Skład chemiczny wód źródlanych w masywie Połoniny Wetlińskiej

2018
journal article
article
dc.abstract.enThe aim of the study was to determine chemical composition of spring water in the Polonina Wetlinska massif (High Bieszczady Mountains) and to identify the natural factors controlling spatial variability of groundwater chemistry. Thirty five spring water samples were collected in September 2017. The spring water was characterized by similar, weak alkaline pH (6.8-8.1) and a relatively wide range of ions concentration (57-208 mg·dm^{-3}). Strong, positive correlation was showed between specific conductivity (SC) and main ions: {HCO_{3}}^{-}, Ca^{2+}, {SO_{4}}^{2}, Mg^{2+}, which shaped the water chemistry most likely due to dissolution of bedrock. K^{+}, Cl^{-}, {NO_{3}}^{-} showed weak or no correlation with SC. The origin of nutrients in the groundwater might have been connected with organic matter conversion into inorganic substance. Two groups of springs were distinguished: 1^{st} group with lower SC and lower concentration of main ions and 2^{nd} group with relatively higher SC. Springs with the lower SC are located on the NE slope of the Polonina Wetlinska, where flysch layers dip towards the same direction as the slope. These conditions promote relatively fast water flow and short residence time within aquifer. On the contrary, discordance of flysch layers dip and slope exposure may cause the relatively longer contact of groundwater with a bedrock and enrichment water with the geogenic ions.pl
dc.affiliationWydział Geografii i Geologii : Instytut Geografii i Gospodarki Przestrzennejpl
dc.affiliationWydział Geografii i Geologii : Instytut Nauk Geologicznychpl
dc.contributor.authorKisiel, Marta - 189551 pl
dc.contributor.authorBochnak, Dawidpl
dc.contributor.authorJastrzębska, Beatapl
dc.contributor.authorMostowik, Karolina - 175074 pl
dc.contributor.authorPufelska, Marta - 217729 pl
dc.contributor.authorRzonca, Bartłomiej - 131769 pl
dc.contributor.authorSiwek, Janusz - 102551 pl
dc.date.accession2018-10-25pl
dc.date.accessioned2018-11-05T09:21:19Z
dc.date.available2018-11-05T09:21:19Z
dc.date.issued2018pl
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.additionalBibliogr. s. 218-221pl
dc.description.physical205-222pl
dc.description.publication1,7pl
dc.description.versionostateczna wersja wydawcy
dc.description.volume26pl
dc.identifier.issn1233-1910pl
dc.identifier.projectROD UJ / OPpl
dc.identifier.urihttps://ruj.uj.edu.pl/xmlui/handle/item/59326
dc.identifier.weblinkhttps://www.bdpn.pl/dokumenty/roczniki/rb26/art12.pdfpl
dc.languagepolpl
dc.language.containerpolpl
dc.rightsUdzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa*
dc.rights.licenceOTHER
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.pl*
dc.share.typeotwarte czasopismo
dc.subject.enchemical compositionpl
dc.subject.engroundwaterpl
dc.subject.enBieszczady Mountainspl
dc.subject.enCarpathianspl
dc.subtypeArticlepl
dc.titleSkład chemiczny wód źródlanych w masywie Połoniny Wetlińskiejpl
dc.title.alternativeChemical composition of spring water in the Polonina Wetlinska massifpl
dc.title.journalRoczniki Bieszczadzkiepl
dc.typeJournalArticlepl
dspace.entity.typePublication
dc.abstract.enpl
The aim of the study was to determine chemical composition of spring water in the Polonina Wetlinska massif (High Bieszczady Mountains) and to identify the natural factors controlling spatial variability of groundwater chemistry. Thirty five spring water samples were collected in September 2017. The spring water was characterized by similar, weak alkaline pH (6.8-8.1) and a relatively wide range of ions concentration (57-208 mg·dm^{-3}). Strong, positive correlation was showed between specific conductivity (SC) and main ions: {HCO_{3}}^{-}, Ca^{2+}, {SO_{4}}^{2}, Mg^{2+}, which shaped the water chemistry most likely due to dissolution of bedrock. K^{+}, Cl^{-}, {NO_{3}}^{-} showed weak or no correlation with SC. The origin of nutrients in the groundwater might have been connected with organic matter conversion into inorganic substance. Two groups of springs were distinguished: 1^{st} group with lower SC and lower concentration of main ions and 2^{nd} group with relatively higher SC. Springs with the lower SC are located on the NE slope of the Polonina Wetlinska, where flysch layers dip towards the same direction as the slope. These conditions promote relatively fast water flow and short residence time within aquifer. On the contrary, discordance of flysch layers dip and slope exposure may cause the relatively longer contact of groundwater with a bedrock and enrichment water with the geogenic ions.
dc.affiliationpl
Wydział Geografii i Geologii : Instytut Geografii i Gospodarki Przestrzennej
dc.affiliationpl
Wydział Geografii i Geologii : Instytut Nauk Geologicznych
dc.contributor.authorpl
Kisiel, Marta - 189551
dc.contributor.authorpl
Bochnak, Dawid
dc.contributor.authorpl
Jastrzębska, Beata
dc.contributor.authorpl
Mostowik, Karolina - 175074
dc.contributor.authorpl
Pufelska, Marta - 217729
dc.contributor.authorpl
Rzonca, Bartłomiej - 131769
dc.contributor.authorpl
Siwek, Janusz - 102551
dc.date.accessionpl
2018-10-25
dc.date.accessioned
2018-11-05T09:21:19Z
dc.date.available
2018-11-05T09:21:19Z
dc.date.issuedpl
2018
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.additionalpl
Bibliogr. s. 218-221
dc.description.physicalpl
205-222
dc.description.publicationpl
1,7
dc.description.version
ostateczna wersja wydawcy
dc.description.volumepl
26
dc.identifier.issnpl
1233-1910
dc.identifier.projectpl
ROD UJ / OP
dc.identifier.uri
https://ruj.uj.edu.pl/xmlui/handle/item/59326
dc.identifier.weblinkpl
https://www.bdpn.pl/dokumenty/roczniki/rb26/art12.pdf
dc.languagepl
pol
dc.language.containerpl
pol
dc.rights*
Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa
dc.rights.licence
OTHER
dc.rights.uri*
http://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.pl
dc.share.type
otwarte czasopismo
dc.subject.enpl
chemical composition
dc.subject.enpl
groundwater
dc.subject.enpl
Bieszczady Mountains
dc.subject.enpl
Carpathians
dc.subtypepl
Article
dc.titlepl
Skład chemiczny wód źródlanych w masywie Połoniny Wetlińskiej
dc.title.alternativepl
Chemical composition of spring water in the Polonina Wetlinska massif
dc.title.journalpl
Roczniki Bieszczadzkie
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations

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