Previous Article | Next Article 
Applied and Environmental Microbiology, January 1999, p. 319-321, Vol. 65, No. 1
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.
Bacterial Leaching of Metal Sulfides Proceeds by
Two Indirect Mechanisms via Thiosulfate or via Polysulfides and
Sulfur
Axel
Schippers* and
Wolfgang
Sand
Abteilung Mikrobiologie, Institut für
Allgemeine Botanik, Universität Hamburg, D-22609 Hamburg,
Germany
Received 20 July 1998/Accepted 22 October 1998
 |
ABSTRACT |
The acid-insoluble metal sulfides FeS2,
MoS2, and WS2 are chemically attacked by
iron(III) hexahydrate ions, generating thiosulfate, which is oxidized
to sulfuric acid. Other metal sulfides are attacked by iron(III) ions
and by protons, resulting in the formation of elemental sulfur via
intermediary polysulfides. Sulfur is biooxidized to sulfuric acid. This
explains leaching of metal sulfides by Thiobacillus
thiooxidans.
 |
TEXT |
Bacterial leaching, the biooxidation
of metal sulfides to soluble metal sulfates and sulfuric acid, is
effected by specialized bacteria. Three species of mesoacidophilic,
chemolithotrophic bacteria are mainly involved: Thiobacillus
ferrooxidans, Thiobacillus thiooxidans, and
Leptospirillum ferrooxidans. T. ferrooxidans oxidizes
reduced sulfur compounds to sulfate and iron(II) to iron(III) ions.
T. thiooxidans is able to oxidize only reduced sulfur
compounds, whereas L. ferrooxidans can oxidize only iron(II)
ions (1, 4, 13, 15).
Recently, we described for pyrite (FeS2) degradation an
iron(III) ion-mediated leaching mechanism via thiosulfate and
polythionates (18). In this thiosulfate mechanism, the
Fe-S2 bond is cleaved, after the S2 group has
been oxidized by iron(III) hexahydrate ions to a thiosulfate group.
Hydrolysis yields thiosulfate and an iron(II) ion. Thiosulfate is
consecutively oxidized via tetrathionate, disulfane-monosulfonic acid,
and trithionate to sulfate. Elemental sulfur occurs as a by-product
only. The function of T. ferrooxidans and L. ferrooxidans is to supply the oxidizing iron(III) ions.
Although FeS2 is the most abundant metal sulfide on earth,
it is not the most valuable one. Consequently, experiments were performed in order to evaluate whether the thiosulfate mechanism is also valid for other metal sulfides. A survey of mineralogical data
on metal sulfides indicated that the structure of pyrite is almost
unique (2, 28). For further tests, the differently structured metal sulfides sphalerite (ZnS), chalcopyrite
(CuFeS2), galena (PbS), hauerite (MnS2),
orpiment (As2S3), realgar
(As4S4), and molybdenite
(MoS2) were selected. For these, the formation of
sulfur compounds by iron(III) ion-mediated chemical oxidation was analyzed. For the experiments, the metal sulfides were crushed, pulverized, and heat sterilized under N2. Fifty
milliliters of a sterile 10 mM FeCl3 solution at pH 1.9 was
added to 1 g of each metal sulfide powder in shake flasks. The
suspension was sampled for analysis of reduced sulfur compounds
(high-pressure liquid chromatography-diode array detection), sulfate
(ion chromatography), metal ions (atomic absorption spectroscopy),
iron(III)-iron(II) ions (photometry), and pH (electrode) as
previously described (18). Experiments were done in
triplicate. The results are shown in Table
1.
View this table:
[in this window]
[in a new window]
|
TABLE 1.
Formation of sulfur compounds by chemical metal sulfide
oxidation with 10 mM Fe(III) chloride (3) at pH 1.9 and 28°C
|
|
The oxidation products in the case of FeS2 and
MoS2 consisted of up to 90% sulfate and about 1 to 2%
polythionates. Because the valence bands of FeS2 and
MoS2 are derived only from the metal orbitals, the valence
bands do not contribute to the chemical bond between the metal and the
sulfur moiety in the crystal (2, 25). Consequently, these
metal sulfides are degradable only by an oxidizing attack, e.g., by
iron(III) ions. None of these compounds is soluble in acid (proton
attack) (21, 25, 26). Furthermore, both metal sulfides
consist of pairs of sulfur atoms. These properties hold for
WS2 as well (25, 26). Consequently, FeS2, MoS2, and WS2 are oxidized by
the same, indirect thiosulfate mechanism. In leaching experiments with
L. ferrooxidans and FeS2 the same sulfur
compounds resulted (18). Thus, the same dissolution mechanism is active in bioleaching.
In contrast, all other metal sulfides mentioned above have valence
bands, to which metal and sulfur orbitals contribute (2, 25,
26). Consequently, they are acid soluble. The experiments with
these metal sulfides yielded elemental sulfur in amounts of more than
90%. Even MnS2, a disulfide like FeS2, but
easily acid soluble, yielded mainly elemental sulfur. To explain the differences in end products, another mechanism for dissolution was sought.
Experiments with T. thiooxidans on the bioleaching of ZnS
demonstrated, in agreement with published data (5, 11), that a pure culture is able to dissolve ZnS and produce zinc(II) ions and
sulfate at an almost constant pH (Fig.
1). It is known that ZnS is soluble
in acid. Chemical experiments demonstrated the dissolution of
this compound, too; however, elemental sulfur was formed (because
sulfur-oxidizing bacteria were not present). Consequently, the pH started to increase and the dissolution of ZnS concomitantly decreased. To explain the mechanism of dissolution, the formation of intermediary polysulfides according to the work of Steudel (22) has to be considered. The mechanism becomes obvious
from the following equations. The dissolution of a metal sulfide (MS) is started by proton attack (equation 1) and a consecutive oxidation of
H2S by Fe(III) ions (equation 2).
|
(1)
|
|
(2)
|
Due to the capability of Fe(III) ions to break metal sulfide bonds
more effectively than protons (
25,
26), the
H
2S
·+ radical may preferentially be formed in
one reaction without
intermediately occurring H
2S (equation
3).
|
(3)
|
Polysulfide formation starts with dissociation of the strong acid
H
2S
·+ to a HS
· radical
(equation 4).
|
(4)
|
Two of the HS
· radicals may react to a disulfide
(equation 5).
|
(5)
|
The disulfide may react again with Fe(III) ions (equation 6) or
with another HS
· radical (equation 7).
|
(6)
|
|
(7)
|
Tetrasulfide occurs by dimerization of two
HS
2· radicals (analogous to equation 5), or
trisulfide occurs by reaction of a
HS
2· with
a HS
· radical. Further chain elongation to polysulfides
proceeds by
analogous reactions.

View larger version (21K):
[in this window]
[in a new window]
|
FIG. 1.
Leaching of ZnS by T. thiooxidans R20
(16). The strain had been adapted to grow on ZnS, before the
experiment was started by addition of 109 cells to 1 g
of ZnS (pulverized) in 50 ml of salt solution in shake flasks at 28°C
in the dark. Tt, assays with T. thiooxidans; c., sterile
control assays. Data are means of three parallel assays. Standard
deviations were less than 15%. The experiment was reproduced twice.
|
|
In acidic solution, polysulfides decompose to rings of elemental
sulfur, mainly S8 rings (>99%) (equation 8).
|
(8)
|
Formation of thiosulfate (polythionates and sulfate) occurs by
side reactions (equations 9 and 10).
|
(9)
|
|
(10)
|
This oxidation mechanism does not necessarily require the presence
of Fe(III) ions. An electron transfer from a semiconductive
metal
sulfide to an O
2 molecule is also possible. The
O
2 molecule
is reduced via a superoxide radical and a
peroxide molecule to
water (
27). However, Fe(III) ions,
usually present in acidic
leach biotopes, are much more efficient in
extracting electrons
from a metal sulfide lattice than is
O
2 (
25,
26).
The series of reactions 1 to 8 inherently explains the formation of
elemental sulfur as the main sulfur compound oxidation product of
acid-hydrolyzable metal sulfides. Thiosulfate, and consequently
polythionates and sulfate, may also arise by side reactions (equations
9 and 10) (22).
According to this polysulfide mechanism, elemental sulfur is formed.
Since sulfur is reasonably stable under experimental and usually also
environmental conditions, only in the case of the presence of
sulfur-oxidizing bacteria can degradation occur (yielding the protons
needed for a further dissolution of ZnS). This mechanism allows for the
first time the unequivocal explanation of the ability of T. thiooxidans to leach some metal sulfides, i.e., the ones which are
susceptible to hydrolysis by proton attack. Polysulfides were detected
on the surface of oxidized chalcopyrite by Hackl et al. (8),
confirming this mechanism. The degradation of metal sulfides via
polysulfides is summarized in Fig. 2. As a consequence, two indirect oxidation mechanisms for metal sulfides exist.
One mechanism is exclusively based on the oxidative attack of
iron(III) ions on the acid-insoluble metal sulfides
FeS2, MoS2, and WS2. Here,
the main sulfur intermediate is thiosulfate. The second mechanism
allows for a dissolution by an attack of iron(III) ions and/or by
protons. In this case, the main sulfur intermediate is
polysulfide (and consequently elemental sulfur). The two
mechanisms may be simplified by the following equations:
Thiosulfate mechanism (FeS2, MoS2,
and WS2)
Polysulfide mechanism (e.g., ZnS, CuFeS
2, or PbS)
Consequently, bioleaching of metal sulfides means that the
bacterial function is to generate sulfuric acid biologically to
supply protons for hydrolysis attack and/or to keep the iron ions
in an
oxidized state [as iron(III) ions] for an oxidative attack
(Fig.
3).

View larger version (22K):
[in this window]
[in a new window]
|
FIG. 3.
Bioleaching proceeds by two different indirect
mechanisms via thiosulfate or via polysulfides and sulfur and is based
on the properties of metal sulfides (MS). Dashed lines indicate
occurrence of intermediate sulfur compounds.
|
|
Our conclusions are in agreement with data from the literature. In the
absence of iron ions, T. ferrooxidans can solubilize acid-hydrolyzable, synthetic, iron-free sulfides like ZnS, CdS, NiS,
CoS, CuS, and Cu2S (14, 24-26) but not the
insoluble sulfides FeS2 (6), MoS2,
and WS2 (25, 26). In the case of the former compounds, the leaching rates correlate with their solubility products
(24, 26). This finding proves that the solubility product,
besides pH, is decisive for the leachability of a metal sulfide in the
case of a proton attack. We consequently conclude that in the absence
of iron ions T. ferrooxidans acts like T. thiooxidans by acid production (sulfur oxidation). This conclusion is in agreement with the recent finding that the solubilization of
Cu2+ from a copper ore is determined by the
sulfur-oxidizing activity of T. ferrooxidans
(23). The addition of iron ions to cultures of T. ferrooxidans growing with hydrolyzable, synthetic, iron-free sulfides generally enhanced leaching rates (25, 26). Because of the additional oxidative iron(III) ion attack, dissolution rates
are much higher than those with T. ferrooxidans lacking iron ions or T. thiooxidans alone (5).
Thus, in summary bioleaching is effected by two indirect leaching
mechanisms: via thiosulfate or via polysulfides and sulfur. Both
mechanisms combine characteristics of the previously differentiated direct and indirect leaching mechanisms. Direct leaching means an
attack on the crystal lattice of a metal sulfide through enzymatic oxidation by attached cells (4). This work shows that the
mineralogy is also a contributing factor to the degradation pathway.
The knowledge of these two mechanisms has implications for
biotechnology and environmental problems connected to bioleaching.
Sulfur compound-metabolizing enzymes are involved in metal sulfide
oxidation. Their regulation or inhibition might influence the balance
of sulfur compounds (9). For example, changing the balance
from sulfur to sulfate would increase dissolution rates in bioleaching
plants for gold recovery (12). Furthermore, cyanide
consumption would be reduced (7). On the other hand, the
formation of environmentally harmful acid rock drainage (17, 19,
20) might be reduced, if the oxidation could be stopped at the
stage of elemental sulfur.
 |
ACKNOWLEDGMENTS |
We thank M. Reiß and E. Gock for X-ray diffraction and ICP measurements.
This work was supported by grants to W.S. from BMBF via UBA (1490954)
and DBU (05333).
 |
FOOTNOTES |
*
Corresponding author. Mailing address: Abteilung
Mikrobiologie, Institut für Allgemeine Botanik,
Universität Hamburg, Ohnhorststraße 18, D-22609 Hamburg,
Germany. Phone:
49(0)40/82282-421. Fax: 49(0)40/82282-423. E-mail: fb6a042{at}botanik.botanik.uni-hamburg.de.
 |
REFERENCES |
| 1.
|
Bosecker, K.
1997.
Bioleaching: metal solubilization by microorganisms.
FEMS Microbiol. Rev.
20:591-604.
|
| 2.
|
Crundwell, F. K.
1988.
The influence of the electronic structure of solids on the anodic dissolution and leaching of semiconducting sulphide minerals.
Hydrometallurgy
21:155-190.
|
| 3.
|
Dutrizac, J. E., and R. J. C. MacDonald.
1974.
Ferric ion as a leaching medium.
Miner. Sci. Eng.
6:59-100.
|
| 4.
|
Ehrlich, H. L.
1996.
Geomicrobiology.
Marcel Dekker, Inc., New York, N.Y.
|
| 5.
|
Garcia, O.,
J. M. Bigham, and O. H. Tuovinen.
1995.
Sphalerite oxidation by Thiobacillus ferrooxidans and Thiobacillus thiooxidans.
Can. J. Microbiol.
41:578-584.
|
| 6.
|
Gehrke, T.,
J. Telegdi,
D. Thierry, and W. Sand.
1998.
Importance of extracellular polymeric substances from Thiobacillus ferrooxidans for bioleaching.
Appl. Environ. Microbiol.
64:2743-2747[Abstract/Free Full Text].
|
| 7.
|
Hackl, R. P., and L. Jones.
1997.
Bacterial sulfur oxidation pathways and their effect on the cyanidation characteristics of biooxidized refractory gold concentrates, p. M14.2.1-M142.10.
In
Proceedings of the International Biohydrometallurgy Symposium IBS '97 Biomine '97. Australian Mineral Foundation, Glenside, South Australia, Australia.
|
| 8.
|
Hackl, R. P.,
D. B. Dreisinger,
E. Peters, and J. A. King.
1995.
Passivation of chalcopyrite during oxidative leaching in sulfate media.
Hydrometallurgy
39:25-48.
|
| 9.
|
Hazeu, W.,
W. H. Batenburg-van der Vegte,
P. Bos,
R. K. van der Pas, and J. G. Kuenen.
1988.
The production and utilization of intermediary elemental sulfur during the oxidation of reduced sulfur compounds by Thiobacillus ferrooxidans.
Arch. Microbiol.
150:574-579.
|
| 10.
|
Hutchins, S. R.,
M. S. Davidson,
J. A. Brierley, and C. L. Brierley.
1986.
Microorganisms in reclamation of metals.
Annu. Rev. Microbiol.
40:311-336[Medline].
|
| 11.
|
Lizama, H. M., and I. Suzuki.
1991.
Interaction of chalcopyrite and sphalerite with pyrite during leaching by Thiobacillus ferrooxidans and Thiobacillus thiooxidans.
Can. J. Microbiol.
37:304-311.
|
| 12.
|
Rawlings, D. E., and S. Silver.
1995.
Mining with microbes.
Bio/Technology
13:773-778.
|
| 13.
|
Rossi, G.
1990.
Biohydrometallurgy.
McGraw-Hill, Hamburg, Germany.
|
| 14.
|
Sakaguchi, H.,
A. E. Torma, and M. Silver.
1976.
Microbiological oxidation of synthetic chalcocite and covellite by Thiobacillus ferrooxidans.
Appl. Environ. Microbiol.
31:7-10[Abstract/Free Full Text].
|
| 15.
|
Sand, W.,
T. Gehrke,
R. Hallmann, and A. Schippers.
1995.
Sulfur chemistry, biofilm, and the (in)direct attack mechanism a critical evaluation of bacterial leaching.
Appl. Microbiol. Biotechnol.
43:961-966.
|
| 16.
|
Sand, W.,
R. Hallmann,
K. Rohde,
B. Sobotke, and S. Wentzien.
1993.
Controlled microbiological in-situ stope leaching of a sulphidic ore.
Appl. Microbiol. Biotechnol.
40:421-426.
|
| 17.
|
Schippers, A.,
R. Hallmann,
S. Wentzien, and W. Sand.
1995.
Microbial diversity in uranium mine waste heaps.
Appl. Environ. Microbiol.
61:2930-2935[Abstract].
|
| 18.
|
Schippers, A.,
P.-G. Jozsa, and W. Sand.
1996.
Sulfur chemistry in bacterial leaching of pyrite.
Appl. Environ. Microbiol.
62:3424-3431[Abstract].
|
| 19.
|
Schippers, A.,
P.-G. Jozsa, and W. Sand.
1998.
Evaluation of the efficiency of measures for sulphidic mine waste mitigation.
Appl. Microbiol. Biotechnol.
49:698-701.
|
| 20.
|
Schrenk, M. O.,
K. J. Edwards,
R. M. Goodman,
R. J. Hamers, and J. F. Banfield.
1998.
Distribution of Thiobacillus ferrooxidans and Leptospirillum ferrooxidans for generation of acid mine drainage.
Science
279:1519-1522[Abstract/Free Full Text].
|
| 21.
|
Singer, P. C., and W. Stumm.
1970.
Acidic mine drainage: the rate-determining step.
Science
167:1121-1123[Abstract/Free Full Text].
|
| 22.
|
Steudel, R.
1996.
Mechanism for the formation of elemental sulfur from aqueous sulfide in chemical and microbiological desulfurization processes.
Ind. Eng. Chem. Res.
35:1417-1423.
|
| 23.
|
Sugio, T., and F. Akhter.
1996.
Solubilization of Cu2+ from copper ore by iron-oxidizing bacteria isolated from the natural environment and identification of the enzyme that determines Cu2+ solubilization activity.
J. Ferment. Bioeng.
82:346-350.
|
| 24.
|
Torma, A. E., and H. Sakaguchi.
1978.
Relation between the solubility product and the rate of metal sulfide oxidation by Thiobacillus ferrooxidans.
J. Ferment. Technol.
56:173-178.
|
| 25.
|
Tributsch, H., and J. C. Bennett.
1981.
Semiconductor-electrochemical aspects of bacterial leaching. 1. Oxidation of metal sulphides with large energy gaps.
J. Chem. Technol. Biotechnol.
31:565-577.
|
| 26.
|
Tributsch, H., and J. C. Bennett.
1981.
Semiconductor-electrochemical aspects of bacterial leaching. Part 2. Survey of rate-controlling sulphide properties.
J. Chem. Technol. Biotechnol.
31:627-635.
|
| 27.
|
Tributsch, H., and H. Gerischer.
1976.
The oxidation and self-heating of metal sulphides as an electrochemical corrosion phenomenon.
J. Appl. Chem. Biotechnol.
26:747-761.
|
| 28.
|
Vaughan, D. J., and J. R. Craig.
1978.
Mineral chemistry of metal sulfides
Cambridge University Press, Cambridge, United Kingdom.
|
Applied and Environmental Microbiology, January 1999, p. 319-321, Vol. 65, No. 1
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.
This article has been cited by other articles:
-
Rzhepishevska, O. I., Valdes, J., Marcinkeviciene, L., Gallardo, C. A., Meskys, R., Bonnefoy, V., Holmes, D. S., Dopson, M.
(2007). Regulation of a Novel Acidithiobacillus caldus Gene Cluster Involved in Metabolism of Reduced Inorganic Sulfur Compounds. Appl. Environ. Microbiol.
73: 7367-7372
[Abstract]
[Full Text]
-
Rivas, M., Seeger, M., Jedlicki, E., Holmes, D. S.
(2007). Second Acyl Homoserine Lactone Production System in the Extreme Acidophile Acidithiobacillus ferrooxidans. Appl. Environ. Microbiol.
73: 3225-3231
[Abstract]
[Full Text]
-
Enders, M. S., Knickerbocker, C., Titley, S. R., Southam, G.
(2006). The Role of Bacteria in the Supergene Environment of the Morenci Porphyry Copper Deposit, Greenlee County, Arizona. Economic Geology
101: 59-70
[Abstract]
[Full Text]
-
Southam, G., Saunders, J. A.
(2005). The Geomicrobiology of Ore Deposits. Economic Geology
100: 1067-1084
[Abstract]
[Full Text]
-
Ramirez, P., Guiliani, N., Valenzuela, L., Beard, S., Jerez, C. A.
(2004). Differential Protein Expression during Growth of Acidithiobacillus ferrooxidans on Ferrous Iron, Sulfur Compounds, or Metal Sulfides. Appl. Environ. Microbiol.
70: 4491-4498
[Abstract]
[Full Text]
-
Gonzalez-Toril, E., Llobet-Brossa, E., Casamayor, E. O., Amann, R., Amils, R.
(2003). Microbial Ecology of an Extreme Acidic Environment, the Tinto River. Appl. Environ. Microbiol.
69: 4853-4865
[Abstract]
[Full Text]
-
Ramirez, P., Toledo, H., Guiliani, N., Jerez, C. A.
(2002). An Exported Rhodanese-Like Protein Is Induced during Growth of Acidithiobacillus ferrooxidans in Metal Sulfides and Different Sulfur Compounds. Appl. Environ. Microbiol.
68: 1837-1845
[Abstract]
[Full Text]
-
Teske, A., Brinkhoff, T., Muyzer, G., Moser, D. P., Rethmeier, J., Jannasch, H. W.
(2000). Diversity of Thiosulfate-Oxidizing Bacteria from Marine Sediments and Hydrothermal Vents. Appl. Environ. Microbiol.
66: 3125-3133
[Abstract]
[Full Text]
-
Fowler, T. A., Holmes, P. R., Crundwell, F. K.
(1999). Mechanism of Pyrite Dissolution in the Presence of Thiobacillus ferrooxidans. Appl. Environ. Microbiol.
65: 2987-2993
[Abstract]
[Full Text]