes) and suffosions. After the reservoir filling the water losses</div><div>were up to <6.4 m3/s. The bottom impermeability has been ensured</div><div>with a 0.4 m thick clay base blanket. During reservoir exploitation,</div><div>suffosions and ponors developed through which 2 m3/s water was</div><div>lost. Such conditions required reservoir repair within a short time</div><div>frame of approximately 10 days during which the power plant was</div><div>shut down. When the reservoir was emptied, a resistivity sounding</div><div>(Wenner electrodes arrangement at five depth levels) was conducted</div><div>on the reservoir bottom and clay blanket. An alternative concept has</div><div>also been considered - the construction of a new reservoir area that</div><div>has similar hydrogeological conditions. The solution for the possible</div><div>impact of groundwater (air) ÒpressureÓ could be the construction of a</div><div>horizontal ÒventÓ in the deepest part of the palaeodepression, where</div><div>the bedrock karstification is the most intensive and the interrelation</div><div>between groundwater and air pressure on the overburden is possible.</div><div>The reservoir bottom impermeability could be resolved with a clay</div><div>blanket or with synthetic materials.</div> |
topic |
Surface water reservoir Karst Water losses Geophysical investigation Gusić polje Croatia |
url |
http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/247 |
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