Tungsten Resources in Mine Waste: Comparison
Please note this is a comparison between Version 3 by Conner Chen and Version 2 by Conner Chen.

Tungsten is recognized as a critical metal due to its unique properties, economic importance, and limited sources of supply. It has wide applications where hardness, high density, high wear, and high-temperature resistance are required, such as in mining, construction, energy generation, electronics, aerospace, and defense sectors. The two primary tungsten minerals, and the only minerals of economic importance, are wolframite and scheelite. Secondary tungsten minerals are rare and generated by hydrothermal or supergene alteration rather than by atmospheric weathering. There are no reported concerns for tungsten toxicity. However, tungsten tailings and other residues may represent severe risks to human health and the environment. Tungsten metal scrap is the only secondary source for this metal but reprocessing of tungsten tailings may also become important in the future.

  • tungsten resources
  • mine waste
  • recycling

1. Tungsten Geochemical Mobility, Toxicity and Environmental Risks

1.1. Geochemical Mobility

Koutsospyros et al. (2006) reported tungsten can be released to aquatic systems through a host of natural and anthropogenic routes from terrestrial, atmospheric and biotic environments. The natural processes of tungsten mobility include the weathering of tungsten-rich rocks and soils, dissolution of tungsten minerals, hydrothermal and volcanic activities, wet and dry atmospheric precipitation, and excretion of metabolites of tungsten enriched plants. They also reported both soluble and particulate forms of tungsten can exist in aquatic environments, but soluble tungsten is of higher environmental concern because of its higher mobility and toxicity [1]. Tungsten and its compounds usually have limited aquatic solubility and mobility. The reactions of tungsten with water play a major role in its mobility. Microbial activities can also promote tungsten mobility in solution. The iron-oxidizing bacteria and manganese-oxidizing bacteria can significantly accelerate the breakdown of tungsten minerals because these bacteria can destroy the crystalline structure of tungsten minerals and release soluble tungsten compounds [2].

Tungsten exists naturally in ocean water and sediments, surface water bodies, and groundwater in areas of hydrothermal activity [1]. Tungsten metal does not occur in nature, but tungstate anion persists and is thermodynamically stable under most environmental conditions. Tungstate anion can polymerize with itself and other oxyanions (e.g., molybdate, phosphate, and silicate) and generate a variety of polymer species. Polymerization of tungstate anion will impact the mobility of tungsten in ground or surface water due to different geochemical properties of the various polytungstates [3].

1.2. Toxicity

Research has shown that tungsten at very high concentrations and long-term contact (occupational exposure and chronic tungsten poisoning) is harmful to humans. For example, occupational exposure to tungsten may lead to pulmonary fibrosis related to hard metal lung disease, while exposure to tungsten at an environmental level concentration by breathing air, eating food, or drinking water has a low possibility to have harmful effects on humans [4]. A report from the US Center for Disease Control and Prevention (US CDC) investigated the cases of childhood leukemia and compared tungsten exposure in a control community with the community of relatively high exposure through drinking water (~45 times higher). There was no direct evidence showing that tungsten would definitively cause childhood leukemia [5], and the latest follow-up papers also supported this conclusion [6][7].

In the natural environment, tungsten is non-toxic to certain microorganisms but plays an essential role in the biology of microorganisms. Experiments even found tungsten could stimulate the growth of some species of microorganisms [8]. Tungsten also formed a variety of metal enzymes in natural biological systems, and these tungsten-containing enzymes played active roles in the anaerobic aspects of the carbon cycle. For example, tungsten could form tungstoenzymes, which occurred and prevailed in thermophilic and hyperthermophilic in the vicinity of deep-sea hydrothermal vents [9]. For plants, a study found that tungsten can be enriched by several plants [10]. For example, rice can enrich tungsten from the soil, and the enrichment factor of tungsten decreased in the following order: root, leaf, stem, and grain [11].

However, a study also reported that tungsten has potential fetus toxicity and affected the early stages of fish development [12]. In addition, Wistar rats also had a significant rise in the DNA damage and micronuclei, and a difference in biochemical levels and histopathological alterations, after 28 days of repeated oral administration of 1000 mg/kg dose of tungsten trioxide (WO3) nanoparticles. Tungsten biodistribution was detected in all tissues in different concentrations. The highest concentration of tungsten was found in the liver, and the lowest, in the brain of treated rats. However, the overall conclusion from this experiment was that tungsten trioxide nanoparticles have little toxicity hazard even at the highest dose (1000 mg/kg bw/day dose) after 28 days of repeated oral exposure, according to the Organization for Economic Cooperation and Development (OECD) test guideline 407 (2008) [13].

1.3. Environmental Risks of Tungsten Waste

Though tungsten showed little toxicity to humans, animals, and plants, the tungsten mine wastes pose non-neglectable threats to the environment. It was reported that most of the tungsten (about 93% on average) in the soil is in the residual fraction, with low mobility and bioavailability [11]. As a result, the major pollutants released from tungsten mine waste do not necessarily relate to tungsten due to its low concentration and low mobility, but other contaminants present in tailings, such as-, Zn- and Pb-bearing sulfides, carbonates, and sulfates [14].

Acid mine drainage (AMD) generated from tungsten tailings storage facilities (TSFs) proved to be another environmental and health risk. Lianhuashan tungsten mine, one of the largest tungsten mines in southern China, is rich in polymetallic sulfide ores. The major minerals of this mine are wolframite, scheelite, arsenopyrite, pyrite, magnetite, chalcopyrite, quartz, sericite, chlorite, and feldspar. This mine was closed in 1991 and left a huge amount of untreated tailings in the TSFs. During the rainy season, AMD and weathered slag were released into the ambient environment and resulted in serious contaminations. Pollutants included Cu, Cd, Zn, Pb, Hg, and As, with As being the prominent pollutant. It also demonstrated that tungsten was not a significant contaminant element in tungsten tailings [15].

Currently, there is no environmental guideline on tungsten pollution in the United States or the European Union, neither in Australia, nor published data on the environmental effects of tungsten are inadequate [16]. Only for major tungsten substances, International Tungsten Industry Association (ITIA) published hazard classifications (Table 1) [17].

Table 1. Hazard classifications for the major tungsten substances. Based on: [17].

Substance Hazard Class (EC1272/2008) Hazard Warning
Ammonium Metatungstate Acute oral toxicity 4 Harmful if swallowed
Ammonium Paratungstate Not classified None
Flotation 30.18% WO3 concentrates with an 80% recovery rate from very fine wolframite slime [24] Sodium Tungstate Acute oral toxicity 4 Harmful if swallowed
Tungsten Powder (0.6–0.9 µm)

. Wolframite ores are of good quality, high grade, easy mining, easy selection, have convenient subsequent treatment, and less environmental hazard [19]. Gravity and magnetic separation are the most common methods for the enrichment of wolframite because it is a paramagnetic, heavy, and dense mineral. But these methods are not suitable for the recovery of ultra-fine wolframite, especially for particle sizes below 20 μm [20]. In comparison, scheelite is amenable to flotation, which is the conventional approach applied in scheelite beneficiation [21]. To date, tungsten tailings are still mainly treated as a waste rather than a resource, and only limited experiments have been done on tungsten tailings reprocessing.

One reprocessing experiment at the Panasqueira tungsten mine in Portugal was carried out to recover ultrafine wolframite from old and new tailings. Froth flotation, magnetic separation, and gravity separation were compared for reprocessing both old and new tailings. The results indicated that froth flotation was the only feasible approach to reprocess new tailings to recover wolframite, while magnetic separation showed low recovery rates at different magnetic intensity levels. A three-stage gravity separation combined with intermediate sulfide flotation generated 50–55% WO3 wolframite concentrates at reasonable recovery from tungsten tailings. However, because the reprocessing of 1 t of tungsten tailings delivered only a few kilograms of tungsten concentrate, it was considered to be uneconomic [22]Table 2 lists a few other reported tailings reprocessing trials for tungsten concentrates recovery.

Table 2. Worldwide reprocessing trials for tungsten recovery from tailings.

Tungsten Tailings Type Deposits Major Tungsten Minerals Tailings Grade, WO3% Reprocessing Methods Reprocessing Results Reference
High-intensity magnetic separation tungsten ore slime Rajasthan (India) Wolframite 2.87 and 5.30 Polymeric dispersant with magnetic separation Wolframite was enriched from tungsten slimes to 5.4–11% WO3 concentrates. The grade of tungsten concentrates was increased to 10% when dispersant is applied [23]
Fine tungsten tailings
Historical mine tailings and current plant slimes tailings Panasqueira (Portugal) Wolframite, most of the particles below 25 µm
Flammable solid 1; Self-heating 2 Flammable solid; Self-heating in large quantities; may catch fire
Dajishan (China) Tungsten Powder (<1.0 µm) Flammable solid 1 Flammable solid
Wolframite Tungsten Powder (1.0–1.5 µm) Flammable solid 2 Flammable solid
0.45 0.1 Flotation, magnetic separation, and gravity concentration A three-stage gravity separation combined with intermediate sulfide flotation produced tungsten concentrates with 50–55% WO3 [22]
Tin mine tailings Potosi Mine tin processing plant (Bolivia) Wolframite 0.64 Chlorination segregation, flotation, high-intensity magnetic separation, and gravity separation 60.22% WO3 concentrate with 64.26% recovery rate; 25.04% copper concentrate with 83.19% recovery; and 40.11% tin concentrate with 65.59% recovery [25] Tungsten Powder (>1.5 µm) Not classified None
Old tailing dumps Kolar and Hutti goldfields (India) Scheelite 0.2 Tabling, flotation, and magnetic separation 65% WO3 concentrate from a feed of tungsten tailings [26]
Old molybdenum mine tailings Tyrnyauz processing plant (Russia) Scheelite 0.05 FlotationTungsten Blue Oxide Not classified None
Tungsten Carbide Not classified None
Tungsten Disulfide Not classified None
Tungsten Trioxide Not classified None

2. Potential Reprocessing Approaches for Tungsten Recovery from Tailings

2.1. A Summary of Previous Reprocessing Trials

The tungsten ores beneficiation process usually consists of pre-concentration, roughing, cleaning and purification after ore crushing and grinding. The final tungsten concentrates usually contain ≥65% WO3 [18]

54–55% WO
3
 concentrate with 61.91–62.08% recovery rate from wolframite-molybdenum sand tailings
[
27][28]

2.2. Gravity Separation

Gravity separation is an important approach in wolframite beneficiation. Compared with other mineral processing technologies, gravity separation has several advantages, such as high separation efficiency, low investment and operation costs, no additional chemical reagents required, and no potential pollution to the environment [29]. But conventional gravity separation is inefficient for the fine and ultrafine fractions of wolframite: it was reported to be below 45% [20]. Due to wolframite’s hard and brittle properties, the generation of over crushed wolframite is inevitable during ore grinding [30]. As a result, a large portion of fine and ultrafine wolframite may be left in tailings after beneficiation by gravity separation. Nevertheless, in the same study, enhanced gravity concentrators were successfully applied for the fine tungsten minerals beneficiation [30]. Hang and vibrate cone concentrator and Falcon concentrator are two very selective separators for fine-sized mineral particles (typically +10–75 μm) and have very high mineral upgrading ratios (typically 20 to 1). An artificial sample consisted of pure and fine minerals of scheelite, wolframite, cassiterite, fluorite, and calcite was prepared to test these two enhanced gravity concentrators for the fine tungsten minerals recovery. Most of the minerals in this sample were distributed in the -74 μm fraction, with the superfine fraction (−19 μm) accounting for more than 30%. The results showed that these two concentrators could respectively achieve 83.15% and 76.38% tungsten recovery rates. However, it was also found that these separators were still not efficient in the recovery of ultrafine (−10 μm) wolframite particles [29].

2.3. Magnetic Separation

In wolframite beneficiation, magnetic separation is usually operated in a high-intensity magnetic separation system for ideal wolframite recovery. In the conventional magnetic separation process, wolframite particle size plays a prominent role, similarly to gravity separation. With a decrease in the wolframite particle size, magnetic forces acting on the wolframite particle would drop quickly and cannot resist a hydrodynamic drag. As a result, the fine fraction of wolframite is lost to tailings. Furthermore, feeding flow and washing water can also wash away ultrafine wolframite from the separation plates in the magnetic field [31]Figure 1 shows that the recovery of wolframite through magnetic separation varies under different particle sizes and magnetic intensities. For the particle sizes above 10 μm, the maximum recovery of wolframite could reach approximately 90% with an increase in magnetic intensity to 1.3 Tesla (1.3 T). However, for wolframite particles below 10 μm, the maximum recovery could only achieve approximately 60%, even with the highest 1.5 T magnetic intensity [31].

Figure 1. Recovery of different size fractions of wolframite as a function of magnetic intensity [31].

Wet high-intensity magnetic separation (WHIMS) has been used as an effective enhanced approach to separate minerals of low magnetic susceptibility from tailings [32]. A WHIMS modeling on tungsten tailings predicted good wolframite recovery rates: approximately 80% (90%) for new tailings and 65% (80%) for old tailings at 0.9 T (1.6 T) magnetic intensity [33]. Another study also found that WHIMS can successfully recover the fine fraction of wolframite from tungsten ore slimes and reach 90% recovery at 1.15 T magnetic intensity [23].

2.4. Flotation

Flotation is a physicochemical separation process for minerals, which usually utilizes various minerals’ surface properties to separate valuable minerals and unwanted gangue minerals. Selective flocculants, dispersants, depressants, and flotation collectors are usually used in flotation. Major influencing factors for flotation are mineral surface wettability, surface lattice ion dissolution, surface electrical properties, and solution chemical properties [34]. For scheelite ores, especially occurring in skarns, fluorite, apatite, and calcite constitute common gangue minerals, flotation is currently the major processing method [35]. Frequently used scheelite flotation depressants are sodium silicate, phosphates, and fluorosilicates [19].

For wolframite, because of its low floatability, selective flotation was hardly used for its beneficiation at an industrial scale. However, for ultrafine wolframite, due to its poor recovery by conventional gravity separation and magnetic separation, flotation was successfully applied. For example, froth flotation, shear flocculation, and spherical agglomeration with highly selective reagents, such as alkyl hydroxamates, phosphonic acid derivatives, and alkylated nitroso-napthols, can significantly enrich fine and ultrafine wolframite from tungsten ore slimes [36]. It was also reported that benzohydroxamic acid (BHA) and sodium oleate (NaOl) as flotation collectors could efficiently improve the fine wolframite collecting capability [37]. While adding lead ions (Pb2+) into flotation collectors could improve the adsorption of BHA onto the wolframite surface in the pH range from 4 to 10.5, which can significantly increase the recovery of fine wolframite in flotation [38]. More recent studies found that a novel surfactant N-(6-(hydroxyamino)-6-oxohexyl) octanamide (NHOO) is a more efficient collector in wolframite flotation [39].

The application of flotation was demonstrated for the fine slimes from a wolframite processing plant. The process could obtain 36.87% WO3 tungsten concentrates with 62.90% recovery from 0.26% WO3 fine wolframite slime [30]. However, though flotation could enrich fine and ultra-fine wolframite and reprocess tungsten tailings, the flotation beneficiation reagents left in the new tailings can result in new contamination to the environment, especially some arsenic (As)-bearing reagents (e.g., arsonic acid).

2.5. Chemical Leaching

Chemical leaching for minerals beneficiation is heap leaching. It is a relatively low-cost processing method, widely used for metal extraction from low-grade ores, including copper (Cu), gold (Au), silver (Ag), and uranium (U) [40]. Furthermore, it was also used in soil remediation, reprocessing agglomerated flotation tailings, and for the treatment of coarse rejects from semi-autogenous grinding circuits [41]. This method usually involves acids, alkalis, and cyanide to mobilize and collect valuable metals in solution. However, the main drawbacks of chemical heap leaching are that it can be slow and inefficient and may result in potential risks to the environment [42].

Although chemical heap leaching could be used to reprocess tailings and residue materials [42], it is unlikely to reprocess tungsten tailings. Scheelite is hard to decompose by acids at normal temperature because the generation of the solid-colloidal layer of tungstic acid (H2WO4) on the scheelite surface would stop its further decomposition [43]. While decomposing scheelite with sodium hydroxide (NaOH) or sodium carbonate (Na2CO3), digestion would require the reaction temperature above 180 °C in an autoclave [44]. It was also reported that scheelite could not be decomposed by NaOH under commercial conditions [45]. Similarly, scheelite leaching with hydrochloric acid (HCl) for tungstic acid would require a reaction temperature above 125 °C [46]. It was almost the same condition needed for wolframite decomposition. Caustic digestion is a conventional method employed to decompose wolframite to produce soluble tungstate (WO42−) in the industry. However, it may require higher temperature, pressure, and some other conditions [47][48]. Therefore, it is not feasible for reprocessing of tungsten tailings through chemical heap leaching under natural conditions.

2.6. Bioleaching

Over the past decades, bioleaching has quickly developed and is used to recover metals from ores in the mining industry. So far, bioleaching has been applied to extract zinc (Zn), cobalt (Co), copper (Cu), nickel (Ni), lead (Pb), gold (Au), and arsenic (As) from minerals in the industry [49][50]. For example, bioleaching of copper can achieve a higher than 90% recovery rate, and each year approximately 20% of global copper is produced through bioleaching [51]. Compared with conventional mineral processing methods, bioleaching is low-cost, highly safe, simple to operate, and environmentally friendly [52].

Currently, bioleaching is more and more frequently applied to extract, recover and remove heavy metals from solid waste as well, including mine tailings and sediments [53][54]. In most cases, acidophilic chemolithotrophic microorganisms are the major microbes for bioleaching. Biological oxidation and complexation reactions are the ways for bioleaching to mobilize metal cations from insoluble minerals [55]. However, bioleaching is sensitive to several conditions, such as solids concentration, temperature, oxygen, pH, redox potential, bacterial strain, and cell concentration. These factors play important roles in the optimization of the bioleaching process [56]. Besides single strain microbe of metal sulfide bioleaching, mixed microbe cultures can be a more efficient way to decompose minerals [57]. Mixed cultures can use elemental sulfur (S0) and ferrous ion (Fe2+) as energy sources and can either fix atmospheric carbon dioxide (CO2) or use organic carbon as a carbon source. Usually, it is a much more stable and effective mineral bioleaching consortium. Different bacterial strains in the consortium can also cooperate to respond better to environmental changes during bioleaching [58]. The feasibility of bioleaching for mine tailing reprocessing can be supported by its successful application in the mining industry worldwide.

The growing demand for metals has already led to the re-assessment of old tailings as a potential resource. A few studies have proved that valuable or toxic elements in tailings can be recovered or removed by bioleaching in appropriate ways. A study has demonstrated a successful application of bioleaching to remove heavy metals from low-grade Zn-Pb mine tailings [59]. The experiments also showed that bioleaching is quite effective in recovering Zn and In from old Zn-Pb tailings, with respective recovery rates of up to 100% and 80% [60]. For tungsten minerals, the latest research demonstrated that some microbes (the extreme thermoacidophile Metallosphaera sedula) can grow on and directly extract tungsten from scheelite, which proposed a new approach for tungsten tailings reprocessing [61]. One successful bioleaching experiment on tungsten tailings was to remove As and manganese (Mn) from tungsten tailings. When mixed cultures of Acidithiobacillus ferrooxidans and Acidithiobacillus thiooxidans were applied, the recovery of As could reach 96.7%, and the recovery of Mn almost 100% [62][63].

References

  1. Koutsospyros, A.; Braida, W.; Christodoulatos, C.; Dermatas, D.; Strigul, N. A review of tungsten: From environmental obscurity to scrutiny. J. Hazard. Mater. 2006, 136, 1–19.
  2. Cao, Y.; Guo, Q. Tungsten speciation and its geochemical behavior in geothermal water: A review. E3S Web Conf. 2019, 98, 07005.
  3. Bednar, A.J.; Boyd, R.E.; Jones, W.T.; McGrath, C.J.; Johnson, D.R.; Chappell, M.A.; Ringelberg, D.B. Investigations of tungsten mobility in soil using column tests. Chemosphere 2009, 75, 1049–1056.
  4. van der Voet, G.B.; Todorov, T.I.; Centeno, J.A.; Jonas, W.; Ives, J.; Mullick, F.G. Metals and Health: A Clinical Toxicological Perspective on Tungsten and Review of the Literature. Mil. Med. 2007, 172, 1002–1005.
  5. Sheppard, P.R.; Ridenour, G.; Speakman, R.J.; Witten, M.L. Elevated tungsten and cobalt in airborne particulates in Fallon, Nevada: Possible implications for the childhood leukemia cluster. Appl. Geochem. 2006, 21, 152–165.
  6. Datta, S.; Vero, S.E.; Hettiarachchi, G.M.; Johannesson, K. Tungsten Contamination of Soils and Sediments: Current State of Science. Curr. Pollut. Rep. 2017, 3, 55–64.
  7. Hobson, C.; Kulkarni, H.V.; Johannesson, K.H.; Bednar, A.; Tappero, R.; Mohajerin, T.J.; Sheppard, P.R.; Witten, M.L.; Hettiarachchi, G.M.; Datta, S. Origin of tungsten and geochemical controls on its occurrence and mobilization in shallow sediments from Fallon, Nevada, USA. Chemosphere 2020, 260, 127577.
  8. Kletzin, A.; Adams, M.W. Tungsten in biological systems. FEMS Microbiol. Rev. 1996, 18, 5–63.
  9. Agamemnon, D.K.; Demetri, A.K.; Nick, S.; Washington, B.; Christos, C. Tungsten: Environmental Pollution and Health Effects. Encycl. Environ. Health 2011.
  10. Strigul, N.; Koutsospyros, A.; Arienti, P.; Christodoulatos, C.; Dermatas, D.; Braida, W. Effects of tungsten on environmental systems. Chemosphere 2005, 61, 248–258.
  11. Lin, C.; Li, R.; Cheng, H.; Wang, J.; Shao, X. Tungsten distribution in soil and rice in the vicinity of the world’s largest and longest-operating tungsten mine in China. PLoS ONE 2014, 9, e91981.
  12. Strigul, N.; Koutsospyros, A.; Christodoulatos, C. Tungsten speciation and toxicity: Acute toxicity of mono- and poly-tungstates to fish. Ecotoxicol. Environ. Saf. 2010, 73, 164–171.
  13. Chinde, S.; Grover, P. Toxicological assessment of nano and micron-sized tungsten oxide after 28days repeated oral administration to Wistar rats. Mutat Res. 2017, 819, 1–13.
  14. Lee, P.-K.; Kang, M.-J.; Jo, H.Y.; Choi, S.-H. Sequential extraction and leaching characteristics of heavy metals in abandoned tungsten mine tailings sediments. Environ. Earth Sci. 2012, 66, 1909–1923.
  15. Liu, C.-P.; Luo, C.-L.; Gao, Y.; Li, F.-B.; Lin, L.-W.; Wu, C.-A.; Li, X.-D. Arsenic contamination and potential health risk implications at an abandoned tungsten mine, southern China. Environ. Pollut. 2010, 158, 820–826.
  16. Strigul, N.; Koutsospyros, A.; Christodoulatos, C. Tungsten in the former Soviet Union: Review of environmental regulations and related research. Land Contam. Reclam. 2009, 17, 189.
  17. International Tungsten Industry Association. Tungsten Health and Environment. Available online: (accessed on 18 February 2021).
  18. Krishna Rao, N. Beneficiation of tungsten ores in India: A review. Bull. Mater. Sci. 1996, 19, 201–265.
  19. Dong, L.; Jiao, F.; Qin, W.; Liu, W. Selective flotation of scheelite from calcite using xanthan gum as depressant. Miner. Eng. 2019, 138, 14–23.
  20. Ai, G.; Huang, W.; Yang, X.; Li, X. Effect of collector and depressant on monomineralic surfaces in fine wolframite flotation system. Sep. Purif. Technol. 2017, 176, 59–65.
  21. Yang, X. Beneficiation studies of tungsten ores—A review. Miner. Eng. 2018, 125, 111–119.
  22. Clemente, D.; Newling, P.; Botelho, d.S.A.; LeJeune, G.; Barber, S.P.; Tucker, P. Reprocessing slimes tailings from a tungsten mine. Miner. Eng. 1993, 6, 831–839.
  23. Pravesh, R.; Pathak, B.P.N. The effect of polymeric dispersant on magnetic separation of tungsten ore slimes. Int. J. Miner. Process. 1996, 47, 213–217.
  24. Lu, J.; Qu, Z.; Li, M. Industrialized Flotation Experiments on the Fine Mud Discharge of a Wolframite Concentrator. China Tungsten Ind. 2015, 30, 36–40.
  25. Xiao, J.H.; Feng, Q.M.; Fan, S.P.; Xu, L.; Wang, Z. Comprehensive utilization of copper, tungsten and tin polymetallic tailings in Bolivia. Zhongguo Youse Jinshu Xuebao Chin. J. Nonferrous Met. 2013, 23, 2949–2961.
  26. Rao, G.M.; Subrahmanyan, N.N. Beneficiation of tungsten ores in India—problems, processes, applications and demands in general on a global scene. Przeróbka Rud Wolframu W Indict Physicochem. Probl. Miner. Process. 1986, 18, 23–37.
  27. Evdokimov, S.S.; Evdokimov, V. Flotation of wolfram-molybdenum sand tailings at Tyrnyauz processing plant. Gorn. Zhurnal 2015, 2015, 63–68.
  28. Khuchunaev, B.M.; Tashilova, A.A.; Kesheva, L.A.; Teunova, N.V. The tailing dumps’ reclamation influence evaluation on atmospheric air at the mining enterprise. IOP Conf. Ser. Mater. Sci. Eng. 2020, 913, 052044.
  29. Yue, T.; Han, H.; Hu, Y.; Wei, Z.; Wang, J.; Wang, L.; Sun, W.; Yang, Y.; Sun, L.; Liu, R.; et al. Beneficiation and Purification of Tungsten and Cassiterite Minerals Using Pb–BHA Complexes Flotation and Centrifugal Separation. Minerals 2018, 8, 566.
  30. Ai, G.; Liu, Y. A study on recycling fine wolframite slime by “flotation desulfurization-centrifugal preconcentration-flotation wolframite” process. IJSSST. 2016, 17.
  31. Meng, Q.; Feng, Q.; Ou, L. Recovery Enhancement of Ultrafine Wolframite through Hydrophobic Flocs Magnetic Separation. Miner. Process. Extr. Metall. Rev. 2017, 38, 298–303.
  32. Svoboda, J.; Guest, R.N.; Venter, W.J.C. The recovery of copper and lead minerals from Tsumeb flotation tailings by magnetic separation. J. S. Afr. Inst. Min. Metall. 1988, 88, 9–19.
  33. Tucker, P. Modelling wet high intensity magnetic separation: A case study. Miner. Eng. 1994, 7, 1281–1300.
  34. Chen, Q.; Kasomo, R.M.; Li, H.; Jiao, X.; Zheng, H.; Weng, X.; Mutua, N.M.; Song, S.; He, D.; Luo, H. Froth flotation of rutile—An overview. Miner. Eng. 2021, 163, 106797.
  35. Filippov, L.O.; Foucaud, Y.; Filippova, I.V.; Badawi, M. New reagent formulations for selective flotation of scheelite from a skarn ore with complex calcium minerals gangue. Miner. Eng. 2018, 123, 85–94.
  36. Pradip. Recent advances in the recovery of tungsten values in the fine and ultrafine size range. Bull. Mater. Sci. 1996, 19, 267–293.
  37. Yang, S.; Feng, Q.; Qiu, X.; Gao, Y.; Xie, Z. Relationship between flotation and Fe/Mn ratio of wolframite with benzohydroxamic acid and sodium oleate as collectors. Physicochem. Probl. Miner. Process. 2014, 50, 747–758.
  38. Yang, S.; Peng, T.; Li, H.; Feng, Q.; Qiu, X. Flotation Mechanism of Wolframite with Varied Components Fe/Mn. Miner. Process. Extr. Metall. Rev. 2015, 37.
  39. Deng, L.; Zhong, H.; Wang, S.; Liu, G. A novel surfactant N-(6-(hydroxyamino)-6-oxohexyl)octanamide: Synthesis and flotation mechanisms to wolframite. Sep. Purif. Technol. 2015, 145.
  40. Padilla, G.A.; Cisternas, L.A.; Cueto, J.Y. On the optimization of heap leaching. Miner. Eng. 2008, 21, 673–678.
  41. Ghorbani, Y.; Franzidis, J.-P.; Petersen, J. Heap Leaching Technology—Current State, Innovations, and Future Directions: A Review. Miner. Process. Extr. Metall. Rev. 2016, 37, 73–119.
  42. Petersen, J. Heap leaching as a key technology for recovery of values from low-grade ores—A brief overview. Hydrometallurgy 2016, 165, 206–212.
  43. Gong, D.; Zhou, K.; Peng, C.; Li, J.; Chen, W. Sequential extraction of tungsten from scheelite through roasting and alkaline leaching. Miner. Eng. 2019, 132, 238–244.
  44. Queneau, P.B.; Beckstead, L.W.; Huggins, D.K. Autoclave Soda Digestion of Scheelite Concentrates with Feedback Control. U.S. Patent No. 4,325,919, 20 April 1982.
  45. Zhao, Z.; Liang, Y.; Liu, X.; Chen, A.; Li, H. Sodium hydroxide digestion of scheelite by reactive extrusion. Int. J. Refract. Met. Hard Mater. 2011, 29, 739–742.
  46. Forward, F.A.; Vizsolyi, A.I. Process for the Production of Tungstic Acid. U.S. Patent US3193347A, 6 July 1965.
  47. Shen, L.; Li, X.; Zhou, Q.; Peng, Z.; Liu, G.; Qi, T.; Taskinen, P. Wolframite Conversion in Treating a Mixed Wolframite–Scheelite Concentrate by Sulfuric Acid. JOM 2018, 70, 161–167.
  48. Leitão, P.; Futuro, A.; Vila, C.; Dinis, L.; Danko, A.; Fiúza, A. Direct Pressure Alkaline Leaching of Scheelite Ores and Concentrates. Min. Metall. Explor. 2019, 36, 993–1002.
  49. Borja, D.; Nguyen, K.A.; Silva, R.A.; Ngoma, E.; Petersen, J.; Harrison, S.T.L.; Park, J.H.; Kim, H. Continuous bioleaching of arsenopyrite from mine tailings using an adapted mesophilic microbial culture. Hydrometallurgy 2019, 187, 187–194.
  50. Gopikrishnan, V.; Vignesh, A.; Radhakrishnan, M.; Joseph, J.; Shanmugasundaram, T.; Doble, M.; Balagurunathan, R. Chapter 10—Microbial leaching of heavy metals from e-waste: Opportunities and challenges. In Biovalorisation of Wastes to Renewable Chemicals and Biofuels; Krishnaraj, R.N., Sani, R.K., Eds.; Elsevier: Amsterdam, The Netherlands, 2020; pp. 189–216.
  51. Brierley, J.A. A perspective on developments in biohydrometallurgy. Hydrometallurgy 2008, 94, 2–7.
  52. Pradhan, N.; Nathsarma, K.C.; Srinivasa, R.K.; Sukla, L.B.; Mishra, B.K. Heap bioleaching of chalcopyrite: A review. Miner. Eng. 2008, 21, 355–365.
  53. Mohanty, S.; Ghosh, S.; Nayak, S.; Das, A.P. Bioleaching of manganese by Aspergillus sp. isolated from mining deposits. Chemosphere 2017, 172, 302–309.
  54. Cheng, Y.; Guo, Z.; Liu, X.; Yin, H.; Qiu, G.; Pan, F.; Liu, H. The bioleaching feasibility for Pb/Zn smelting slag and community characteristics of indigenous moderate-thermophilic bacteria. Bioresour. Technol. 2009, 100, 2737–2740.
  55. Ye, M.; Li, G.; Yan, P.; Ren, J.; Zheng, L.; Han, D.; Sun, S.; Huang, S.; Zhong, Y. Removal of metals from lead-zinc mine tailings using bioleaching and followed by sulfide precipitation. Chemosphere 2017, 185, 1189–1196.
  56. Liu, Y.G.; Zhou, M.; Zeng, G.M.; Wang, X.; Li, X.; Fan, T.; Xu, W.H. Bioleaching of heavy metals from mine tailings by indigenous sulfur-oxidizing bacteria: Effects of substrate concentration. Bioresour. Technol. 2008, 99, 4124–4129.
  57. Okibe, N.; Johnson, D.B. Biooxidation of pyrite by defined mixed cultures of moderately thermophilic acidophiles in pH-controlled bioreactors: Significance of microbial interactions. Biotechnol. Bioeng. 2004, 87, 574–583.
  58. Rawlings, D.E.; Johnson, D.B. The microbiology of biomining: Development and optimization of mineral-oxidizing microbial consortia. Microbiology 2007, 153, 315–324.
  59. Li, S.; Zhong, H.; Hu, Y.; Zhao, J.; He, Z.; Gu, G. Bioleaching of a low-grade nickel-copper sulfide by mixture of four thermophiles. Bioresour. Technol. 2014, 153, 300–306.
  60. Martin, M.; Janneck, E.; Kermer, R.; Patzig, A.; Reichel, S. Recovery of indium from sphalerite ore and flotation tailings by bioleaching and subsequent precipitation processes. Miner. Eng. 2015, 75, 94–99.
  61. Blazevic, A.; Albu, M.; Mitsche, S.; Rittmann, S.K.R.; Habler, G.; Milojevic, T. Biotransformation of Scheelite CaWO4 by the Extreme Thermoacidophile Metallosphaera sedula: Tungsten-Microbial Interface. Front. Microbiol. 2019, 10, 1492.
  62. Nguyen, V.K.; Ha, M.G.; Shin, S.; Seo, M.; Jang, J.; Jo, S.; Kim, D.; Lee, S.; Jung, Y.; Kang, P.; et al. Electrochemical effect on bioleaching of arsenic and manganese from tungsten mine wastes using Acidithiobacillus spp. J. Environ. Manag. 2018, 223, 852–859.
  63. Lee, E.; Han, Y.; Park, J.; Hong, J.; Silva, R.A.; Kim, S.; Kim, H. Bioleaching of arsenic from highly contaminated mine tailings using Acidithiobacillus thiooxidans. J. Environ. Manag. 2015, 147, 124–131.
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