Sheikhy Narany T, Bittner D, Disse M, Chiogna G (2019)
Publication Type: Journal article
Publication year: 2019
Book Volume: 78
Article Number: 273
Journal Issue: 9
DOI: 10.1007/s12665-019-8276-2
Dolomite karst systems are less common and less exploited than limestone systems, but still they can significantly contribute to drinking water supply in many countries. The knowledge about spatial and temporal variations of hydrochemical parameters of such systems is much more limited than for limestone karst aquifers. In the present research, 40-year-long observations of hydrochemical parameters gathered from five springs and a pumping well in Waidhofen an der Ybbs (Austria) were used to show the variability of chemical water composition in a small-scale (~ 10 km2) dolomite karst system. Integration of classic geochemical methods and multivariate statistical analysis revealed that the hydrofacies correlate directly with the lithofacies (dolomite) in the study area. At the same time, measured concentrations of Ca2+, Mg2+, Na+, Cl−, and HCO
APA:
Sheikhy Narany, T., Bittner, D., Disse, M., & Chiogna, G. (2019). Spatial and temporal variability in hydrochemistry of a small-scale dolomite karst environment. Environmental Earth Sciences, 78(9). https://doi.org/10.1007/s12665-019-8276-2
MLA:
Sheikhy Narany, Tahoora, et al. "Spatial and temporal variability in hydrochemistry of a small-scale dolomite karst environment." Environmental Earth Sciences 78.9 (2019).
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