Anoushiravan Mohseni-Bandpia,
Babak Kakavandib,
Roshanak Rezaei Kalantary*c,
Ali Azarid and
Azam Keramatid
aDepartment of Environmental Health Engineering, School of Public Health, Shahid Beheshti University of Medical Sciences, Tehran, Iran
bDepartment of Environmental Health Engineering, School of Public Health, Ahvaz Jundishapur University of Medical Sciences, Ahvaz, Iran
cDepartment of Environmental Health Engineering, School of Public Health, Iran University of Medical Sciences, Tehran, Iran. E-mail: rezaei.r@iums.ac.ir; Fax: +98 21 86709487; Tel: +98 21 86704775
dDepartment of Environmental Health Engineering, School of Public Health, Tehran University of Medical Sciences, Tehran, Iran
First published on 24th August 2015
Magnetic nanoparticles (MNPs) have recently been adopted by researchers in the field of adsorption/biosorption for separation of pollutants from aqueous solutions. In this paper, chitosan was impregnated with magnetite nanoparticles through a chemical co-precipitation method to fabricate hybrid adsorbents of Fe3O4–chitosan. The physicochemical and structural properties of the adsorbent were characterized, and then the performance of the adsorbent was evaluated for fluoride removal from water. The operational factors affecting the adsorption process, including pH, contact time, adsorbent dosage, initial fluoride concentration, and temperature, were studied. Various isotherm and kinetic models were also used to evaluate the fit of the experimental data with the modeled results. The equilibrium data were well described by the Freundlich model. The kinetics of the adsorption process followed the pseudo-second-order model. Recycling results suggested that the Fe3O4–chitosan particles maintain a great reusability potential for five consecutive cycles. Findings also showed that the Fe3O4–chitosan can be easily regenerated via acid treatment. The results of the present work highlighted the potential of using the Fe3O4–chitosan magnetic composite for the removal of fluoride from water. In conclusion, Fe3O4–chitosan can be considered as an appropriate adsorbent for fluoride removal from water, because it can be separated both quickly and easily, it has high efficiency, and it does not lead to secondary pollution.
A wide variety of methods have been used to remove fluoride from drinking water, including adsorption and biosorption,3,4 chemical precipitation mostly with calcium and aluminum salts,5,6 ion exchange, and membrane process such as reverse osmosis, nanofiltration, and electrodialysis.7,8 All these methods have proven efficient; however, adsorption is the most widely used method for the removal of excessive fluoride from water, due primarily to its low costs, high efficiency, and being environmentally friendly.9
During the past few years, a large number of studies have been carried out on the efficiency of composite materials that contain natural polymers and have inorganic origins, which have proven effective.9 Chitosan is a copolymer with favorable biological characteristics, which is also harmless to humans.10 Due to its excellent adsorption properties, chitosan has been widely used, alone or in combination with other materials, for the removal of a variety of environmental pollutants, including fluoride in drinking water.11,12 Other beneficial characteristics of chitosan include its biodegradability, flexibility, hydrophilicity, biocompatibility, and versatility.9 However, pure chitosan does not have optimal adsorption because it easily dissolves in acidic solution and has weak chemical resistance.13
Magnetic nanoparticles (MNPs) have recently been adopted by researchers in the field of adsorption/biosorption for separation of pollutants from water,14,15 mainly because the application of such materials makes the separation of both the adsorbent and the adsorbate much easier from water. Therefore, the water does not need to be filtered or centrifuged after the adsorption process, which is considered a critical advantage. In addition, the sorbent can be easily recovered and reused. Combination of the Fe3O4 MNPs and chitosan can effectively avoid the chemical weakness of chitosan. Moreover, the hydroxyl groups on the surface of Fe3O4 can interact with amine groups and hydroxyl groups of chitosan through hydrogen-bond interaction to keep chitosan stable under acidic conditions.13 It is noteworthy that the magnetic chitosan composite has been widely and successfully utilized to remove contaminants such as dye,13,16 heavy metals,17,18 humic acid19 and uranyl.20
To the best of our knowledge, few studies have so far been conducted to evaluate the efficiency of magnetic chitosan for fluoride removal from aqueous solutions. Therefore, we aimed at synthesizing a novel magnetic chitosan composite (Fe3O4–chitosan) and evaluating its efficiency for the removal of fluoride from water, which is a major concern in southern parts of Iran.
:
20. Afterwards, the remaining shell was washed with DI-water until reaching a neutral pH. In order to separate the inorganic matter from the shell, the remaining shell from the previous stage was put into a 1.4 N HCl solution and kept for 1 h. In this stage, the weight ratio of shell to acid was 1
:
10. Then, the remaining shell was washed with deionized water until reaching a neutral pH. The extracted chitin was yellow, which was decolorized through acetone washing.
Chitosan was extracted from the chitin using the deacetylation method. For this purpose, the collected chitin was put into a 50% NaOH solution and kept at 100 °C for 6 h. It was then filtered and washed with deionized water until reaching a neutral pH. The extracted substance, chitosan, was dried at 60 °C for 1 h. The extracted chitosan, was hydrated and put into a 0.1 M NaOH solution to increase its pH to 8; 0.5 M chloroacetic acid was then added to this solution and the mixture was kept at room temperature for 10 h to change the hydroxyl groups into carboxyl ones. The carboxylated chitosan was then washed with deionized water to reach a neutral pH.
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A VSM (7400, Lakeshore, USA) was applied to determine the magnetic properties of the adsorbent at ±10 kOe at 25 °C. The BET analysis (Quantachrome, 2000, NOVA) was applied to determine the surface area, size, and volume of the pores of the synthesized MNPs and the generated composite. Prior to the measurement, the sample was degassed at 100 °A °C for 8 h in an out-gassing station to remove any adsorbed water or entrapped gases in the sample. Fourier transform infrared spectrophotometer (FTIR) spectra of the Fe3O4–chitosan composite were obtained using Tensor 27, Bruker, (Germany) model to confirm the functional groups present in it.
In this study, we initially evaluated the effect of pH on the adsorption capacity in the range of 3–9. Then, the adsorption equilibrium was determined at the optional pH for a time period of 3 h and, subsequently, the adsorption kinetic parameters were calculated. In the next step, we evaluated the effect of fluoride (1–10 mg L−1) and the adsorbent (ranging from 0.25–2 g L−1) concentrations at the optimal pH and contact time in order to determine the isothermic parameters of the adsorption equilibrium. Finally, we explored the effect of temperature on the adsorption capacity in order to determine the thermodynamic parameters. The removal efficiency as well as the adsorption capacity were calculated using the following equations:
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The specific surface area, volume, and average pore diameter for MNPs and Fe3O4–chitosan were measured using the BET method, and the results are given in Table 1. The results indicated that the highest surface area of the MNPs and Fe3O4–chitosan were 93.5 and 498.5 m2 g−1, respectively, indicating that the composite provides a higher adsorption capacity for pollutants compared to the MNPs. As given in Table 1, the surface area, mean size and volume of pores of Fe3O4–chitosan were larger than those of the MNPs, which can be due to the agglomeration of MNPs. The average pore size was estimated to be 2.9 and 3.4 nm for the MNPs and the composite, respectively. According to the IUPAC classification, the average sizes of 2.9 and 3.4 nm can be classified as mesopores groups.24
| Adsorbent | Surface area (m2 g−1) | Pore volume (cm3 g−1) | Mean pore diameter (nm) | Pore structure |
|---|---|---|---|---|
| MNPs | 93.5 | 2.37 | 2.9 | Mesopore |
| Fe3O4–chitosan | 498.5 | 3.68 | 3.4 | Mesopore |
According to Fig. 2, the highest magnetization saturation of 46.7, 34.5, and 28.8 emu g−1 were obtained for Fe3O4, Fe3O4–chitosan before adsorption, and Fe3O4–chitosan after adsorption of fluoride, respectively, which suggests a super-paramagnetic characteristic for the adsorbents. This rate is much higher than what has been previously reported by researchers as a sufficient magnetization amount.14,25 The magnetization value for the Fe3O4–chitosan composite was less than that of naked Fe3O4, which can be due to the presence of non-magnetic chitosan on the surface of the magnetic particles.17 As seen in Fig. 2, the observed decrease in the saturation magnetization of the composite was not significant after the adsorption process. This implies that the Fe3O4–chitosan composite is a stable adsorbent. These results ensure that the composite can be potentially applied as a magnetic adsorbent to remove contaminants from the aqueous environment to avoid a secondary pollution.
X-ray diffraction (XRD) can provide very useful information about the physical and chemical form of the magnetic particles embedded in the chitosan matrix.17 The XRD patterns of the samples are shown in Fig. 3(a). The X-ray pattern of chitosan exhibited characteristic crystalline peaks at 2θ = 8.0° and 20.1°, respectively. However, these peaks were observed much less intensively in chitosan–carbocycle and Fe3O4–chitosan, due to the elimination of the chitosan in the calcination step at 100 ± 2 °C.26 The higher crystallinity of chitosan than its carbocycled compound allowed for better accessibility for fluoride and, thus, higher activity. The synthesized MNPs could take the form of maghemite (Fe2O3) or magnetite (Fe3O4). Fe3O4 is black in color, while Fe2O3 has a brown color.27 After the synthesis process, we observed that the color of the suspension containing the nanoparticles was black, demonstrating the formation of Fe3O4 nanoparticles. Fig. 3(a) indicates the XRD pattern of the synthesized nanoparticles, which is quite similar to that of pure magnetite. Moreover, the absence of peaks correspond to maghemite, ranging from a 2θ angle of 20° to 30°, also verify that the black powder was magnetite. This suggests the lack of impurities in the maghemite. The main peaks at 2θ = 30.1°, 35.4°, 43.1°, 53.4°, 56.9°, and 62.5° correspond to the (220), (311), (400), (422), (511), and (440) plane of the orthorhombic Fe3O4 (JCPDS card no. 19-0629).13 The XRD pattern confirmed the presence of Fe3O4 particles within the structure of chitosan, so the prepared composite could be separated from aqueous solutions by magnet. As illustrated in Fig. 4(a), after magnetization of chitosan, the peaks assigned to chitosan (2θ = 8° and 20°) and Fe3O4 (2θ = 30.1° and 35.4°) were still observed, indicating successful synthesis of Fe3O4 crystals on the chitosan surface. The average particle size of the MNPs was calculated using the Scherrer's equation, which were found to be in the range of 20–51.2 nm. This was in accordance with the results from the TEM analysis.
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| Fig. 3 (a) XRD pattern and (b) FTIR spectra of chitosan, chitosan–carbocycle, Fe3O4, and Fe3O4–chitosan composite. | ||
Since adsorption reactions mostly take place on the surface of the adsorbent, the functional groups on the surface of the adsorbent can play a significant role in the adsorption process. In order to characterize the functional groups on the surface of the samples and to measure the binding mechanism of the pollutants (inorganic or organic), Fourier transform infrared spectroscopy (FTIR) spectra were recorded on a Tensor 27, Bruker, (Germany) spectrometer (Fig. 3(b)). The bonds observed in the range of 3413–3440 cm−1 in the spectra of chitosan, chitosan–carbocycle, and Fe3O4–chitosan indicated the presence of O–H bond stretching and N–H bond stretching.9,28,29 The bands at 3046 cm−1 and 2900 cm−1 that can be assigned to the aliphatic stretching vibrations of –CH had very low intensity in the chitosan–carbocycle sample, indicating the presence of residual carbon matter after calcinations.26 The absorption peaks at 2927 cm−1 and 2860 cm−1 are due to the C–H stretching vibration of the –CH2 groups in chitosan.13 The bands around 1600 cm−1 were assigned to the OH bending vibrational mode due to the adsorption of moisture when FTIR sample disks were prepared in an open-air atmosphere. According to Fig. 3(b), the bonds around 1657 cm−1 were observed in the spectra of the chitosan, chitosan–carbocycle, and Fe3O4–chitosan samples, which can correspond to C
O of NH
C
O bond stretching. The peak observed at 1366 cm−1 can be assigned to C–N stretching vibration. The peaks at 1083 cm−1 and 1023 cm−1 can be attributed to C–OH bond stretching.17,30 For Fe3O4 spectra, absorption peaks at 578.6 cm−1 can be attributed to Fe–O band vibration of Fe3O4. As shown in Fig. 3(b), the FTIR spectrum of Fe3O4–chitosan adsorbent was a hybrid of chitosan with Fe3O4 nanoparticles. The spectrum of Fe3O4–chitosan composite peaks at 3430 cm−1 due to amine N–H stretching vibration and –OH moieties in the chitosan, at ∼1661 cm−1 due to N–H scissoring from the primary amine because of free amino groups in the cross-linked chitosan, and at ∼580 cm−1 for the Fe–O group due to pure Fe3O4.17 The FTIR spectrum clearly confirms the existence of chitosan and Fe3O4 in the Fe3O4–chitosan composite.
However, it is noteworthy that the variations in the removal efficiency were not significant under acidic and basic conditions; the removal efficiency was 78.8 and 81% for pH 3 and 9, respectively. This demonstrates that the Fe3O4–chitosan still provides very good fluoride uptake in media with various pH values. It can be concluded that the Fe3O4–chitosan is capable of satisfactorily removing fluoride from aqueous solutions even without pH adjustment. In addition, the pH of fluoride-contaminated groundwater usually ranges between 6 and 8. Therefore, the adsorption by Fe3O4–chitosan could become a sound alternative in full-scale fluoride removal facilities as the pH range is wide.
In the present work, we employed four kinetic models, including pseudo-first-order, pseudo-second-order, intraparticle diffusion, and Elovich models, to investigate the kinetics of fluoride adsorption onto the Fe3O4–chitosan. The equations for each of the models are as follows:
Pseudo-first-order: ln(qe − qt) = ln qe − kft
| (4) |
| Pseudo-second-order: t/qt = t/qe + 1/ksqe2 | (5) |
Elovich: qt = β ln(αβ) + β ln t
| (6) |
| Intraparticle diffusion: qt = kit0.5 | (7) |
Table 2 presents the values of kinetic models parameters for fluoride adsorption onto Fe3O4–chitosan. Results of the kinetic models showed that the adsorption kinetics of fluoride can be better described by the pseudo-second-order model. According to the r2 values, the pseudo-second-order model had the best fit with the experimental data, implying that the concentrations of both the adsorbent and the adsorbate were the rate-controlling step for the process of fluoride adsorption onto the Fe3O4–chitosan.15 This also suggests that chemisorption was the dominant mechanism in the adsorption process, which involves the exchange or sharing of electrons between fluoride and the binding sites on the Fe3O4–chitosan particles.37 It has been reported that the chemisorption process that is limited to one layer of molecules on the surface of the adsorbent is commonly followed by added layers of the physically adsorbed molecules of the adsorbate.38
| Kinetic models | Parameters | Values |
|---|---|---|
| Pseudo-first-order | ||
| qe,Cal (mg g−1) | 5.45 | |
| k1 (min−1) | 0.039 | |
| r2 | 0.877 | |
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| Pseudo-second-order | ||
| qe,Cal (mg g−1) | 8.62 | |
| k2 (g mg−1) (min−1) | 0.02 | |
| r2 | 0.997 | |
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| Elovich | ||
| α | 37.38 | |
| β | 0.993 | |
| r2 | 0.936 | |
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||
| Intraparticle diffusion | ||
| ki | 0.53 | |
| Ci | 3.08 | |
| r2 | 0.665 | |
| Experimental qe | 8.36 | |
The pseudo-second-order of the adsorption process was also strongly confirmed by the very good agreement between the calculated qe and the experimental qe values. This finding was also confirmed by the curves presented in Fig. 5. Our results are in-line with those of the previous works,9,33,34 in which the authors reported that the pseudo-second-order model had the best fit with their experimental data.
We also applied the intraparticle diffusion model to investigate the possibility of pore diffusion, in which the ions of the adsorbate transport from the solution to the pores in the adsorbent due mainly to the stirring applied to the batch process.15 However, the low r2 value (0.66) of the intraparticle diffusion model implied that the pore diffusion is not the rate controlling step. This is also consistent with the findings of the study of Ma et al.33 As observed in Table 2, the value of Ci was measured to be 3.08 mg g−1, indicating that intra-particle diffusion is not the only controlling step for fluoride adsorption and the process is also controlled, to some extent, by boundary layer diffusion.15,39
| Langmuir: Ce/qe = Ce/q0 + 1/kLq0 | (8) |
Freundlich: ln qe = ln kf + n−1 ln Ce
| (9) |
Temkin: qe = B ln kt + B ln Ce
| (10) |
The results of the fluoride adsorption isotherm modeling experiments, which were conducted at a pH of 7, an adsorbent dose of 1 g L−1, a contact time of 60 min, and operational temperatures of 20, 35, and 50 °C are presented in Table 3. As presented in the table, the values of correlation coefficients (r2) were larger than 0.95 for Langmuir and Freundlich isotherm models, indicating that both models fit very well with the experimental data. Similar findings have been reported in the literature for the removal of fluoride by different types of adsorbents.29,36 However, the Freundlich isotherm model had the best fit with the experimental data; r2 values of above 0.99 for all studied temperatures. This implies that the process of fluoride adsorption onto Fe3O4–chitosan follows a heterogeneous (multi-layer) mechanism. This finding was also confirmed by the good agreement between the equilibrium data for the fluoride adsorption experiments and the Freundlich equilibrium isotherm, as shown in Fig. 7. The desirability of the adsorption process was confirmed by the Freundlich exponent, n, since its value was 1 < n < 10 at all temperatures.15,36 Based on the Langmuir model, the maximum adsorption capacities improved with increasing of solution temperatures, indicating the occurrence of an endothermic process.
| Isotherm models | Constants | ||
|---|---|---|---|
| Langmuir | kL | qm (mg g−1) | r2 |
| 20 °C | 2.57 | 9.26 | 0.956 |
| 35 °C | 3.45 | 9.34 | 0.964 |
| 50 °C | 4.41 | 9.43 | 0.958 |
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| Freundlich | kf | n | r2 |
| 20 °C | 5.971 | 2.16 | 0.996 |
| 35 °C | 6.606 | 2.32 | 0.993 |
| 50 °C | 7.056 | 2.6 | 0.992 |
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| Temkin | kt | B | r2 |
| 20 °C | 61.29 | 1.505 | 0.906 |
| 35 °C | 101.92 | 1.429 | 0.9 |
| 50 °C | 217.76 | 1.278 | 0.869 |
The kf and n values reported in Table 3 for the Freundlich isotherm model, which respectively represent adsorption capacity and intensity, were found to increase by increasing of operational temperature; the kf and n values increased from 5.97 and 2.16 at 20 °C to 7.05 and 2.6 at 50 °C, respectively. This indicates that the adsorption capacity and intensity increased with increasing of operational temperature, which is an indicator of the chemisorption mechanism for the adsorption of fluoride onto Fe3O4–chitosan and further substantiates our previous results presented earlier.44,45
The maximum adsorption capacity, qm, of the Fe3O4–chitosan was compared with the fluoride adsorption capacities of other adsorbents (Table 4). Based on the Langmuir equilibrium model, the maximum level of fluoride uptake per unit mass of Fe3O4–chitosan was 9.43 mg g−1. It is noticeable from Table 4 that the Fe3O4–chitosan has a higher maximum adsorption capacity compared to other adsorbents. The observed differences in the adsorption capacities for the listed adsorbents can be due to structure, surface area, and the properties of functional groups in each adsorbent.
| Adsorbent | pH | Temp. (°C) | Isotherm | Kinetic | qm (mg g−1) | References |
|---|---|---|---|---|---|---|
| Hydrous ferric oxide doped alginate beads | 7.0 | 29 | Freundlich | Pseudo-second order | 8.9 | 46 |
| Meso porous Al–chitosan | 7.0 | 30 ± 3 | Langmuir | Pseudo-second order | 8.26 | 26 |
| Chitosan supported mixed oxide beads | 7.0 | 50 | Langmuir | Not done | 6.48 | 2 |
| Activated alumina | 7.0 | — | Langmuir | Pseudo-first-order | 2.41 | 47 |
| Fe(III) carboxylated chitosan | 7.0 | 50 | Freundlich | Intraparticle diffusion | 12.34 | 48 |
| Hydrous ferric oxide | 6.5 | 24 ± 1 | Langmuir | Pseudo-second order | 6.71 | 29 |
| Pine bark biochar | 2.0 | 25 | Langmuir | **** | 9.77 | 49 |
| 35 | 10.53 | |||||
| 45 | 8.4 | |||||
| Cerium loaded silica gel/chitosan (Ce-SGCS) | 7.0 | 50 | Langmuir | Pseudo-second order | 10.54 | 9 |
| Magnetic corn stover biochar (MCSBC) | 2.0 | 25 | — | Pseudo-first order | 4.11 | 50 |
| Chitosan supported zirconium(IV) tungstophosphate composite | 7.0 | 50 | Freundlich | Pseudo-second-order and intraparticle diffusion | 9.901 | 51 |
| Alumina/chitosan composite | 7.0 | 50 | Freundlich | Pseudo-second order | 23.81 | 28 |
| Polypyrrole/Fe3O4 magnetic nanocomposite | 6.5 | 45 | Langmuir–Freundlich | Pseudo-second order | 17.6–22.3 | 52 |
| Fe3O4–chitosan | 7.0 | 50 | Freundlich | Pseudo-second order | 9.43 | The present study |
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ΔGo = −RT ln Ko
| (12) |
| Temperature (K) | ΔGo (kJ mol−1) | ΔHo (kJ mol−1) | ΔSo (kJ mol−1 K−1) |
|---|---|---|---|
| 293 | −5.5 | 10.36 | 0.54 |
| 308 | −6.54 | ||
| 323 | −7.1 |
As given in the table, the value of ΔSo was positive, indicating that Fe3O4–chitosan particles have affinity for fluoride ions. The negative values of ΔGo suggest that the adsorption process was feasible and had a spontaneous nature.53 Furthermore, it can be observed that the absolute values of −ΔGo increased with increasing of operational temperature; the absolute −ΔGo value rose from −5.5 kJ mol−1 at 20 °C to −7.1 at 50 °C. This indicates that the adsorption of fluoride ions onto Fe3O4–chitosan is more favorable at higher temperatures.15 Moreover, studies have suggested that the observed increase in the absolute value of ΔGo at higher operational temperatures is most likely because both the adsorbent and the adsorbate dry out; this, in turn, facilitates the chemical reaction between the two and leads to more favorable conditions for the adsorption process at higher operational temperatures. The positive value obtained for ΔHo shows that fluoride adsorption onto Fe3O4–chitosan is an endothermic reaction.15 Similar results (+ΔSo, −ΔGo and +ΔHo) have been obtained for the adsorption of fluoride ions on other adsorbents such as Fe(III) loaded carboxylated chitosan beads,48 chitosan supported mixed metal oxides beads,2 and alumina/chitosan composite.28
Results from the desorption study indicated that for all cycles, the desorption ability of HCl is higher than those of other desorbing solutions. According to Fig. 8(b), HCl solution could desorb 93.6% of fluoride from Fe3O4–chitosan surface in the first cycle. It was also observed that the desorption efficiency did not noticeably change in the next desorption cycles; the desorption efficiency of fluoride by HCl decreased from 93.6 to 88.5% after five cycles. This high desorption efficiency may be explained by the protonation of the adsorbent surface with an acidic agent.54 This observation showed that the Fe3O4–chitosan can be easily recovered with acid treatment. Hence, it can be used as an economical and effective adsorbent for fluoride removal from water due to its high potential for reusability. The stability of the adsorbent was evaluated through determining the concentrations of the dissolved iron ions in the solution during the five consecutive cycles. It was observed that the concentrations of the dissolved iron ions in the solution were at a minimal level (<0.2 mg L−1) during all the cycles; this was below the maximum acceptable iron concentration in drinking water, i.e. 0.3 mg L−1, set by the WHO.1 This ensures that leaching of iron from Fe3O4–chitosan surface might not cause metal pollution in water. Therefore, it can be concluded that Fe3O4–chitosan exhibited good stability and can be applied as a promising adsorbent to remove fluoride from contaminated water with negligible loss of its magnetic properties.
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