Bacterial leaching of manganese ores

Leaching of various types of ores, containing 12–30% manganese, by the thiobacterium Acidithiobacillus ferrooxidans was studied. Leaching of reduced ores (manganocalcite and manganiferous limestone) was mediated mainly by degradation of manganiferous minerals (by sulfuric acid produced in the course of bacterial oxidation of pyrite or sulfur). Bacterial treatment of the ores for 144 and 192 h allowed solubilization of 96–98% of manganese. Inoculation of bacteria into pulp with pyrite increased the rate of leaching of oxide ore (psilomelane) by 37%, and the degree of its extraction within 180 h increased from 80 to 97%.     

功能菌群耦合黄铁矿浸出软锰矿的研究

【目的】将3种不同来源的环境样品混合后接种至含1%黄铁矿和1%软锰矿的培养基中进行富集培养,初步得到有一定浸矿功能的混合微生物菌群。【方法】菌群继续用于黄铁矿和低品位软锰矿共同浸出,设置未接种的体系作为对照。【结果】对浸出过程中菌群结构的变化、pH、锰浸出率和浸出残渣的成分进行分析,结果发现接种过微生物菌群的浸出体系在反应15 d后,锰浸出率达到92.48%,远高于未接菌对照组的40.34%;菌群中Thiomonas sp.所占比例从最初的2%上升到浸出结束时的93%。实验组的pH从最初的4.0下降到2.5;X射线衍射(XRD)分析发现,通过生物作用浸出的残渣中含有黄钾铁矾,说明生物代谢产生了大量的硫酸。【结论】证明微生物在两矿浸出过程中通过促进黄铁矿解离,维持体系低pH等作用加速反应的进行。结果为进一步研究微生物浸矿的作用机制和开发低品位锰矿的生物浸出工艺打下了基础。     

Physiology and kinetics of manganese‐reducing bacillus polymyxa strain D1 isolated from manganiferous silver ore

Manganese‐reducing bacteria were isolated from a manganiferous silver ore mining site using enrichment procedures. The most rapid Mn(IV) reducer was identified as Bacillus polymyxa and was designated as strain D1. Isolate D1 has no growth‐factor requirements and is mesophilic and neutrophilic. D1 respires glucose aerobically, under which conditions cyanide is bactericidal. Nonfermentable substrates such as lactate, acetate, citrate, and succinate cannot serve as sole carbon sources. D1 ferments glucose anaerobically, producing acetic acid, ethanol, and butanediol as major metabolic end products. Both anaerobic conditions and direct physical contact with pyrolusite (MnO₂) particles were necessary for manganese reduction. Strain D1 is unique in that manganese serves as an ancillary electron acceptor during anaerobic fermentation. Kinetic experiments showed that D1 reduced manganese three to five times as rapidly as the widely studied Mn(IV)/Fe(III)‐reducing microorganisms Shewanella putrefaciens MR‐1 and Shewanella putrefa‐ciens sp. 200. Strain D1 is capable of liberating silver via the reductive dissolution of refractory manganiferous ores.     

Importance of Extracellular Polymeric Substances from Thiobacillus ferrooxidans for Bioleaching

Leaching bacteria such as Thiobacillus ferrooxidans attach to pyrite or sulfur by means of extracellular polymeric substances (EPS) (lipopolysaccharides). The primary attachment to pyrite at pH 2 is mediated by exopolymer-complexed iron(III) ions in an electrochemical interaction with the negatively charged pyrite surface. EPS from sulfur cells possess increased hydrophobic properties and do not attach to pyrite, indicating adaptability to the substrate or substratum.     

Manganese-induced apoptosis in rat myocytes

Manganese can be toxic to the heart, causing dysfunction following long exposure. In our experiments, we examined the cytotoxicity of manganese in neonatal rat ventricular myocytes (NRVM) by MTT assays in vitro. Results showed that after incubation in the different concentrations of manganese for 24 h, apparent cytotoxicity was observed. At 500, 1000, and 1500 2 microM of manganese, the percentage of cell viability dropped to 82% +/- 6.13, 78% +/- 5.28, and 66% +/- 4.22, respectively. When cells were treated for 48 h, all concentrations tested exerted toxic effect; especially from 500 to 1500 microM the cell viability dropped from 67% +/- 4.84 to 37% +/- 3.25. Apoptosis in NRVM was then examined by flow cytometry. Results showed that the percentage of apoptotic cells treated with 500 microM of manganese for 24 h increased from 4% +/- 0.84 to 7% +/- 1.16. After 48 h of incubation, this percentage increased to 11% +/- 0.91. There was no significant difference between control groups (0 microM manganese) after 24 and 48 h incubation. The morphological changes of NRVM nuclei were visualized with the fluorescent DNA-binding dye Hoechst33342 after incubation in 500 microM of manganese for 48 h. Compared with normal nuclei, apoptotic nuclei showed the typical features of fragmentation and condensation. To investigate whether there are any apoptotic gene expression changes during apoptosis, we examined the expression level of Bcl-2, Bax, and P53 mRNAs after treatment with 500 microM of manganese for 48 h. The Bcl-2 mRNA expression decreased while the expression of Bax as well as P53 mRNAs increased. These results suggested that manganese cytotoxicity on NRVM could induce apoptosis in NRVM cells. The apoptosis process might involve, and be promoted by, the changes of the expression levels of P53, Bcl-2, and Bax proteins.     

Effect of anions on selective solubilization of zinc and copper in bacterial leaching of sulfide ores

Bacterial leaching of sulfide ores using Thiobacillus ferrooxidans, Thiobacillus thiooxidans, or a combination of the two was studied at various concentrations of specific anions. Selective zinc and copper solubilization was obtained by inhibiting iron oxidation without affecting sulfur/sulfide oxidation. Phosphate reduced iron solubilization from a pyrite (FeS(2))-sphalerite (ZnS) mixture without significantly affecting zinc solubilization. Copper leaching from a chalcopyrite (CuFeS(2))-sphalerite mixture was stimulated by phosphate, whereas chloride accelerated zinc extraction. In a complex sulfide ore containing pyrite, chalcopyrite, and sphalerite, both phosphate and chloride reduced iron solubilization and increased copper extraction, whereas only chloride stimulated zinc extraction. Maximum leaching obtained was 100% zinc and 50% copper. Time-course studies of copper and zinc solubilization suggest the possibility of selective metal recovery following treatment with specific anions.     

锰氧化细菌的分离鉴定及其锰氧化特性的分析

利用选择性培养基对锰矿样品进行分离、筛选, 得到一株高效锰氧化细菌(MN1405)。经形态特征、生理生化特征以及16S rRNA 基因序列分析, 将菌株MN1405 鉴定为Arthrobacter echigonensis。在培养条件下, MN1405 对培养基中的锰离子去除率可达93.38%, 且其培养所获得的培养液也具有良好的除锰效果。     

Rate controls on the oxidation of heaps of pyritic material imposed by upper temperature limits on the bacterially catalysed process

Abstract: Oxidation of a fraction of the pyrite in gold-bearing pyrite ores before leaching often increases gold recovery rates. There are a number of techniques availablc, one of which is dump oxidation. Commercial viability of such an operation requires a net oxidation of 50% or more in 1 year. This is possible in a dump provided convection is established quickly. Since convection requires temperatures in the dump to be well above ambient, a question arises as to the constraints that might be imposed by the upper temperature limit ( T _kill) of the microorganisms which catalyse the oxidation of the pyrite. Our objective is to investigate, by way of a computer model, the importance of T _kill as a parameter effecting the oxidation rate and the fraction of pyrite oxidised after 1 year in dumps where the goal is to oxidise about 50% of the pyrite in a year or less.     

Bacterial Oxidation of Refractory Sulfide Ores for Gold Recovery

Abstract

The microbiological leaching of refractory sulfide ores (pyrite, arsenopyrite) for recovery of gold is reviewed in this article. The underlying physiological, biochemical, and genetic fundamentals of the bacteria involved (Thiobacillus and Sulfolobus spp.) are complex and have yet to be elucidated in depth. The chemistry of acid and biological leaching of pyrite and arsenopyrite minerals is also complex, and many of the individual reactions are not known in detail. Bacterial leaching is discussed in relation to chemical speciation at acid pH values. Attempts to develop models for a better understanding of bioleaching processes are summarized. The importance of pH, redox potential, temperature, sulfur balance, and toxic metals is evaluated for optimizing conditions for bacterial activity. Gold is finely disseminated in refractory sulfide ores, thereby decreasing Au recoveries upon conventional cyanidation for gold dissolution. In the bioleaching process, bacteria remove the sulfide minerals by oxidative dissolution and thus expose Au to extraction with cyanide solution. Stirred tank reactors appear most suited for this biological leaching process. The overall oxidation of the sulfides is an important variable for gold recovery. Pilot- and commercial-scale bioleaching processes for gold-containing pyrite and arsenopyrite ores are reviewed. This application of mineral biotechnology competes favorably with pressure leaching and roasting processes, both of which are problematic and energy-intensive alternatives for pretreatment of auriferous pyrite/arsenopyrite ores.     

Effect of Organic Carbon Source on Pyrite Biooxidation by Moderately Thermophilic Acidophilic Microorganisms

Microbiology - Iron- and sulfur-oxidizing auto-, mixo- and heterotrophic bacteria and archaea dominate in the bioleaching of pyrite from sulfide ores and concentrates both in natural conditions and...     

Influence of manganese ions on cellular behavior of human osteoblasts in vitro

Divalent cations like Mn(2+) are known to strongly influence the integrin affinity to ligands and - in consequence - cell adhesion to extracellular matrix proteins. Therefore, divalent cation supplementation of biomaterials could be a promising approach to improve the ingrowth and the integration of implants. We were interested, whether manganese ions affect cellular functions like spreading, proliferation as well as gene expression in human osteoblasts. MG-63 osteoblastic cells were cultured in DMEM with 10% FCS. MnCl(2) was added at a concentration range of 0.01-0.5mM for 24h and 48 h. Spreading (cell area in microm(2)) of PKH26-stained cells (cell membrane dye) was analyzed using confocal microscopy. Cell proliferation was measured by flow cytometry. Quantification of the phosphorylation status of signaling proteins was estimated using the Bio-Plex 200 system. Gene expression of osteogenic markers at the mRNA and protein level was analyzed by quantitative real time RT-PCR and Western blot, respectively. The results demonstrated that at higher concentrations of Mn(2+) cells revealed a spindle shaped morphology. Further analyses indicated a reduced spreading, proliferation as well as phosphorylation of signaling proteins due to the influence of Mn(2+) in a concentration-dependent manner. Although expression of bone sialo protein (BSP) at the mRNA level increased both after 24h and 48 h in the presence of manganese, no increased expression of BSP was detected at the protein level. The expression of alkaline phosphatase (ALP) and collagen 1 (Col 1) mRNA decreased at >0.1mM MnCl(2). We speculate that the effect of manganese cations on cell functions is strongly concentration-dependent and the release of manganese when incorporated in a biomaterial surface has to be thoroughly adjusted.     

Manganese‐Rich layers in calcareous deposits along the Western shore of the Dead Sea May have a bacterial origin

Spore formers were detected in samples of calcareous crust with manganiferous laminations and in water from the Dead Sea in Israel. They were able to grow in media made with fresh water but not with synthetic Dead Sea water. Some of these spore formers were also able to oxidize Mn (II) in fresh water. No other bacteria capable of both growth and Mn(II) oxidation in hypersaline media prepared with synthetic Dead Sea water were found in the samples. However, bacteria capable of growth and Mn(II) oxidation in fresh water media were detected in water and sediment from fresh water springs at Ein Feshkha and in lake water and sediment from the beach near Wadi Kidron. Both sites are located on the western shore of the lake. These findings suggest that the manganiferous laminations in calcareous crusts and concretions in the Dead Sea along its western shore may have originated, at least in part, from manganese oxide formed by bacteria in fresh water environments on shore and washed into the lake in runoff, with subsequent incorporation into the crusts and concretions.     

Effects of melanin and manganese on DNA damage and repair in PC12-derived neurons

The mechanism of neurotoxicity produced by the interaction of melanin with manganese was investigated in PC12-derived neuronal cell cultures. The cells were incubated with melanin (25-500 microg/ml), MnCl2 (10 ng/ml-100 microg/ml) and a combination of both substances for 24 and 72 h. Incubation with either toxicant alone resulted in a minimal decrease in cell viability. The combination of melanin and manganese caused significant (up to 60%) decreases in viability of PC12 cells in a dose-dependent manner. Increases in oxidative DNA damage, indicated by levels of 8-hydroxy-2'deoxyguanosine (8-oxodG), was associated with decreased cell viability. Melanin alone, but not manganese alone, resulted in increased oxidative DNA damage. The maximal increase in 8-oxodG caused by melanin was about seven times higher than control after 24 h of exposure. The activity of the DNA repair enzyme, 8-oxoguanine DNA glycosylase (OGG1), was increased in cells incubated with single toxicants and their combinations for 24 h. On the third day of incubation with the toxicants, activity of OGG1 declined below control levels and cell viability significantly decreased. Melanin was observed to have an inhibitory effect on OGG1 activity. Study of the regulation of OGG1 activity in response to melanin and manganese may provide insights into the vulnerability of nigral neurons to oxidative stress in Parkinson's disease.     

Suppression of pyritic sulphur during flotation tests using the bacterium Thiobacillus ferrooxidans

Environmental concern about sulphur dioxide emissions has led to the examination of the possibility of removing pyritic sulphur from coal prior to combustion during froth flotation, a routine method for coal cleaning at the pit-head. The bacterium Thiobacillus ferrooxidans was effective in leaching 80% and 63% -53 mum pyrite at 2% and 6% pulp density in shake flasks in 240 and 340 h, respectively.The natural floatability of pyrite was significantly reduced in the Hallimond tube following 2.5 min of conditioning in membrane-filtered bacterial liquor prior to flotation. The suppression effect was greatly enhanced in the presence of Thiobacillus ferrooxidans. A bacterial suspension in pH 2.0 distilled water showed 85% suppression, whereas in spent growth liquor this value was 95%. The optimum bacterial density was 3.25 x 10(10) cells/g pyrite in 230-ml distilled water (2% pulp density) in the Hallimond tube. The degree of suppression by the cells was related to particle size but not to pH or temperature. The sulphur content of a synthetic coal/pyrite mixture was reduced from 10.9 to 2.1% by flotation after bacterial preconditioning. It is postulated that pyrite removal in coals which are cleaned by froth flotation could be significantly reduced using a bacterial preconditioning stage with a short residence time of 2.5 min.     

Electrochemical Reduction of Carbon Dioxide on Pyrite as a Pathway for Abiogenic Formation of Organic Molecules

A wide spectrum of electrode potentials of minerals that compose sulfide ores enables the latter, when in contact with hydrothermal solutions, to form galvanic pairs with cathode potentials sufficient for electrochemical reduction of CO2. The experiments performed demonstrated the increase of cathode current on the rotating pyrite disc electrode in a range of potentials more negative than -800 mV in presence of CO2. In high-pressure experiments performed in a specially designed electrochemical cell equipped with a pyrite cathode and placed into autoclave, accumulation of formate was demonstrated after 24 hr passing of CO2 (50 atm, room temperature) through electrolyte solution. The formation of this product started on increasing the cathode potential to -800 mV (with respect to saturated silver chloride electrode). The yield grew exponentially upon cathode potential increase up to -1200 mV. The maximum current efficiency (0.12%) was registered at cathode potentials of about -1000 mV. No formate production was registered under normal atmospheric pressure and in the absence of imposed cathode potential. Neither in experiments, nor in control was formaldehyde found. It is proposed that the electrochemical reduction of CO2 takes part in the formation of organic molecules in hydrothermal solutions accompanying sulfide ore deposits and in 'black smokers' on the ocean floor.     

Extraction of manganese from electrolytic manganese residue by bioleaching

Extraction of manganese from electrolytic manganese residues using bioleaching was investigated in this paper. The maximum extraction efficiency of Mn was 93% by sulfur-oxidizing bacteria at 4.0 g/l sulfur after bioleaching of 9days, while the maximum extraction efficiency of Mn was 81% by pyrite-leaching bacteria at 4.0 g/l pyrite. The series bioleaching first by sulfur-oxidizing bacteria and followed by pyrite-leaching bacteria evidently promoted the extraction of manganese, witnessing the maximum extraction efficiency of 98.1%. In the case of sulfur-oxidizing bacteria, the strong dissolution of bio-generated sulfuric acid resulted in extraction of soluble Mn2+, while both the Fe2+ catalyzed reduction of Mn4+ and weak acidic dissolution of Mn2+ accounted for the extraction of manganese with pyrite-leaching bacteria. The chemical simulation of bioleaching process further confirmed that the acid dissolution of Mn2+ and Fe2+ catalyzed reduction of Mn4+ were the bioleaching mechanisms involved for Mn extraction from electrolytic manganese residues.     

Dependence of the genotypic characteristics of Acidithiobacillus ferrooxidans 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 hole-type (p-type) conductivity, or pyrite 2, with an electron-type (n-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 1 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 (KTEMF); during bacterial-chemical oxidation, the KTEMF of pyrite 1 changed insignificantly, whereas the KTEMF of pyrite 2 decreased.     

A new look at microbial leaching patterns on sulfide minerals

Leaching patterns on sulfide minerals were investigated by high-resolution scanning electron microscopy (SEM). Our goal was to evaluate the relative contributions of inorganic surface reactions and reactions localized by attached cells to surface morphology evolution. Experiments utilized pyrite (FeS(2)), marcasite (FeS(2)) and arsenopyrite (FeAsS), and two iron-oxidizing prokaryotes in order to determine the importance of cell type, crystal structure, and mineral dissolution rate in microbially induced pit formation. Pyrite surfaces were reacted with the iron-oxidizing bacterium Acidithiobacillus ferrooxidans (at 25 degrees C), the iron-oxidizing archaeon 'Ferroplasma acidarmanus' (at 37 degrees C), and abiotically in the presence of Fe(3+) ions. In all three experiments, discrete bacillus-sized (1-2 μm) and -shaped (elliptical) pits developed on pyrite surfaces within 1 week of reaction. Results show that attaching cells are not necessary for pit formation on pyrite. Marcasite and arsenopyrite surfaces were reacted with A. ferrooxidans (at 25 degrees C) and 'F. acidarmanus' (at 37 degrees C). Cell-sized and cell-shaped dissolution pits were not observed on marcasite or arsenopyrite at any point during reaction with A. ferrooxidans, or on marcasite surfaces reacted with 'F. acidarmanus'. However, individual 'F. acidarmanus' cells were found within individual shallow (<0.5 μm deep) pits. The size and shape (round rather than elliptical) of the pits conformed closely to the shape of F. acidarmanus (cells) pits on arsenopyrite. We infer these pits to be cell-induced. We attribute the formation of pits readily detectable (by SEM) to the higher reactivity of arsenopyrite compared to pyrite and marcasite under the conditions the experiment was conducted. These pits contributed little to the overall surface topographical evolution, and most likely did not significantly increase surface area during reaction. Our results suggest that overall sulfide mineral dissolution may be dominated by surface reactions with Fe(3+) rather than by reactions at the cell-mineral interface.     

Bioleaching of manganese (IV) oxide and application to its recovery from ores

Summary Bioleaching of manganese (IV) oxide with Thiobacillus thiooxidans has been studied in media with and without sulfur, ferrous sulfide and ferrous sulfate. The knowledge of the role played by the bacteria and the reducing substances suggest that the leaching of manganese (IV) ores through the use of thiobacteria is only justified when suitable amounts of sulfur or metal sulfides are present.     

H2O2-Induced Inhibition of Photosynthetic O2 Evolution by Anabaena variabilis Cells

Hydrogen peroxide inhibits photosynthetic O2 evolution. It has been shown that H2O2 destroys the function of the oxygen-evolving complex (OEC) in some chloroplast and Photosystem (PS) II preparations causing release of manganese from the OEC. In other preparations, H2O2 did not cause or caused only insignificant release of manganese. In this work, we tested the effect of H2O2 on the photosynthetic electron transfer and the state of OEC manganese in a native system (intact cells of the cyanobacterium Anabaena variabilis). According to EPR spectroscopy data, H2O2 caused an increase in the level of photooxidation of P700, the reaction centers of PS I, and decreased the rate of their subsequent reduction in the dark by a factor larger than four. Combined effect of H2O2, CN-, and EDTA caused more than eight- to ninefold suppression of the dark reduction of P700+. EPR spectroscopy revealed that the content of free (or loosely bound) Mn2+ in washed cyanobacterial cells was ~20% of the total manganese pool. This content remained unchanged upon the addition of CN- and increased to 25-30% after addition of H2O2. The content of the total manganese decreased to 35% after the treatment of the cells with EDTA. The level of the H2O2-induced release of manganese increased after the treatment of the cells with EDTA. Incubation of cells with H2O2 for 2 h had no effect on the absorption spectra of the photosynthetic pigments. More prolonged incubation with H2O2 (20 h) brought about degradation of phycobilins and chlorophyll a and lysis of cells. Thus, H2O2 causes extraction of manganese from cyanobacterial cells, inhibits the OEC activity and photosynthetic electron transfer, and leads to the destruction of the photosynthetic apparatus. H2O2 is unable to serve as a physiological electron donor in photosynthesis.