Main and trace elements in groundwater from the quaternary sediments in southern Great Plain, Hungary

Hrabovszki Erika and Varsányi Irén: Main and trace elements in groundwater from the quaternary sediments in southern Great Plain, Hungary. In: Acta mineralogica-petrographica, (39). pp. 151-167. (1998)

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Abstract

Chemical composi.tion of groundwater samples ffom the southem part of the Great Hungárián Plain was determined. Cluster analysis based on major elements, and based on minor and trace elements resulted in similar separation of the study area. The units correspond to three hydrogeological regions: the River Körös basin, the River Maros alluvial fan and the River Danube deposits. Processes controlling both major and trace element concentrations are dissolution of carbonate minerals, ion exchange, oxidation-reduction, albite weathering and formation of secondary minerals. In the Körös basin water movements is restricted. In the River Maros alluvial fan the direction of water flow is from south-southeast to north-northwest, and in the River Danube deposits it is from west to east.

Item Type: Article
Journal or Publication Title: Acta mineralogica-petrographica
Date: 1998
Volume: 39
ISSN: 0365-8066
Page Range: pp. 151-167
Language: English
Publisher: University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Place of Publication: Szeged
Related URLs: http://acta.bibl.u-szeged.hu/39418/
Uncontrolled Keywords: Kőzettan, Ásványtan, Földtan
Additional Information: Bibliogr.: p. 165-167. ; ill. ; összefoglalás angol nyelven
Subjects: 01. Natural sciences
01. Natural sciences > 01.05. Earth and related environmental sciences
Date Deposited: 2016. Oct. 17. 09:58
Last Modified: 2022. Jul. 27. 14:07
URI: http://acta.bibl.u-szeged.hu/id/eprint/29502

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