Thursday, October 15, 2015

Bioleaching/Biocorrosion
 Metals/Biomining


Presented to: Dr. Michael Broaders

1.     Biocorrosion
By Lisa Smith

Physicochemical interactions between a metallic material and its environment can lead to corrosion.
Corrosion is a “naturally occurring process by which materials fabricated of pure metals and/or other mixtures undergo chemical oxidation from ground state to an ionized species” (Beech, 2003). The process proceeds through a series of oxidation (anodic) and reduction (cathodic) reactions of chemical species in direct contact with, or in close proximity to, the metallic surface.
In natural habitats and man-made systems, surface-associated microbial growth, i.e. biofilms, influence the physico-chemical interactions between metals and the environment, frequently leading to deterioration of the metal. For example in a marine environment the presence of a biofilm can accelerate corrosion rates of carbon steel by several orders of magnitude. However, in contrast, certain types of biofilms produce a protective barrier effect resulting in a significant decrease in corrosion rates of metals.

Deterioration of metal under a biological influence is termed biocorrosion or microbiologically influenced corrosion (MIC).
“Biocorrosion is a result of interactions between metal surfaces and bacterial cells and their metabolites” (Beech, Sunner, 2004).
The main types of bacteria associated with metals in terrestrial (and aquatic) environments are sulfate-reducing bacteria (SRB), sulfur-oxidising bacteria, iron-oxidising/reducing bacteria, manganese –oxidising bacteria and bacteria secreting organic acids and slime. These organisms coexist in naturally occurring biofilms.
SRB are the main group of microorganisms and are generally anaerobic, however some genra tolerate oxygen and even grow in its presence. They are distributed within two domains: Archaea and Bacteria.
There is increasing recognition that microbes such as bacteria play an even larger role in all forms of corrosion than previously thought.  It is now reported that up to 70% of all corrosion in water systems is caused or accelerated by microbes.

2. Biooxidation
By Deborah Mc Auliffe

Many biotechnology-derived processes use microorganisms to help ease the usage of harmful chemicals in various industrial processes. The mining industry uses microorganisms and their natural ability to digest, absorb, and change the quality of different chemicals and metals, to refine ores.


Biooxidation also uses microorganisms, not to extract metals, but to make the metals ready for extraction. Oxidation is the chemical reaction in which an element is changed by the addition of oxygen. Rust is an example of the oxidization of iron.

Biooxidation is mainly used in gold mining. Gold is often found in ores with gold particles scattered throughout, called refractory ores, and the small particles of gold are covered by insoluble minerals. These minerals make the extraction difficult. Therefore, microorganisms that can "eat away" at the mineral coating are used to pre-treat the gold ores before they can be extracted.

Bioleaching of copper, and biooxidation of refractory gold ores are the only well-established large scale processes that are commercially carried out today.

Currently, 25 percent of all copper worldwide is produced through biomining. The process is used on a variety of other metals such as gold and uranium. Biomining is not yet a proven or profitable technology to apply to other metals such as zinc, nickel and cobalt.



3. Bioleaching
By Marian Cummins

3.1 History of Bioleaching


Although mining is one of the oldest technologies known it has succeeded in escaping the
major technological advances seen in that of agriculture and medicine. Many minerals and metals are mined today in exactly the same manner, as they were hundreds of years previous. The crude ores are dug from the earth, crushed and the mineral is extracted by either by extreme heat or due to the addition of toxic chemicals. But due to the environmentally unfriendly aspect of these mining techniques new methods, which are kinder and more environmentally friendly, are being used which uses microorganisms, which leach out the metals- that of Bioleaching

One of the earliest recordings of bioleaching comes from Cyprus, reported by Galen, a naturalist and physician AD166 who reported on the in situ leaching of copper. Surface water was allowed to flow through permeable rock and as it percolated through the rock, the copper minerals dissolved so the result was a high concentration of copper sulphate in solution. This solution was allowed to evaporate with the resultant crystallation of copper sulphate. Pliny (23-79 AD) reported the similar practice of copper extraction as copper sulphate was widely used in Spain.
          Prior to electrolysis, the recovery of the copper from copper sulphate was by cementation (precipitation). It is thought that this process was known in Pliny time but no written records of this have survived. Its is known that the Romans used to place scrap iron into the river and over a period of a few months the copper precipated around the iron. The pure copper was then recovered by smelting, but what the Romans didn’t realize was microorganisms played a major biological contribution to this process by generating the copper in the water. The Chinese were also aware of the process (cementation) as documented by King Lui- An (177-122 BC). The Chinese implemented the commercial production of copper from copper sulphate when the Chiangshan cementation plant started operation in 1096 with an annual production of 190ton Cu/annum. Bioleaching and cementation were also described by Paracelsus the Great (1493-1541). He noted the copper deposition onto iron at a spring in the Zifferbrunnen in Hungary. Although he confused this deposition with that of transmutation, he assisted in the use of bioleaching and by 1750 approx 200t/annum Cu were obtained in the Zifferbrunnen area of Hungary using this process of bioleaching.
           Even though these earlier bioleaching operations were difficult to document, it is known that copper leaching was well established at the Rio Tinto mine in Spain by the 18th century. Rio Tinto literally means “coloured fiver”, a name given to the acidified fiver that issues from the Sierra San Cristobol mountains on the fiver bed and on the abundant microbial mats, the dense floating masses made up of different microorganisms (reference 1). At Rio Tinto the process of heap leaching of copper sulphides was carried out on an industrial scale in 1752. In this process the ore is heaped and crushed onto open-air pads. The layers of ore were altered with beds of wood. Once the heap was constructed the wood was ignited which resulted in the roasting of copper and iron sulphides. Water was then added to the top of the heap. The addition of water caused the copper and iron to dissolve which formed copper and iron sulphates. But due to the significant environmental damage caused by the production of sulphuric acid in this process, the process was stopped in 1888. This heap leaching process minus the roasting step continued at Rio Tinto until the 1970’s.The reason for it’s success was unknown, but it was thought to be due to “some obscure quality either of the Rio Tinto ore or the Spanish climate’. But it is now widely accepted and known that it was in fact the microorganism Thiobacillus ferroxidans that contributed to the success of Rio Tinto.
          
In the 1940’s in America, several million tons of sulphuric acid was discovered in the Ohio River, this discharge was attributed to the weathering of subbitumous coal. Naturally enough this pollution incident was unacceptable and it led to widespread investigation by universities and several US government institutions, such as the US Bureau of Mines as to the source of the pollution. The cause of the sulphuric acid was due to the oxidation of pyrite, which is present in the subbitumuous coal, but it was also noted that this oxidation occurred much more rapidly than could be contributed to by that of inorganic chemistry. Also an important observation was that of the presence of sulphur oxidizing bacteria. And in 1950 a couple of years after the incident a new species was identified that of Thiobacillus ferrooxidans. This organism is able to oxidize elemental sulphur and ferrous ions at a much higher rate than that achieved by inorganic chemistry. It is this catalysis of the oxidation of ferrous ions that makes Thiobacillus ferrooxidans and other iron and sulphur oxidizing microorganisms such important catalysts in the bioleaching process.

3.2 Why has Bioleaching become such an attractive alternative?


Bioleaching is a very attractive alternative to to the conventional mining techniques and it is very desirable in today’s world due to the continued depletion of high grade reserves and so it allows the more economically extraction of minerals by from low grade ores, it also arise from the resulting tendency for mining to be extended deeper underground and also it is a much more environmental friendly alternative to that of the conventional mining methods to which there is a growing awareness of the environmental issues associated with the smelting of sulphide minerals and the burning of sulphur rich fossil fuels and of course there is the enormous energy costs that is associated with the conventional methods. Bimining also improves recovery rates, reduces capital and operating costs.

There has being a very widespread and rapid interest in the exploitation of biomining especially in the copper industry, due to the fact that the copper in the low grade ore is bound up in a sulfide matrix, it can be recovered by traditional smelting only at great cost. In addition the world is running out of smelting capacity because of the depletion of the high-grade ores means that more ore has to be smelted to produce the same amount of copper. Oxidising bacteria can reduce the need for these expensive smelters. Whereas a new smelter can cost 1 billion dollars the technology required for biomining I pretty uncomplicated.

In order to understand the process of microbial mining or biomiining a number of considerations must be understood and answered, such as what microorganisms are involved in the extraction of the metals from the rocks and where in nature do they occur? What biochemical functions do these microorganisms perform and what do they require in the need of nutrient and environmental conditions in order to maintain their activity? What are the constraints of the commercial exploitation of such biological techniques? And what impact will the new tools of genetic engineering have on the future of biomining?

3.3 General Properties of the Microorganisms


The bacteria involved in biomining are among the most remarkable life forms known. They are described as chemolithotrophic, which basically means rock eating, that is they obtain their energy from the oxidation of inorganic substances. Many of them are also autotrophic that is they utilize carbon dioxide in the atmosphere as the carbon source. These microorganisms live in very inhospitable environments, which other microbes would find it impossible to survive or tolerate; for example the sulphuric acid and soluble metals concentrations are often very high. Some thermophilic microorganisms require temperatures above 50 degree Celsius (122 degree Fahrenheit), and a few strains have been found at temperatures close to that of the boiling point of water.

4.4 Specific Microorganisms

For many years the general impression was that Thiobacillus ferrooxidans was the only microorganism responsible for the leaching proceeds. As previously stated this microorganism wasn’t discovered until 1957 in the acidic water draining coal mines, where it was then determined the relationship between the existence of this microorganism and the dissolution of metals in copper- leaching operations. Since its discovery in the Rio Tinto Mine in Spain a wealth of information has be collected regarding its characteristics and also more importantly on the role it plays in bioleaching of the metals.

T. ferrooxidans is rod shaped (usually single or in pairs), non- spore forming, gram negative, and single pole flagellated ( HORAN, 1999;KELLY and HARRISON, 1984; LEDUC and FERRONI, 1994; MURR, 1980). T. ferrooxidans is also acidophilic; it tends to be found in hot springs, volcanic fissures and in sulfide ores deposits that have high sulphuric acid concentrations. It is also moderately thermophilic, thriving in temperatures between 20 and 35 degree C. It obtains its energy for growth from the oxidation of either iron or sulphur. The iron must be in the ferrous or bivalent form (Fe2+), and it is converted by the action of T. ferrooxidans to the ferric or trivalent form (Fe3+). The nitrogen source utilized is that of ammonium. T. ferrooxidans obtains carbon autotrophically from the atmosphere as carbon dioxide. Although T. ferrooxidans has been characterized as being a strictly aerobic organism, it can also grow on elemental sulphur or metal sulphides under anoxic conditions using ferric iron as an electron acceptor. (Donti et al., 1997; Pronk et al., 1992). It is generally found in environment with a Ph OF 2.0.

As important and all T. ferrooxidans is in the leaching process another important microorganism taking part ii that of T. thioxidans, this is also a rod shaped bacteria, very similar to T. ferrooxidans but it can’t oxidized Fe3+ it is also gram negative Its maximum growth rate is at 35 degrees C, and it is the dominant microbe found at low Ph environments. It has being found that mixed cultures of bacteria are responsible for the extraction of metals from their ores such as is the case with the combined effects of T ferrooxidans and T. thiooxidans are more effective in leaching certain ores together than as an individual organism. Also Leptospirillium ferrooxidans and T. organaparus can degrade pyrite (FeS2) and chalopyrite (CuFeS2), a feat, which neither species can do alone.

4.5 Bioleaching Processes


The process of bioleaching falls under 2 methods that of direct leaching and indirect leaching. Direct leaching is the process where the bacteria attack the minerals which are susceptible to leaching by enzymes. By obtaining the energy from the inorganic material the bacteria aid in the transferring of electrons from iron or sulphur to oxygen.  The more oxidized product is generally the more soluble the product. The inorganic material never enter the bacterial cell, the electrons released by the oxidation reaction are transported through the cell membrane (and in aerobic organisms) to oxygen atoms forming water. ATP (adenosine triphosphate) is produced when the transferred electrons give up their energy.
   Indirect leaching, in cons tract does not occur by the bacteria attacking the minerals. The bacteria produce ferric iron (Fe3+) by oxidizing soluble ferrous iron (Fe2+) which is a powerful oxidizing agent that reacts with the other metals, and transforms them into a soluble oxidisable form in a sulphuric acid solution. In this way the ferrous iron is produced again and is rapidly oxidized by the bacteria thus it is a continuous cycle. This indirect leaching is generally known as bacterial assisted leaching. T. ferrooxidans can speed up the oxidation of iron by a factor of more than a million than without the bacteria being present in the solution.



3.6 The Process


In the case of the extraction of copper from its ore the aforementioned bacteria T.ferrooxidans and T. thiooxidans are involved in this process, which is a 2-stage process that of direct and indirect as previously discussed.
In stage 1, the bacteria break down the mineral arsenopyrite (FeAsS) by oxidizing the sulphur ant the metal (arsenic ions) to a higher oxidation state whilst reducing dioxygen by H2 and Fe3+ This allows the soluble products to dissolve as such

              FeAsS(s) -> Fe2+(aq) + As3+(aq) + S6+(aq)
This process of  direct leaching as described previously occurs at the cell membrane of the bacteria. The electrons pass into the cells and are used in biochemical processes to produce energy for the bacteria to reduce oxygen molecules to water.
In stage 2, that of indirect leaching the  bacteria  oxidise Fe2+ to Fe3+ (whilst reducing O2).
Fe2+ -> Fe3+
They then oxidise the metal to a higher positive oxidation state. With the electrons gained from that, they reduce Fe3+ to Fe2+ to continue the cycle. This stage involves both ditect and indirect leaching.
M3+ -> M5+
The gold is now separated from the ore and in solution.
The process for copper is very similar. The mineral chalcopyrite (CuFeS2) follows the two stages of being dissolved and then further oxidised, with Cu2+ ions being left.
In the process of extracting copper (Cu2+) from a mixture, the copper ions are removed by solvent extraction, which leaves the other ions in solution. The copper is removed by bonding to a ligand, which is essentially a large molecule consisting of a number of smaller groups each processing a lone pair. The ligand is then dissolved in kerosene (organic solvent) and shaken with the resultant reaction:

  Cu2+(aq) + 2LH(organic) -> CuL2(organic) + 2H+(aq)

Electrons are donated to the copper, producing a complex, copper bonded to 2 molecules of the ligand. As this complex has no charge as as it is no longer attracted to the polar water molecules it dissolves in the kerosene and is then seperated from solution.This initail reaction is reversible as so is pH dependent. The copper ions go back into an aqueoeus solution by adding concentrated acid.

To increase the purity of the copper an electric current is added to the copper ions as it passes through an electro-winning process. The copper ions which have a 2+ charge are  attracted to the negative electrode and thus collected.
The copper can also be concentarted and recovered by using scrap iron which replaces the copper in the reaction as thus:

             Cu2+(aq) + Fe(s) -> Cu(s) + Fe2+(aq)

As described biomining has being extremely successful in the case of copper.But gold can also be obtained in a similar manner. Up until recently the gold mining industry depended on high grade ores near the surface og the earth.But by the 1980 and the depletion  of  these ores forced miners to rely on the lower grade ores which were located deeper in the mines. These low grade ores were more difficult to process in comparsion to the high grade ores at the surface as they were naturally oxidized by bacteria, sunlight and water. But the low grade ores are generally encased in sulphide minerals a and so processing of these ores requires roasting or pressure oxidation and then treatment with cyanide.Biomining means that the costly procedures of roasting and pressure oxidation can be surpasssed by usinf T. ferrooxidans for the pretreatment of the gold ores. The first mine to take advantage of this was Fairview mine in South Africa (owned by Gencor (Pty) Ltd. )where most of the ore was the refractory sulphide type. By using biomining at Fairview the recovery rate of the gold increased from 70 % to 95%.And due to this success rate Gencor opened 4 more biomining sites, Harbour Lights, Tonkin Springs, Wiluna and Younmi in Australia, San Bento in South America and the huge Ashanti plant in Ghana which  started in 1994 and by 1998 it was producing 800t/ day of gold concentrate.


Although gold and copper are probably the most important and valuable metals and undoubtedly this is what has pushed the huge interest there now is in biomining. But biomining has also played a big part in the phosphates industry. Phosphates are definitely not as valuable as the metals but their extraction is definitely plays a part in big time mining. Phosphates for fertilisers is the world’s second largest agricultural chemical (after nitrogen); about 5 .5 million tons are produced every year in the US alone. Another 1.1 million tons of higher quality phosphates are used as an additive in soft drinks and in the manufacture of detergents, rubber, and industrial chemicals.
        The traditional method of extracting phosphates from ores was by burning at high temperatures with the resultant of solid phosphorus, or else by treatment with sulphuric acid with phosphoric acid and huge amounts of useless low-grade gypsum being the result. But with the process of biomining a much milder technique was available. This new technique used two bacteria that of Pseudomonas cepacia E-37 and Erwinia herbicola, these bacteria were chosen from hundreds of bacteria as they have the unusual ability: a direct oxidative pathway of converting glucose into gluconic and 2 ketogluconic acids, which means that sulfuric acid doesn’t have to be used in the process and also this milder technique it performed at room temperature and so it is a much more environmentally friendly process.

3.7 Methods to increase biomining efficiencies and the impacts of Genetic Engineering on Biomining


As biomining is now at an all time high it the next challenge is to increase its efficiency. At the present time it is only indigenous microorganisms that naturally occur in dumps or mine run off that are used in the bioleaching process. So now the focus is on finding microbial strains that are better suited to large scale industrial processing.  One draw back is that the bioleaching process releases large amounts of heat and 
Can raise the temperature so much that the bacteria that are being in use are killed or slowed down. To combat this work has being and is still currently being done on using Archaebacteria for use in biomining. These primitive thermophiles, or heat loving bacteria are so far poorly studied and they are found in deep-sea vents and in hot springs such as in Yellowstone National Park, Iceland and in New Zealand. They thrive in temperatures of up to 100 C or higher. They are currently being put to test at the Younami mine in Western Australia.

Another challenge is to find or engineer strains that can stand up to the presence of heavy metals such as mercury, arsenic, cadmium, these metals poison the microbes currently being used in biomining and thus slow down biomining. Some steps have being taken toward finding resistant strains to these poisons by showing that some microbes have enzymes that can work in 2 ways that of protecting their basic activities from heavy metals or by pumping the metals out of the bacteria. Also some work but not a lot has being done on identifying genes that help the microbes deal with the heavy metals and these genes may be used to genetically engineer resistant strains. The genetically engineering of bacteria to resist heavy metal poisoning is not an easy achievement.

As much less is known about the Thiobacillus species and the other microbes used in biomining than is known for E. coli, which is of course a lab favourite? But hopefully this genetically engineering of these microorganisms will take place at a much quicker pace than the two millennia is took the Roman miners at Rio Tinto to become a major improvement in biomining, but it is fairly safe to say that these developments will take place sooner rather than later as biomining has become a worldwide accepted process


3.8 Metal extraction operations


Insitu leaching is a promising alternative for the recovery of metals from low-grade ores, which are in inaccessible places. Also this has the advantages as this technology has minimal impact on the environment and it is currently used to extract residual minerals from abandoned mines. The way this is performed is the leaching solution is applied directly to the walls and the roof of the intact stope (an underground excavation from which the ore has being removed) or else to the rubble of the fractured workings. Insitu leaching has been successful to the recovery of copper and uranium,

Dump leaching is also a method employed for the extraction of metals but as in the case for copper it is not a very fast or efficient process. The dumps often contain boulders and large rocks which have a very low surface- to – volume ratio for the action of bacteria. Also the interior of a large dump is low in oxygen, which is a requirement for the oxidation of iron and sulphur compounds, and the temperature can also rise to over 50 degree C. because the oxidation process are exothermic. Also there is a significant channeling of the acidified water as it percolates through the rocks, so the copper solubiislation is restricted to only a minor portion of the dump. Despite these disadvantages dump leaching is a low cost and a low-tech method or recovery.

Heap leaching is the most popular metal extraction method used, in particular used for copper. In this method the ore is heaped onto open air leach pads with a base of asphalt or impervious plastic sheeting. The heaps are no more than a few meters high by a few meters wide so as to allow the oxygen to diffuse to all parts of the heap and reduce the build- up of heat from the leaching process. The heaps are sprayed with sulphuric acid (for copper extraction) and with cyanide (for gold extraction) which contain a fraction of the bacterial population, the rest being attached to the mineral, in a controlled manner and the run off is collected on the plastic shheting.When the desired metal concentration is obtained, the rich liquor is pumped to the solvent extraction section and then sent to the electro winning, where the fine metal is recovered or where the purity can also be increased as described earlier in the bioleaching process. The finely ground copper concentrate provides a large surface to volume ratio and so promote bioleaching. Nutrients such as phosphates can be added to promote growth if necessary. Heap leaching is a more environmentally friendly option and is also more economic and it is especially attractive for mines in remote areas or for small operations where only a small body of ore is to be extracted. Although heap operation is simple and adequate to handle large volumes of minerals, but their productivity and yields are limited due to the severe difficult in maintaining an adequate process control.
       Heap and dump leaching present a number of advantages such as simple operation, low investment and operation costs and acceptable yields. On the other hand the processes suffer from some serious limitations such as the piled material is very heterogeneous and practically no close process control can be exerted, except for intermittent pH adjustment and the addition of some nutrients. The rates of oxygen and carbon dioxide transfer that can be obtained are low, and extended periods of operation are required in order to achieve sufficient conversions (Acevedo and Gentina, 1989).

Heap leaching can also be used for the recovery of gold. Most of the world’s gold reserves contain the metal bound up in the small particles in the rocks. After grinding up the rocks the gold is then recovered by gravity separation or by treatment with cyanide. But more often theses techniques are proving to be ineffective in the recovery of the gold. For example if the gold is found associated with pyrite, usually arsenopyrite, it can’t be recovered by gravity, while the cyanide reacts with the pyrite before it can complex with the gold, making the process too expensive and environmentally hazardous due to the large releases of cyanide. The gold in this case can be recovered by oxidizing the pyrite at high pressure in an autoclave or by roasting, followed by recovery with cyanide. Both techniques are very expensive and also pose a serious environmental risk as the liberated gases contain arsenic.
             Sometimes the gold can also be found as fine particles in carbonaceous sulphide ores. By grinding the gold is liberating but it has a tendency to stick to the carbonaceous compounds making it difficult to recover by conventional techniques.
              It was discovered that microorganisms could oxidize the gold bearing pyrite and arsenopyrite ores and also the carbonaceous ones. Also this process of using microorganism’s means that the cyanide quantities needed is sufficiently reduced. Commercial bacterial oxidation of refractory gold ores (those that were difficult to recover by conventional methods) was first used at Gencor’s Fairview plant in South Africa in 1986 (as previously mentioned). At that time the process used at Fairview was that of oxidizing the gold by roasting, but wanted to expand its capacity by using the bioleaching process and if improved successful to replace the traditional method with that of bioleaching. By 1997 it was producing 40t/day of gold and the roasters had been removed.
             The technology used at Fairview is very different to that have the dump and heap bioleaching processes used for copper. The finely ground gold arsenopyrite concentrate is suspended and stirred in large tanks or bioreactors. Missing bacterial nutrients are added and the pH is adjusted to 2. Oxygen is supplied and after about 5 days about 1/5 of the arsenopyrite has been oxidized by the microorganisms and thus recovering up to 90% of the gold. As previously stated the Fairview mine in South Africa was the first mine to take advantage of the bioleaching process with recovery rates increasing from 70% to 95% and due to this success rate other mines followed suit.
        Bioreactors also have their own drawbacks associated with their operation. The choice of material for their construction is important and also the costs involved at maintaining them at their correct temperature. The temperature inside the reactors can rise rapidly to 50 degree C or higher, whereas the microorganisms predominantly prefer temperatures of 20-40 degree C, so the reactors have d to be cooled to keep the microorganisms alive. Although some plants are currently using extremely thermophilic microorganisms which can grow at higher temperatures as is the case with the Youanmi plant in Australia. This plant operates at 50 degree C. In all cases the bioreactors operate at a pH of about 2 as previously stated and so associated with this is the problem of acid corrosion.Severeal plants initially built rubber- lined metal bioreactors where this wasn’t a problem but the more favored choice is that of stainless steel.

3.9 Examples of current Industrial Bioleaching Operations


■ Acid Mine Drainage
             ■ Rio Tinto, Spain
■ Dump Leaching
             ■ Bagdad, USA
           ■ Pinto Valley, USA
             ■ Sierrita, USA
             ■ Morenci, USA
■Heap Leaching
              ■ Cerro Colorado, Chile
              ■    Cananea, Mexico
              ■     Chuquicamata SBL, Chile
              ■   Collahuasi, Chile
              ■     Giilambone, Australia
              ■    Ivan Zar Chile
              ■ Morenci, USA
              ■ Punta del Cobre, Chile
                 
■ Bioleaching of Gold Concentrates
             ■Ashanti, Ghana
             ■ Fairview, Zambia
             ■ Harbour Lights, Australia
             ■ Mount Leyshon, Australia
             ■    Sao Bento, Brazil
             ■ Wiluna, Australia
             ■ Youanmi, Australia

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