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...

Full description

Bibliographic Details
Main Authors: Ante Pavičić, Davor Benamatić, Damir Pešt, Marijan Marasović
Format: Article
Language:English
Published: Croatian Geological Survey 2002-06-01
Series:Geologia Croatica
Subjects:
Online Access:http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/247
id doaj-b42e885d319b4afb9511b946082fa51f
record_format Article
spelling 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 &lt;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) &Ograve;pressure&Oacute; could be the construction of a</div><div>horizontal &Ograve;vent&Oacute; 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 &lt;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) &Ograve;pressure&Oacute; could be the construction of a</div><div>horizontal &Ograve;vent&Oacute; 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
work_keys_str_mv AT antepavicic waterreservoirwithinthekarstfieldoverburdengusicpoljecroatia
AT davorbenamatic waterreservoirwithinthekarstfieldoverburdengusicpoljecroatia
AT damirpest waterreservoirwithinthekarstfieldoverburdengusicpoljecroatia
AT marijanmarasovic waterreservoirwithinthekarstfieldoverburdengusicpoljecroatia
_version_ 1725093410114633728