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2007_6_Nr6_EEMJ

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Metals concentration in soils adjacent to waste deposits<br />

environment are soil, dust, seawater, volcanic<br />

eruptions and forest fires. All soil contains some<br />

amount of cobalt. The average concentration of cobalt<br />

in soils around the world is 8 mg/kg dry weight.<br />

Toxic effects on plants are unlikely to occur below<br />

soil cobalt concentrations of 40 ppm. One of the most<br />

important soil properties is soil acidity. The more<br />

acidic the soil, the greater are the potential for cobalt<br />

toxicity, at any concentration.<br />

Co conc., mg/kg<br />

d.w.<br />

16<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

a)<br />

Apr Iun Aug Oct<br />

month<br />

surface<br />

depth<br />

b)<br />

Co conc., mg/kg d.w.<br />

14<br />

12<br />

10<br />

8<br />

6<br />

4<br />

2<br />

0<br />

Apr Iun Aug Oct<br />

month<br />

surface<br />

depth<br />

Fig. 2. Cobalt concentration evolution in soil adjacent to<br />

waste deposits in April-October 2006 (mean values, mg/kg<br />

dry weight); a) Eforie Sud; b) Techirghiol<br />

Fig. 1. Cadmium concentration evolution in soil adjacent to<br />

waste deposits in April-October 2006 (mean values, mg/kg<br />

dry weight); a) Eforie Sud; b) Techirghiol<br />

The cobalt concentration evolution in studied<br />

soil samples are presented in the Fig. 2.<br />

All founded values are lower than 15 mg/kg<br />

dry weight, the normal Co concentrations in soil.<br />

Chromium is a trace component in the earth’s<br />

crust (0.02%), a unique element in soil, because of<br />

essentiality to human and animal life and nonessentiality<br />

for the vegetable kingdom and its possible<br />

presence in two main oxidation forms, trivalent and<br />

hexavalent which show opposite properties. The<br />

reported mean total chromium concentration in<br />

lithosphere is 69 mg/kg dry weight. The two forms<br />

have completely different effects on living organisms:<br />

the first Cr(III) is apparently useful or harmless at<br />

reasonable concentrations, while the second Cr(VI) is<br />

extremely toxic. In addition, Cr(III) is not mobile in<br />

soil, therefore the risks of leaching are negligible,<br />

while Cr(VI), mainly present in the forms of<br />

chromates (CrO 4 2− ) and dichromates (Cr 2 O 7 2− ), is<br />

generally mobile and often is part of crystalline<br />

minerals.<br />

Conversion of Cr(III) to Cr(VI) has been<br />

shown in some particular soils: rich in manganese<br />

oxides, poor in organic matter and high redox<br />

potential. On the contrary, the reverse transformation<br />

of Cr(VI) to Cr(III) is very common and easier, so<br />

that it is difficult to find hexavalent chromium forms<br />

in soil solution or in leaching waters. The problem of<br />

Cr enrichment in soil has been often discussed not<br />

only in relation to the discharge of tannery wastes, but<br />

also to the possibility of Cr presence in soil<br />

amendments, mainly organics, and to the existence of<br />

excellent organic fertilizers produced from leather<br />

residues or wastes.<br />

Fig. 3 presents the mean total chromium<br />

concentration in studied soil samples.<br />

In Eforie Sud soil samples Cr concentration<br />

ranged between 3.24 – 28.72 mg/kg dry weight in<br />

surface samples and 7.25 – 30.06 mg/kg dry weight in<br />

depth samples. Soil samples from Techirghiol<br />

registered similar Cr concentrations (7.50 – 28.55<br />

mg/kg dry weight in surface samples and 8.40 – 19.32<br />

mg/kg dry weight in depth samples). All determined<br />

Cr concentrations were below the normal limit in soil.<br />

Copper is also a trace element in the earth’s<br />

crust (0.007%); Cu is among the trace elements<br />

essential for life, in the case of plants toxic effects<br />

occur at 20 or more mg/kg dry weight. In the past, the<br />

499

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