BEHAVIOR OF SOME TRACE-ELEMENTS IN ALLUVIAL SEDIMENTS, ZAGREB WATER-WELL FIELD AREA, CROATIA

Citation
A. Vertacnik et al., BEHAVIOR OF SOME TRACE-ELEMENTS IN ALLUVIAL SEDIMENTS, ZAGREB WATER-WELL FIELD AREA, CROATIA, Water research, 29(1), 1995, pp. 237-246
Citations number
15
Categorie Soggetti
Engineering, Civil","Environmental Sciences","Water Resources
Journal title
ISSN journal
00431354
Volume
29
Issue
1
Year of publication
1995
Pages
237 - 246
Database
ISI
SICI code
0043-1354(1995)29:1<237:BOSTIA>2.0.ZU;2-S
Abstract
Trace elements concentrations were determined in alluvial sediment are a threatened by construction and operation of the pharmaceutical/chemi cal plant. Results gained by instrumental neutron activation analysis (INAA), electrothermal atomic absorption spectrophotometry (ETAAS), co ld vapour AAS (CVAAS), optical emission spectrography (OES) show great differences in element distribution between two solid phases at the p ollution source; high concentrations of Cr, Cu, Pb, Hg, Ni and Zn in c reek sediments and indication of pollution in the upper soil layer at the Sava river banks downstream at the creek mouth. Concentrations and enrichment factors of elements determined in upper, bottom and water- bearing layers between creek and water-field area are of natural value s. Some enrichment found for Sr, Ba and Ag could be explained with hig h calcite-dolomite content. For the time being, soil upper layers act as chemical filter preventing vertical infiltration. At the same time, Gorjak (Smrdljivka) creek sediments, rich in organic matter, cause cl ogging and prevent intensive pollution of groundwater. Thus the qualit y of water exploited from the water-well field is not endangered so fa r.