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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 />

the mineral and the cultural medium and after 14 days by<br />

direct and indirect influence of bacteria At. ferrooxidans. This<br />

fact demonstrates the comparison of the Fe dissolution curve<br />

shape of At. ferrooxidans and abiotic control. It confirms the<br />

bioleaching of pyrite (FeS 2 ).<br />

Fig. <strong>2.</strong> Dissolution of the Sb by bacteria Acidithiobacillus ferrooxidans<br />

from the sample of gold-bearing antimony sulfide<br />

minerals. . c – concentration of Sb, t – time of bioleaching,<br />

– Acidithiobacillus ferrooxidans, – abiotic control<br />

Fig. 3. Influence of bacteria Desulfovibrio desulfuricans for the<br />

Fe dissolution under the alkaline leaching of gold-bearing antimony<br />

sulfide minerals. c – concentration of Fe, t – time of bioleaching,<br />

– Desulfovibrio desulfuricans, – abiotic control<br />

Fig. <strong>2.</strong> shows the trend of the Sb dissolving. Initially,<br />

during 7 days the concentration of Sb increases in the At. ferrooxidans<br />

presence and abiotic control, probably due to<br />

interaction between the mineral and the cultural medium. After<br />

7 days the abiotic control allocated the circa constant Sb<br />

concentration in liquid phase until the end. After 35 days was<br />

recorded the depression as follows was observed the decreasing<br />

of the Sb concentration until the end of experiments in<br />

the At. ferrooxidans presence. This fact can be interpreted on<br />

the bases the creation of the insoluble antimony oxosulphates<br />

– (SbO) 2 SO 4 according the reaction (1) 11 :<br />

s410<br />

Sb 2 S 3 + 6O 2 + 2H 2 O → (SbO) 2 SO 4 + 2H 2 SO 4<br />

Figure 3 presents the Fe concentration in liquid phase at<br />

the using bacteria Dsv. desulfuricans that was from beginning<br />

until the end almost zero. Although the little increase was<br />

observed after 19 days. This situation can be resolve by the<br />

Fe precipitation with bacterially produced hydrogen sulphide<br />

under the influence of bacteria Dsv. desulfuricans After 40<br />

days it’s the intense increase was recorded in the experiments<br />

without bacteria. Just now concerning this fact we have not<br />

the adequate understanding. At the end of the experiments the<br />

Fe concentration at presence SRB and abiotic control were<br />

again almost zero.<br />

Figure 4 shows the Sb concentration in the liquid phase<br />

at the using bacteria Dsv. desulfuricans From the confrontation<br />

of the Sb concentration curve shape in the abiotic control<br />

and in the presence bacteria you can see that the influence of<br />

bacteria Dsv. desulfuricans was not significant. The contamination<br />

of the abiotic control by bacteria Dsv. desulfuricans<br />

was not evidence. After 20 days was observed the formation<br />

of the shined cover on the reactor wall in the presence bacteria.<br />

Its can be explain to the Sb concentration decreasing.<br />

Fig. 4. Influence of bacteria Desulfovibrio desulfuricans for the<br />

Sb dissolution under the alkaline leaching of gold-bearing antimony<br />

sulfide minerals. c – concentration of Sb, t – time of bioleaching,<br />

– Desulfovibrio desulfuricans, – abiotic control<br />

After ending the solid phases were recovered by filtration<br />

from solution. The solid phases were saved for the<br />

consequently test of cyanidation and liquid phases for the<br />

electrowinning.<br />

Conclusions<br />

Experimental studies confirmed:<br />

• the bacteria At. ferrooxidans have the positive influence<br />

on the dissolving of pyrite (FeS2 ) and stibnite (Sb2S3 )<br />

to occur in the used sample of gold-bearing antimony<br />

sulphide minerals,<br />

• the increase, subsequent the depression and the decreasing<br />

of the Sb concentration during the bioleaching<br />

(1)

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