Mineralogical and Chemical Changes after Reduction Roasting of Xinjiang Iron Ore, China

: The mineralogical and chemical changes in Chinese Xinjiang iron ore containing impurities, lead, and zinc as a result of reduction roasting were studied via chemical analysis, optical microscopy, X-ray ﬂuorescence (XRF), electron probe microanalysis (EPMA), and energy-dispersive spectroscopy (EDS). Analysis showed that hematite was the main iron-bearing mineral, with small amounts of magnetite and iron silicate; lead impurities were mainly lead oxide and lead–iron alum, while zinc oxide was the main zinc impurity. X-ray ﬂuorescence analysis for raw samples indicated the presence of quartz, hematite, magnetite, chlorite, calcite, and dolomite. The results of the analysis of roasted samples showed an increase in hematite at temperatures of 750 ◦ C and 950 ◦ C, while the elemental iron increased at a temperature of 1200 ◦ C, along with the conversion of galena to lead oxide and sphalerite to zinc oxide, with a stable quartz ratio. The chemical analysis of the raw sample showed that the TFe grade of the sample was 47.04%, while the contents of harmful Pb and Zn impurities were 0.39% and 0.30%, respectively, both of which exceed the index (less than 0.10%) required by the iron industry for raw materials. The content of harmful sulfur impurities was also high, at 1.19%, which needs to be eliminated or reduced. The results of EPMA and EDS analysis of pre-roasting raw samples showed that chemical compositions vary in different locations in the hematite, magnetite, sphalerite, and galena micro-zones. It has also been observed that quartz is mostly diffused with magnetite and hematite, and sulfur appears in small quantities in most regions. The analysis after roasting showed that the percentages of lead, zinc, and sulfur impurities decreased by a large rate. It is clear that the roasting process plays a major role in removing impurities such as sulfur, which appears in a small percentage after the roasting process, and also helps in oxidizing the impurities of lead and zinc, which helps in removing them.


Iron Ore
Iron is one of the most common elements in the world, and forms 5.6% of the Earth's crust [1]. China is one of the largest producers of iron ore, where in 2012 the iron ore production amounted to 1.3 billion tons, representing~45% of global production [2]. Iron is one of the most abundant minerals, and the most ores in which iron is found are:: magnetite (Fe 3 O 4 ), hematite (Fe 2 O 3 ), siderites (FeCO 3 ), or limonite (2Fe 2 O 3 ·3H 2 O) [3,4].

Geological Characterization of Xinjiang Iron Ore
The Xinjiang Uygur region occupies about 1/6 of the total land area in China; it is located in northwest China, where many deposits of gold, copper, iron, zinc, and lead have

Impurities in Iron Ore
Blast furnace slag usually contains Zn, C, CaO, S, Pb, Cd, Cr, As, and alkali metals (K, Na, etc.) [7]. These elements are associated with iron ores of various kinds, which represent the basic use of furnaces. Cu, Ni, Cr, Cd, Pb, and Zn are among the most common heavy metal contaminants of industrial pollution [8,9]. Impacts of impurities are shown according to environmental risk indicator for heavy metals, as follows: Cd > Zn > Cu > As > Pb [10]. It has been found that the sequence of harmful elements entering the smelting furnace is K > Na > Zn > Pb [11].
Impurities of Pb and Zn are present in iron, and form complex ores, which are difficult to remove at high temperatures. These impurities lead to a decrease in iron productivity [6], which seriously affects the lifetime of blast furnaces and the benefits of ironmaking [12]. These impurities are easy to reduce or oxidize, and can expand and form lead-containing precipitations and zinc-containing dust, seriously affecting the production of the blast furnace. At present, problems related to the use and recycling of mineral waste are common in all integrated steel mills. The continued emphasis of environmental regulations on landfills and their storage has made the effective management of these wastes a high priority [13]. Direct recycling of the iron waste in the blast furnace (BF) is impeded by its chemistry (0.1% Zn in the charge), as well as by the presence of lead [7]. For effective continuous recycling of iron units, it is necessary to identify their sources, determine their structure, and develop a suitable device/technology for the processing of zinc and lead [14].
Although the iron content of the ore is relatively high in Xinjiang, Yunnan, Guizhou, and other remote iron-ore-producing areas in the west of China, many iron ore areas contain lead and zinc impurities, and the content of lead and zinc in some ores is relatively high [11].
Through a previous study conducted on the effects of lead and zinc impurities on the iron industry, and methods of their removal, it was found that most of the removal methods take place after the iron production. Thus, we decided to conduct experiments to clarify the effect of separation before the iron production.

Experimental
A sample with a size of~100 mm was taken from an iron mine in the Xinjiang Uygur Autonomous Region, China; its appearance was reddish-brown. The three-stage and closed crushing processes were used to reduce the size. The appropriate amount of the sample to be observed was cut and polished to form a light sheet under a Nikon Lv100pol polarized The microstructure and microelemental composition of the sample were analyzed with an electronic probe microanalyzer (EPMA) along with a spectrometer manufactured by JEOL Ltd., model number JXA-8230/ INCAX-ACT (energy-dispersive spectrometer) Made in Japan Electronics Co., Ltd. [15].
EPMA techniques offer the option of identifying and investigating phases and segregations of a sample material [16]. These techniques are focused on analyzing the microstructure and microelemental composition of samples from the Xinjiang region by electron microscope. The constituent elements were determined by the characteristic wavelength of each element in both raw and roasted samples.
Reduction roasting is now a subject of interest in treating many low-grade ores [17]. Several factors affect roasting processes, such as temperature, time, and usage of carbon in iron recovery. Thus, these roasting conditions must be optimized and controlled [18,19]. The recovery of iron is influenced by the time of roasting [20]. As can be seen, the time of roasting, temperature, and flow rate have significant effects on the decomposition of zinc ferrite [21]. Reduction roasting was used to study changes in metal properties, and to examine the effects of removing lead and zinc impurities from Xinjiang iron ore.
Magnetization reduction roasting/weak magnetic separation is an effective method to treat difficult-to-select hematite. High-temperature reduction roasting is used to directly reduce Fe 2 O 3 in the ore to magnetic iron, or even elemental iron. Due to the strong magnetism of artificial magnetite and elemental iron, they are separated from the gangue minerals by grinding and dissociating, and the method of weak magnetic separation is used to obtain reduced iron ore powder mainly composed of magnetite or elemental iron. The reaction principle depends on the reduction temperature; from low to high, the reduction occurs in the order of Fe 2 O 3 →Fe 3 O 4 →FeO→Fe. At the same time, the lead and zinc impurities contained in iron ore will simultaneously undergo oxidation and reduction reactions during the roasting process. Although the boiling points of elemental lead and zinc are 1749 • C and 907 • C, respectively, when the temperature is low, elemental lead is highly volatile, and flows away with the air.
Each ore sample was weighed to 40 g with a 0.01 g balance, mixed with coal powder, and then the mixture was placed a quartz crucible and covered to maintain a sufficient reducing atmosphere. The sample crucible was placed in a high-temperature furnace to perform a reduction test, and the temperature was set to increase to 750 • C; after the roasting reaction was completed, the sample was taken out and quickly quenched, before being dried at a low temperature (60 • C). A portion of the sample was taken and ground to~0.037 mm, accounting for 90%, and the magnetic field strength was 120 kA/m. Subsequently, magnetic separation was performed to obtain the corresponding sorting products. The same experiment was conducted for other temperatures. Table 1 shows the total iron (TFe), along with the contents of harmful Pb and Zn impurities, which exceed the index of 0.10% required from raw materials in the iron industry. The content of harmful sulfur impurities is also high, and needs to be eliminated or reduced, as do the contents of the gangue mineral components SiO 2 and Al 2 O 3, Chemical analysis was carried out via AAS and ICP-MS. Through the microscopic analysis, we found that the main minerals in the ore were magnetite, hematite, goethite FeO (OH), and limonite. Magnetite (Mt) accounted for~15%, with a semi-self-shaped structure (Figure 1a,b). We also observed small amounts of pyrite, sphalerite, pyrrhotite, spinel, and natural iron. Pyrite (Py) accounted for~1%, with a self-formed or semi-self-shaped granular structure. Pyrrhotite (Po) was also present in a small amount, with an irregular granular shape that is replaced by limonite along the edges (Figure 1c,d).

Iron Ores
Through the microscopic analysis, we found that the main minerals in the ore were magnetite, hematite, goethite FeO (OH), and limonite. Magnetite (Mt) accounted for ~15%, with a semi-self-shaped structure (Figure 1a,b). We also observed small amounts of pyrite, sphalerite, pyrrhotite, spinel, and natural iron. Pyrite (Py) accounted for ~1%, with a selfformed or semi-self-shaped granular structure. Pyrrhotite (Po) was also present in a small amount, with an irregular granular shape that is replaced by limonite along the edges (Figure 1c,d).

Lead/Zinc Impurities
Microscopically, a small amount of galena (Gn) was distributed in an irregular, granular fashion along the transparent mineral grains in the rock fissures; as shown in Figure  2a, this exists as a filling structure. Sphalerite occurs in irregular granular form, and chalcopyrite (Ccp) is especially found within sphalerite in opaque form (Figure 2b), showing solid solution decomposition structure, and metasomatizing magnetite and hematite. Although the phase analysis of lead and zinc shows that more than 90% of the impurities of lead and zinc exist in oxidized forms, no crystalline minerals with oxidized states of lead

Lead/Zinc Impurities
Microscopically, a small amount of galena (Gn) was distributed in an irregular, granular fashion along the transparent mineral grains in the rock fissures; as shown in Figure 2a, this exists as a filling structure. Sphalerite occurs in irregular granular form, and chalcopyrite (Ccp) is especially found within sphalerite in opaque form (Figure 2b), showing solid solution decomposition structure, and metasomatizing magnetite and hematite. Although the phase analysis of lead and zinc shows that more than 90% of the impurities of lead and zinc exist in oxidized forms, no crystalline minerals with oxidized states of lead and zinc were found under the microscope. The results of microscopic identification show that the oxidation of the ore is more intense in the later stage; the mineralization of limonite (iron cap) is intense, and the suspected oxidation state of lead and zinc may be sporadically distributed in oxidation zones such as limonite, showing the characteristics of metasomatism or residual leaching. The suspected areas containing lead and zinc oxide were delineated under the microscope and then scanned by EMPA and EDS, before being analyzed and identified by microanalysis. and zinc were found under the microscope. The results of microscopic identification show that the oxidation of the ore is more intense in the later stage; the mineralization of limonite (iron cap) is intense, and the suspected oxidation state of lead and zinc may be sporadically distributed in oxidation zones such as limonite, showing the characteristics of metasomatism or residual leaching. The suspected areas containing lead and zinc oxide were delineated under the microscope and then scanned by EMPA and EDS, before being analyzed and identified by microanalysis.

Roasted Sample
Through microscopic analysis of samples roasted at different temperatures, the percentages of the main minerals vary with temperature, as do the percentages of impurities. The first sample was roasted at 750 °C for 60 min, and then a microscopic study was conducted, the results of which showed that the main minerals in the sample were magnetite, hematite, fullerene, and limonite, with small amounts of pyrite, sphalerite, galena, and chalcopyrite ( Figure 3a).
Magnetite accounts for 12 vol.%, and appears in a semi-automorphic to allomorphic granular form, with the particle size ranging between ~0.002 and 0.2 mm. Hematite (Hem) (~36%) has a semi-automorphic to allomorphic granular structure, with fine acicular crystal morphology and a particle size between 0.002 and 0.1 mm. Sphalerite (Sp) is irregularly distributed, with a particle size between 0.002 and 0.01 mm. Galena (Gn) has an irregular granular distribution in transparent minerals, with particle size between 0.002 and 0.01 mm.

Roasted Sample
Through microscopic analysis of samples roasted at different temperatures, the percentages of the main minerals vary with temperature, as do the percentages of impurities. The first sample was roasted at 750 • C for 60 min, and then a microscopic study was conducted, the results of which showed that the main minerals in the sample were magnetite, hematite, fullerene, and limonite, with small amounts of pyrite, sphalerite, galena, and chalcopyrite ( Figure 3a). analyzed and identified by microanalysis.

Roasted Sample
Through microscopic analysis of samples roasted at different temperatures, the percentages of the main minerals vary with temperature, as do the percentages of impurities. The first sample was roasted at 750 °C for 60 min, and then a microscopic study was conducted, the results of which showed that the main minerals in the sample were magnetite, hematite, fullerene, and limonite, with small amounts of pyrite, sphalerite, galena, and chalcopyrite ( Figure 3a).
Magnetite accounts for 12 vol.%, and appears in a semi-automorphic to allomorphic granular form, with the particle size ranging between ~0.002 and 0.2 mm. Hematite (Hem) (~36%) has a semi-automorphic to allomorphic granular structure, with fine acicular crystal morphology and a particle size between 0.002 and 0.1 mm. Sphalerite (Sp) is irregularly distributed, with a particle size between 0.002 and 0.01 mm. Galena (Gn) has an irregular granular distribution in transparent minerals, with particle size between 0.002 and 0.01 mm.  Magnetite accounts for 12 vol.%, and appears in a semi-automorphic to allomorphic granular form, with the particle size ranging between~0.002 and 0.2 mm. Hematite (Hem) (~36%) has a semi-automorphic to allomorphic granular structure, with fine acicular crystal morphology and a particle size between 0.002 and 0.1 mm. Sphalerite (Sp) is irregularly distributed, with a particle size between 0.002 and 0.01 mm. Galena (Gn) has an irregular granular distribution in transparent minerals, with particle size between 0.002 and 0.01 mm.
The second sample was roasted at 900 • C for 60 min; the main minerals in the sample were hematite, fullerene, and pyrite, along with small amounts of sphalerite, galena, smithsonite, limonite, and copper blue.
Hematite (Hem) accounts for~5%, with a semi-automorphic to allomorphic granular structure, fine tabular crystals, and a particle size of 0.002-0.1 mm.
FeO accounts for 65%, appearing as an irregular granular structure, strongly metasomatic with hematite and magnetite, and partially metasomatic with pyrite, limonite, etc., in angular, veinlet, or inclusion structures, with a particle size ranging from 0.002 to 0.1 mm.
Sphalerite (Sp) is very small, and has an irregular granular distribution in transparent minerals, with a particle size of 0.002~0.03 mm.
Galena (Gn) appears in trace amounts with irregular granular distribution in transparent minerals, occasionally associated with sphalerite; its particle size ranges between 0.002 and 0.02 mm.
Limonite (Lm) accounts for~3%, and has an irregular, granular, metasomatic distribution along the gap or fracture of pyrite and fullerene particles; the aggregate size is from 0.002 to 0.1 mm (Figure 4).
Hematite (Hem) accounts for ~5%, with a semi-automorphic to allomorphic granular structure, fine tabular crystals, and a particle size of 0.002-0.1 mm.
FeO accounts for 65%, appearing as an irregular granular structure, strongly metasomatic with hematite and magnetite, and partially metasomatic with pyrite, limonite, etc., in angular, veinlet, or inclusion structures, with a particle size ranging from 0.002 to 0.1 mm.
Sphalerite (Sp) is very small, and has an irregular granular distribution in transparent minerals, with a particle size of 0.002~0.03 mm.
Galena (Gn) appears in trace amounts with irregular granular distribution in transparent minerals, occasionally associated with sphalerite; its particle size ranges between 0.002 and 0.02 mm.
Limonite (Lm) accounts for ~3%, and has an irregular, granular, metasomatic distribution along the gap or fracture of pyrite and fullerene particles; the aggregate size is from 0.002 to 0.1 mm (Figure 4). The third sample was roasted at 1200 °C for 60 min; the main minerals in the sample were natural copper, magnetite, galena, limonite, etc., with more carbonaceous residues.
Magnetite (Mt) appears in small amounts, in a semi-automorphic to allomorphic granular form, distributed among the transparent mineral particles, and may be formed by recrystallization; the particle size is between 0.002 and 0.1 mm.
Elemental iron (Fe) accounts for ~58%; it is obviously formed by recrystallization, with a smooth edge. The aggregate particle size is between 0.002 and 0.3 mm.
Galena (Gn) appears in trace quantities, showing an irregular granular distribution in transparent minerals, with a particle size ranging between 0.002 and 0.01 mm.
Limonite (Lm) account for ~2%, with an irregular granular structure, along with the natural iron ball; the aggregate size ranges from 0.002 to 0.05 mm ( Figure 5). The third sample was roasted at 1200 • C for 60 min; the main minerals in the sample were natural copper, magnetite, galena, limonite, etc., with more carbonaceous residues.
Magnetite (Mt) appears in small amounts, in a semi-automorphic to allomorphic granular form, distributed among the transparent mineral particles, and may be formed by recrystallization; the particle size is between 0.002 and 0.1 mm.
Elemental iron (Fe) accounts for~58%; it is obviously formed by recrystallization, with a smooth edge. The aggregate particle size is between 0.002 and 0.3 mm.
Galena (Gn) appears in trace quantities, showing an irregular granular distribution in transparent minerals, with a particle size ranging between 0.002 and 0.01 mm.
Limonite (Lm) account for~2%, with an irregular granular structure, along with the natural iron ball; the aggregate size ranges from 0.002 to 0.05 mm ( Figure 5).

XRF of Raw Sample
The main metallic minerals in the ore were hematite (Fe2O3), limonite, and magnetite, with small amounts of pyrite, sphalerite (Zn, Fe) S, and galena PbS, and traces of pyrrhotite, chalcopyrite, tetrahedrite, and copper blue. The content of transparent minerals was ~28-30%, and the main component in it was quartz. The main mineral compositions and their contents are shown in Table 2.

XRF of Raw Sample
The main metallic minerals in the ore were hematite (Fe 2 O 3 ), limonite, and magnetite, with small amounts of pyrite, sphalerite (Zn, Fe) S, and galena PbS, and traces of pyrrhotite, chalcopyrite, tetrahedrite, and copper blue. The content of transparent minerals was 28-30%, and the main component in it was quartz. The main mineral compositions and their contents are shown in Table 2.  Table 3 represents the results of XRF analysis for roasted samples at 750 • C, 900 • C, and 1200 • C. The results of the analysis show that the main metallic minerals in the roasted samples were hematite and total iron (TFe), with small amounts of sphalerite, galena, manganese oxide, and chalcopyrite, in addition to the presence of quartz in large percentages.

Phase Properties of Iron Ores and Lead/Zinc Minerals
Phases with specific physical and chemical properties in the material, and the phase state of the mineral, are the important factors that normally affect the beneficiation method and technical indicators. Therefore, the results of the phase analysis of iron-bearing minerals and harmful lead/zinc mineral impurities are shown in Tables 4-6.  Iron in the sample mainly exists in the form of hematite, with an iron content of 42.97%, and a distribution rate of 91.35% of the total iron, followed by magnetite with 1.89% and iron silicate (Fe 2 O 4 Si) with 2.01%, while iron sulfide and iron carbonate are present in minor amounts. Hematite and magnetite are the main sources of iron in the separation process, with a proportion of 95.37%. Lead-containing impurities are mainly present in the form of lead oxide and jarosite, accounting for 49.03% and 41.29%, respectively, for a total of 90.32%; meanwhile, zinc oxide is the main zinc-containing impurity, accounting for 90.60%. Lead in zinc sulfide is less, accounting for 7.23% and 5.71%. Because the existence of lead and zinc impurities is harmful to the iron-making process, it is expected that most sulfur can be removed at the same time as removing lead and zinc impurities.

Electron Probe Microanalysis (EPMA)
The results of the analysis are shown in the pictures below. Tables 7-12 show values for points taken at the level of ore samples and samples after roasting. Each metal in the samples appears in a different color and different grain gradation.  The analysis was performed for the first samples that appear in Figures 6-11. For each sample in the Figure 6 Tables 7-9 show the weight percentages of the elements that were identified in the survey areas.  Tables 7-9 show the weight percentages of the elements that were identified in the survey areas.

Roasted Samples
EPMA analysis of roasted samples was carried out after the roasting process in order to determine the elements present in the samples. The results are shown below and in Figure 12. The roasting temperature for the sample was 750 • C for 60 min. The area specified in the circle in Figure 12a is the area corresponding to the element mapping analyses, while the area in Figure 12b was selected for the spot analyses at 90 µm, and this region represents the presence of galena and limonite, as shown in the results of the microscopic analysis.
Elemental distribution map observed by EPMA for area 4 is shown in Figure 13. EPMA analysis of a sample that was taken at a roasting temperature of 900 • C for 60 min, is shown in Figure 14. Figure 15 represents analysis for area 5. Further, another sample was roasted at 1200 • C for 60 min, and EPMA analysis was performed; the results are shown in Figure 16. In the end, Figure 17 represents analysis for area 6.   EPMA analysis of roasted samples was carried out after the roasting process in order to determine the elements present in the samples. The results are shown below and in Figure 12. The roasting temperature for the sample was 750 °C for 60 min. The area specified in the circle in Figure 12a is the area corresponding to the element mapping analyses, while the area in Figure 12b was selected for the spot analyses at 90 μm, and this region represents the presence of galena and limonite, as shown in the results of the microscopic analysis. Elemental distribution map observed by EPMA for area 4 is shown in Figure 13. EPMA analysis of a sample that was taken at a roasting temperature of 900 °C for 60 min, is shown in Figure 14. Figure 15 represents analysis for area 5. Further, another sample was roasted at 1200 °C for 60 min, and EPMA analysis was performed; the results are shown in Figure 16. In the end, Figure 17 represents analysis for area 6.
In Figures 13, 15, and 17 the presence of zinc (Zn), lead (Pb), iron (Fe), copper (Cu), oxygen (O), sulfur (S), and silicon (Si) were highlighted. The values in Tables 10-12 show the weight percentages of the elements that were observed in the survey areas. Elemental distribution map observed by EPMA for area 4 is shown in Figure 13. EPMA analysis of a sample that was taken at a roasting temperature of 900 °C for 60 min, is shown in Figure 14. Figure 15 represents analysis for area 5. Further, another sample was roasted at 1200 °C for 60 min, and EPMA analysis was performed; the results are shown in Figure 16. In the end, Figure 17 represents analysis for area 6.
In Figures 13, 15, and 17 the presence of zinc (Zn), lead (Pb), iron (Fe), copper (Cu), oxygen (O), sulfur (S), and silicon (Si) were highlighted. The values in Tables 10-12 show the weight percentages of the elements that were observed in the survey areas.                 Tables 10-12 show the weight percentages of the elements that were observed in the survey areas.
During reduction roasting, hematite was reduced to magnetite through a solid-state reaction, and the particle sizes of Fe-bearing minerals showed no significant differences before and after roasting. In comparison, deep reduction achieved the full reduction of hematite into metallic iron, and promoted the increase in the particle size of metallic iron.  During reduction roasting, hematite was reduced to magnetite through a solid-state reaction, and the particle sizes of Fe-bearing minerals showed no significant differences before and after roasting. In comparison, deep reduction achieved the full reduction of hematite into metallic iron, and promoted the increase in the particle size of metallic iron.
The corresponding chemical reactions are as shown in Equations (1)-(3). At the same time, the lead and zinc impurities contained in iron ore will simultaneously undergo oxidation and reduction reactions during the roasting process, as shown in Equations (4)- (8).
Although the boiling points of elemental lead and zinc are 1749 °C and 907 °C, respectively, when the temperature is low, elemental lead is highly volatile, and flows away with the air. The sulfide of zinc is first converted to oxides, and then reduced to gaseous zinc in the high-temperature zone above 1000 °C, and enters the gas system. Alternatively, lead and zinc are dissolved in the water-quenching liquid to achieve the purpose of removing harmful impurities.
When the temperature is greater than 570 °C, the reaction as shown in Equation (1) begins: When the temperature is greater than 1000 °C, the main chemical reactions that occur are as follows: FeO + CO→Fe + CO2 When the calcination temperature is 500~800 °C, the oxidation reaction will occur first, and then the reduction reaction will occur: PbO + CO = Pb + CO2 If the reduction temperature reaches 950 °C: The corresponding chemical reactions are as shown in Equations (1)-(3). At the same time, the lead and zinc impurities contained in iron ore will simultaneously undergo oxidation and reduction reactions during the roasting process, as shown in Equations (4)- (8).
Although the boiling points of elemental lead and zinc are 1749 • C and 907 • C, respectively, when the temperature is low, elemental lead is highly volatile, and flows away with the air. The sulfide of zinc is first converted to oxides, and then reduced to gaseous zinc in the high-temperature zone above 1000 • C, and enters the gas system. Alternatively, lead and zinc are dissolved in the water-quenching liquid to achieve the purpose of removing harmful impurities.
When the temperature is greater than 570 • C, the reaction as shown in Equation (1) When the calcination temperature is 500~800 • C, the oxidation reaction will occur first, and then the reduction reaction will occur: PbO + CO = Pb + CO 2 If the reduction temperature reaches 950 • C: When the temperature is above 1000 • C: ZnO + C=Zn + CO ZnO + Fe = Zn + FeO (8)

EDS Analysis
In order to examine the elemental compositions and equivalent contents in "microzones" of the scanning areas, EDS was carried out to conduct energy spectrum analysis for the micro-zones of hematite, magnetite, sphalerite, chalcopyrite, quartz, and galena. Tables 8-10, the surfaces show high contents of lead, zinc, manganese, quartz, and sulfur, meaning that they represent the main impurities identified in hematite and magnetite. This constant is also observed in Figure 18b,c, where the peaks of lead, zinc, manganese, sulfur, and silicon are found.

According to analysis results by EDS in
ZnO + Fe = Zn + FeO (8)

EDS Analysis
In order to examine the elemental compositions and equivalent contents in "microzones" of the scanning areas, EDS was carried out to conduct energy spectrum analysis for the micro-zones of hematite, magnetite, sphalerite, chalcopyrite, quartz, and galena.
According to analysis results by EDS in Tables 8-10, the surfaces show high contents of lead, zinc, manganese, quartz, and sulfur, meaning that they represent the main impurities identified in hematite and magnetite. This constant is also observed in Figure 18b,c, where the peaks of lead, zinc, manganese, sulfur, and silicon are found. It should be noted that the percentages of sulfur, lead, and zinc decreased significantly after roasting, as shown in Tables 10-12 and the EDS curves shown in Figure 18df, while the percentages of impurities decreased whenever the roasting temperature increased from 750 °C to 1200 °C.

Effects of Reduction Roasting Temperature
To determine the optimal reduction roasting temperature, the refractory iron ore containing lead and zinc was reduced at various temperatures between 750 °C and 1200 °C, while keeping other process parameters constant; the amount of reducing agent was 11% under low-temperature conditions (the molar ratio of C:O selected during the high-temperature stage was 1.5), and the reduction roasting time was 1 h. The effects of the reduction roasting temperature on the iron recovery are presented in Figure 19. It should be noted that the percentages of sulfur, lead, and zinc decreased significantly after roasting, as shown in Tables 10-12 and the EDS curves shown in Figure 18d-f, while the percentages of impurities decreased whenever the roasting temperature increased from 750 • C to 1200 • C.

Effects of Reduction Roasting Temperature
To determine the optimal reduction roasting temperature, the refractory iron ore containing lead and zinc was reduced at various temperatures between 750 • C and 1200 • C, while keeping other process parameters constant; the amount of reducing agent was 11% under low-temperature conditions (the molar ratio of C:O selected during the hightemperature stage was 1.5), and the reduction roasting time was 1 h. The effects of the reduction roasting temperature on the iron recovery are presented in Figure 19.
It can be seen from Figure 19 that the reduction roasting temperatures of 800 • C and 1200 • C obtained better iron recovery, and the magnetic separation concentrates of the iron grade and iron recovery were 56.66%, 90.51% and 92.39%, 76.86%, respectively. The reduction roasting temperature has a greater impact on the iron grade and iron recovery rate of the magnetic separation concentrates. As the reduction roasting temperature increases, the concentration of carbon monoxide in the system continuously increases, and the iron oxide is gradually reduced to elemental iron, which makes the iron grade of the magnetic separation concentrate continuously increase.