DBPapers
DOI: 10.5593/SGEM2014/B12/S2.056

GROUNDWATER LEVEL REGIME IN THE FORELAND OF THE MALE KARPATY MOUNTAINS, SLOVAKIA

D.Stojkovova,S. Smidovicova, D. Vrablikova, M. Fendekova,M. Fendek
Wednesday 1 October 2014 by Libadmin2014

References: 14th International Multidisciplinary Scientific GeoConference SGEM 2014, www.sgem.org, SGEM2014 Conference Proceedings, ISBN 978-619-7105-08-7 / ISSN 1314-2704, June 19-25, 2014, Book 1, Vol. 2, 441-448 pp

ABSTRACT
The main aim of the study was to evaluate temporal element of groundwater regime formation in Quaternary and Neogene sediments of the Danube lowland in the area adjacent to Male Karpaty Mts., Slovakia. Data on groundwater heads in five observation wells and yields of one spring located along the Male Karpaty Mts. foreland and climatic data in five stations in Male Karpaty Mts. and in its foreland were used in the study. Data were statistically processed. Because of skewed frequency distribution of the most of them, Spearman rank correlation was used to identify the mutual relationships. Cross-correlation method was also used to identify the delay of groundwater head fluctuation and spring yields after the precipitation events.

Keywords: groundwater level, regime type, inflow retardation, statistical methods.