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2. ENVIRONMENTAL ChEMISTRy & TEChNOLOGy 2.1. Lectures

2. ENVIRONMENTAL ChEMISTRy & TEChNOLOGy 2.1. Lectures

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Chem. Listy, 102, s265–s1311 (2008) Environmental Chemistry & Technology<br />

notably high accumulation of trace elements including<br />

As in the most contaminated sample KY-100 (3,208 mg As kg –1 )<br />

with the lowest relative mobility, is likely due to high contents<br />

of the Fe, Al, Mn oxohydroxides. The relative mobility<br />

of As was inversely related to the oxalate-extractable<br />

Mn content (r = –0.960, P < 0.05) and not significantly to the<br />

oxalate-extractable Fe content such that diffusion in hydrated<br />

micropores of amorphous Fe and Mn oxides might be the rate<br />

limiting mechanism of the As release (Fig. <strong>2.</strong>).<br />

Fig. <strong>2.</strong> Relationship between the relative mobility of As and the<br />

ammonium oxalate-extractable Mn, Fe contents in the log-log<br />

form<br />

The amount of As released from samples KY-1000 and<br />

KY-2000 increased rapidly within short extraction times, reaching<br />

the apparent equilibrium after 174 min. The relative<br />

mobility of As in KY-1000 and KY-2000 was approximately<br />

s510<br />

the same as in impoundment material although the total Fe,<br />

Mn contents in KY-1000, 2000 are 2-times lower as compared<br />

with KY-0. The total contents of elements Cd, Cr, Fe, Hg,<br />

Mn, Pb, Zn, Al, As and Sb were determined after digestion<br />

with acid mixture.<br />

Conclusions<br />

The fractions of As released in column experiments were<br />

generally less than 10 % (5.32–7.83 %) of its total contents,<br />

but they represented high absolute amounts of readily available<br />

and water-soluble As (83 mg kg –1 ). The fraction released<br />

from the source impoundment material (132 mg kg –1 ) represented<br />

high As concentration in its leachates, reaching up to<br />

8,000 μg dm –3 . As concentrations in the leachates from all<br />

the samples exceed maximum permissible level in drinking<br />

water (10 μg dm –3 ; Decision of the Slovak Health Ministry<br />

no. 151/2004).<br />

This work has been supported by the Slovak Grant<br />

Agency under VEGA project No.1/2037/05.<br />

REFEREnCES<br />

1. Jurkovič ľ., Kordík J., Slaninka I.: Slovak Geol. Mag.<br />

12, 31 (2006).<br />

<strong>2.</strong> Tao Y., Zhang S., Jian W., Yuan CH., Shan X.: Chemosphere<br />

65, 1281 (2006).<br />

3. Williams L. E., Barnett M. O., Kramer T. A., Melville<br />

J. G.: J. Environ. Qual. 32, 841 (2003).<br />

4. Gao S., Fujii R., Chalmers A. T., Tanji K. K.: Soil Sci.<br />

Soc. Am. J. 68, 89 (2004).<br />

5. Smith E., naidu R., Alston A.M.: J. Environ. Qual. 31,<br />

557 (2002).<br />

6. Ganne P., Cappuyns V., Vervoort A., Buvé L., Swennen<br />

R.: Sci. Total Environ. 356, 69 (2006).

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