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Applied and Environmental Microbiology, March 2000, p. 1031-1037, Vol. 66, No. 3
0099-2240/00/$04.00+0
Copyright © 2000, American Society for Microbiology. All rights reserved.
Selective Inhibition of the Oxidation of Ferrous
Iron or Sulfur in Thiobacillus ferrooxidans
Lesia
Harahuc,1
Hector M.
Lizama,2 and
Isamu
Suzuki1,*
Department of Microbiology, University of
Manitoba, Winnipeg, Manitoba,1 and
Cominco Research Limited, Trail, British
Columbia,2 Canada
Received 23 August 1999/Accepted 12 December 1999
 |
ABSTRACT |
The oxidation of either ferrous iron or sulfur by
Thiobacillus ferrooxidans was selectively inhibited or
controlled by various anions, inhibitors, and osmotic pressure. Iron
oxidation was more sensitive than sulfur oxidation to inhibition by
chloride, phosphate, and nitrate at low concentrations (below 0.1 M)
and also to inhibition by azide and cyanide. Sulfur oxidation was more
sensitive than iron oxidation to the inhibitory effect of high osmotic
pressure. These differences were evident not only between iron
oxidation by iron-grown cells and sulfur oxidation by sulfur-grown
cells but also between the iron and sulfur oxidation activities of the same iron-grown cells. Growth experiments with ferrous iron or sulfur
as an oxidizable substrate confirmed the higher sensitivity of iron
oxidation to inhibition by phosphate, chloride, azide, and cyanide.
Sulfur oxidation was actually stimulated by 50 mM phosphate or
chloride. Leaching of Fe and Zn from pyrite (FeS2) and
sphalerite (ZnS) by T. ferrooxidans was differentially
affected by phosphate and chloride, which inhibited the solubilization of Fe without significantly affecting the solubilization of Zn.
 |
INTRODUCTION |
Thiobacillus ferrooxidans
is a gram-negative acidophilic chemolithoautotroph, using
CO2 as a carbon source and obtaining its energy for growth
from the oxidation of ferrous iron, sulfur, and reduced sulfur
compounds (26). T. ferrooxidans was initially isolated from acidic copper-leaching waters and believed to be the
dominant bacterium responsible for metal sulfide solubilization (18). Iron oxidation in response to pH (1, 28),
organic acids (40), anions (2, 17), and cations
(21, 38) has been extensively studied. Sulfur oxidation has
received substantially less attention, with limited references to
certain anions (26).
Thiobacilli have considerable economic importance in the treatment of
acid mine drainage (10, 22) and desulfurization of waste
gases (SO2 and H2S) (10, 12, 29).
The use of bacteria in the mining industry is a growing field of
interest (4, 25). Levels of tolerance of key metals by
T. ferrooxidans growth on Fe2+ are as follows:
Cd2+, 0.75 M; Ni2+, 1 M; Zn2+, 1 M;
Cu2+, 0.6 M; Co2+, 0.15 M; Cr3+,
0.075 M; Pb2+, 1 mM; Hg+, 0.1 mM;
Hg2+, 10 µM; and Ag+, 1 µM (21).
The naturally occurring counterion sulfate is not inhibitory at 0.14 M
(26, 39), and the concentration may reach as high as 1.25 M
during bacterial leaching of sulfide minerals (7).
Metal extraction from mineral ore by T. ferrooxidans is
achieved through two reactions: the oxidation of ferrous to ferric iron
(2Fe2+ + 1/2 O2 + 2H+
2Fe3+ + H2O) and that of sulfide/sulfur to
sulfuric acid (H2S + 2O2
H2SO4 or S0 + 1 1/2O2 + H2O
H2SO4). Uranium solubilization from uraninite, for example, requires only iron oxidation (UO2 + 2Fe3+
2Fe2+ + UO22+, 2Fe2+ + 1/2
O2 + 2H+
2Fe3+ + H2O), while zinc solubilization from sphalerite
necessitates sulfide oxidation (ZnS + 2O2
ZnSO4). Metal extraction becomes complicated when ores
contain mineral combinations (19, 27). In a
pyrite-sphalerite mixture T. ferrooxidans will oxidize both sulfide (ZnS + 2O2
ZnSO4) and iron
plus sulfide [4FeS2 + 15O2 + 2H2O
2Fe2(SO4)3 + 2H2SO4], creating difficulty in further zinc
recovery from the leachate. Low concentrations of ferric sulfate are
beneficial in the indirect leaching of mineral ores. Higher
concentrations, however, result in the production of jarosite, a ferric
iron precipitate which can cover the ore surface, preventing further
leaching from occurring. Higher jarosite levels also produce an
additional disposal problem.
We propose to show that the iron and sulfur oxidation activities of
T. ferrooxidans can be differentially controlled through the
use of specific anions and inhibitors. Under certain conditions iron
oxidation can be blocked with little to no effect on sulfur oxidation
and vice versa. Through this type of manipulation we hoped to achieve
specific metal extraction from an ore sample, with the absence or at
least reduction of contaminating metals.
 |
MATERIALS AND METHODS |
Media.
T. ferrooxidans strain SM-4 (20) was
grown in modified 9K medium (M9K): 0.4 g of
(NH4)2SO4, 0.1 g of
K2HPO4, 0.4 g of MgSO4 · 7H2O, and 33.3 g of FeSO4 · 7H2O per liter, adjusted to pH 2.3 with
H2SO4. Cells used for sulfur oxidation were
grown in Starkey no. 1 medium (33) after adaptation on
sulfur (37): 0.3 g of (NH4)2SO4, 3.5 g of
KH2PO4, 0.5 g of MgSO4
· 7H2O, 0.25 g of CaCl2, and 18 mg of
FeSO4 · 7H2O per liter, adjusted to pH
2.3 with H2SO4. Powdered sulfur (10 g of BDH
sulfur per liter) was spread evenly over the surface after inoculation.
Thiobacillus thiooxidans strain SM-6 grown on sulfur was
used for most of the growth experiments on sulfur, since sulfur-adapted
T. ferrooxidans was not available. The results of key
experiments, however, were later confirmed with sulfur-adapted T. ferrooxidans strain SM-4.
Culture procedures.
Iron-grown cells were cultured in M9K
using a 10% inoculum. The flasks were incubated at 25°C and placed
on a rotary shaker at 150 rpm for 48 h. The culture was passed
through Whatman no. 1 filter paper to remove the majority of the
precipitated ferric iron. The supernatant was centrifuged at
8,000 × g for 10 min. The cell pellet was resuspended
in 0.1 M
-alanine sulfate buffer (pH 2.3) and centrifuged at
1,000 × g for 5 min to allow further ferric iron
sedimentation. The supernatant was transferred to a secondary tube and
centrifuged at 10,000 × g for 10 min. The cells were
centrifuged a fourth time, generating a final suspension of 50 mg of
cells (wet weight) per ml in the same buffer. The protein concentration
was determined using bovine serum albumin as the standard
(37).
Sulfur-grown cells were cultured in Starkey no. 1 medium using a 2.5%
inoculum. The stationary flasks were incubated at 28°C for 4 days.
The cell collection procedure was identical to that for iron-grown cells.
Determination of iron and sulfur oxidation using cell
suspensions.
The rates of iron and sulfur oxidation were measured
using a Gilson oxygraph equipped with a Clark oxygen electrode at
25°C. The reaction vessel contained 10 µl of cell suspension
(sulfur- or iron-grown cells), 0.1 ml of sulfur suspension (32 g of BDH S0 in 100 ml, plus 500 ppm of Tween 80) (for sulfur
oxidation) or 0.5 µmol of FeSO4 · 7H2O
(for iron oxidation), and various concentrations of potassium salts of
anions, sucrose, or
-alanine buffer (all at pH 3.0 unless otherwise
stated) to make a total volume of 1.2 ml. The effect of azide and
cyanide was studied in 0.1 M
-alanine sulfate at pH 3. For sulfur
oxidation by iron-grown cells, however, 100 µl of the cell suspension
was required for accurate rate determinations. All tests whose results
are shown in Fig. 1 were performed at pH 3 rather than pH 2.3 (growth
pH) because of the lower sulfur oxidation activity at pH 2.3. Duplicate
experiments using the same batch of cells were impossible to carry out
for all of the conditions tested due to the instability of activity
after more than 2 days of storage. Results, however, were reproducible
with other batches of cells, although absolute activities varied from 10 to 20%. Standard deviations in the activity determinations fell
within 10% of the stated values except for sulfur oxidation by
iron-grown cells, where the values could deviate by as much as 20%. It
should be noted that all of the experiments testing iron and sulfur
oxidation were repeated with T. ferrooxidans ATCC 19859, with similar results.
Determination of iron and sulfur oxidation and carbon dioxide
fixation using growing cell cultures.
The rates of iron and sulfur
oxidation in growing cell cultures were measured using a Micro-oxymax
respirometer (Columbus Instruments) at Cominco Research Limited, Trail,
British Columbia, Canada. The reaction vessel contained a 5% inoculum,
12 mmol of FeSO4 · 7H2O (for iron
oxidation) or 1 g of BDH sulfur sprinkled on the surface plus 18 mg of FeSO4 · 7H2O per liter (for sulfur oxidation), various concentrations of anionic salts or inhibitors, and
M9K at pH 2.3, making a total volume of 100 ml. The reaction was
stirred with a magnetic stirrer, and both O2 consumption
(oxidation) and CO2 consumption (autotrophic growth) were
measured at 26°C.
Shake flask leaching of metals.
Flotation tailings, provided
by Cominco Research Limited, contained 3.3% Zn as sphalerite and 5.5%
Fe as pyrite (FeS2) and were in the form of a finely ground
powder. Five grams of tailings was placed in a 250-ml Erlenmeyer flask
with 100 ml of M9K at pH 2.3 with or without additional potassium
phosphate. The flask was inoculated with 5 ml of T. ferrooxidans SM-4 (grown on FeSO4) and left stationary
at 25°C for 24 h, followed by shaking on rotary shaker at 180 rpm for the remainder of the experiment. Five-milliliter samples were
taken at time zero, 2 and 14 days, filtered through Whatman no. 1 filter paper, and analyzed for dissolved Fe and Zn content by atomic
absorption spectrophotometry. The extent of metal leaching was
calculated as percent extraction from the total metal content of the tailings.
 |
RESULTS AND DISCUSSION |
Effect of anions on iron and sulfur oxidation.
Cell
suspensions were initially used to determine the effects of anions and
selective inhibitors on the iron and sulfur oxidation activities of
T. ferrooxidans. The reaction in each case was carried out
at pH 3, an acidic pH comparable to natural growing conditions. The
specific activities of iron (Fig. 1A) and
sulfur (Fig. 1B and C) oxidation in buffer concentrations ranging from
0.01 to 0.5 M were determined. Enzymes required for iron and sulfur
oxidation are differentially expressed depending on the bacterial
growth substrate (14, 23, 37). Cells grown on ferrous iron
showed only low levels of sulfur-oxidizing activities (Fig. 1B)
compared to sulfur-grown cells (Fig. 1C). Although not shown in Fig. 1, iron oxidation experiments were also carried out at pHs 2.3 and 1.8, and they showed a stronger inhibition by the potassium salts. Sucrose
was not inhibitory at all pH values, while
-alanine was less
inhibitory than the potassium salts at lower pH values.

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FIG. 1.
Effects of concentrations of various anions, sucrose,
and -alanine on the oxidation of ferrous iron and sulfur in
iron-grown T. ferrooxidans strain SM-4 and of sulfur in
sulfur-grown T. ferrooxidans strain SM-4. Please note the
different scales on the y axes.
|
|
Sulfate is an anion that is normally associated with the environment in
which the organism is found, e.g., acid mine drainage
water. It was
initially believed to act as a bridging ligand between
ferrous iron and
the cell (
16,
17). Further experiments showed
its role in
the transfer of electrons from an iron sulfur cluster
to the copper(II)
ion of rusticyanin in the oxygen-dependent iron
oxidation electron
transport chain (
8). A sulfate requirement
for rusticyanin
reduction by ferrous iron was also reported with
a partially purified
iron:rusticyanin oxidoreductase (
3). Figure
1 shows that
sulfate up to a concentration of 0.2 M had very little
effect on either
the iron or sulfur oxidation pathway. Beyond
this point, iron oxidation
was only marginally affected, while
sulfur oxidation showed a dramatic
drop in activity. This apparent
preferential inhibition of sulfur
oxidation at high sulfate concentrations
is believed to be caused by
changes in osmotic pressure, as it
was observed in all other buffers at
high concentrations (Fig.
1) except nitrate, a specific inhibitor of
iron oxidation (
17),
as discussed below. High osmotic
pressure inhibited sulfur oxidation
in all the buffers tested both with
iron-grown (Fig.
1B) and sulfur-grown
(Fig.
1C) cells. Iron oxidation
by the same iron-grown cells,
however, was insensitive to high osmotic
pressure (Fig.
1A).
Chloride is a known inhibitor of cell growth and ferrous iron oxidation
(
17,
26). It is an inhibitor of cell-free iron-cytochrome
c reductase (
6). A concentration of 0.14 M was
reported as
being toxic to the bacteria in its initial description in
1963
(
26). Figure
1A shows that chloride is indeed
inhibitory compared
to sulfate for iron oxidation even at the lowest
concentration
used, 10 mM. Increased chloride concentrations resulted
in a marginal
added decrease in specific activity. Sulfur oxidation, on
the
other hand, was inhibited only at very high chloride
concentrations.
Iron-grown cells were inhibited at 0.2 M chloride (Fig.
1B), while
sulfur-grown cells were relatively unaffected up to a
concentration
of 0.4 M (Fig.
1C).
Phosphate is required for normal bacterial function (
2).
Cells grown with phosphate limitation present a filamentous morphology
due to a lack of cell division (
31,
32). Phosphate
starvation
studies show changes in the degree of synthesis of at least
25
proteins, some of which are exclusively synthesized under starvation
conditions (
30-32). A number of these proteins have been
linked
to the bacterial surface, suggesting the existence of a
phosphate
scavenging system in
T. ferrooxidans (
13,
30). Phosphate concentrations
used in this study were not
limiting but rather in excess. The
lowest phosphate concentration used,
10 mM, allowed for maximal
iron and sulfur oxidation in iron- and
sulfur-grown cells, respectively
(Fig.
1A and C). Additional phosphate
resulted in a sharp decrease
in iron oxidation up to 0.1 M, followed by
a moderate return of
activity. Sulfur oxidation in iron-grown cells
(Fig.
1B) showed
both activation at low phosphate concentrations and
inhibition
at high phosphate concentrations. Sulfur-grown cells, on the
other
hand, showed inhibition only at high phosphate concentrations,
similar to sulfate or chloride. Thus, iron-grown cells with low
sulfur-oxidizing activities and sulfur-grown cells with high oxidizing
activities responded differently at low phosphate concentrations
yet
similarly at high phosphate concentrations, distinct from
their
response in iron
oxidation.
Nitrate is an inorganic anion known to inhibit oxidation by and growth
of
T. ferrooxidans on ferrous iron (
17). Iron
oxidation
using cell suspensions was completely inhibited by sodium
nitrate
concentrations of 1 to 94 mM (
17,
26). The large
degree in
variation is due to experimental design and strain
specificity.
T. ferrooxidans strain SM-4 was sensitive to
nitrate at the lowest
concentration used. Increased levels of nitrate
completely inhibited
iron oxidation. Sulfur oxidation was more
resistant, showing little
to no inhibition up to 0.1 M. Higher nitrate
concentrations, however,
resulted in a substantial drop in sulfur
oxidation. It should
be noted that nitrate was more strongly inhibitory
in growth experiments
on sulfur at pH 2.3, as shown
below.
The sucrose and

-alanine buffers used in this study were adjusted
with sulfuric acid. The purpose of these buffers was to
show the effect
of osmotic pressure on the two key reactions examined
(iron and sulfur
oxidation). Ferrous iron oxidation is believed
to take place on the
outer surface of the cell membrane (
11).
The ferrous ion is
soluble and is expected to interact with the
polynuclear iron coat
surrounding the cell (
11) or the iron-cytochrome
c reductase on the exterior membrane (
9). Only
the electrons
enter the cell, moving through the electron transport
system,
with the final reduction of oxygen to water. In this general
scheme,
osmotic pressure is not expected to have any significant effect
on iron oxidation. Sucrose and

-alanine at high concentrations,
i.e., high osmotic pressure, had little effect on iron oxidation
(Fig.
1A). Sulfur oxidation, on the other hand, in both iron-
and
sulfur-grown cells (Fig.
1B and C) was inhibited by high osmotic
pressure.
As shown in Fig.
1, phosphate, chloride, and nitrate all preferentially
inhibited iron oxidation. Phosphate caused 50% inhibition
of iron
oxidation at 100 mM, the concentration at which sulfur
oxidation was
maximal. Sulfur oxidation activities of iron-grown
cells and
sulfur-grown cells were equally inhibited by increasing
osmotic
pressures, created by high concentrations of either inorganic
salts
(K
2SO
4, KCl, KP
i, or
KNO
3), sucrose, or

-alanine sulfate
(Fig.
1).
Essentially identical results were obtained with
T. ferrooxidans ATCC 19859. Since growth on sulfur induces new
proteins
in iron-grown
T. ferrooxidans (
23), it
is surprising that the
two types of cells responded similarly. This
uniform effect must
be directly related to the mechanism of sulfur
oxidation, which
is different from that of iron oxidation. Sulfur,
unlike ferrous
iron, is an insoluble substrate. At high osmotic
pressure the
cells lose water and the membranes shrink, making contact
with
the sulfur particles and their subsequent oxidation difficult.
Similar inhibition of sulfur oxidation by high osmotic pressure
has
been obtained with
T. thiooxidans (
36). The
general trend
observed with cell suspensions (Fig.
1) was found to be
applicable
to growing cell cultures, as shown
below.
Effects of azide and cyanide on iron and sulfur oxidation.
The
sulfur and iron oxidation pathways and their interactions are
surrounded by a great deal of controversy. Sugio et al. suggest that
ferric iron reduction is coupled to sulfur oxidation under both aerobic
and anaerobic conditions (34, 35). An alternate theory
proposed by Corbett and Ingledew suggests that the iron and sulfur
oxidation pathways are two separate entities but that ferric iron can
replace oxygen as a terminal electron acceptor under anaerobic
conditions (5). Iron- and sulfur-dependent oxygen uptake
occurs via two separate oxidases (24). Azide at low
concentrations is a specific inhibitor of the terminal oxidase of
ferrous iron oxidation, but not that of sulfur oxidation
(24). The results in Table 1
agree with the concept of two terminal oxidases being differentially
inhibited by azide. Inhibition of iron oxidation by 50% required only
0.7 µM azide, while that of sulfur oxidation required 19 to 32 µM
azide. Cyanide is also a specific inhibitor of the terminal oxidase. It
behaved in a manner similar to that of azide, preferentially inhibiting
iron oxidation. As shown in Table 1, only 3.2 µM cyanide was required
to cut the iron oxidation in half, while 77 to 323 µM was necessary
to produce a similar effect on sulfur oxidation.
Effects of anions and inhibitors on cell growth.
The second
part of this paper deals with the use of the above-mentioned anions and
inhibitors on growing cell cultures. Cells growing on single substrates
were monitored in a Micro-oxymax respirometer. Iron oxidation and
sulfur oxidation were measured in terms of cumulative oxygen
consumption. Since we did not have sulfur-grown T. ferrooxidans SM-4 available for these growth experiments, we used
sulfur-grown T. thiooxidans SM-6 instead for experiments on
sulfur. Important findings were later confirmed with sulfur-adapted T. ferrooxidans. Figure 2
shows the effects of increasing concentrations of phosphate on iron and
sulfur oxidation by growing cells. The control in each case contained a
5% inoculum along with ferrous sulfate or precipitated sulfur as the
substrate. Cumulative oxygen consumption was plotted as a function of
time for each of the reaction vessels. Iron oxidation (Fig. 2A) was
decreased by half in the presence of 50 mM phosphate. Sulfur oxidation
(Fig. 2B), on the other hand, increased to twice the control level in
the presence of 50 mM phosphate. Similar results were obtained with 50 mM chloride, which also inhibited iron oxidation and stimulated sulfur
oxidation, although slightly less extensively (data not shown).

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FIG. 2.
Effect of phosphate concentration on oxygen consumption.
(A) Growth of T. ferrooxidans on Fe2+; (B)
growth of T. thiooxidans on S0.
|
|
Cumulative carbon dioxide consumption was used to measure the cellular
growth rate. Figure
3 shows the effects
of phosphate
ions on growth using either ferrous iron or elemental
sulfur as
a substrate. A phosphate concentration of 50 mM caused a 50%
drop
in iron oxidation and was equally effective in inhibiting growth
on ferrous iron (Fig.
3A). Growth on elemental sulfur (Fig.
3B)
required more than twice as much phosphate for 50% inhibition.
At 50 mM, potassium phosphate stimulated growth on sulfur (Fig.
3B) as well
as sulfur oxidation (Fig.
2B). The stimulatory effect
of phosphate was
confirmed with
T. ferrooxidans adapted on sulfur;
75 mM
potassium phosphate increased growth on sulfur by 20% and
sulfur
oxidation by 30%.

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FIG. 3.
Effect of phosphate concentration on carbon dioxide
consumption. (A) Growth of T. ferrooxidans on
Fe2+; (B) growth of T. thiooxidans on
S0.
|
|
Table
2 provides a summary of the effects
of anions and inhibitors on cell growth (CO
2 consumption)
and iron and sulfur oxidation
(O
2 consumption). As
mentioned above, half as much phosphate was
required to inhibit 50% of
the oxidation and growth on iron compared
to sulfur. Chloride had a
similar effect, inhibiting oxidation
and growth on iron while
stimulating those on sulfur at lower
anion concentrations (data not
shown). Nitrate was unique among
the anions in its strong inhibitory
effect on both cell cultures.
Azide and cyanide both showed significant
differences with respect
to the two cell types. Iron growth was 2.5 times more sensitive
to azide and 3 to 4 times more sensitive to
cyanide inhibition
than sulfur growth.
Effect of anions on metal leaching.
Leaching of Fe and Zn from
pyrite and sphalerite by T. ferrooxidans was differentially
affected by phosphate concentrations, as shown in Fig.
4. Phosphate at or above 25 mM inhibited
the solubilization of Fe completely while allowing the zinc
solubilization to proceed with only some rate reduction. The effect at
75 and 100 mM was essentially the same as that at 50 mM. Although not shown in Fig. 4, KCl at 50 mM inhibited Fe solubilization by 84 and
35% after 2 and 14 days, respectively, and did not inhibit Zn
solubilization at all. KNO3 also inhibited the leaching of Fe more strongly than that of Zn, inhibiting Fe solubilization by 86%
and Zn solubilization by only 16% at 50 mM after 14 days. The effect
of NaN3 and NaCN at 0.1 to 5 µM was not apparent after 14 days because of their volatility at pH 2.3 as HN3 and HCN
escaping from the flasks through the cotton plugs. After 2 days,
however, 1 µM NaN3 and 5 µM NaCN inhibited Fe
solubilization by 65% without significantly affecting Zn
solubilization (14 and 25% inhibition for NaCN and NaN3,
respectively). These preliminary leaching experiments support the
concept of differential leaching of Fe and Zn by inhibiting iron
oxidation but not sulfur oxidation, thus favoring the solubilization of
Zn from ZnS over the solubilization of Fe from FeS2.
Detailed studies (L. Harahuc, H. M. Lizama, and I. Suzuki,
submitted for publication; I. Suzuki and L. Harahuc, June 1998, Canadian Patent Office) of selective solubilization of metals from
sulfide ores by this method support its potential application in
bacterial leaching.

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FIG. 4.
Effect of phosphate concentration on the extraction of
Fe and Zn from a mixture of pyrite and sphalerite.
|
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Bioleaching has become an increasingly important process due to the
growing need to use lower-grade ores, the relative ease
of
implementation, and the low start-up costs required compared
to those
of a conventional mining operation (
4). Under natural
conditions an ore body may show a tendency for selective solubilization
of certain metals. The mineral that is extensively oxidized is
(i) the
most hydrophobic, (ii) the lowest of an electrochemical
series, or
(iii) behaving as the anode of a galvanic cell (
14).
We have
demonstrated in this study that the bacterial activities
responsible
for metal leaching, the oxidation of ferrous iron
and that of sulfur,
can be selectively controlled by manipulation
of the media, leading to
differential leaching of Fe and Zn. This
control of bacterial
activities raises the potential of successful
bacterial leaching beyond
the three physical criteria listed
above.
 |
ACKNOWLEDGMENTS |
We thank the Natural Sciences and Engineering Research Council of
Canada for a grant to I.S. in support of the research and for the
Industrial Postgraduate Scholarship to L.H., and we thank Cominco
Research Limited for sponsoring the scholarship and for making their
research facilities available to her.
 |
FOOTNOTES |
*
Corresponding author. Mailing address: Department of
Microbiology, University of Manitoba, Winnipeg, Manitoba, Canada R3T 2N2. Phone: (204) 474-9690. Fax: (204) 474-7603. E-mail:
isuzuki{at}cc.umanitoba.ca.
 |
REFERENCES |
| 1.
|
Amaro, A. M.,
D. Chamorro,
M. Seeger,
R. Arredondo,
I. Peirano, and C. A. Jerez.
1991.
Effect of external pH perturbations on in vivo protein synthesis by the acidophilic bacterium Thiobacillus ferrooxidans.
J. Bacteriol.
173:910-915[Abstract/Free Full Text].
|
| 2.
|
Beck, J. V., and F. M. Shafia.
1964.
Effect of phosphate ion and 2,4-dinitrophenol on the activity of intact cells of Thiobacillus ferrooxidans.
J. Bacteriol.
88:850-857[Abstract/Free Full Text].
|
| 3.
|
Blake, R. C., II, and E. A. Shute.
1994.
Respiratory enzymes of Thiobacillus ferrooxidans. Kinetic properties of an acid-stable iron:rusticyanin oxidoreductase.
Biochemistry
33:9220-9228[CrossRef][Medline].
|
| 4.
|
Brierley, C. L.
1978.
Bacterial leaching.
Crit. Rev. Microbiol.
6:207-219.
|
| 5.
|
Corbett, C. M., and W. J. Ingledew.
1986.
Is Fe3+/2+ cycling an intermediate in sulfur oxidation by Fe2+-grown Thiobacillus ferrooxidans?
FEMS Microbiol. Lett.
41:1-6.
|
| 6.
|
Din, G. A., and I. Suzuki.
1967.
Mechanism of Fe2+-cytochrome c reductase of Ferrobacillus ferrooxidans.
Can. J. Biochem.
45:1547-1556[Medline].
|
| 7.
|
Espejo, R. T., and J. Romero.
1997.
Bacterial community in copper sulfide ores inoculated and leached with solution from a commercial-scale copper leaching plant.
Appl. Environ. Microbiol.
63:1344-1348[Abstract].
|
| 8.
|
Fry, I. V.,
N. Lazaroff, and L. Packer.
1986.
Sulfate-dependent iron oxidation by Thiobacillus ferrooxidans: characterization of a new EPR detectable electron transport component on the reducing side of rusticyanin.
Arch. Biochem. Biophys.
246:650-654[CrossRef][Medline].
|
| 9.
|
Fukumori, Y. F.,
T. Yano,
A. Sato, and T. Yamanaka.
1988.
Fe(II)-oxidizing enzyme purified from Thiobacillus ferrooxidans.
FEMS Microbiol. Lett.
50:169-172[CrossRef].
|
| 10.
|
Imaizumi, T.
1986.
Some industrial applications of inorganic microbial oxidation in Japan.
Biotechnol. Bioeng. Symp.
16:363-371.
|
| 11.
|
Ingledew, W. J.,
J. C. Cox, and P. J. Halling.
1977.
A proposed mechanism for energy conservation during F2+ oxidation by Thiobacillus ferrooxidans: chemiosmotic coupling to net H+ influx.
FEMS Microbiol. Lett.
2:193-197.
|
| 12.
|
Jensen, A. B., and C. Webb.
1995.
Treatment of H2S-containing gases: a review of microbiological alternatives.
Enzyme Microb. Technol.
17:2-10[CrossRef].
|
| 13.
|
Jerez, C. A.,
M. Seeger, and A. M. Amaro.
1992.
Phosphate starvation affects the synthesis of outer membrane proteins in Thiobacillus ferrooxidans.
FEMS Microbiol. Lett.
98:29-34[CrossRef].
|
| 14.
|
Kupla, C. F.,
N. Mjoli, and M. T. Roskey.
1986.
Comparison of iron and sulfur oxidation in Thiobacillus ferrooxidans: inhibition of iron oxidation by growth on sulfur, p. 289-295.
In
H. L. Ehrlich, and D. S. Holmes (ed.), Workshop on biotechnology for the mining, metal-refining and fossil fuel processing industries. John Wiley and Sons, New York, N.Y.
|
| 15.
|
Lawrence, J. R.,
Y. T. J. Kwong, and G. D. W. Swerhone.
1997.
Colonization and weathering of natural sulfide mineral assemblages by Thiobacillus ferrooxidans.
Can. J. Microbiol.
43:178-188.
|
| 16.
|
Lazaroff, N.
1963.
Sulfate requirement for iron oxidation by Thiobacillus ferrooxidans.
J. Bacteriol.
85:78-83[Abstract/Free Full Text].
|
| 17.
|
Lazaroff, N.
1977.
The specificity of the anionic requirements for iron oxidation by Thiobacillus ferrooxidans.
J. Gen. Microbiol.
101:85-91.
|
| 18.
|
Leduc, L. G., and G. D. Ferroni.
1994.
The chemolithotrophic bacterium Thiobacillus ferrooxidans.
FEMS Microbiol. Rev.
14:103-120[CrossRef].
|
| 19.
|
Le Roux, N. W., and K. B. Mehta.
1978.
Examination of a copper ore after leaching with bacteria, p. 463-476.
In
L. E. Murr, A. E. Torma, and J. A. Brierley (ed.), Metallurgical applications of bacterial leaching and related microbiological phenomena. Academic Press, New York, N.Y.
|
| 20.
|
Lizama, H. M., and I. Suzuki.
1988.
Bacterial leaching of a sulfide ore by Thiobacillus ferrooxidans and Thiobacillus thiooxidans. I. Shake flask studies.
Biotechnol. Bioeng.
32:110-116[CrossRef].
|
| 21.
|
Magnin, J.,
F. Baillet,
A. Boyer,
R. Zlatev,
M. Luca,
A. Cheruy, and P. Ozil.
1998.
Augmentation, par régénération électrochimique du substrat, de la production d'une biomasse (Thiobacillus ferrooxidans DSM 583) pour un procédé biologique de récupération de métaux.
Can. J. Chem. Eng.
76:978-984.
|
| 22.
|
Murayama, T.,
Y. Konno,
T. Sakata, and T. Imaizumi.
1987.
Application of immobilized Thiobacillus ferrooxidans for large-scale treatment of acid mine drainage.
Methods Enzymol.
136:530-540.
|
| 23.
|
Ohmura, N.,
K. Tsugita,
J. Koizumi, and H. Saiki.
1996.
Sulfur-binding protein of flagella of Thiobacillus ferrooxidans.
J. Bacteriol.
178:5776-5780[Abstract/Free Full Text].
|
| 24.
|
Pronk, J. T.,
K. Liem,
P. Bos, and J. G. Kuenen.
1991.
Energy transduction by anaerobic ferric iron respiration in Thiobacillus ferrooxidans.
Appl. Environ. Microbiol.
57:2063-2068[Abstract/Free Full Text].
|
| 25.
|
Rawlings, D. E., and S. Silver.
1995.
Mining with microbes.
Bio/Technology
13:773-778.
|
| 26.
|
Razzell, W. E., and P. C. Trussell.
1963.
Isolation and properties of an iron-oxidizing Thiobacillus.
J. Bacteriol.
85:595-603[Abstract/Free Full Text].
|
| 27.
|
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].
|
| 28.
|
Sand, W.
1989.
Ferric iron reduction by Thiobacillus ferrooxidans at extremely low pH values.
Biogeochemistry
7:195-201[CrossRef].
|
| 29.
|
Satoh, H.,
J. Yoshizawa, and S. Kametani.
1988.
Bacteria help desulfurize gas.
Hydrocarbon Processing
67:76-78.
|
| 30.
|
Seeger, M., and C. A. Jerez.
1992.
Phosphate limitation affects global gene expression in Thiobacillus ferrooxidans.
Geomicrobiol. J.
10:227-237.
|
| 31.
|
Seeger, M., and C. A. Jerez.
1993.
Phosphate-starvation induced changes in Thiobacillus ferrooxidans.
FEMS Microbiol. Lett.
108:35-42[CrossRef][Medline].
|
| 32.
|
Seeger, M., and C. A. Jerez.
1993.
Response of Thiobacillus ferrooxidans to phosphate limitation.
FEMS Microbiol. Rev.
11:37-42.
|
| 33.
|
Starkey, R. L.
1925.
Concerning the physiology of Thiobacillus thiooxidans, an autotrophic bacterium oxidizing sulfur under acid conditions.
J. Bacteriol.
10:135-163[Free Full Text].
|
| 34.
|
Sugio, T.,
T. Katagiri,
K. Inagaki, and T. Tano.
1989.
Actual substrate for elemental sulfur oxidation by sulfur:ferric ion oxidoreductase purified from Thiobacillus ferrooxidans.
Biochim. Biophys. Acta
973:250-256.
|
| 35.
|
Sugio, T.,
T. Katagiri,
M. Moriyama,
Y. L. Zhen,
K. Inagaki, and T. Tano.
1988.
Existence of a new type of sulfite oxidase which utilizes ferric ions as an electron acceptor in Thiobacillus ferrooxidans.
Appl. Environ. Microbiol.
54:153-157[Abstract/Free Full Text].
|
| 36.
|
Suzuki, I.,
D. Lee,
B. Mackay,
L. Harahuc, and J. K. Oh.
1999.
The effect of various ions, pH, and osmotic pressure on the oxidation of elemental sulfur by Thiobacillus thiooxidans.
Appl. Environ. Microbiol.
65:5163-5168[Abstract/Free Full Text].
|
| 37.
|
Suzuki, I.,
T. L. Takeuchi,
T. D. Yuthasatrakosol, and J. K. Oh.
1990.
Ferrous iron and sulfur oxidation and ferric iron reduction activities of Thiobacillus ferrooxidans are affected by growth on ferrous iron, sulfur, or a sulfide ore.
Appl. Environ. Microbiol.
56:1620-1626[Abstract/Free Full Text].
|
| 38.
|
Torma, A. E.
1977.
The role of Thiobacillus ferrooxidans in hydrometallurgical processes.
Adv. Biochem. Eng.
6:1-37.
|
| 39.
|
Tuovinen, O. H., and D. P. Kelly.
1972.
Biology of Thiobacillus ferrooxidans in relation to the microbiological leaching of sulfide ores.
Z. Allg. Mikrobiol.
12:311-346[Medline].
|
| 40.
|
Tuttle, J. H., and P. R. Dugan.
1976.
Inhibition of growth, and sulfur oxidation in Thiobacillus ferrooxidans by simple organic compounds.
Can. J. Microbiol.
22:719-730[Medline].
|
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