Hydrothermal Conversion of Red Mud into Magnetic Adsorbent for E ff ective Adsorption of Zn ( II ) in Water

Red mud, a Fe-rich waste generated from the aluminum industry, was recovered as an adsorbent for wastewater treatment. The separation process of red mud from water after adsorption, including centrifugation and filtration, was complicated. This study demonstrated an alternative option to recycle red mud for preparing magnetic adsorbent via a facile hydrothermal route using ascorbic acid as reductant. Red mud is weakly magnetized and consists of andradite, muscovite, hematite, and cancrinite. After hydrothermal treatment, andradite in red mud was reductively dissolved by ascorbic acid, and transformed into magnetite and morimotoite. With increasing hydrothermal temperature, the dissolution of andradite accelerated, and the crystallite size of magnetite increased. When the hydrothermal temperature reached 200 ◦C, the prepared adsorbent P-200 showed a desirable saturation magnetization of 4.1 Am2/kg, and could be easily magnetically separated from water after adsorption. The maximum adsorption capacity of P-200 for Zn2+ was 89.6 mg/g, which is eight-fold higher than that of the raw red mud. The adsorption of Zn2+ by P-200 fitted the Langmuir model, where cation exchange was the main adsorption mechanism. The average distribution coefficient of Zn2+ at low ppm level was 16.81 L/g for P-200, higher than those of the red mud (0.3 L/g) and the prepared P-120 (1.48 L/g) and P-270 (5.48 L/g), demonstrating that P-200 had the best adsorption capacity for Zn2+ and can be served as a practical adsorbent for real-world applications. To our knowledge, this is the first study to report the conversion of red mud into a magnetic adsorbent under mild conditions.


Introduction
Red mud is a solid waste and abundantly produced from the treatment of bauxite with sodium hydroxide during Al extraction.For 1 ton of alumina extracted, approximately 1 to 2 tons of red mud residual is produced [1].Due to its high calcium and sodium hydroxide contents, red mud is relatively toxic and causes severe environmental pollution and ecological damage [2].Thus, safe disposal methods have been developed for red mud (including dewatering, drying, and landfilling [3]), which cause additional cost and require regular management.
The resource utilization of red mud could solve its disposal problems [4][5][6][7][8].Recently, research has focused on utilizing red mud for the removal of toxic heavy metals [9], phosphate [10], and harmful organics [11].Sahu et al. [9] investigated the pretreatment of red mud by a combined method of CO 2 neutralization and calcining at 500 • C, and found that the pretreated red mud showed high adsorption capacity of Zn 2+ (14.9 mg/g).Wang et al. [10] reported that after hydrochloric acid neutralization, the neutralized red mud exhibited higher adsorption capacity for phosphate (108.6 mg/g) than untreated red mud.However, the separation process of red mud from water after adsorption, including high-speed centrifugation, precipitation, coagulation and/or filtration [5,9,10], was tedious, which limited its application for wastewater treatment.An optimal method to rapidly separate red mud from water was to convert weakly magnetized red mud into magnetically separated adsorbent.
The Fe oxides in red mud can be converted into magnetic magnetite after roasting under addition of pyrite [12], coal [13], or by injecting H 2 [14] and methane [15].Liu et al. [12] reported that part of the Fe oxides in red mud was converted into magnetite with pyrite as exogenous ferrous and reducing regent after calcination at 600 • C. Samouhos et al. [14] reported that 87% of the hematite (Fe 2 O 3 ) in red mud was transformed into magnetite after roasting at 480 • C using H 2 as reductant.However, high temperatures were applied in these methods to promote the breakdown of the Fe-O-Si or Fe-O-Al bonds into the form of Fe-O-Fe linkage [16].The breakdown of Fe-O-Si or Fe-O-Al bonds can be achieved at low temperature [17].For instance, by adding iron powder, red mud could be converted to magnetite-containing materials after hydrothermal treatment at 260 • C [18].However, the obtained magnetite was probably generated from the oxidation of iron powder.Iron-bearing minerals, such as andradite and hematite [6], were abundant in red mud, and can be converted into magnetic minerals by adding reductants under mild condition.However, the phase transformation of Fe-bearing minerals in red mud has not yet been studied.
In this study, red mud was converted into magnetic adsorbent via a facile hydrothermal route using ascorbic acid as reductant.To demonstrate the potential applications of red mud, the ability of the synthesized magnetic adsorbent to remove Zn 2+ from water was investigated.

Synthesis of Magnetic Adsorbent
Approximately 1 g of dry red mud was dispersed in 30 mL 4 mol/L NaOH to form a brownish suspension.Ascorbic acid was then dumped into the suspension at a molar ratio of ascorbic acid to iron of 2in the red mud.The suspension was magnetically stirred for 10 min, and then transferred to a Teflon kettle to heat at 120 • C for 10 h.After cooling down to room temperature, the precipitate was collected and then washed five times with deionized water, followed by vacuum-drying at 50  24 h.The obtained sample was named P-120.The controls were conducted according to the procedures as described above.In the controls, the hydrothermal temperature was changed from 120 • C to 200 • C and 270 • C, and the obtained adsorbents were denoted P-200 and P-270, respectively.

Adsorption Experiment
The adsorption performances of red mud and the prepared adsorbents were investigated using Zn 2+ as target.Stock solutions with Zn 2+ concentrations in the range of 0-120 mg/L were prepared, and adjusted to pH 4 by adding 5% NaOH and 5% HCl.20 mL stock solution was mixed with 0.01 g adsorbent in a series of triangular flasks.The flasks were placed in an incubator (THZ-98C, Shanghai Yiheng) and then shaken at shaken at 150 rpm for 12 h.After adsorption, the obtained magnetic adsorbents P-200 and P-270, respectively, were magnetically separated, while red mud and P-120 were centrifuged at 5500 rpm for 5 min.The concentration of Zn 2+ in the supernatant was measured by an inductively coupled plasma emission spectrometer (ICP-OES, Avio 200, PerkinElmer, USA).
The adsorbed amount (q e1 , mg/g) of Zn 2+ was calculated via Equation (1): where C 1 and C e1 represent the initial Zn 2+ concentration and the equilibrium concentration (mg/L) after adsorption, V represents the solution volume (L), and m 1 represents the adsorbent weight (g).The Na + concentration in the supernatant was measured using an ion chromatograph (883 Basic, Metrohm, Switzerland) coupled with a C4 cation column (Metrohm, Switzerland).The released amount (q e2 , mg/g) of Na + was calculated via Equation (2): where C 2 and C e2 represent the initial concentration of Na + in the solution and the equilibrium concentration after adsorption (mg/L).

Surface Site Concentration
The adsorption of Zn 2+ on red mud and P-120, P-200, and P-270 was related to the concentration of surface coordination sites of these adsorbents.The surface site concentrations (H s ) were measured by a potentiometric titrator (ZDJ-4A, Leici, China).In the titration experiments, 0.1 g of the adsorbents was mixed with 50 mL of 0.01 mol/L NaNO 3 in a conical flask, followed by bubbling with pure N 2 .After that, the pH value of the solution was adjusted to 4 with 0.6 mol/L nitric acid, and then back-titrated to approximately 10 with 0.3 mol/L NaOH.
When nitric acid was added to the solution, a cationic exchange reaction between the H + in the solution and the coordinated cations (denoted as Me, e.g., Na + , K + , Ca 2+ , and Mg 2+ ) on the surface coordination sites ≡SO − (S represents Fe, Si, or Al) of the adsorbents occurred as shown in Equation (3).Thus, part of the free H + was associated with the coordination sites of the adsorbent.By adding NaOH, the free H + in the liquid fraction was first neutralized with OH − , and then, the coordinated H + on the surface sites ≡SO − of the adsorbents was replaced by cationic Na + via cationic exchange (Equation ( 4)).Finally, the pH of the solution increased due to the addition of overdosed NaOH: The Gran function value (denoted as G) was calculated via Equations ( 5) and ( 6): Under alkaline conditions, G = ( where V 0 , V 1 , and V 2 represent the volume (mL) of the initial solution, the titrated HNO 3 and NaOH, separately.The H s (mmol/g) of the adsorbents was calculated with the following equation: where V eb1 and V eb2 represent the volume of the consumed NaOH for the neutralization of free H + in the liquid solution, and the total H + in the liquid solution and the adsorbents surface; C NaOH represents the NaOH concentration (mol/L); m 2 represents the adsorbent weight (g).

Characteristics
The crystal structure of red mud and the adsorbents were determined by an X-ray powder diffraction (XRD, RAPID-S, Rigaku, Japan).The saturation magnetization of red mud and the adsorbents were detected by a superconducting quantum interference devices magnetometer (SQUID-VSM, Quantum Design, San Diego, CA, USA).X-ray photoelectron spectroscopy (XPS) measurements were performed with a spectrometer (ADES 400, VG-ADES, UK).The composition of red mud and the adsorbents was analyzed by XRF spectroscopy.The morphology of red mud and the adsorbents were recorded by field-emission scanning electron microscopy (SEM, FE-SEM, FEI Co., Hillsboro, OR, USA).

Conversion of Red Mud into Magnetic Adsorbent
To determine the crystallography of both red mud and the adsorbents, XRD experiments were conducted.The observed peaks in Figure 1 in the red mud indicate the presence of andradite (JCPDS 87-1971), hematite (JCPDS 33-0664), cancrinite (JCPDS 72-2076), clinochlore (79-1270), muscovite (JCPDS 07-0042), and morimotoite (JCPDS 47-1877).After hydrothermal treatment at 120 • C, no apparent change of the XRD pattern of P-120 was observed.When the temperature increased to 200 • C, two typical muscovite peaks at 2θ = 8.8 • and 26.8 • were not observed and the major peak of andradite at 2θ = 32.3• was significantly reduced in the diffraction pattern of P-200.Instead, the peaks of cancrinite, clinochlore, and morimotoite increased.Notably, new peaks at 2θ = 30.1 • and 35.4 • appeared, which belonged to an inverse spinel magnetite (JCPDS 19-0629) [19].Those results indicated that the dissolution of muscovite occurred with the temperature increasing from 120 • C to 200 • C, followed by the reductive dissolution of andradite and hematite with ascorbic acid at a higher temperature.
Ascorbic acid was a typical reductant, and could react with andradite and hematite at room temperature [20,21]; however, the process was inhibited by the Si/Al coating (e.g., amorphous aluminosilicate) [22] on the surface of andradite and hematite.With the temperature increasing form 120 • C to 200 • C, similar to the dissolution of muscovite in red mud, the Si/Al coating on andradite and hematite was also attacked by hydroxyl with generation of SiO 3 2− and Al(OH) 4 − into the liquid fraction [23,24].Thus, andradite and hematite were exposed to the liquid fraction, and reduced by ascorbic acid.Without adding ascorbic acid, andradite was stable in alkaline conditions, and generated in the presence of cancrinite and hematite during the hydrothermal treatment of red mud [25].
In the hydrothermal process, Si, Al and Fe from the dissolution of muscovite, andradite, and hematite were involved in the recrystallization of Fe 2+ -containing minerals, such as morimotoite, clinochlore, and magnetite.With the absence of Fe 2+ , Si and Al were recrystallized in the form of cancrinite, which was in agreement with the report of Zhang et al. [26].The cages of cancrinite's 12-membered ring channels conferred it enough sites for anions coordination [27] and preferentially selected CO 3 2− as structure stabilizer over OH − [28] when the former was generated from the oxidation of ascorbic acid and present in solution.
Appl.Sci.2019, 9, x FOR PEER REVIEW 5 of 15 Ascorbic acid was a typical reductant, and could react with andradite and hematite at room temperature [20,21]; however, the process was inhibited by the Si/Al coating (e.g., amorphous aluminosilicate) [22] on the surface of andradite and hematite.With the temperature increasing form 120°C to 200°C, similar to the dissolution of muscovite in red mud, the Si/Al coating on andradite and hematite was also attacked by hydroxyl with generation of SiO3 2-and Al(OH)4 − into the liquid fraction [23,24].Thus, andradite and hematite were exposed to the liquid fraction, and reduced by ascorbic acid.Without adding ascorbic acid, andradite was stable in alkaline conditions, and generated in the presence of cancrinite and hematite during the hydrothermal treatment of red mud [25].
In the hydrothermal process, Si, Al and Fe from the dissolution of muscovite, andradite, and hematite were involved in the recrystallization of Fe 2+ -containing minerals, such as morimotoite, clinochlore, and magnetite.With the absence of Fe 2+ , Si and Al were recrystallized in the form of cancrinite, which was in agreement with the report of Zhang et al. [26].The cages of cancrinite's 12membered ring channels conferred it enough sites for anions coordination [27] and preferentially selected CO3 2− as structure stabilizer over OH − [28] when the former was generated from the oxidation of ascorbic acid and present in solution.
When the temperature was increased to 270°C, the major peaks of andradite and hematite decreased, while the peaks of morimotoite and magnetite increased.By increasing temperature, the dissolution rates of Al and Si were greatly enhanced [29], which accelerated the dissolution of Si/Al When the temperature was increased to 270 • C, the major peaks of andradite and hematite decreased, while the peaks of morimotoite and magnetite increased.By increasing temperature, the dissolution rates of Al and Si were greatly enhanced [29], which accelerated the dissolution of Si/Al coating on the surface of andradite and hematite.Accordingly, the transformation of andradite and hematite into morimotoite and magnetite was promoted.
The formation of magnetite in P-200 and P-270 was accompanied by considerable changes in magnetic behavior.Red mud was weakly magnetized (Figure 2A) and not magnetically separated (Figure 2B).Similar to red mud, P-120, prepared at a hydrothermal temperature of 120 • C, showed a weak magnetic response due to the lack of magnetic species (e.g., magnetite).When the red mud was treated at 200 • C, the prepared P-200 exhibited magnetization of 4.1 Am 2 /kg, which had a magnetic response and can be magnetically separated from liquid fraction after use (Figure 2B).As the temperature increased to 270 • C, the saturation magnetization of P-270 further increased to 11.9 Am 2 /kg.This finding was consistent with the presence of magnetite in P-200 and P-270, as shown in Figure 1.
(Figure 2B).Similar to red mud, P-120, prepared at a hydrothermal temperature of 120°C, showed a weak magnetic response due to the lack of magnetic species (e.g., magnetite).When the red mud was treated at 200°C, the prepared P-200 exhibited magnetization of 4.1 Am 2 /kg, which had a magnetic response and can be magnetically separated from liquid fraction after use (Figure 2B).As the temperature increased to 270°C, the saturation magnetization of P-270 further increased to 11.9 Am 2 /kg.This finding was consistent with the presence of magnetite in P-200 and P-270, as shown in Figure 1.
-10000 -5000 0 5000 10000 The dissolution of muscovite and andradite in red mud after hydrothermal treatment indicated the difference in the composition of the prepared adsorbents.As shown in Figure 3A, the Si content was 10.7 wt.% for red mud, which slightly decreased to 9.6 wt.% for P-120.Accordingly, the Si concentration in the supernatant of P-120 was 24.1 mg/L.The loss of Si in P-120 was subjected to the dissolution of Si-containing minerals, such as muscovite and andradite.
When the temperature increased from 120°C to 200°C, the Si content remained unchanged, and the contents of both Ca and Fe increased from 16.1 wt.% and 12.7 wt.% for P-120 to 19.3 wt.% and 16.2 wt.% for P-200.In contrast, the Al content dramatically decreased from 12.1 wt.% for P-120 to 7.5 wt.% for P-200.This finding was attributed to the reductive dissolution of muscovite and andradite.When the structural Fe in the muscovite and andradite was reduced to Fe 2+ by ascorbic acid, dissolution of muscovite and andradite occurred, followed by a release of Al into the liquid solution.The released Al was rapidly converted into Al(OH)4 − under alkaline conditions, and coordinated to the surface sites of residual minerals [16].However, abundant OH -was present in the liquid solution and competed with the coordinated Al(OH)4 − via ion exchange reaction, which led to release of Al(OH)4 − into the liquid solution.Thus, the high-loss of Al in P-200 was observed.Furthermore, the Al concentration in the supernatant was 281.6 mg/L for P-120, and was considerably higher for P-200 (4466 mg/L), which was consistent with the loss of Al in P-200 in comparison to that of P-120.This finding indicates that the dissolution of muscovite and andradite accelerated when the temperature was above 200°C.With the temperature increasing from 200°C to 270°C, P-270 showed a similar composition to P-200 except that the Fe content was slightly decreased from 16.2 wt.% for P-200 to 15.8 wt.% for P-270.Accordingly, the Fe concentration in the supernatant increased from 33 mg/L for P-200 to 86 mg/L for P-270.Muscovite was completely dissolved with the temperature increasing to The dissolution of muscovite and andradite in red mud after hydrothermal treatment indicated the difference in the composition of the prepared adsorbents.As shown in Figure 3A, the Si content was 10.7 wt.% for red mud, which slightly decreased to 9.6 wt.% for P-120.Accordingly, the Si concentration in the supernatant of P-120 was 24.1 mg/L.The loss of Si in P-120 was subjected to the dissolution of Si-containing minerals, such as muscovite and andradite.The major iron-bearing minerals in red mud were andradite and hematite.During the hydrothermal process, muscovite was dissolved under alkaline conditions by increasing the temperature to 200°C.When ascorbic acid was added, it has the ability to provide electrons to the structural Fe in andradite and hematite with the formation of Fe 2+ and dehydroascorbic acid (DHA) [21].This led to the reductive dissolution of andradite and hematite (Equation ( 8)).During the dissolution of muscovite, andradite, hematite, Ca, Fe, Si, and Al were released into the liquid fraction (Figure 4 (Step 1)).Simultaneously, ascorbic acid also reacted with dissolved oxygen, which accelerated the consumption of ascorbic acid.When ascorbic acid was exhausted, extra dissolved oxygen was left.Under the alkaline conditions, the released Fe 2+ was rapidly hydrolyzed to Fe(OH)2 (Equation ( 9)), which was further reoxidized to Fe 3+ by the dissolved oxygen (Equation (10) and Figure 4 (Step 2)), and coprecipitated with adjacent Fe 2+ to form Fe3O4 (Equation 11 and Figure 4 (Step  3)) [30,31]: When the temperature increased from 120 • C to 200 • C, the Si content remained unchanged, and the contents of both Ca and Fe increased from 16.1 wt.% and 12.7 wt.% for P-120 to 19.3 wt.% and 16.2 wt.% for P-200.In contrast, the Al content dramatically decreased from 12.1 wt.% for P-120 to 7.5 wt.% for P-200.This finding was attributed to the reductive dissolution of muscovite and andradite.When the structural Fe in the muscovite and andradite was reduced to Fe 2+ by ascorbic acid, dissolution of muscovite and andradite occurred, followed by a release of Al into the liquid solution.The released Al was rapidly converted into Al(OH) 4 − under alkaline conditions, and coordinated to the surface sites of residual minerals [16].However, abundant OH − was present in the liquid solution and competed with the coordinated Al(OH) 4 − via ion exchange reaction, which led to release of Al(OH) 4 − into the liquid solution.Thus, the high-loss of Al in P-200 was observed.Furthermore, the Al concentration in the supernatant was 281.6 mg/L for P-120, and was considerably higher for P-200 (4466 mg/L), which was consistent with the loss of Al in P-200 in comparison to that of P-120.This finding indicates that the dissolution of muscovite and andradite accelerated when the temperature was above 200 • C. With the temperature increasing from 200 • C to 270 • C, P-270 showed a similar composition to P-200 except that the Fe content was slightly decreased from 16.2 wt.% for P-200 to 15.8 wt.% for P-270.Accordingly, the Fe concentration in the supernatant increased from 33 mg/L for P-200 to 86 mg/L for P-270.Muscovite was completely dissolved with the temperature increasing to 200 • C. Thus, the loss of Fe in P-270 was subjected to the release of Fe 2+ via the reduction of structural Fe in andradite.
The major iron-bearing minerals in red mud were andradite and hematite.During the hydrothermal process, muscovite was dissolved under alkaline conditions by increasing the temperature to 200 • C. When ascorbic acid was added, it has the ability to provide electrons to the structural Fe in andradite and hematite with the formation of Fe 2+ and dehydroascorbic acid (DHA) [21].This led to the reductive dissolution of andradite and hematite (Equation ( 8)).During the dissolution of muscovite, andradite, hematite, Ca, Fe, Si, and Al were released into the liquid fraction (Figure 4 (Step 1)).Simultaneously, ascorbic acid also reacted with dissolved oxygen, which accelerated the consumption of ascorbic acid.When ascorbic acid was exhausted, extra dissolved oxygen was left.Under the alkaline conditions, the released Fe 2+ was rapidly hydrolyzed to Fe(OH) 2 (Equation ( 9)), which was further reoxidized to Fe 3+ by the dissolved oxygen (Equation (10) and Figure 4 (Step 2)), and coprecipitated with adjacent Fe 2+ to form Fe 3 O 4 (Equation (11) and Figure 4 (Step 3)) [30,31]: Moreover, the generated Fe 2+ was also involved in the crystallization of morimotoite ( The major iron-bearing minerals in red mud were andradite and hematite.During the hydrothermal process, muscovite was dissolved under alkaline conditions by increasing the temperature to 200°C.When ascorbic acid was added, it has the ability to provide electrons to the structural Fe in andradite and hematite with the formation of Fe 2+ and dehydroascorbic acid (DHA) [21].This led to the reductive dissolution of andradite and hematite (Equation ( 8)).During the dissolution of muscovite, andradite, hematite, Ca, Fe, Si, and Al were released into the liquid fraction (Figure 4 (Step 1)).Simultaneously, ascorbic acid also reacted with dissolved oxygen, which accelerated the consumption of ascorbic acid.When ascorbic acid was exhausted, extra dissolved oxygen was left.Under the alkaline conditions, the released Fe 2+ was rapidly hydrolyzed to Fe(OH)2 (Equation ( 9)), which was further reoxidized to Fe 3+ by the dissolved oxygen (Equation (10) and Figure 4 (Step 2)), and coprecipitated with adjacent Fe 2+ to form Fe3O4 (Equation 11and Figure 4 (Step  3)) [30,31]: Fe 2OH Fe(OH) Moreover, the generated Fe 2+ was also involved in the crystallization of morimotoite (Figure 4  (Step 4)).In the absence of Fe, the released Ca, Si, and Al were recrystallized in the formation of cancrinite (Figure 4 (Step 5)) [32].

Morphology
The morphologies of red mud and the prepared adsorbents were shown in Figure 5.The red mud was an amorphous agglomerate with small particles on the surface (Figure 5A).P-120 showed a similar morphology to the red mud (Figure 5B).When the temperature reached 200 • C, P-200 exhibited fine particles with the size of 0.2-2 µm (Figure 5C), which was related to the dissolution of muscovite and andradite in red mud.Compared to P-200, a new octahedron with the size of 1-4 µm belonged to the inverse spinel Fe 3 O 4 [33], indicating that the high temperature promoted the crystal growth of magnetite.
The morphologies of red mud and the prepared adsorbents were shown in Figure 5.The red mud was an amorphous agglomerate with small particles on the surface (Figure 5A).P-120 showed a similar morphology to the red mud (Figure 5B).When the temperature reached 200°C, P-200 exhibited fine particles with the size of 0.2-2 m (Figure 5C), which was related to the dissolution of muscovite and andradite in red mud.Compared to P-200, a new octahedron with the size of 1-4 m belonged to the inverse spinel Fe3O4 [33], indicating that the high temperature promoted the crystal growth of magnetite.

Adsorption
Zn 2+ is a common heavy metal ion, which is widely distributed in the wastewater from smelting, electroplating, and steel rolling industries.Thus, the adsorption performance of red mud and the prepared adsorbents on Zn 2+ were investigated.As shown in Figure 6, the adsorption of Zn 2+ was ranked in the following order: red mud  P-120  P−270  P-200.The adsorption data was fitted with the non-linear Langmuir and Freundlich models, respectively, and the results showed that the regression coefficient values (R 2 ) of Langmuir model were approximately 0.99 for red mud and the three adsorbents (Table 1), which exceeded those of the Freundlich model.This finding indicated that the red mud and the prepared adsorbents have an energetically homogeneous surface [34] for the adsorption of Zn 2+ .P-200 showed the desirable adsorption capacity for Zn 2+ (89.6 mg/g), higher than that of red mud, P-120, P-270, and other reported magnetic adsorbents, such as graphene oxide (73 mg/g) [35], magnetic nano-silicon materials (51.2 mg/g) [36], and dry algae (60 mg/g) [37].Therefore, P-200 has great potential for Zn 2+ adsorption.

Adsorption
Zn 2+ is a common heavy metal ion, which is widely distributed in the wastewater from smelting, electroplating, and steel rolling industries.Thus, the adsorption performance of red mud and the prepared adsorbents on Zn 2+ were investigated.shown in Figure 6, the adsorption of Zn 2+ was ranked in the following order: red mud < P-120 < P−270 < P-200.The adsorption data was fitted with the non-linear Langmuir and Freundlich models, respectively, and the results showed that the regression coefficient values (R 2 ) of Langmuir model were approximately 0.99 for red mud and the three adsorbents (Table 1), which exceeded those of the Freundlich model.This finding indicated that the red mud and the prepared adsorbents have an energetically homogeneous surface [34] for the adsorption of Zn 2+ .P-200 showed the desirable adsorption capacity for Zn 2+ (89.6 mg/g), higher than that of red mud, P-120, P-270, and other reported magnetic adsorbents, such as graphene oxide (73 mg/g) [35], magnetic nano-silicon materials (51.2 mg/g) [36], and dry algae (60 mg/g) [37].Therefore, P-200 has great potential for Zn 2+ adsorption.The adsorption capacity of Zn 2+ was in agreement with the number of surface coordination sites on red mud and the three adsorbents, which could be determined by H s with the Gran method.As shown in Figure 7 and Table 1, H s could be listed in the following order: red mud < P-120 < P-270 < P-200, which was consistent with the adsorption capacities of Zn 2+ on these adsorbents.P-200 showed the optimal H s of 4.35 mmol/g, indicating that it had sufficient surface coordination sites for Zn 2+ adsorption.The adsorption capacity of Zn 2+ was in agreement with the number of surface coordination sites on red mud and the three adsorbents, which could be determined by Hs with the Gran method.As shown in Figure 7 and Table 1, Hs could be listed in the following order: red mud  P-120  P-270  P-200, which was consistent with the adsorption capacities of Zn 2+ on these adsorbents.P-200 showed the optimal Hs of 4.35 mmol/g, indicating that it had sufficient surface coordination sites for Zn 2+ adsorption.The distribution coefficient (K d ) was a useful index for comparing the adsorption capacities of red mud and the obtained adsorbents for Zn 2+ under the same experimental condition [38,39], and calculated according to the following equation: where q e is the amount of Zn 2+ adsorbed on red mud or the obtained adsorbents (mg/g), and C e is the equilibrium concentration of Zn 2+ in the solution.
As shown in Figure 8A, K d decreased with the increase of the initial concentration of Zn 2+ .Generally, at a high initial concentration of Zn 2+ , the surface sites of P-200 became saturated with Zn 2+ [39,40], which caused large number of unabsorbed Zn 2+ remaining in the liquid fraction and apparently exhibited low K d (Figure 8A and Table 2).However, at a low initial concentration of Zn 2+ , P-200 showed a high value of K d in comparison with P-120, P-270 and commercial adsorbents (Table 2), such as graphene oxide [36] and Tunisian smectite [41], demonstrating that P-200 had desirable performance for sorption of Zn 2+ .Other adsorbents, such as magnetic core-silica shell particles [36], dry algae [37], and magnetic modified chitosan [42], showed very low K d (Table 2), indicating that they were fairly ineffective for Zn 2+ adsorption.
apparently exhibited low Kd (Figure 8A and Table 2).However, at a low initial concentration of Zn 2+ , P-200 showed a high value of Kd in comparison with P-120, P-270 and commercial adsorbents (Table 2), such as graphene oxide [36] and Tunisian smectite [41], demonstrating that P-200 had desirable performance for sorption of Zn 2+ .Other adsorbents, such as magnetic core-silica shell particles [36], dry algae [37], and magnetic modified chitosan [42], showed very low Kd (Table 2), indicating that they were fairly ineffective for Zn 2+ adsorption.The plots of adsorption capacity versus equilibrium concentration in solution did not yield a straight line (Figure 8A).Thus, an average K d value (K d medium ) was calculated according to the method of Lu and Xu [43] and used to compare the adsorption performance of red mud and the obtained adsorbents for Zn 2+ adsorption.As shown in Figure 8B, K d medium of Zn 2+ on red mud and the obtained adsorbents were in the following order: P-200 > P-270 > P-120 > red mud, which was in agreement with the order of the surface site concentrations and the maximum adsorption capacities of red mud and the obtained adsorbents.
As shown in Table 2, K d of raw red mud and the CO 2 neutralized red mud [9] were similar at the low initial concentration of Zn 2+ , demonstrating that the method of CO 2 neutralization for red mud treatment was inefficient.However, K d of red mud dramatically increased from 0.71 L/g to 42.3 L/g after hydrothermal treatment at 200 • C. The improvement of K d value indicated enhancement of adsorption affinity and adsorption capacity of P-200 [44].Thus, the hydrothermal method was better than that of CO 2 neutralization for improving the adsorption performance of red mud.
XPS experiments were conducted to characterize P-200 before and after Zn 2+ adsorption.As shown in Figure 9A, the spectrum of P-200 contained the typical peaks of Al, Si, Ca, O, Fe, and Na.After Zn 2+ adsorption, the peak of Na 1s at 1072 eV disappeared (Figure 9A), and new peaks at the binding energies of 1020.7 eV and 1043.8 eV (Figure 9B) belonged to Zn 2+ [45].This demonstrated that Zn 2+ was adsorbed on P-200, and that Na + was released from P-200.During the adsorption, the amount of Na + desorbed from P-200 showed a positive correlation with the amount of adsorbed Zn 2+ on P-200 (Figure 9C).This confirmed that the adsorption of Zn 2+ on P-200 was dominated by cationic exchange.P-200 was a mixture of magnetite, hematite and Si/Al compounds, and exhibited functional sites SO ¯ on its surface (S representing Fe, Si, or Al).In P-200 synthesis, Na + attached to the surface sites to form SO ¯Na + with the addition of NaOH, which was replaced by H + when pH decreased (Equation (3)).Therefore, both Na + and H + attached on P-200 surface in Zn 2+ adsorption.Zn 2+ was divalent- P-200 was a mixture of magnetite, hematite and Si/Al compounds, and exhibited functional sites ≡SO − on its surface (S representing Fe, Si, or Al).In P-200 synthesis, Na + attached to the surface sites to form ≡SO − Na + with the addition of NaOH, which was replaced by H + when pH decreased (Equation (3)).Therefore, both Na + and H + attached on P-200 surface in Zn 2+ adsorption.Zn 2+ was divalent-charged, which showed higher affinity to ≡SO − than monovalent Na + and H + [46], and the surface-bound Na + or H + were subsequently replaced (Equations ( 13) and ( 14)).The pH of the solution was equilibrated to 6.3, in which Zn was predominated in the form of Zn 2+ and ZnOH + [47].Thus, zinc adsorption on P-200 appeared to occur via exchange of Zn 2+ and ZnOH + with surface-bond Na + and H + (Equations ( 15) and ( 16)).A similar observation was reported in Zn 2+ adsorption on groundwater treatment sludge, which had the similar ≡SO − sites [23].Of the three obtained adsorbents, P-200 had the optimal surface sites concentration (Hs), and thus exhibited the highest adsorption capacity.
The operation cost of the adsorbent P-200 for Zn 2+ adsorption was important in wastewater treatment.Synthesis of one ton of magnetic adsorbent needed 0.01 ton of ascorbic acid, 0.27 ton of caustic soda, and 45 kW h power, and the total production cost was US$ 158.8.Disposal of red mud accounted for about 5% of alumina production [48], and the alumina price was US$ 439 per ton in China [49].The disposal cost of red mud was nearly US$ 22 per ton, which could be deducted from the production cost of P-200.Thus, the net cost of P-200 production was about US$ 136.8 per ton.For treating Zn 2+ -containing wastewater, the operation cost of P-200 was approximately US$ 1.45 per ton, lower than the widely used adsorbents, such as granular active carbon [50] and zero-valent nanometer iron [51], indicating that the application of P-200 for heavy metal removal was economically feasible.

Conclusions
Red mud is an alkaline solid waste and abundant in andradite, muscovite, hematite, and cancrinite.Red mud was converted to a magnetic adsorbent via a facile hydrothermal route using ascorbic acid as reducing agent.With hydrothermal treatment, the magnetic adsorbent was formed in the following steps: (1) the dissolution of muscovite under alkaline conditions, (2) the reductive dissolution of andradite with the generation of Fe 2+ , (3) the reoxidization of Fe 2+ to Fe 3+ by dissolved oxygen and the coprecipitation of Fe 3+ and Fe 2+ in the form of Fe 3 O 4 , and (4) the crystallization of cancrinite and morimotoite.By increasing the hydrothermal temperature, the reductive dissolution of andradite was promoted and the crystal size of magnetite was enlarged.When the temperature increased to 200 • C, the prepared P-200 showed a well saturation magnetization of 4.1 Am 2 /kg, an ideal adsorption capacity of Zn 2+ (89.6 mg/g), and a high average K d value of 16.8 L/g, and thus exhibited desirable Zn 2+ adsorption under real-world conditions.Cationic exchange was the dominated mechanism for Zn 2+ adsorption on P-200.Those advantages indicated that P-200 was a promising adsorbent for the treatment of Zn 2+ containing wastewater.

Figure 3 .
Figure 3. (A) Composition of red mud, P-120, P-200, and P-270, and (B) the major cationic concentrations in the supernatant after hydrothermal treatment.

Figure 3 .
Figure 3. (A) Composition of red mud, P-120, P-200, and P-270, and (B) the major cationic concentrations in the supernatant after hydrothermal treatment.

Figure 4 .
Figure 4.The proposed conversion route of iron mud into magnetic adsorbent.Step 1 represents the reductive dissolution of red mud; Step 2 represents the oxidization of ferrous Fe; Steps 3 to 5 represent the crystallization of magnetite, morimotoite, and cancrinite, respectively.

Table 1 .
Parameters of the isotherm models and the surface sites concentrations of red mud and the obtained adsorbents.

Table 1 .
Parameters of the isotherm models and the surface sites concentrations of red mud and the obtained adsorbents.

Table 1 .
Parameters of the isotherm models and the surface sites concentrations of red mud and the obtained adsorbents.