Hydrogeological conditions of the Kroparica recharge area, Jelovica, Slovenia

Eastern part of highly karstified plateau of Jelovica (west Slovenia) that represents big fissured and karstified aquifer is drained by the group of Kroparica springs that are positioned approximately 1 km in the south of the city Kropa. Kroparica is represented by several springs that mainly flow o...

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Main Author: Mihael Brenčič
Format: Article
Language:English
Published: Geological Survey of Slovenia 2003-12-01
Series:Geologija
Subjects:
Online Access:http://www.geologija-revija.si/dokument.aspx?id=543
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author Mihael Brenčič
author_facet Mihael Brenčič
author_sort Mihael Brenčič
collection DOAJ
description Eastern part of highly karstified plateau of Jelovica (west Slovenia) that represents big fissured and karstified aquifer is drained by the group of Kroparica springs that are positioned approximately 1 km in the south of the city Kropa. Kroparica is represented by several springs that mainly flow out from the triasic Ba~a dolomite. Some of them are positioned in the hill slope sediments. In the article litostratigraphical and structural conditions in the background of the springs are represented together with simple hydrogeologicalbalance of Kroparica aquifer recharge. It was determined that the recharge area is between 3,8 and 6,5 km2 and that the average yearly outflow is between 224 and 386 l/s. Maximum outflows are much larger and are higher than some m3/s. High fluctuation of discharges are the consequence of high karstification level of Kroparica aquifer.
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spelling doaj.art-4005335e8ad144488fd4de869e3acc2e2023-01-23T08:10:14ZengGeological Survey of SloveniaGeologija0016-77891854-620X2003-12-01462281306Hydrogeological conditions of the Kroparica recharge area, Jelovica, SloveniaMihael BrenčičEastern part of highly karstified plateau of Jelovica (west Slovenia) that represents big fissured and karstified aquifer is drained by the group of Kroparica springs that are positioned approximately 1 km in the south of the city Kropa. Kroparica is represented by several springs that mainly flow out from the triasic Ba~a dolomite. Some of them are positioned in the hill slope sediments. In the article litostratigraphical and structural conditions in the background of the springs are represented together with simple hydrogeologicalbalance of Kroparica aquifer recharge. It was determined that the recharge area is between 3,8 and 6,5 km2 and that the average yearly outflow is between 224 and 386 l/s. Maximum outflows are much larger and are higher than some m3/s. High fluctuation of discharges are the consequence of high karstification level of Kroparica aquifer.http://www.geologija-revija.si/dokument.aspx?id=543karstic springkarstic aquiferhydrogeologygeomorphologyKroparicaJelovicaSlovenia
spellingShingle Mihael Brenčič
Hydrogeological conditions of the Kroparica recharge area, Jelovica, Slovenia
Geologija
karstic spring
karstic aquifer
hydrogeology
geomorphology
Kroparica
Jelovica
Slovenia
title Hydrogeological conditions of the Kroparica recharge area, Jelovica, Slovenia
title_full Hydrogeological conditions of the Kroparica recharge area, Jelovica, Slovenia
title_fullStr Hydrogeological conditions of the Kroparica recharge area, Jelovica, Slovenia
title_full_unstemmed Hydrogeological conditions of the Kroparica recharge area, Jelovica, Slovenia
title_short Hydrogeological conditions of the Kroparica recharge area, Jelovica, Slovenia
title_sort hydrogeological conditions of the kroparica recharge area jelovica slovenia
topic karstic spring
karstic aquifer
hydrogeology
geomorphology
Kroparica
Jelovica
Slovenia
url http://www.geologija-revija.si/dokument.aspx?id=543
work_keys_str_mv AT mihaelbrencic hydrogeologicalconditionsofthekroparicarechargeareajelovicaslovenia