ARTYKUŁY NAUKOWE Występowanie i reżim Źródeł szczaw i wód kwasowęglowych w zlewni górnej Muszynki
Occurrence and regimes of carbonated waters and carbonic acid water in the upper Muszynka River basin.A b s t r a c t. CO2-reach springs are the natural treasure of the Polish Carpathians, including the research region (ca. 11.5 km2) of the Muszynka River basin, located in the areas of Tylicz-Spa an...
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ftjgq:oai:geojournals.pgi.gov.pl:article/27036 2024-09-09T19:36:07+00:00 ARTYKUŁY NAUKOWE Występowanie i reżim Źródeł szczaw i wód kwasowęglowych w zlewni górnej Muszynki Buczyński, Sebastian Modelska, Magdalena Wcisło, Marek 2017-01-20 application/pdf https://gq.pgi.gov.pl/pg/article/view/27036 pol pol Państwowy Instytut Geologiczny - PIB https://gq.pgi.gov.pl/pg/article/view/27036/18757 https://gq.pgi.gov.pl/pg/article/view/27036 Copyright (c) 2020 Przegląd Geologiczny Przegląd Geologiczny; Vol. 65 No. 1 (2017); 23 - 31 Przegląd Geologiczny; Tom 65 Nr 1 (2017); 23 - 31 0033-2151 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion artykuł naukowy 2017 ftjgq 2024-07-30T03:29:09Z Occurrence and regimes of carbonated waters and carbonic acid water in the upper Muszynka River basin.A b s t r a c t. CO2-reach springs are the natural treasure of the Polish Carpathians, including the research region (ca. 11.5 km2) of the Muszynka River basin, located in the areas of Tylicz-Spa and Krynica-Spa with developed mineral water industry. Previous investigations suggest that springs are partially vanishing or their hydrochemical and hydrodynamic regime is disturbed. To clear this problem, the authors analyzed periodical or stationary measurements made in the course of documenting, water producer operation, and own observations within a period of good data availability (1973–2014) for CO2-rich springs. The springs investigated in the Tylicz region are characterized by a variable and strongly time-dependent CO2 content (ranging from 352 mg/dm3 to 3 g/dm3). The discharge is relatively low and rarely exceeds 0.05 dm3/s. The research results show disappearance of two springs (T-10 and T-15) within the period of interest. Massive floods (in 1997, 1998, 2002–2004, 2010) are indicated as the probable main reason. In another three springs (T-13, T-14, T-17) the CO2 content dropped below 250 mg/dm3. The stationary measurements of two springs (Zdrój Główny and Bradowiec in Tylicz) allow concluding about poor correlation between investigated parameters (temperature, pH, CO2 content, electrical conductivity) and apparent influence of meteorological agents. Potential anthropogenic agents (borehole discharge, digging works) probably do not influence the CO2-rich spring regime or it has not been detected yet. Article in Journal/Newspaper Carbonic acid Geological Quarterly |
institution |
Open Polar |
collection |
Geological Quarterly |
op_collection_id |
ftjgq |
language |
Polish |
description |
Occurrence and regimes of carbonated waters and carbonic acid water in the upper Muszynka River basin.A b s t r a c t. CO2-reach springs are the natural treasure of the Polish Carpathians, including the research region (ca. 11.5 km2) of the Muszynka River basin, located in the areas of Tylicz-Spa and Krynica-Spa with developed mineral water industry. Previous investigations suggest that springs are partially vanishing or their hydrochemical and hydrodynamic regime is disturbed. To clear this problem, the authors analyzed periodical or stationary measurements made in the course of documenting, water producer operation, and own observations within a period of good data availability (1973–2014) for CO2-rich springs. The springs investigated in the Tylicz region are characterized by a variable and strongly time-dependent CO2 content (ranging from 352 mg/dm3 to 3 g/dm3). The discharge is relatively low and rarely exceeds 0.05 dm3/s. The research results show disappearance of two springs (T-10 and T-15) within the period of interest. Massive floods (in 1997, 1998, 2002–2004, 2010) are indicated as the probable main reason. In another three springs (T-13, T-14, T-17) the CO2 content dropped below 250 mg/dm3. The stationary measurements of two springs (Zdrój Główny and Bradowiec in Tylicz) allow concluding about poor correlation between investigated parameters (temperature, pH, CO2 content, electrical conductivity) and apparent influence of meteorological agents. Potential anthropogenic agents (borehole discharge, digging works) probably do not influence the CO2-rich spring regime or it has not been detected yet. |
format |
Article in Journal/Newspaper |
author |
Buczyński, Sebastian Modelska, Magdalena Wcisło, Marek |
spellingShingle |
Buczyński, Sebastian Modelska, Magdalena Wcisło, Marek ARTYKUŁY NAUKOWE Występowanie i reżim Źródeł szczaw i wód kwasowęglowych w zlewni górnej Muszynki |
author_facet |
Buczyński, Sebastian Modelska, Magdalena Wcisło, Marek |
author_sort |
Buczyński, Sebastian |
title |
ARTYKUŁY NAUKOWE Występowanie i reżim Źródeł szczaw i wód kwasowęglowych w zlewni górnej Muszynki |
title_short |
ARTYKUŁY NAUKOWE Występowanie i reżim Źródeł szczaw i wód kwasowęglowych w zlewni górnej Muszynki |
title_full |
ARTYKUŁY NAUKOWE Występowanie i reżim Źródeł szczaw i wód kwasowęglowych w zlewni górnej Muszynki |
title_fullStr |
ARTYKUŁY NAUKOWE Występowanie i reżim Źródeł szczaw i wód kwasowęglowych w zlewni górnej Muszynki |
title_full_unstemmed |
ARTYKUŁY NAUKOWE Występowanie i reżim Źródeł szczaw i wód kwasowęglowych w zlewni górnej Muszynki |
title_sort |
artykuły naukowe występowanie i reżim źródeł szczaw i wód kwasowęglowych w zlewni górnej muszynki |
publisher |
Państwowy Instytut Geologiczny - PIB |
publishDate |
2017 |
url |
https://gq.pgi.gov.pl/pg/article/view/27036 |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_source |
Przegląd Geologiczny; Vol. 65 No. 1 (2017); 23 - 31 Przegląd Geologiczny; Tom 65 Nr 1 (2017); 23 - 31 0033-2151 |
op_relation |
https://gq.pgi.gov.pl/pg/article/view/27036/18757 https://gq.pgi.gov.pl/pg/article/view/27036 |
op_rights |
Copyright (c) 2020 Przegląd Geologiczny |
_version_ |
1809905369409912832 |