Mapping Freshwater Carbonate Deposits by Using Ground-Penetrating Radar at Lake Kolon, Hungary

Freshwater carbonate deposit, as a special phenomenon in the Danube-Tisza Interfluve, located in the centre of Hungary, is a significant geological heritage in the Carpathian Basin. At present there is not any applicable method to investigate the presence of carbonate layers in an undisturbed way, a...

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Main Authors: Pécsi Eszter, Katona Orsolya, Barta Károly, Sipos György, Biró Csaba
Format: Article
Language:English
Published: University of Szeged 2014-11-01
Series:Journal of Environmental Geography
Subjects:
Online Access:https://doi.org/10.2478/jengeo-2014-0008
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author Pécsi Eszter
Katona Orsolya
Barta Károly
Sipos György
Biró Csaba
author_facet Pécsi Eszter
Katona Orsolya
Barta Károly
Sipos György
Biró Csaba
author_sort Pécsi Eszter
collection DOAJ
description Freshwater carbonate deposit, as a special phenomenon in the Danube-Tisza Interfluve, located in the centre of Hungary, is a significant geological heritage in the Carpathian Basin. At present there is not any applicable method to investigate the presence of carbonate layers in an undisturbed way, as neither vegetation nor morphological characteristics indicate unambiguously these formations. Ground-penetrating radar technology is widely used in various earth science related researches, and the number of applications is steadily increasing. The aim of the study was to determine the spatial extension of freshwater limestone using geophysical methods near Lake Kolon, Hungary. The lake, which is now a protected wetland area with opened water surfaces, was formed in the paleo-channel of the River Danube. Measurements were performed with the help of ground-penetrating radar, the results were calibrated by high spatial resolution drillings. Investigations have been made since 2012, and freshwater limestone was detected at several locations determining the more exact extension of the formation. Ground-penetrating radar proved to be an appropriate method to detect the compact and fragmented freshwater limestone layers in such an environment. However, based on the results the method can be best applied under dry soil or sediment conditions while the uncertainty of the results increases significantly as a matter of higher soil moisture. Further control measurements are necessary verified by several drillings in order to give an exact method to determine freshwater limestone.
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spelling doaj.art-0eb14fd0133e4376b55e3e40659ddccf2022-12-22T02:47:27ZengUniversity of SzegedJournal of Environmental Geography2060-467X2014-11-0173-4131910.2478/jengeo-2014-0008Mapping Freshwater Carbonate Deposits by Using Ground-Penetrating Radar at Lake Kolon, HungaryPécsi Eszter0Katona Orsolya1Barta Károly2Sipos György3Biró Csaba4Department of Physical Geography and Geoinformatics, University of Szeged, Egyetem u. 2-6, H-6722 Szeged, HungaryDepartment of Physical Geography and Geoinformatics, University of Szeged, Egyetem u. 2-6, H-6722 Szeged, HungaryDepartment of Physical Geography and Geoinformatics, University of Szeged, Egyetem u. 2-6, H-6722 Szeged, HungaryDepartment of Physical Geography and Geoinformatics, University of Szeged, Egyetem u. 2-6, H-6722 Szeged, HungaryDirectorate of Kiskunság National Park, Liszt F. u. 19, H-6000 Kecskemét, HungaryFreshwater carbonate deposit, as a special phenomenon in the Danube-Tisza Interfluve, located in the centre of Hungary, is a significant geological heritage in the Carpathian Basin. At present there is not any applicable method to investigate the presence of carbonate layers in an undisturbed way, as neither vegetation nor morphological characteristics indicate unambiguously these formations. Ground-penetrating radar technology is widely used in various earth science related researches, and the number of applications is steadily increasing. The aim of the study was to determine the spatial extension of freshwater limestone using geophysical methods near Lake Kolon, Hungary. The lake, which is now a protected wetland area with opened water surfaces, was formed in the paleo-channel of the River Danube. Measurements were performed with the help of ground-penetrating radar, the results were calibrated by high spatial resolution drillings. Investigations have been made since 2012, and freshwater limestone was detected at several locations determining the more exact extension of the formation. Ground-penetrating radar proved to be an appropriate method to detect the compact and fragmented freshwater limestone layers in such an environment. However, based on the results the method can be best applied under dry soil or sediment conditions while the uncertainty of the results increases significantly as a matter of higher soil moisture. Further control measurements are necessary verified by several drillings in order to give an exact method to determine freshwater limestone.https://doi.org/10.2478/jengeo-2014-0008freshwater limestoneground-penetrating radarlake kolondrilling
spellingShingle Pécsi Eszter
Katona Orsolya
Barta Károly
Sipos György
Biró Csaba
Mapping Freshwater Carbonate Deposits by Using Ground-Penetrating Radar at Lake Kolon, Hungary
Journal of Environmental Geography
freshwater limestone
ground-penetrating radar
lake kolon
drilling
title Mapping Freshwater Carbonate Deposits by Using Ground-Penetrating Radar at Lake Kolon, Hungary
title_full Mapping Freshwater Carbonate Deposits by Using Ground-Penetrating Radar at Lake Kolon, Hungary
title_fullStr Mapping Freshwater Carbonate Deposits by Using Ground-Penetrating Radar at Lake Kolon, Hungary
title_full_unstemmed Mapping Freshwater Carbonate Deposits by Using Ground-Penetrating Radar at Lake Kolon, Hungary
title_short Mapping Freshwater Carbonate Deposits by Using Ground-Penetrating Radar at Lake Kolon, Hungary
title_sort mapping freshwater carbonate deposits by using ground penetrating radar at lake kolon hungary
topic freshwater limestone
ground-penetrating radar
lake kolon
drilling
url https://doi.org/10.2478/jengeo-2014-0008
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