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
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.