Copper is vital for economic and societal growth since it is a conductor of heat and electricity, ductile, resistant to corrosion, and recyclable. For instance, a hybrid vehicle contains approximately 45 kilograms of copper in its wiring, motors, radiators, and brakes. The high demand for copper is coinciding with a sharp decline in the grade of copper reserves, and as a result, the cost of copper production is expected to escalate in the coming decades. Researchers project a global peak in the copper industry by the year 2050 due in part to the high costs of copper production. The development of new processing techniques of copper-containing ore is important to reduce the costs of copper production and extend the availability of new copper for several decades. The vast majority of copper reserves are in the form of chalcopyrite (CuFeS2), and the development of hydrometallurgical technologies to convert this mineral phase into copper may have environmental benefits over existing processes.
CuFeS2 is the most abundant mineral composite including copper found in nature, accounting for approximately 70% of global copper reserves. The two most common routes for processing these minerals are pyrometallurgy and hydrometallurgy. CuFeS2 typically undergoes a pyrometallurgical route to produce copper. The pyrometallurgical route is characterized by high investment costs, high operating costs, and the potential release of environmentally deleterious products such as sulfur dioxide gas and arsenic. A life cycle assessment shows the extent of energy consumption, water consumption, CO2 emission, and SO2 emission for this processing route. Pyrometallurgical operations produce a concentrate of valuable metal sulfides, which is then smelted and refined to produce copper. However, isolating copper using heat is both harmful to the environment, e.g., releases sulfur dioxide and arsenic, and inefficient for copper extraction from lower-grade ore, which is becoming a problem as copper sources dwindle. Because of an increase in copper scarcity, there has been a recent interest in obtaining copper from lower-grade ores. This is not easily achieved via pyrometallurgy, as the concentrate produced is not clean enough to extract copper. Moreover, these heat-based techniques cannot be applied to lower-grade ore due to the reduced purity, which is becoming a problem as ideal copper sources dwindle. There is also mounting concern regarding the effects of pyrometallurgic extraction of copper on the environment, specifically the high levels of greenhouse gas emissions.
Hydrometallurgy, or the extraction of metals from their ores using aqueous solutions, has presented itself as an attractive and environmentally friendly alternative for extraction of copper from chalcopyrite. Hydrometallurgy can also be applied to lower-grade ore, as there is no concentration step required. However, there are few described hydrometallurgical methods for copper extraction from chalcopyrite that have reached commercial-scale operation.
The hydrometallurgical leaching of CuFeS2 is generally conducted with Fe3+ as the oxidant, although regents such as O2, H2O2, and Ag+ have also been studied. The diffusion of the oxidant is generally inhibited by the formation of a passivation layer on the surface of the mineral. There persists a disagreement regarding the chemical makeup of the passivation layer and the mechanism of its formation. In various media, elemental sulfur, disulfide, and polysulfide have been identified on the chalcopyrite surface, which likely contribute to the passivation. The indigenous bacteria that increase the kinetics for the oxidation of other copper-sulfides do not significantly improve the kinetics of CuFeS2 oxidation.
Studies showed that CuFeS2 can be converted to Cu2S using solid copper, sulfur dioxide gas, iron, and aluminum as reducing agents. The chemical reducing agents, however, typically yield relatively low conversions and require fine CuFeS2 particle sizes or high temperatures. An alternative approach has been developed to electrochemically reduce CuFeS2 to Cu2S in acidic solution. Studies have been conducted to analyze the effects of operating parameters such as acid concentration, CuFeS2 pulp density, and temperature. In more recent studies, a sulfur passivation layer on the CuFeS2 surface during the electrochemical reaction was proposed to cause a decrease in faradaic efficiency over reaction time. Also, experiments conducted with hydrochloric acid in a reactor divided by an anion-selective membrane showed the formation of Cu2O as the final product, although the use of an anion-selective membrane and corrosive chloride ions increase the capital costs and electricity costs for processing. Experimental conditions that lead to different mineral products are currently not well-understood in the literature.
The refractory nature of CuFeS2 has prohibited the widespread use of hydrometallurgical treatment in industry. Bioleaching of CuFeS2 proceeds with a slow dissolution rate due to the formation of passivation layers on the surface of the mineral. Polysulfide, elemental sulfur, and insoluble sulfate (typically in the form of jarosite) have been identified on chalcopyrite surfaces under various conditions and have been attributed to causing the passivation. Some studies, however, disregard polysulfide as the passivating species due to its instability, and other studies disregard elemental sulfur because it is easily oxidized. The passivation is likely dependent on several factors including the oxidative potential and the involvement of microorganisms. Regardless, the slow leaching kinetics are linked to passivation and have prevented the bioleaching of CuFeS2 on the industrial scale.
Alternative hydrometallurgical processes have been developed to mitigate the environmental impact of large-scale copper production. For instance, the dissolution of CuFeS2 has been shown to occur rapidly under high temperatures and pressures, although such conditions may be too costly for industrial processing. The incorporation of small amounts of silver into the heap leach has been shown to alleviate the severity of passivation and improve the kinetics of copper extraction. Incorporating potassium iodide into the leaching media has shown to increase the kinetics of leaching by utilizing iodine as an oxidizing agent. Lastly, the galvanically assisted reduction of CuFeS2 with pyrite (FeS2) has been shown to enhance copper recovery at atmospheric pressure and relatively low temperature.
The conversion of CuFeS2 into less refractory mineral phases prior to chemical oxidation may be a more promising hydrometallurgical route for copper recovery. As discussed above, it has been demonstrated that CuFeS2 can be reduced to Cu2S using copper, sulfur dioxide, iron, and aluminum as reducing agents. These reducing agents, however, tend to require fine particle sizes or high temperatures, and therefore, have not been adopted on the industrial scale. Further, to date, few studies have been conducted to assess the electrochemical treatment of CuFeS2 by a continuous reactor.
Accordingly, some embodiments of the present disclosure relate to a method for production of copper ions. In some embodiments, the method includes providing a sample including an amount of chalcopyrite (CuFeS2); providing an electrochemical reactor including an anode, a cathode, and an electrolyte in communication with the anode and the cathode; providing the sample to the electrochemical reactor; applying a potential between the anode and the cathode to produce a first product including cuprite (Cu2O); and applying an oxidizing agent to the first product to oxidize the Cu2O to produce a second product including copper ions. In some embodiments, applying a potential between the anode and the cathode to produce a first product including cuprite (Cu2O) includes operating the electrochemical reactor at a current density less than about 50 mA/cm2. In some embodiments, providing a sample including an amount of CuFeS2 further comprises grinding the sample to have an average particle size between about 50 μm and about 110 μm.
In some embodiments, a porous separator is positioned between the sample and the anode. In some embodiments, the anode is covered by the porous separator. In some embodiments, the porous separator includes filter paper. In some embodiments, the cathode is composed of niobium, tungsten, platinum, copper, aluminum, lead, or combinations thereof. In some embodiments, the anode is composed of niobium, tungsten, platinum, copper, aluminum, lead, or combinations thereof. In some embodiments, the cathode further comprises a bed of cathode material particles. In some embodiments, the ratio of cathode surface area (cm2) to electrochemical reactor volume (mL) is above about 0.15. In some embodiments, the oxidizing agent includes a source of Fe3+ ions.
Some embodiments of the present disclosure relate to a system for production of copper ions. In some embodiments, the system includes a source of chalcopyrite (CuFeS2); an electrochemical reactor in communication with the source of CuFeS2, the electrochemical reactor including an anode covered by a porous separator; a cathode; an electrolyte in communication with the anode and the cathode; and at least one product outlet, a first product stream in communication with the at least one product outlet, the first product stream including cuprite (Cu2O); a source of Fe3+ ions in communication with the first product stream; and a second product stream in communication with the first product stream, the second product stream including copper ions.
In some embodiments, the ratio of cathode surface area (cm2) to electrochemical reactor volume (mL) is above about 0.15. In some embodiments, the cathode is composed of niobium, tungsten, platinum, copper, aluminum, lead, or combinations thereof. In some embodiments, the anode is composed of niobium, tungsten, platinum, copper, aluminum, lead, or combinations thereof. In some embodiments, the cathode further comprises a bed of cathode material particles. In some embodiments, the electrochemical reactor is operated at a current density less than about 50 mA/cm2.
Some embodiments of the present disclosure relate to a system for production of copper ions. In some embodiments, the system includes a source of chalcopyrite (CuFeS2); a source of Fe3+ ions; an electrochemical reactor in communication with the source of CuFeS2 and the source of Fe3+ ions, the electrochemical reactor including an anode; a cathode; an electrolyte in communication with the anode and the cathode; a potentiostat; and at least one product outlet, and, a product stream in communication with the at least one product outlet, the product stream including copper ions, wherein the ratio of cathode surface area (cm2) to reactor volume (mL) is above about 0.15, and the potentiostat operates the electrochemical reactor at a current density less than about 50 mA/cm2. In some embodiments, a porous separator is positioned to isolate the anode from contact with the CuFeS2. In some embodiments, the anode is covered by at least one layer of filter paper. In some embodiments, the cathode is composed of niobium, tungsten, platinum, copper, aluminum, lead, or combinations thereof. In some embodiments, the anode is composed of niobium, tungsten, platinum, copper, aluminum, lead, or combinations thereof. In some embodiments, the cathode further comprises a bed of cathode material particles.
The drawings show embodiments of the disclosed subject matter for the purpose of illustration. However, it should be understood that the present application is not limited to the precise arrangements and instrumentalities shown in the drawings, wherein:
Referring now to
Referring specifically to
Still referring to
In some embodiments, the volume of electrochemical reactor 104A is any suitable size to accommodate the amount of mineral composite sample to achieve the desired product output, as will be discussed in greater detail below. In some embodiments, the ratio of cathode 112A surface area (cm2) to electrochemical reactor 104A volume (mL) is above about 0.01. In some embodiments, the ratio of cathode 112A surface area (cm2) to electrochemical reactor 104A volume (mL) is above about 0.015. In some embodiments, the ratio of cathode 112A surface area (cm2) to electrochemical reactor 104A volume (mL) is above about 0.1. In some embodiments, the ratio of cathode 112A surface area (cm2) to electrochemical reactor 104A volume (mL) is above about 0.15. In some embodiments, the ratio of cathode 112A surface area (cm2) to electrochemical reactor 104A volume (mL) is above about 0.2.
In some embodiments, electrochemical reactor 104A includes a potentiostat 116A in communication with anode 110A and cathode 112A. In some embodiments, electrochemical reactor 104A is operated at a current density less than about 300 mA/cm2. In some embodiments, electrochemical reactor 104A is operated at a current density less than about 100 mA/cm2. In some embodiments, electrochemical reactor 104A is operated at a current density less than about 50 mA/cm2. In some embodiments, electrochemical reactor 104A is operated at a current density less than about 10 mA/cm2. In some embodiments, electrochemical reactor 104A includes an electrolyte 118A in communication with anode 110A and cathode 112A. Electrolyte 118A can be any suitable electrolyte for use with the particular materials used anode 110A and cathode 112A.
In some embodiments, electrochemical reactor 104A includes a porous separator 120A. In some embodiments, porous separator 120A is configured and positioned within electrochemical reactor 104A to limit contact between the sample of the mineral composite and anode 110A. In some embodiments, porous separator 120A is configured and positioned within electrochemical reactor 104A to prevent contact between the sample of the mineral composite and anode 110A. In some embodiments, porous separator 120A includes one or more layers positioned on anode 110A. In some embodiments, porous separator 120A includes one or more layers covering one or more surfaces of anode 110A. In some embodiments, porous separator 120A includes one or more layers covering all surfaces of anode 110A. In some embodiments, porous separator 120A includes one or more layers including filter paper.
Still referring to
Without wishing to be bound by theory, system 100A facilitates electrochemical conversion of mineral composites to less refractory mineral phases, e.g., conversion of CuFeS2 through a chalcocite (Cu2S) intermediate. Specifically, CuFeS2 reacts at cathode 112A of electrochemical reactor 104A to release iron and forms an intermediate Cu2S mineral phase according to the following Reaction 1:
2CuFeS2+6H++2e−→Cu2S+2Fe2++3H2S [1]
However, allowing Cu2S to contact anode 110A leads to the formation of a covellite (CuS) mineral phase according to the following Reaction 2:
Cu2S→CuS+Cu2++2e− [2]
Covering anode 110A limits or prevents the mineral from anode contact, limiting conversion of Cu2S to CuS according to Reaction 2. Instead, a slower reaction between Cu2S and cathode 112A leads to the formation of Cu2O mineral phase according to Reaction 3:
2e−+Cu2S+2H++O2→2Cu2O+H2S [3]
Covering anode 110A showed minimal effect on the cell potential or release of iron ions into electrochemical reactor 104A. The surface of the minerals showed no significant passivation from elemental sulfur. Cu2O is more readily oxidized than CuS. Thus, copper ions are extracted from the Cu2O by an Fe3+ oxidant according to Reaction 4:
2Cu2O+8Fe3+→4Cu2++8Fe2++O2 [4]
Referring now to
X-ray Powder Diffraction (XRD) was performed to characterize the solid residues of each chalcopyrite reduction experiment.
In some embodiments, system 100A is operated continuously, semi-continuously, as a batch system, as a semi-batch system, or combinations thereof. In some embodiments, the residence time of reactants in electrochemical reactor 104A is about 10 s, 15 s, 20 s, 25 s, 30 s, 35 s, 40 s, 45 s, 50 s, 55 s, 60 s, 2 minutes, 3 minutes, 4 minutes, 5 minutes, 10 minutes, 15 minutes, 20 minutes, 25 minutes, 30 minutes, 35 minutes, 40 minutes, 45 minutes, 50 minutes, 55 minutes, 60 minutes, or greater than 60 minutes. In some embodiments, conditions in electrochemical reactor 104A are configured according to Table 1.
In some embodiments, iron concentrations of 0.1M are achieved for loading of 20 g/L of CuFeS2. Without wishing to be bound by theory, the ratio of mineral to copper product is dependent on the electrochemical reactor design (for example, the choice of anode and cathode materials). The ratio and type of mineral (covellite, chalcocite, roxbyite, etc.) will depend on other factors.
Referring now to
As discussed above, in some embodiments, electrochemical reactor 104B includes an anode 110B, a cathode 112B, and an electrolyte 118B in communication with anode 110B and cathode 112B. In some embodiments, anode 110B is composed of niobium, tungsten, platinum, copper, aluminum, lead, or combinations thereof. In some embodiments, cathode 112B further comprises a bed 114B of cathode material particles. In some embodiments, cathode 112B is composed of niobium, tungsten, platinum, copper, aluminum, lead, or combinations thereof. In some embodiments, the ratio of cathode 112B surface area (cm2) to electrochemical reactor 104B volume (mL) is above about 0.01. In some embodiments, the ratio of cathode 112B surface area (cm2) to electrochemical reactor 104B volume (mL) is above about 0.015. In some embodiments, the ratio of cathode 112B surface area (cm2) to electrochemical reactor 104B volume (mL) is above about 0.1. In some embodiments, the ratio of cathode 112B surface area (cm2) to electrochemical reactor 104B volume (mL) is above about 0.15. In some embodiments, the ratio of cathode 112B surface area (cm2) to electrochemical reactor 104B volume (mL) is above about 0.2. Electrolyte 118B can be any suitable electrolyte for use with the particular materials used anode 110B and cathode 112B.
In some embodiments, electrochemical reactor 104B includes a porous separator 120B. In some embodiments, porous separator 120B is configured and positioned within electrochemical reactor 104B to limit contact between the sample of the mineral composite and anode 110B. In some embodiments, porous separator 120B is configured and positioned within electrochemical reactor 104B to prevent contact between the sample of the mineral composite and anode 110B. In some embodiments, a porous separator 120B is positioned to isolate anode 110B from contact with the CuFeS2. In some embodiments, porous separator 120B includes one or more layers positioned on anode 110B. In some embodiments, porous separator 120B includes one or more layers covering one or more surfaces of anode 110B. In some embodiments, porous separator 120B includes one or more layers covering all surfaces of anode 110B. In some embodiments, porous separator 120B includes one or more layers including filter paper.
In some embodiments, electrochemical reactor 104B includes a potentiostat 116B. In some embodiments, potentiostat 116B operates electrochemical reactor 104B at a current density less than about 300 mA/cm2. In some embodiments, potentiostat 116B operates electrochemical reactor 104B at a current density less than about 100 mA/cm2. In some embodiments, potentiostat 116B operates electrochemical reactor 104B at a current density less than about 50 mA/cm2. In some embodiments, potentiostat 116B operates electrochemical reactor 104B at a current density less than about 10 mA/cm2.
In some embodiments, electrochemical reactor 104B includes at least one product outlet 122B. In some embodiments, system 100B includes a product stream 124B in communication with product outlet 122B. In this exemplary embodiment, product stream 124B includes a concentration of copper ions. As discussed above, CuFeS2 from source 102B reacts at cathode 112B of electrochemical reactor 104B to release iron and form an intermediate Cu2S mineral phase. The intermediate Cu2S mineral phase is then converted at cathode 112B to form a Cu2O mineral phase. The presence of Fe3+ ions from source 126B then oxidize the Cu2O mineral phase to copper ions, which can be removed from system 100B via product stream 124B. In some embodiments, system 100B is operated continuously, semi-continuously, as a batch system, as a semi-batch system, or combinations thereof. In some embodiments, the residence time of reactants in electrochemical reactor 104B is about 10 s, 15 s, 20 s, 25 s, 30 s, 35 s, 40 s, 45 s, 50 s, 55 s, 60 s, 2 minutes, 3 minutes, 4 minutes, 5 minutes, 10 minutes, 15 minutes, 20 minutes, 25 minutes, 30 minutes, 35 minutes, 40 minutes, 45 minutes, 50 minutes, 55 minutes, 60 minutes, or greater than 60 minutes.
Referring now to
At 506, the sample is provided to the electrochemical reactor. In some embodiments, the sample is first ground to a desired particle size. In some embodiments, the sample is ground to have an average particle size between about 50 μm and about 110 μm. At 508, a potential is applied between the anode and the cathode to produce a first product. In some embodiments, the electrochemical reactor is operated at a current density less than about 300 mA/cm2. In some embodiments, the electrochemical reactor is operated at a current density less than about 100 mA/cm2. In some embodiments, the electrochemical reactor is operated at a current density less than about 50 mA/cm2. In some embodiments, the electrochemical reactor is operated at a current density less than about 10 mA/cm2. In some embodiments, the first product is more suited to chemical oxidation and is further oxidized to produce a desired product. In some embodiments, the first product includes Cu2O. At 510, an oxidizing agent is applied to the first product to oxidize the first product, e.g., the Cu2O, to produce a second product. In some embodiments, the oxidizing agent includes a source of Fe3+ ions. In some embodiments, the oxidizing agent includes iron (III) sulfate hydrate. In some embodiments, the second product includes copper ions.
Electrochemical reactors consistent with embodiments of the present disclosure were prepared. The electrochemical reductions were tracked by AAS. The solid products formed are then characterized by XRD and XPS.
Chalcopyrite mineral concentrate was provided by Freeport McMoran. It was analyzed by the supplier with energy dispersion X-ray diffraction to have the following composition:
The mineral concentrate used in experimentation was sieved (−140+270 mesh) to confine the size distribution of the particles to be within 53-106 μm. The electrochemical conversion experiments were conducted in an undivided batch reactor including 50.0 mL of 1.00 M H2SO4 and 20.0 g/L of the sieved concentrate. The reactor was stirred constantly at 300 rpm and utilized a two-electrode configuration. Lead foil (Alfa Aesar) was used as the anode material, and for some trials, the lead anode was covered with Whatman filter paper of pore size 2.5 μm (Sigma Aldrich) to prevent mineral contact. Either lead foil or copper foil (Alfa Aesar) was used as the cathode material. Kapton tape (McMaster Carr) was used to confine the area of the electrodes to be 1 cm2 on either face in solution. An IviumnStat potentiostat was used to apply a constant current density of 0.3 A/cm2 between the electrodes while continuously measuring the cell potential. The current was chosen to achieve a high conversion of CuFeS2 for X-ray diffraction (XRD) and X-ray photoelectron spectroscopy (XPS) analysis.
The concentrations of Fe and Cu ions within the reactor were measured to probe the reactions over time. Upon the application of current, samples of 0.2 mL were taken from the reactor at time points of 0, 15, 30, 60, 90, 120, 150, and 180 minutes. The solid minerals within the samples were settled by centrifugation at 6000 rpm for approximately one minute. The samples were subsequently diluted with de-ionized (DI) water to lower ion concentrations to within the range of 0-4 ppm. Concentrations of the samples were measured using a Thermo Scientific iCE 30000 Series atomic absorption spectrometer (AAS). Known standards ranging from 0-4 ppm were used to construct a linear five-point calibration curve (R2>0.99) and were measured immediately before the collected samples. The fractions of Fe and Cu ions released from CuFeS2 into solution were calculated with the following Equations 1 and 2:
where XFe, cFe, PCuFeS2, WCuFeS2, and WFe represent the percent of Fe2+ released, the measured concentration of Fe2+ in solution, the pulp density of mineral concentrate initially placed in solution, the weight fraction of chalcopyrite in the mineral concentrate, and the weight fraction of Fe in CuFeS2, respectively. It was assumed that pyrite (FeS2) did not release Fe ions into solution. For some trials, a fraction of the mineral products were oxidized with iron (III) sulfate hydrate (Sigma Aldrich) to measure the release of Cu2+ ions from the products of the electrochemical reactor.
The mineral products of the electrochemical reactions were filtered from solution with a Rocker 300 vacuum pump and were subsequently allowed to air-dry for one to five hours. The solid samples were then stored in pure nitrogen or argon gas to minimize oxidation in air. The mineral products were placed on a zero-diffraction plate made of silicon crystal (MTI corporation). The solid mineral product powder was adhered in place with Apiezon grease to ensure a flat surface, consistent across the samples. A PANalytical XPert3 Powder X-ray diffractor with filtered Empyrean Cu Kα radiation (λ=0.15418 nm), operating at a tube voltage of 45 kV and current of 40 mA, was used to analyze the bulk composition of the mineral products. The mineral samples were scanned continuously in the range of 10-100° with a step size of 0.002°, on a spinning sample plate with a revolution time of 2.0 s. The intensity was recorded by a PIXcel1D detector. The XRD data were analyzed by Rietveld refinement using the software MAUD to estimate the quantitative compositions of the solids.
The mineral products, which had been protected from long term exposure to oxygen via storage in argon or nitrogen gas, were placed on PELCO Tabs™ carbon tape (Ted Pella, Inc.) in order to ensure a flat, uniform surface for XPS analysis. The elemental state of the mineral surface was measured by X-ray photoelectron spectroscopy (XPS) with a Phi 5500 XPS spectrophotometer equipped with a monochromatic Al Kα source (photon energy 1486 eV, work function 3.41, scale factor 20.0119.) Scans for S 2p3, S 2s and Cu 2p3 were recorded for the samples. The charge of each sample was corrected based on a C 1s scan for adventitious carbon. A scan rate of 655 ms per step was employed with 0.025 eV per step, and multiple scans were used when needed for greater clarity. The experimental data were fit using XPSPEAK 4.1 software in order to determine the fraction of each elemental state.
Table 3 shows the composition of the mineralogy estimated from the Rietveld refinement throughout the progression of the reactions. The fraction of CuFeS2 in the mineralogy diminished over time, at a rate which is consistent with the release of Fe ions into solution as tracked by the AAS data. Without wishing to be bound by theory, the FeS2 and SiO2 quantities did not significantly change, indicating that these minerals were unreactive during the electrochemical processing.
For the electrode arrangement of a Pb cathode and an open Pb anode, the estimated compositions show that Cu2S (with some defects) was the primary product after a duration of two hours and that CuS was the primary product after a duration of five hours. Without wishing to be bound by theory, Reaction 1 above shows that contact between CuFeS2 and the cathode material leads to the formation of Cu2S on the particle surface. Reaction 2 above shows that subsequent contact between Cu2S and the anode leads to the formation of CuS on the particle surface and the removal of a Cu2+ ion. Reaction 5 shows the well-established reaction that Cu2+ ions precipitate as CuS in the presence of H2S with fast kinetics.
Cu2++H2S→CuS+2H+ [5]
As a consequence of Reaction 5, few Cu2+ ions were measured in solution, as shown in
Referring now to
The Rietveld refinement technique was employed to estimate the compositions of the mineral products, and the results are shown in Table 3. The compositions show that Cu2S was the primary product after 3 hours and that Cu2O was the primary product after 5 hours.
X-ray photoelectron spectroscopy (XPS) was performed to determine elemental states of copper and sulfur on the minerals.
Referring now to
The atom ratio of S/Cu on the surface of the particles was calculated from the relative peak areas of the two elements. The results do not indicate that there is a passivation layer of elemental sulfur on the surface of the products, as has been postulated. Rather, the XPS spectra revealed the outer layer of the solids to be similar to the reaction products, which is consistent with a shrinking core model. When the Pb anode was open to the reactor, the S/Cu ratio on the surface of the mineral product was approximately equal to one, which is consistent with the formation of CuS. When the Pb anode was covered, the S/Cu ratio approached values significantly less than one, which is consistent with the formation of Cu2O. The S/Cu ratio did not reach zero due to the measurement of sulfur on the inert FeS2 phases within the mineral concentrate. The presence of iron on the surface could not be measured with significant intensity, which indicates that CuFeS2 is present in the bulk of the particle rather than the surface. A summary of the analysis of the XPS data is shown in Table 4.
Referring now to
Batch experiments were conducted to assess the effect of the cathode material, the applied current density, the ratio of electrode surface area to reactor volume, and the use of a separator on the electrochemical conversion of CuFeS2 to less refractory mineral phases. The electrode materials explored in this study resulted in similar faradaic efficiencies, indicating that low-cost materials such as lead or copper should be used. Low current densities and high ratios of electrode surface area to reactor volume resulted in the most efficient processing of CuFeS2. The use of a porous separator to isolate the anode from mineral contact allowed for the electrochemical formation of Cu2O, and thus improved the subsequent extraction of copper. Based on the design principles of the batch reactor experiments, a fixed bed cathode reactor was developed for the continuous electrochemical conversion of CuFeS2. The fixed bed reactor enabled rapid and relatively efficient processing of CuFeS2 concentrate and may be economically viable if scaled-up for high conversion.
Chalcopyrite mineral concentrate was kindly provided by Freeport-McMoRan. It was analyzed by the supplier with energy dispersion X-ray diffraction to have the following composition:
The mineral concentrate used in experimentation was sieved (−140+270 mesh) to confine the size distribution of the particles to be within 53-106 which is amenable to industrial practice. The sieved concentrate was rinsed with DI water followed by 1M H2SO4, followed by DI water to remove soluble iron and copper ions that were found to reside within the concentrate dust.
Samples were taken from the reactor at time points of 0, 15, 30, 60, 90, 120, 150, and 180 minutes. The solid minerals within the samples were settled by centrifugation at 6000 rpm for approximately one minute and were subsequently diluted with DI water to lower the Fe2+ concentration to be within the range of 0-4 ppm. Concentrations of Fe2+ in the diluted samples were measured with a Thermo Scientific iCE 3000 Series atomic absorption spectrometer (AAS). A linear (R2>0.99) five-point calibration curve was measured immediately before the collected samples.
The fraction of the applied current that led to Reaction 1 is defined to be the faradaic efficiency (f), which is given by Equation 3. It was assumed that one electron releases one Fe2+ ion and hence converts one CuFeS2 according to the stoichiometry of Reaction 1.
Where V represents the volume of the reactor, cFe represents the concentration of Fe2+, i represents the current density, F represents Faraday's coefficient, and t represents time.
Cu2S+2Fe3+→CuS+Cu2+2Fe2+ [6]
CuS+2Fe3+→Cu2++2Fe2++S [7]
The XRD spectra also indicate that FeS2 and silicates are inert throughout the electrochemical treatment.
Continuous treatment of CuFeS2 was conducted with an electrochemical packed bed reactor with the methodology illustrated in
where Q is the volumetric flow rate of the slurry through the reactor. The packed bed cathode surface area was an order of magnitude greater than the anode surface area; however, the electrically active area of the cathode may be limited to regions near the anode. Therefore, the current is normalized by the anode surface areas for the current densities shown. The residence time (τ) of CuFeS2 in the reactor was approximately 22 s. After approximately 160 residence times, the release of Fe2+ ions from the minerals reached a steady-state. The reason that the Fe2+ release increased and then subsequently decreased with time is not fully understood but is thought to be associated with the accumulation of minerals within the reactor. The results are promising despite the low yield due to the small residence time of 22 s. Without wishing to be bound by theory, increased residence times should provide greater CuFeS2 conversion.
The cell potential (Vcell) across the electrochemical packed bed reactor was approximately 2.5, 2.7, and 2.8 V at current densities of 17, 43, and 170 mA/cm2, respectively. The results are consistent with the batch experiments, which show that it may be desirable to process CuFeS2 at low current densities for greater faradaic and voltage efficiencies. The power requirement, which is related to electricity costs, is directly related to Vcell by Equation 5.
P=IV
cell [5]
The cost of electricity associated with CuFeS2 conversion from concentrate is approximately $0.21/kg Cu by assuming an industrial cost of electricity of $0.07/kWh, a cell potential of 2.5V, and a faradaic efficiency of 35%. However, there are additional operating costs associated with pumping the concentrate slurry.
Methods and systems of the present disclosure are advantageous to electrochemical process chalcopyrite to another mineral that can be more easily processed by hydrometallurgy while simultaneously producing copper metal, which is more environmentally sustainable. The lead cathode and covered lead anode allow for efficient and inexpensive processing of chalcopyrite by preventing the mineral from contacting the lead anode allows for further conversion into a copper-oxide mineral phase. The cost of this technique is comparable to industry standards, and moreover, has a much smaller environmental footprint than heat-based copper extraction. In all, this technology provides a safe, affordable way to extract copper from chalcopyrite, regardless of the quality of the ore. A preliminary cost analysis suggests that the total cost is approximately $6.2 per kg of copper, which makes the process competitive with industrial standards. Thus, the present disclosure represents a means of increased domestic production of copper, using a process that can probably more easily exploit renewables.
Although the disclosed subject matter has been described and illustrated with respect to embodiments thereof, it should be understood by those skilled in the art that features of the disclosed embodiments can be combined, rearranged, etc., to produce additional embodiments within the scope of the invention, and that various other changes, omissions, and additions may be made therein and thereto, without parting from the spirit and scope of the present invention.
This application claims the benefit of U.S. Provisional Application No. 63/058,544, filed Jul. 30, 2020, which is incorporated by reference as if disclosed herein in its entirety.
This invention was made with government support under grant no. DGE 1644869 awarded by the National Science Foundation. The government has certain rights in the invention.
Number | Date | Country | |
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63058544 | Jul 2020 | US |