Dependence of the Phenotypic Characteristics of <Emphasis Type="Italic">Acidithiobacillus ferrooxidans</Emphasis> on the Physical,Chemical, and Electrophysical Properties of Pyrites

Comparison of Acidithiobacillus ferrooxidans strains TFV-1 and TFBk with respect to their capacity to oxidize pyrite 1, with an electron-type (n-type) conductivity, or pyrite 2, with hole-type (p-type) conductivity, showed that, at a pulp density of 1%, both before and after its adaptation to the pyrites, strain TFBk, isolated from a substrate with a more complex mineral composition, grew faster and oxidized the pyrites of both conductivity types more efficiently than strain TFV-1, which was isolated from a mineralogically simple ore. At a pulp density of 3–5%, the oxidation of pyrite 2 by strain TFV-1 and both of the pyrites by strain TFBk began only after an artificial increase in Eh to 600 mV. If the pulp density was increased gradually, strain TFBk could oxidize the pyrites at its higher values than strain TFV-1, with the rate of pyrite 2 oxidation being higher than that of pyrite 1. During chemical oxidation of both of the pyrites, an increase was observed in the absolute values of the coefficients of thermoelectromotive force (K_TEMF); during bacterial-chemical oxidation, the K_TEMF of pyrite 1 changed insignificantly, whereas the K_TEMF of pyrite 2 decreased.     

Dependence of the Genotypic Characteristics of <Emphasis Type="Italic">Acidithiobacillus ferrooxidans</Emphasis> on the Physical,Chemical, and Electrophysical Properties of Pyrites

This study focused on the effect of physical, chemical, and electrophysical properties of two pyrites, pyrite 1, which had electron-type (n-type) conductivity, and pyrite 2, with hole-type (p-type) conductivity, on the genotypic characteristics of Acidithiobacillus ferrooxidans strains TFV-1 and TFBk, which were isolated from different substrates. After the adaptation of the strains to the pyrites at a pulp density of 1%, pulsed-field electrophoresis revealed changes in the chromosomal DNA of strain TFV-1 adapted to pyrite 1, and strain TFBk adapted to either of the pyrite types. In pyrite-adapted strain TFBk, the plasmid composition was the same as after growth on a medium containing ferrous iron, whereas, in strain TFV-1, changes in plasmid sizes or both in plasmid sizes and plasmid number occurred. After an increase in the density of the pyrite 2 pulp from 1 to 10%, the plasmid number increased from three to four, and, after an increase in the density of the pyrite 1 pulp from 1 to 7%, the plasmid number increased from two to six.     

Patterns of growth and oxidation of natural pyrites by the representatives of acidophilic chemolithotrophic microorganisms

The patterns of the growth and oxidation of different types of natural pyrites were studied for the three microbial species adapted to these substrates and belonging to phylogenetically remote groups: gram-negative bacterium Acidithiobacillus ferrooxidans, gram-positive bacterium Sulfobacillus thermotolerans, and the archaeon Ferroplasma acidiphilum. For both A. ferrooxidans strains, TFV-1 and TFBk, pyrite 4 appeared to be the most difficult to oxidize and grow; pyrite 5 was oxidized by both strains at an average rate, and pyrite 3 was the most readily oxidized. On each of the three pyrites, growth and oxidation by TFBk were more active than by TFV-1. The effectiveness of the adaptation of S. thermotolerans Kr1^T was low compared to the A. ferrooxidans strains; however, the adapted strain Kr1^T showed the highest growth rate on pyrite 3 among all the cultures studied. No adaptation of strain Kr1^T to pyrite 5 was observed; the rates of growth and pyrite oxidation in the third transfer were lower than in the first transfer. The strain F. acidiphilum Y^T was not adapted to pyrites 3 and 5; the rates of growth and pyrite oxidation were the same in the first five transfers. The strains of three species of the microorganisms studied, A. ferrooxidans, S. thermotolerans, and F. acidiphilum, grew on pyrite 3 (holetype (p) conductivity) and oxidized it better than pyrite 5 (mixed-type (n-p) conductivity). The most readily oxidized were the pyrites with a density of 5.6–5.7 g/cm³ and high resistance values (ln R = 8.8). The pyrite oxidation rate did not depend on the type of conductivity. Changes in the chromosomal DNA structure were revealed in strain TFBk on adaptation to pyrites 3 and 4 and in the TFV-1 plasmid profile on adaptation to pyrite 3. Correlation between genetic variability and adaptive capabilities was shown for A. ferrooxidans. No changes in the chromosomal DNA structure were found in S. thermotolerans Kr1^T and F. acidiphilum Y^T on adaptation to pyrites 3 and 5. Plasmids were absent in the cells of these cultures.     

Characteristics of the restriction profile of chromosomal DNA in strains of Acidithiobacillus ferroxidans,adapted to various oxidation substrates

Restriction profiles of chromosomal DNA were studied in different Acidithiobacillus ferrooxidans strains grown on medium with Fe2+ and further adapted to another oxidation substrate (S0, FeS2, or sulfide ore concentrates). The restriction endonuclease XbaI digested the chromosomal DNA from different strains into different numbers of fragments of various sizes. Adaptation of two strains (TFBk and TFN-d) to new oxidation substrates resulted in structural changes in XbaI-restriction patterns of their chromosomal DNA. Such changes in the DNA restriction patterns occurred in strain TFBk after the adaptation to precyanidated gravitational pyrite-arsenopyrite concentrate (no. 1) from the Nezhdaninskoe deposit or to copper-containing ore from the Udokanskoe deposit and also in strain TFN-d adapted to untreated pyrite-arsenopyrite concentrate (no. 2) from the Nezhdaninskoe deposit. No changes in the number or size of the XbaI-restriction patterns of chromosomal DNA were revealed in either strain TFBk cultivated on media with pyrite from the Angren and Tulun deposits or in strains TFN-d and TFO grown on media with S0 and pyrite. Neither were changes observed in the XbaI-restriction patterns of the DNA from strain TFV-1, isolated from the copper ore of the Volkovskoe deposit, when Fe2+ was substituted with alternative substrates--S0, pyrite or concentrate no. 2 from the ore of Nezhdaninskoe deposit. In strain TFO, no differences in the XbaI-restriction patterns of the chromosomal DNA were revealed between the culture grown on medium containing concentrate no. 2 or the concentrate of surface-lying ore from Olimpiadinskoe deposit and the culture grown on medium with Fe2+. When strain TFO was cultivated on the ore concentrate from deeper horizons of the Olimpiadinskoe deposit, which are characterized by lower oxidation degree and high antimony content, mutant TFO-2 differing from the parent strain in the chromosomal DNA structure was isolated. The correlation between the lability of chromosomal DNA structure in A. ferrooxidans strains and the physical and chemical peculiarities of the isolation substrate and habitat is discussed.     

Leaching of Pyrites of Various Reactivities by Thiobacillus ferrooxidans

Wide variations were found in the rate of chemical and microbiological leaching of iron from pyritic materials from various sources. Thiobacillus ferrooxidans accelerated leaching of iron from all of the pyritic materials tested in shake flask suspensions at loadings of 0.4% (wt/vol) pulp density. The most chemically reactive pyrites exhibited the fastest bioleaching rates. However, at 2.0% pulp density, a delay in onset of bioleaching occurred with two of the pyrites derived from coal sources. T. ferrooxidans was unable to oxidize the most chemically reactive pyrite at 2.0% pulp density. No inhibition of pyrite oxidation by T. ferrooxidans occurred with mineral pyrite at 2.0% pulp density. Experiments with the most chemically reactive pyrite indicated that the leachates from the material were not inhibitory to iron oxidation by T. ferrooxidans.     

Identification of IS elements in <Emphasis Type="Italic">Acidithiobacillus ferrooxidans</Emphasis> strains grown in a medium with ferrous iron or adapted to elemental sulfur

IS elements were identified in the genomes of five Acidithiobacillus ferrooxidans strains isolated from various media. IST2 elements were revealed in all the strains grown in a medium with ferrous iron, ISAfe1 elements were detected in four strains (TFBk, TFL-2, TFV-1 and TFO). Three strains (TFV-1, TFN-d and TFO) were found to contain IS elements, ~600 bp long. These were named preliminary as ISAfe600. Partial sequencing of the 5′- and 3′-terminal nucleotide stretches of an ISAfe1 element in TFBk and TFL-2 strains and complete sequencing of the ISAfe1 element in the TFBk strain has revealed nucleotide substitutions as compared to the prototype, i.e., the ISAfe1 element of an ATCC 19859 strain. Partial sequencing of the 5′- and 3′-terminal nucleotide stretches of the IST2 elements in TFO, TFBk and TFL-2 strains has shown numerous nucleotide substitutions when compared to the IST2 element of an ATCC 19859 strain. Complete sequencing of the IST2 element in the TFBk strain has revealed: the divergence between the IST2 elements in the TFBk strain and the prototype was 21.2%. Southern hybridization of EcoRI fragments of the chromosomal DNA from five A. ferrooxidans strains grown in a medium with ferrous iron using an internal region of ISAfe1, a full-length ISAfe1 or a full-length IST2 as probes has shown them to differ in the number of copies of IS elements and their localization on the chromosomes. Adaptation to elemental sulfur in A. ferrooxidans strains caused changes in the number, intensity and localization of hybridization bands. The authors discuss the role of IS elements in the adaptation of A. ferrooxidans to the new energy substrate. The nucleotide sequence data reported in this paper were deposited in GenBank under accession numbers: AY823401, the ISAfe1 from A. ferrooxidans TFBk; AY825254, the IST2 from TFBk; DQ002894, the 5′-terminal nucleotide sequence of ISAfe1 from TFL-2; DQ002895, the 3′-terminal nucleotide sequence of ISAfe1 from TFL-2; DQ005952, the 5′-terminal nucleotide sequence of IST2 from TFV-1; DQ005953, the 3′-terminal nucleotide sequence of IST2 from TFV-1.     

Phenotypic characteristics of Thiobacillus ferrooxidans strains

Phenotypic polymorphism of strains of Thiobacillus ferrooxidans isolated from various ecological niches was studied. The strains differed both in rates of growth and oxidation of Fe2+, S0, FeS2, and sulfide minerals contained in concentrate. Each strain, irrespective of its original environment, required a period of adaptation to a new substrate. Strains TFN-d, TFBk, TFO, and TFL-2, isolated from ores and concentrates rich in oxidized substrates, showed an equal adaptation pace (five culture transfers) but differed in their adaptation efficiency. Strain TFV-1, isolated from base ore and showing the lowest rates of growth and oxidation of all the substrates, required five culture transfers to adapt to S0 and FeS2 and seven culture transfers to adapt to the concentrate. It is concluded that the phenotypic properties of the strains correlate with their genotypic polymorphism and the environmental conditions under which their microevolution took place.     

Restriction Profiles of the Chromosomal DNA from Acidithiobacillus ferrooxidans Strains Adapted to Different Oxidation Substrates

Restriction profiles of chromosomal DNA were studied in different Acidithiobacillus ferrooxidans strains grown on medium with Fe²⁺ and further adapted to another oxidation substrate (S⁰, FeS₂, or sulfide ore concentrates). The restriction endonuclease XbaI digested the chromosomal DNA from different strains into different numbers of fragments of various sizes. Adaptation of two strains (TFBk and TFN-d) to new oxidation substrates resulted in structural changes in XbaI-restriction patterns of their chromosomal DNA. Such changes in the DNA restriction patterns occurred in strain TFBk after the adaptation to precyanidated gravitational pyrite-arsenopyrite concentrate (no. 1) from the Nezhdaninskoe deposit or to copper-containing ore from the Udokanskoe deposit and also in strain TFN-d adapted to untreated pyrite-arsenopyrite concentrate (no. 2) from the Nezhdaninskoe deposit. No changes in the number or size of the XbaI-restriction patterns of chromosomal DNA were revealed in either strain TFBk cultivated on media with pyrite from the Angren and Tulun deposits or in strains TFN-d and TFO grown on media with S⁰ and pyrite. Neither were changes observed in the XbaI-restriction patterns of the DNA from strain TFV-1, isolated from the copper ore of the Volkovskoe deposit, when Fe²⁺ was substituted with alternative substrates—S⁰, pyrite or concentrate no. 2 from the ore of the Nezhdaninskoe deposit. In strain TFO, no differences in the XbaI-restriction patterns of the chromosomal DNA were revealed between the culture grown on medium containing concentrate no. 2 or the concentrate of surface-lying ore from the Olimpiadinskoe deposit and the culture grown on medium with Fe²⁺. When strain TFO was cultivated on the ore concentrate from deeper horizons of the Olimpiadinskoe deposit, which are characterized by lower oxidation degrees and high antimony content, mutant TFO-2 differing from the parent strain in the chromosomal DNA structure was isolated. The correlation between the lability of the chromosomal DNA structure in A. ferrooxidans strains and the physical and chemical peculiarities of the isolation substrate and habitat is discussed.     

Patterns of pyrite oxidation by different microorganisms

The bacterial-chemical oxidation of natural pyrites with different physical, chemical, and electrophysical characteristics by bacteria Acidithiobacillus ferrooxidans, Sulfobacillus thermotolerans, and the archaeon Ferroplasma acidiphilum were studied. The electrophysical characteristics of three natural pyrites differed in the K _thermoEMF value (pyrites 3, 4, hole conduction (p-type conductivity); pyrite 5, mixed type conductivity (n-p)) and in the logarithm of electric resistance. Chemical oxidation of pyrites 3 and 5 resulted in no changes of K _thermoEMF. When pyrite 4 was oxidized chemically, the K _thermoEMF values remained in the same range as in the initial sample, but the ratio of grains with different K _thermoEMF values in the sample was changed: the number of grains with a higher K _thermoEMF value increased. The same changes were also observed in the course of bacterio-chemical oxidation of pyrite 4. Of the three pyrites studied, an increase in the logarithm of resistance was observed only for chemical oxidation of pyrite 4 at 28°C. At higher experimental temperatures, the logarithm of resistance increased accordingly; more active bacterial-chemical oxidation resulted in a more pronounced increase in the logarithm of resistance than chemical oxidation. On bacterial-chemical oxidation of pyrites 3 and 5 by A. ferrooxidans and S. thermotolerans strains, iron was leached more actively than sulfur. Preferred bacterial-chemical oxidation of certain fractions from the pyrite samples was shown, namely of the pyrite 3 fraction with higher K _thermoEMF values by the F. acidiphilum strain and of a fraction from the pyrite 5 sample with medium K _thermoEMF values by the A. ferrooxidans and S. thermotolerans strains. The comparative assessment of bacterial-chemical pyrite oxidation by three types of microorganisms showed the direction of changes in the K _thermoEMF values to be the same in the case of bacteria Acidithiobacillus ferrooxidans and Sulfobacillus thermotolerans and different in the case of the archaeon Ferroplasma acidiphilum.     

Plasmid profiles of Acidithiobacillus ferrooxidans strains adapted to different oxidation substrates

Plasmid profiles were studied in five Acidithiobacillus ferrooxidans strains of various origin cultivated on medium with Fe2+, as well as adapted to such oxidation substrates as S0, FeS2, and sulfide concentrate. The method used revealed plasmids in all A. ferrooxidans strains grown on medium with Fe2+. One plasmid was found in strain TFL-2, two plasmids, in strains TFO, TFBk, and TFV-1, and three plasmids were detected in strain TFN-d. The adaptation of strain TFN-d to sulfide concentrate and the adaptation of strain TFV-1 to S0, FeS2, or sulfide concentrate resulted in a change in the number of plasmids occurring in cells. In cells of strain TFN-d adapted to sulfide concentrate, the number of plasmids decreased from three to two. The number of plasmids in cells of strain TFV-1 adapted to different substrates varied from three to six depending on the energy source present in the medium: three plasmids were found after growth on FeS2, four after growth on S0, and six after growth on sulfide concentrate. The possible role of plasmids in the adaptation of A. ferrooxidans to new energy substrates and in the regulation of the intensity of their oxidation is discussed.     

Plasmid Profiles of Acidithiobacillus ferrooxidans Strains Adapted to Different Oxidation Substrates

Plasmid profiles were studied in five Acidithiobacillus ferrooxidans strains of various origin cultivated on a medium with Fe²⁺, as well as adapted to such oxidation substrates as S⁰, FeS₂, and sulfide concentrate. The method used revealed plasmids in all A. ferrooxidans strains grown on a medium with Fe²⁺. One plasmid was found in strain TFL-2; two plasmids, in strains TFO, TFBk, and TFV-1; and three plasmids were detected in strain TFN-d. The adaptation of strain TFN-d to sulfide concentrate and the adaptation of strain TFV-1 to S⁰, FeS₂, or sulfide concentrate resulted in a change in the number of plasmids occurring in cells. In cells of strain TFN-d adapted to sulfide concentrate, the number of plasmids decreased from three to two. The number of plasmids in cells of strain TFV-1 adapted to different substrates varied from three to six depending on the energy source present in the medium: three plasmids were found after growth on FeS₂, four after growth on S⁰, and six after growth on sulfide concentrate. The possible role of plasmids in the adaptation of A. ferrooxidans to new energy substrates and in the regulation of the intensity of their oxidation is discussed.     

Phenotypic Characteristics of Thiobacillus ferrooxidansStrains

Phenotypicpolymorphism of Thiobacillus ferrooxidansstrains isolated from various ecological niches was studied. The strains differed both in rates of growth and oxidation of Fe²⁺, S⁰, FeS₂, and sulfide minerals contained in concentrate. Each strain, irrespective of its original environment, required a period of adaptation to a new substrate. Strains TFN-d, TFBk, TFO, and TFL-2, isolated from ores and concentrates rich in oxidizable substrates, showed an equal adaptation rate (five culture transfers) but differed in their adaptation efficiency. Strain TFV-1, isolated from low-grade ore and showing the lowest rates of growth and oxidation of all the substrates, required five culture transfers to adapt to S⁰and FeS₂and seven culture transfers to adapt to the concentrate. It is concluded that the phenotypic properties of the strains correlate with their genotypic polymorphism and the environmental conditions under which their microevolution took place.     

Strain polymorphism of the plasmid profiles in Acidithiobacillus ferrooxidans

Plasmid profiles were studied in 27 Acidithiobacillus ferrooxidans strains isolated from different geographic zones and substrates differing in the composition of the main sulfide minerals, and also in experimentally obtained strains with acquired enhanced resistance to the ions of heavy metals (Fe, Ni, Cu, Zn, As). In 16 out of 20 strains isolated from different substrates, one to four 2- to 20-kb and larger plasmids were revealed. Plasmids were found in all five strains isolated from gold-containing pyrite-arsenopyrite ores and concentrates, in nine of 11 strains isolated from the ores and concentrates containing nonferrous metals, and in two of four strains isolated from the oxidation substrates of simple composition (mine waters, pyritized coals, active sludge). Changes in the plasmid profiles in some A. ferrooxidans strains (TFZ, TFI-Fe, TFV-1-Cu) with experimentally enhanced resistance to Zn2+, Fe3+, and Cu2+, respectively, were noted as compared with the initial strains. After 30 passages on S0-containing medium, strain TFBk showed changes in the copy number of plasmids. The role of plasmids in the processes of oxidation of energy substrates and in the acquired enhanced resistance to the heavy metal ions is discussed.     

Strain Polymorphism of the Plasmid Profiles in Acidithiobacillus ferrooxidans

Plasmid profiles were studied in 27 Acidithiobacillus ferrooxidans strains isolated from different geographic zones and substrates differing in composition of the main sulfide minerals, and also in experimentally obtained strains with acquired enhanced resistance to the ions of heavy metals (Fe, Ni, Cu, Zn, As). In 16 out of 20 strains isolated from different substrates, one to four 2- to 20-kb and larger plasmids were revealed. Plasmids were found in all five strains isolated from gold-containing pyrite–arsenopyrite ores and concentrates, in nine of 11 strains isolated from the ores and concentrates containing nonferrous metals, and in two of four strains isolated from the oxidation substrates of simple composition (mine waters, pyritized coals, active sludge). Changes in the plasmid profiles in some A. ferrooxidans strains (TFZ, TFI-Fe, TFV-1-Cu) with experimentally enhanced resistance to Zn²⁺, Fe³⁺, and Cu²⁺, respectively, were noted as compared with the initial strains. After 30 passages on a S⁰-containing medium, strain TFBk showed changes in the copy number of plasmids. The role of plasmids in the processes of oxidation of energy substrates and in the acquired enhanced resistance to heavy metal ions is discussed.     

Thermoacidophilic microbial community oxidizing the gold-bearing flotation concentrate of a pyrite-arsenopyrite ore

An aboriginal community of thermophilic acidophilic chemolithotrophic microorganisms (ACM) was isolated from a sample of pyrite gold-bearing flotation concentrate at 45–47°C and pH 1.8–2.0. Compared to an experimental thermoacidophilic microbial consortium formed in the course of cultivation in parallel bioreactors, it had lower rates of iron leaching and oxidation, while its rate of sulfur oxidation was higher. A new thermophilic acidophilic microbial community was obtained by mutual enrichment with the microorganisms from the experimental and aboriginal communities during the oxidation of sulfide ore flotation concentrate at 47°C. The dominant bacteria of this new ACM community were Acidithiobacillus caldus (the most active sulfur oxidize) and Sulfobacillus thermotolerans (active oxidizer of both iron and sulfur), while iron-oxidizing archaea of the family Ferroplasmaceae and heterotrophic bacteria Alicyclobacillus tolerans were the minor components. The new ACM community showed promise for leaching/oxidation of sulfides from flotation concentrate at high pulp density (S : L = 1 : 4).     

Influence of pulp density and bioreactor design on microbial desulphurization of coal

Summary Pyrite was microbiologically removed by Thiobacillus ferrooxidans in pure and mixed cultures from German bituminous coal at 10% pulp density with maximum pyrite oxidation rate of 350 mg pyritic S/l per day. However, at pulp densities above 20% bacterial growth and consequently pyrite oxidation were completely prevented both in a conventional airlift reactor and in a stirred-tank reactor. Modifying the airlift reactor by adapting a conical bottom part, bacterial growth and pyrite oxidation could be achieved even at 30% pulp density, resulting in a pyrite removal of more than 90% at a pyrite oxidation rate of 230 mg pyritic S/l per day.Dedicated to Prof. Dr. H. Jüntgen on the occasion of his 60th birthday     

Rate Equations and Kinetic Parameters of the Reactions Involved in Pyrite Oxidation by Thiobacillus ferrooxidans

Rate equations and kinetic parameters were obtained for various reactions involved in the bacterial oxidation of pyrite. The rate constants were 3.5 μM Fe²⁺ per min per FeS₂ percent pulp density for the spontaneous pyrite dissolution, 10 μM Fe²⁺ per min per mM Fe³⁺ for the indirect leaching with Fe³⁺, 90 μM O₂ per min per mg of wet cells per ml for the Thiobacillus ferrooxidans oxidation of washed pyrite, and 250 μM O₂ per min per mg of wet cells per ml for the T. ferrooxidans oxidation of unwashed pyrite. The K_m values for pyrite concentration were similar and were 1.9, 2.5, and 2.75% pulp density for indirect leaching, washed pyrite oxidation by T. ferrooxidans, and unwashed pyrite oxidation by T. ferrooxidans, respectively. The last reaction was competitively inhibited by increasing concentrations of cells, with a K_i value of 0.13 mg of wet cells per ml. T. ferrooxidans cells also increased the rate of Fe²⁺ production from Fe³⁺ plus pyrite.     

Sulfide oxidation by spheroplasts of Thiobacillus ferrooxidans.

Thiobacillus ferrooxidans is an acidophilic organism important to metal leaching of low-grade ores. The aforementioned importance is related to the ability of the bacterium to oxidize reduced iron and sulfur, principally found in nature as pyrite (FeS2). The present study dealt with sulfide oxidation at low pH values and the involvement of the cell envelope in the process of the inorganic oxidations. Sulfide oxidation was noted in spheroplasts of T. ferrooxidans prepared by enzymatic and chemical treatments and partially purified by differential centrifugation. No enzyme activities were noted in membrane fractions containing enrichments of lipopolysaccharide symbolic of outer membrane material or in membrane vesicles containing (or associated with) higher levels of proteins. Results to date indicate that in an acid milieu the envelope structure containing both the outer membrane and the intact inner cytoplasmic membrane is required for sulfide oxidation.     

Leaching of Pyrite by Acidophilic Heterotrophic Iron-Oxidizing Bacteria in Pure and Mixed Cultures

Seven strains of heterotrophic iron-oxidizing acidophilic bacteria were examined to determine their abilities to promote oxidative dissolution of pyrite (FeS₂) when they were grown in pure cultures and in mixed cultures with sulfur-oxidizing Thiobacillus spp. Only one of the isolates (strain T-24) oxidized pyrite when it was grown in pyrite-basal salts medium. However, when pyrite-containing cultures were supplemented with 0.02% (wt/vol) yeast extract, most of the isolates oxidized pyrite, and one (strain T-24) promoted rates of mineral dissolution similar to the rates observed with the iron-oxidizing autotroph Thiobacillus ferrooxidans. Pyrite oxidation by another isolate (strain T-21) occurred in cultures containing between 0.005 and 0.05% (wt/vol) yeast extract but was completely inhibited in cultures containing 0.5% yeast extract. Ferrous iron was also needed for mineral dissolution by the iron-oxidizing heterotrophs, indicating that these organisms oxidize pyrite via the “indirect” mechanism. Mixed cultures of three isolates (strains T-21, T-23, and T-24) and the sulfur-oxidizing autotroph Thiobacillus thiooxidans promoted pyrite dissolution; since neither strains T-21 and T-23 nor T. thiooxidans could oxidize this mineral in yeast extract-free media, this was a novel example of bacterial synergism. Mixed cultures of strains T-21 and T-23 and the sulfur-oxidizing mixotroph Thiobacillus acidophilus also oxidized pyrite but to a lesser extent than did mixed cultures containing T. thiooxidans. Pyrite leaching by strain T-23 grown in an organic compound-rich medium and incubated either shaken or unshaken was also assessed. The potential environmental significance of iron-oxidizing heterotrophs in accelerating pyrite oxidation is discussed.     

Intermediary sulfur compounds in pyrite oxidation: implications for bioleaching and biodepyritization of coal

Accumulation of elemental sulfur during pyrite oxidation lowers the efficiency of coal desulfurization and bioleaching. In the case of pyrite bioleaching by Leptospirillum ferrooxidans, an iron(II)-ion-oxidizing organism without sulfur-oxidizing capacity, from the pyritic sulfur moiety about 10% elemental sulfur, 2% pentathionate, and 1% tetrathionate accumulated by a recently described cyclic pyrite oxidation mechanism. In the case of pure cultures of Thiobacillus ferrooxidans and mixed cultures of L. ferrooxidans and T. thiooxidans, pyrite was nearly completely oxidized to sulfate because of the capacity of these cultures to oxidize both iron(II) ions and sulfur compounds. Pyrite oxidation in acidic solutions, mediated chemically by iron(III) ion, resulted in an accumulation of similar amounts of sulfur compounds as obtained with L. ferrooxidans. Changes of pH to values below 2 or in the iron ion concentration are not decisive for diverting the flux of sulfur compounds. The literature on pyrite bioleaching is in agreement with the findings indicating that the chemistry of direct and indirect pyrite leaching is identical. Received: 20 April 1998 / Received revision: 27 August 1998 / Accepted: 3 September 1998