Open Access Article
Vu Thi Haua,
Nguyen Thuy Chinhb,
Pham Hoai Linhb,
Nguyen Thi To Loan
a,
Ngo Thi Mai Vieta,
Dang Duc Dung
c and
Nguyen Quoc Dung
*a
aFaculty of Chemistry, Thai Nguyen University of Education, 20 Luong Ngoc Quyen, Thai Nguyen, Vietnam. E-mail: dungnq@tnue.edu.vn
bInstitute of Materials Science, Vietnam Academy of Science and Technology, 18 Hoang Quoc Viet, Nghia Do, Ha Noi, Vietnam
cMultifunctional Ferroics Materials Lab., Faculty of Engineering Physics, Ha Noi University of Science and Technology, 1 Dai Co Viet Road, Ha Noi, Vietnam
First published on 17th December 2025
Magnetic spinel ferrites are attractive adsorbents for complex wastewaters because they couple high affinity with rapid magnetic recovery. Here, a series of Zn-substituted ferrites (Fe1−xZnxFe2O4, x = 0.0–1.0) was synthesized by co-precipitation and systematically characterized. The series samples display particles in the nanoscale range from 8–50 nm, single phase with spinel structure, tunable magnetization, and mesoporosity where the highest surface area of 228 m2 g−1 were estimated for Fe0.4Zn0.6Fe2O4 samples. The point of zero charge is obtained around 6.26, consistent with strong uptake of anionic species under mildly acidic conditions. Batch adsorption toward an organic dye (Direct Red 79, DR79) and an inorganic oxyanion (hexavalent chromium, Cr(VI)) shows optimal removal at pH = 3, with equilibrium contact times of ∼120 min for DR79 and ∼90 min for Cr(VI). Nonlinear kinetic fitting indicates Elovich behaviour for DR79 (heterogeneous chemisorption with site-energy distribution) and pseudo-second-order kinetics for Cr(VI). Intraparticle diffusion contributes to the rate of reaction but is not rate-limiting. Nonlinear isotherm analysis indicates that Freundlich is applicable to both solutes, while Langmuir capacities reach approximately 95.3 mg g−1 and 62.1 mg g−1 for DR79 and Cr(VI), respectively. Thermodynamic analysis reveals spontaneous adsorption in all cases. The uptake of DR79 is endothermic (ΔH° ≈ +79.1 kJ mol−1; ΔG° ≈ −4.5 to −8.5 kJ mol−1; ΔS° ≈ +0.271 kJ mol−1 K−1), whereas Cr(VI) is exothermic (ΔH° ≈ −40.0 kJ mol−1; ΔG° ≈ −2.0 to −0.15 kJ mol−1; ΔS° ≈ −0.126 kJ mol−1 K−1). The results highlight Fe0.4Zn0.6Fe2O4 composition displayed as a magnetically retrievable, dual-function adsorbent capable of treating mixed organic/inorganic contaminants with reliable nonlinear model parameterization for process design.
Conventional treatment methods for dyes and heavy metals (such as chemical precipitation, redox reactions, membrane filtration, and advanced oxidation) often suffer from high cost or generate secondary waste.2,10,11 In contrast, adsorption has emerged as a simple, safe, and economical approach for removing both dyes and metal ions from contaminated water.12,13 The adsorption process is highly flexible and can achieve high removal efficiencies without producing harmful by-products. A wide variety of adsorbent materials – from activated carbons and clays to novel nanomaterials – have been investigated, many of which offer high capacity and reusability.13 In particular, in situ adsorption using solid sorbents is attractive for its operational simplicity and the ease of incorporating adsorbents into water treatment systems.
Nanoscale adsorbents are especially effective due to their large surface area and tunable surface chemistry.14 Among these, magnetic iron oxides and ferrites have gained considerable attention for water treatment.1,15 Ferrites are iron oxide-based magnetic compounds that can be quickly recovered after use by applying an external magnetic field. This feature is a key advantage in wastewater treatment, as it allows for facile separation of the spent adsorbent without filtration or centrifugation. For example, zinc ferrite (ZnFe2O4) is a magnetic spinel that has been widely studied for pollutant removal due to its chemical stability, non-toxicity, low cost, and insolubility in water.12 Unlike pure magnetite (Fe3O4, referred as Fe12+Fe23+O4) which can undergo oxidation or phase changes over time, spinel ferrites like ZnFe2O4 exhibit high phase stability and corrosion resistance.12 They also remain stable in acidic conditions (pH = 2–6), where many metal-oxide adsorbents lose capacity, making them suitable for treating acidic effluents.16,17 Furthermore, the strong magnetization of such materials enables easy recovery and reuse; studies have shown that magnetically separable nano-adsorbents can be regenerated multiple times, maintaining significant removal efficiency over successive cycles.18
Doped or substituted spinel ferrites of the form Fe1−xMxFe2O4 (where M is a divalent metal) allow tuning of the adsorbent's properties.1 Partial substitution of Fe2+ with other cations (e.g. Co2+, Zn2+, Mn2+) can modify the surface chemistry and magnetic behavior of the ferrite, potentially enhancing adsorption performance. In particular, zinc-substituted magnetite (Fe1−xZnxFe2O4) offers a way to adjust the Fe2+/Fe3+ ratio and magnetization of the particles.19 Prior work on analogous ferrites has shown improved dye adsorption at certain doping levels – for instance, Fe1−xCoxFe2O4 with x ≈ 0.5 exhibited optimal uptake of Direct Red 79 at low pH.1 Zinc ferrite and its composites have likewise demonstrated effective removal of organic dyes: ZnFe2O4 on reduced graphene oxide removed ∼98% of methylene blue in 30 minutes under optimal conditions,12 and pure ZnFe2O4 achieved high uptake of anionic dyes like Congo Red at acidic pH (e.g. >90% removal at pH ∼ 3.5).12 However, there have been comparatively fewer studies focusing on a single magnetic nanoadsorbent that can address both heavy metal anions and organic dyes simultaneously. Deploying a dual-function adsorbent for different classes of pollutants is desirable for integrated wastewater treatment, provided it maintains high affinity for both types of contaminants.
To design an efficient adsorption system, it is essential to understand the kinetics and equilibrium behavior of pollutant uptake. Adsorption kinetics reveal how quickly contaminants can be sequestered and often provide insight into the rate-limiting steps (film diffusion, pore diffusion, surface re action, etc.). Many dye and heavy metal adsorption processes follow a pseudo-second-order kinetic model, suggesting chemisorption as the rate-controlling mechanism.20 For instance, studies on similar ferrite nanoadsorbents reported that Direct Red 79 removal obeyed pseudo-second-order kinetics, with intraparticle (intragranular) diffusion also contributing to the overall rate.1 In the case of Cr(VI) adsorption, the uptake rate is often rapid initially and fits well to pseudo-second-order kinetics as well, indicating strong affinity and possible chemical interactions.2 Equilibrium isotherm analysis is equally important: isotherm models such as Langmuir, Freundlich, Temkin, and Redlich–Peterson are commonly applied to describe how pollutants partition between solution and solid phases at equilibrium.1 A Langmuir model assumes monolayer adsorption on a homogeneous surface, while Freundlich and Temkin models account for heterogeneous surface energies and adsorbate–adsorbent interactions. In recent years, researchers have favored non-linear regression methods to determine isotherm and kinetic parameters, rather than linearizing these models. Non-linear fitting avoids the bias and error amplification that can arise from linear transformations of models.21 Indeed, it has been shown that non-linear regression yields more accurate isotherm constants and better reflects the true adsorption capacity.20,21 In this work, we adopt non-linear analysis of adsorption data to obtain reliable kinetic and isotherm parameters, ensuring robust evaluation of the adsorption performance.
Analyzing adsorption thermodynamics provides deeper insight into the nature of the sorption process. The key thermodynamic parameters that are to be considered are the change in Gibbs free energy (ΔG°), enthalpy (ΔH°), and entropy (ΔS°) for adsorption. The spontaneous adsorption process is indicated by negative values of the free energy change (ΔG°), and the magnitude of the enthalpy change ΔH° can distinguish physisorption from chemisorption.1 In general terms, a, ΔH° of less than 20–40 kJ mol−1 is indicative of physisorption, whereby weak forces are the governing forces. Conversely, a ΔH° in the order of 40–200 kJ mol−1 implies chemisorption, involving stronger bonding or possibly surface reactions.1 Temperature-dependent equilibrium studies allow calculation of these parameters. For example, adsorption of DR79 on cobalt-doped ferrite was found to be spontaneous (ΔG° ∼ −5 to −11 kJ mol−1 over 303–323 K) and strongly endothermic (ΔH° ≈ 74.9 kJ mol−1), indicating a chemisorption mechanism.1 Similarly, Cr(VI) adsorption is often enhanced at higher temperatures, which manifests as positive ΔH° (endothermic uptake) and increased adsorption capacity with temperature.2 Besides thermodynamics, mechanistic studies are vital to confirm how contaminants are bound or transformed by the adsorbent. In the case of Cr(VI), iron-based adsorbents can not only attract the anionic Cr(VI) species (such as HCrO4−) electrostatically but also chemically reduce Cr(VI) to the far less toxic Cr(III) form.22 X-ray photoelectron spectroscopy (XPS) and other analyses have indeed confirmed the reduction of Cr(VI) to Cr(III) on Fe-based magnetic sorbents, implicating surface Fe2+ as the electron donor in the redox adsorption mechanism.22 The resulting Cr(III) may remain immobilized on the nanoparticle surface (as Cr(III) complexes or precipitates), effectively removing it from solution In the case of organic dyes such as DR79, the proposed adsorption mechanisms generally involve electrostatic attraction between the negatively charged sulfonate groups of the dye and the positively charged adsorbent surface (at an acidic pH), as well as the potential for π–π interactions or hydrogen bonding with surface functional groups.5 Changes in the adsorbent's FTIR spectra and zeta potential before vs. after dye uptake can provide evidence for these interactions.5 Furthermore, the reusability of the adsorbent is an important practical consideration tied to mechanism: a robust adsorbent should retain its structure and active sites over multiple adsorption–desorption cycles. Magnetic ferrite nanoparticles can be regenerated and reused, though some loss of capacity is expected after repeated cycles.1 For instance, Zn/Co-doped ferrite nanoparticles retained a majority of their dye removal efficiency after a few reuses, until active site saturation gradually reduced performance.1 This highlights the balance between strong binding (good for high initial uptake) and ease of desorption (good for complete regeneration).
Nanoparticles as dual adsorbents for Cr(VI) and Direct Red 79 are aimed at developing a single magnetic nanoadsorbent capable of removing both an inorganic contaminant (Cr(VI)) and an organic dye (DR79) from water. In this work, Zn-substituted iron ferrite nanoparticles were synthesized and characterized, and their dual adsorption performance was evaluated. Batch adsorption experiments were conducted to measure removal efficiencies under varying conditions, and the data were analyzed with multiple kinetic models (pseudo-first-order, pseudo-second-order, intraparticle diffusion) and isotherm models (Langmuir, Freundlich, etc.). Non-linear regression was employed to fit the models for accurate parameter determination, following best practices in adsorption modeling.21 Thermodynamic parameters (including of ΔG°, ΔH°, ΔS°) were calculated to determine the spontaneity and heat changes of the adsorption of Cr(VI) and DR79. Finally, we investigated the adsorption mechanisms for each pollutant by examining factors such as pH effects, potential redox interactions, and changes in the adsorbent's properties after uptake. By focusing on both magnetic retrievability and broad-spectrum adsorption capability, this study provides insight into the design of versatile nanoadsorbents for comprehensive wastewater remediation.1,12 The findings provide a mechanistic understanding of the application of magnetic Fe1−xZnxFe2O4 in the treatment of wastewater contaminated with a mixture of organic and inorganic pollutants. In addition, they offer practical guidance on its utilisation.
The fabrication process of Fe1−xZnxFe2O4 was used to similar to that of Fe1Fe2O4 nanoparticles. However, instead of using FeCl2, a portion of the mixed solution was replaced by ZnCl2 in a certain ratio, as shown in Table S1. The pure ferrite sample (Fe1Fe2O4) and zinc-doped ferrite (Fe1−xZnxFe2O4) samples with Zn concentrations of 20%, 40%, 50%, 60%, 80%, and 100% were prepared and labeled as FZ0, FZ2, FZ4, FZ5, FZ6, FZ8, and FZ10, respectively.
To investigate the adsorption mechanisms, the experimental kinetic data were fitted using the following nonlinear kinetic models:
Pseudo-first-order model (PFO):
| qt = qe(1 − e−k1t) |
Pseudo-second-order (PSO):
Elovich:
Intraparticle diffusion (Weber–Morris):
| qt = kid × t1/2 + C |
The fitting quality of each model was assessed using the coefficient of determination R2, root mean square error (RMSE), and the consistency of calculated qe with experimental values.
Equilibrium adsorption data were further fitted using nonlinear forms of classical isotherm models.
Where qm (mg g−1) is the maximum adsorption capacity, R is the universal gas constant (8.314 J mol−1 K−1), and T is the absolute temperature (K).
Langmuir isotherm:
Freundlich isotherm:
| qe = KFC1/ne |
Temkin isotherm:
Dubinin–Radushkevich (D–R) isotherm:
| qe = qm × e−Bε2 |
, E is mean adsorption energy
; qm is theoretical saturation capacity (mg g−1); B is D–R constant related to mean adsorption energy (mol2 kJ−2); and ε is Polanyi adsorption potential (J mol−1).
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| Fig. 1 FE-SEM images of Fe1−xZnxFe2O4 nanoparticles with varying Zn2+ substitution ratios: (a) FZ0, (b) FZ2, (c) FZ4, (d) FZ5, (e) FZ6, (f) FZ8, and (g) FZ10. | ||
Transmission electron microscopy (TEM) images further confirm the nanoscale morphology of the Fe1−xZnxFe2O4 nanoparticles as shown in Fig. 2(a–g) for FZ0 to FZ10 samples, respectively. FZ0 and FZ2 (Fig. 2(a and b)) show relatively more agglomerated structures, suggesting stronger interparticle interactions possibly due to limited zinc substitution. Across all samples (FZ0 to FZ10), the particles appear as loosely aggregated clusters composed of fine, quasi-spherical nanocrystallites with typical sizes in the range of 8–10 nm. As the Zn2+ content increases (FZ4–FZ6, Fig. 2(c–e)), the particles appear better dispersed, with slightly reduced agglomeration. This suggests that Zn2+ substitution may disrupt the magnetic interactions between Fe sites, reducing aggregation. FZ8 and FZ10 (Fig. 2(f and g)) still maintain nanoscale morphology but show increased particle overlapping and darker contrast, which may indicate either increased particle size or stacking of multiple nanocrystallites.
The XRD patterns of the synthesized Fe1−xZnxFe2O4 (FZ0–FZ10) samples are shown in Fig. 3(a). All samples exhibit characteristic diffraction peaks at 2θ ≈ 30.1°, 35.5°, 43.1°, 53.5°, 57.0°, and 62.6°, which correspond to the (220), (311), (400), (422), (511), and (440) planes of the cubic spinel structure, respectively, and are in good agreement with the standard JCPDS card no. 22-1086 for Fe1Fe2O4 crystal structure. This confirms the formation of a single-phase spinel structure. With increasing Zn2+ content, the diffraction peaks slightly shift toward lower angles, indicating lattice expansion due to the substitution of Fe2+ (ionic radius ∼0.78 Å) with larger Zn2+ ions (ionic radius ∼0.82 Å). The observed distortion in the lattice parameters of the Fe1Fe2O4 samples as a function of Zn dopant concentration supports the random distribution of Zn ions within the host lattice of Fe1Fe2O4 crystals. Furthermore, the evidence of the random substitution of Zn2+ cations into the host lattice of Fe1Fe2O4 crystals was supported by Raman spectroscopy, where the presence of Zn2+ cations altered the characteristic vibrational modes of Fe1Fe2O4.
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| Fig. 3 (a) XRD patterns, (b) Raman spectra, (c) FTIR spectra, and (d) magnetic hysteresis loops at room temperature. | ||
In the Raman spectra (Fig. 3(b)), all samples exhibit a prominent peak in the region of ∼675–680 cm−1, which corresponds to the A1g symmetric stretching vibration mode of the metal–oxygen (M–O) bond in the tetrahedral sites of the spinel lattice. As the Zn2+ content increases from FZ0 to FZ10, a noticeable red shift of this peak is observed accompanied by a progressive broadening of the peak profile. This shift toward lower wavenumbers indicates a structural change resulting from the substitution of Fe2+ ions by Zn2+ ions at the tetrahedral sites. Since Zn2+ has a larger ionic radius (0.82 Å) than Fe2+ (0.77 Å) and forms weaker Zn–O bonds, the replacement reduces the vibrational frequencies, thereby accounting for the observed peak shift and broadening. Additionally, the incorporation of nonmagnetic Zn2+ weakens the superexchange interactions between tetrahedral and octahedral sites, leading to decreased lattice stiffness. The broadened and red-shifted Raman peak also reflects increased cation redistribution and local structural disorder within the spinel lattice. These observations provide further evidence for the successful formation of a Fe1−xZnxFe2O4 solid solution structure and are consistent with the phase evolution revealed by XRD analysis. The absence of secondary ZnO diffraction peaks in the XRD patterns confirms that Zn2+ ions are incorporated into the spinel lattice rather than forming a separate ZnO phase.
In addition, the random distribution of Zn2+ cations into the host Fe1Fe2O4 crystal structure was investigated using Fourier Transform Infrared (FTIR) spectroscopy. The substitution of Fe2+ by Zn2+ led to modifications in the Fe–O vibrational modes, indicating changes in the bonding environment due to Zn incorporation. The effect of Zn2+ ion substitution on the chemical structure of Fe1−xZnxFe2O4 (FZ0–FZ10) samples was investigated through Fourier transform infrared spectra (Fig. 3(c)). The IR absorption bands of the spinel ferrite at low wavenumber related to the vibrational groups of metal–oxygen bonds.23 Although the spectrum was run from 500 cm−1 to 4000 cm−1, the bands related to metal-oxide bonds below 1200 cm−1 are considered. The bands with peaks at 635 and 590 cm−1 are the characteristic absorption bands of Fe–O bonds in Fe1Fe2O4 nanoparticles.24,25 The bands with peaks at 635 and 590 cm−1 correspond to the stretching vibrations of Fe3+–O bonds and Fe2+–O bonds in tetrahedral sites (A-sites). Compared with the pristine Fe1Fe2O4 nanoparticles, the intensity and peak positions of Fe–O bond sites have a slight shift and become narrowed when increasing the concentration of Zn2+ ion substitution. This evidence shows a change in the chemical structure of Fe1−xZnxFe2O4 samples, demonstrating that Fe2+ ions are substituted by Zn2+ cations at A-sites in the crystal lattice of Fe1Fe2O4 lead to change in crystalline field effect and strain in lattice by the increase of Zn2+ amounts.
Indirect evidence of the replacement of Fe2+ cations in the host lattice by Zn2+ cations indicated a significant effect on the magnetic properties of the Fe1Fe2O4 material. Magnetic hysteresis loops (Fig. 3(c)) at room temperature confirm the ferromagnetic nature of the synthesized nanoparticles, with a notable decrease in saturation magnetization (MS) values as Zn2+ concentration increases. Pure Fe1Fe2O4 exhibits the highest saturation magnetization value, approximately 92.8 emu g−1. This value decreases monotonically with increasing Zn2+ substitution, reaching around 18.2 emu g−1 for ZnFe2O4 (ZF10 sample). The reduction in MS values correlate directly with Zn2+ substitution, indicating that Zn2+ ions replace Fe2+ in the tetrahedral sites. This substitute consequently dilutes the magnetic interactions, as Zn2+ cations are non-magnetic and do not contribute to the overall magnetic moment.
Fig. 4(a) presents the UV-Vis diffuse reflectance spectra (DRS) of the Zn2+-doped Fe1Fe2O4 samples with various of Zn amounts. All samples exhibited strong absorption in visible and near-infrared regions, characteristic of Fe1Fe2O4-based materials. With increasing Zn2+ content, the absorption edge gradually shifted toward longer wavelengths (red-shift), indicating a narrowing of the optical band gap. This red-shift can be attributed to the substitution of Fe2+/Fe3+ of host Fe1Fe2O4 crystal structural by Zn2+ ions, which alters the electronic structure and induces lattice distortions, thereby generating defect states within the band gap. The Tauc plots, (αhv)2 as function of absorption photon energy (hv), in Fig. 4(b–h) was used to determine the direct optical band gap energies (Eg), revealing a progressive decrease from approximately 2.299 eV for FZ0 to 1.933 eV for FZ10. As shown in Fig. 4(i), the reduction in Eg values follow a non-linear trend, with a slow decrease for Zn dopant concentration below 40 mol% and a more pronounced drop for Zn dopant amounts over 80 mol%, possibly due to the solubility limit of Zn2+ in the Fe1Fe2O4 lattice and the associated structural distortions. The narrowed band gap enhances visible-light absorption and may promote surface activation under ambient light. In other words, the substitution of Zn2+ cations into the host Fe1Fe2O4 crystal significantly affected the crystal structure and strongly modified the properties of the host material.
For further characterization of the absorbance properties of Zn-modified Fe1Fe2O4 samples, surface area and pore volume are important parameters that must be optimized prior to evaluating their adsorption performance for Direct Red 79 (DR79). The nitrogen adsorption–desorption isotherms presented in Fig. 5(a and b) exhibit typical type IV behavior with H3-type hysteresis loops, confirming the presence of mesoporous structures. This mesoporosity is attributed to interparticle voids originating from the aggregated Fe1−xZnxFe2O4 nanoparticles, in agreement with the morphology observed in the TEM images.
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| Fig. 5 Nitrogen adsorption–desorption isotherms of Fe1−xZnxFe2O4 samples with different Zn2+ substitution levels: (a) FZ0, FZ2, and FZ4; (b) FZ5, FZ6, FZ8, and FZ10. | ||
Table 1 presents detailed BET surface area and pore characteristics, showing that the BET surface area significantly increases with Zn content, peaking at 228.109 m2 g−1 for sample FZ6, before declining at higher Zn concentrations. The increase in surface area is consistent with decreased particle and pore size, suggesting enhanced porosity and higher active sites availability for adsorption.
| Samples | BET area (m2 g−1) | Pore volume (cm3 g−1) | Pore size (nm) |
|---|---|---|---|
| FZ0 | 142.25 | 0.310 | 9.0 |
| FZ2 | 142.19 | 0.296 | 8.0 |
| FZ4 | 163.19 | 0.276 | 6.8 |
| FZ5 | 165.10 | 0.281 | 6.8 |
| FZ6 | 228.11 | 0.225 | 4.2 |
| FZ8 | 181.41 | 0.243 | 5.4 |
| FZ10 | 101.12 | 0.137 | 5.5 |
The full DLS intensity distributions of the samples are provided in Fig. S1. The mean hydrodynamic diameters in Fig. 6(a) were extracted from the dominant peak in each distribution to ensure consistent comparison, since FZ0 exhibited a secondary peak associated with a minor agglomerated fraction.
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| Fig. 6 (a) Mean hydrodynamic diameter of Fe1−xZnxFe2O4 samples obtained from the dominant peak in the DLS distributions; (b) zeta potentials of the samples; and (c) point of zero charge (pHi) of FZ6. | ||
Fig. 6(a) shows the hydrodynamic particle sizes of the Fe1−xZnxFe2O4 samples measured in deionized water. All samples consist of nanoscale primary crystallites but form secondary aggregates in dispersion due to magnetic dipole–dipole interactions. Among the series, the FZ6 sample displays a relatively narrow and symmetric size distribution, whereas FZ0 exhibits a bimodal profile and FZ10 shows a broader distribution associated with partial agglomeration. The mean hydrodynamic diameter of FZ6 (239.7 nm) therefore reflects a more stable dispersion state compared to the other compositions.
The zeta potential values in Fig. 6(b) further supports this observation. All samples possess negative surface charge, consistent with the presence of deprotonated surface –OH groups. However, the magnitude of the negative potential reaches a maximum in FZ6 (−85.2 mV), indicating stronger electrostatic repulsion between particles and enhanced colloidal stability. Although the absolute zeta potential is expected to shift under the acidic conditions used for adsorption (pH 3), the relative trend in surface charge among the samples remains unchanged and thus remains mechanistically meaningful.
Overall, although the BET surface area increases with Zn substitution and reaches its maximum for FZ6 (Table 1), the choice of FZ6 as the representative sample is further supported by its physicochemical dispersion behavior. As seen in Fig. 6, FZ6 exhibits a relatively narrow hydrodynamic size distribution and the most negative zeta potential (−85.2 mV), indicating superior colloidal stability compared to the other samples. The combination of large accessible surface area, reduced agglomeration, and strong negative surface charge suggests that FZ6 provides more effective active sites and enhanced interaction with aqueous pollutants. Therefore, FZ6 was selected for the subsequent adsorption and mechanistic studies.
The ΔpH − pHi profile (Fig. 6(c)) gives a point of zero charge of 6.3 ± 0.1. Accordingly, the surface of FZ6 is positively charged below pH of 6.3 and negatively charged above this value. This explains the markedly higher uptake of anionic species, HCrO4−/Cr2O72− for Cr(VI) and sulfonated DR79−, under mildly acidic conditions via electrostatic attraction and specific interaction with surface
M–OH2+ sites. When pH exceeds pHi, deprotonation (
M–O−) leads to electrostatic repulsion and a pronounced drop in capacity; residual adsorption is attributed to hydrogen bonding and π–π interactions. The speciation shift of Cr(VI) (pKa of 6.5) from HCrO4− to CrO42− above pH of 6.3 further strengthens this trend.
At pH values of 3, extensive protonation maximizes the density of
M–OH2+ sites, which electrostatically attract the sulfonated dye anions DR79−, leading to high uptake. When pH values over 6.26, deprotonation produces
M–O− sites; electrostatic repulsion dominates, and the adsorption efficiency drops sharply. In addition, excess OH− at high pH competes with dye anions for surface sites.26,27 These observations agree with Dai et al.,28 who reported that cationic dyes are favored at high pH whereas anionic dyes are favored at low pH values. A similar pH-dependence has been reported for DR79 adsorption on FZ6. Based on these results, pH values of 3 were selected as the optimal pH for subsequent DR79 adsorption experiments on FZ6.
, a van't Hoff analysis (Fig. 7(c) and Table 2) usingΔG° = −RT ln KD = ΔH° − TΔS° |
| T° (K) | 1/T° (K−1) | Ce (mg L−1) | qe (mg g−1) | KD | ΔG° (kJ mol−1) | ΔH° (kJ mol−1) | ΔS° (kJ mol−1 K−1) |
|---|---|---|---|---|---|---|---|
| 308 | 0.003247 | 14.064 | 82.420 | 5.860 | −4.528 | 79.092 | 0.271 |
| 313 | 0.003195 | 10.941 | 86.323 | 7.890 | −5.375 | ||
| 318 | 0.003145 | 6.344 | 92.070 | 14.514 | −7.073 | ||
| 323 | 0.003096 | 4.025 | 94.969 | 23.596 | −8.489 |
The parameters determined at the investigated temperatures are summarized in Table 2.
Linear regression of the van't Hoff plot (ln
KD vs. t/T) yields ΔH°, and ΔS°, consequently, ΔG°, −RT
ln
KD ranges from −4.528 to −8.489 kJ mol−1, confirming spontaneity and increasing favorability with temperature. The positive enthalpy changes ΔH° values of 79.092 kJ mol−1, indicates an endothermic process; increasing temperature enhances dye uptake, which is commonly associated with activation of chemisorptive interactions and/or reduced hydration of dye anions at the solid–liquid interface. The positive entropy changes ΔS° values of 0.271 kJ mol−1 K−1, suggests an increase in randomness during adsorption, plausibly due to the release of structured water molecules from the hydrated dye and surface sites upon complexation.
Combining the pH, kinetic, and thermodynamic results, DR79 removal by FZ6 proceeds most efficiently under mildly acidic conditions (pH values of 3) with an equilibrium contact time of around 120 min and is favored at elevated temperatures. The electrostatic attraction between protonated ferrite surfaces and sulfonated dye anions is the primary driving force, while the magnitude of ΔH° points to a significant chemisorption contribution.
KD and
(Fig. 8(c) and Table 3 yields thermodynamic parameters: the standard Gibbs free energy change ΔG° ranges from −2.032 to −0.146 kJ mol−1, indicating a spontaneous but weakly driven process; the enthalpy change is ΔH° values of −40.011 kJ mol−1, evidencing an exothermic adsorption, i.e., lower temperatures favor uptake; and the entropy change is ΔS° values of −126 J mol−1 K−1, implying decreased randomness at the solid–liquid interface, likely due to the ordering/immobilization of chromate and interfacial water upon adsorption.
| T (K) | 1/T (K−1) | Ce (mg L−1) | qe (mg g−1) | KD | ΔG° (kJ mol−1) | ΔH° (kJ mol−1) | ΔS° (kJ mol−1 K−1) |
|---|---|---|---|---|---|---|---|
| 303 | 0.00330 | 7.163 | 16.047 | 2.240 | −2.032 | −40.011 | −0.126 |
| 308 | 0.00325 | 8.624 | 14.220 | 1.650 | −1.281 | ||
| 313 | 0.00320 | 9.813 | 12.734 | 1.298 | −0.678 | ||
| 318 | 0.00315 | 10.839 | 11.452 | 1.057 | −0.146 |
In summary, FZ6 removes Cr(VI) most effectively under mildly acidic conditions (pH values of 3) with an equilibrium contact time of around 90 min; adsorption is spontaneous, exothermic, and accompanied by an entropy decrease consistent with formation of ordered surface complexes.
As summarized in SI – Table S2, the Elovich model exhibited the best fitting performance across all concentrations. For instance, at C0 of 40 mg L−1, the Elovich model yielded a reduced χ2 value of 0.452, R2 = 0.9684, and an adjusted R2 = 0.9639, significantly outperforming other models. A similar trend was observed for C0 of 50 mg L−1 and 60 mg L−1, where the Elovich model consistently showed the lowest reduced χ2 (1.023 and 1.476, respectively) and the highest R2 values (0.9670 and 0.9605, respectively).
These results indicate that the Elovich model provides the most accurate description of the adsorption kinetics. The suitability of this model suggests that the adsorption process involves heterogeneous surface binding and chemisorption, which is consistent with the presence of energetically non-uniform sites on the composite surface. Moreover, the poor fitting of the PFO and IPD models, particularly their relatively high χ2 and low R2 values, further confirms that the adsorption process does not follow simple diffusion or first-order kinetics.
Therefore, the Elovich model can be considered the most appropriate kinetic model for describing the adsorption behavior of the material under the tested conditions.
To evaluate the adsorption behavior of the material, four common isotherm models, including of Langmuir, Freundlich, Temkin, and Dubinin–Radushkevich (D–R), were fitted to the experimental data using nonlinear regression. The fitted curves are shown in Fig. 9(d), and the corresponding model parameters along with the goodness-of-fit indicators are summarized in Table 4. Among the models, the Freundlich isotherm provided the best fit to the data, with the highest coefficient of determination (R2 of 0.9991) and the lowest reduced chi-square value (0.013). This suggests that the adsorption occurred on a heterogeneous surface with multilayer coverage and varying adsorption energies. The Langmuir model also showed a strong correlation (R2 = 0.9916), indicating a significant monolayer adsorption component on the surface. The maximum adsorption capacity (qmax) was estimated to be 95.3 mg g−1. The Temkin model (with a moderate R2 value of 0.9892), suggests that interactions between adsorbate molecules may be involved during the adsorption process. The Temkin constant B (22.87) also indicates moderate heat of adsorption.
| Model | Main parameters | R2 | χ2 |
|---|---|---|---|
| Langmuir | qmax = 95.295, KL = 0.01387 | 0.9916 | 0.259 |
| Freundlich | KF = 4.170, n = 1.751 | 0.9991 | 0.013 |
| Temkin | BT = 22.87, KT = 0.111 | 0.9892 | 0.334 |
| D–R | qmax = 53.757, β = 0.31275 | 0.9474 | 1.620 |
In contrast, the D–R model showed the poorest fit (R2 values of 0.9474 and χ2 values of 1.620), indicating that pore-filling mechanisms were less dominant in this adsorption process.
Based on these results, the Freundlich and Langmuir models were found to be the most appropriate for describing the adsorption behavior, while the D–R and Temkin models provided limited predictive value.
Langmuir, Freundlich, Temkin, and Dubinin–Radushkevich (D–R) models were investigated and are shown in Fig. 10(d) and Table 5. Among these models, the Freundlich model showed the highest correlation coefficient (R2 = 0.9938) and the lowest reduced χ2 value (0.437), suggesting that the adsorption process follows a heterogeneous multilayer mechanism. The adsorption intensity n = 1.786 further confirms a favorable adsorption process (since 1 < n < 10). The Langmuir model also provided a good fit, with R2 values of 0.99112 and qmax values of 62.063 mg g−1, indicating a relatively high adsorption capacity assuming monolayer coverage. However, its slightly higher chi-square value compared to Freundlich implies less agreement with the experimental data. The Temkin model yielded a lower correlation (R2 values of 0.9899), with BT values of 14.675 and KT values of 0.22272, indicating moderate interactions between adsorbate and adsorbent. The D–R model, on the other hand, showed the poorest fit (R2 values of 0.9245 and high χ2 values of 5.314), suggesting that its assumptions may not be suitable for describing the Cr(VI) adsorption onto FZ6 in this case. In summary, the adsorption of Cr(VI) on FZ6 is best described by the Freundlich isotherm, highlighting the heterogeneous nature of the surface and the possibility of multilayer adsorption.
| Model | Main parameters | χ2 | R2 |
|---|---|---|---|
| Langmuir | qmax = 62.063, KL = 0.02685 | 0.625 | 0.9911 |
| Freundlich | KF = 4.037, n = 1.786 | 0.437 | 0.9938 |
| Temkin | BT = 14.675, KT = 0.22272 | 0.710 | 0.9899 |
| D–R | qmax = 36.168, β = 0.07641 | 5.314 | 0.9245 |
As summarized in Table 6, FZ6 delivers a Langmuir capacity of 95.30 mg g−1 for DR79 at pH values of 3 (dose 0.8 g L−1, t = 120 min, C0 = 50 mg L−1). This value exceeds that of Fe1−xCoxFe2O4 (56.85 mg g−1)1 and is slightly higher than a Fe3O4/CeO2 nanocomposite (90.5 mg g−1)31 under similarly acidic conditions. It is 2–10 time greater than low-cost biosorbents (palm-tree waste 9.79 mg g−1; wastewater sludge 13.4 mg g−1; coffee husk 36.63 mg g−1 and also surpasses an iron-oxide/carbon composite (45.8 mg g−1).10 Considering its magnetic retrievability, FZ6 thus couples competitive capacity with facile separation-an advantage over many non-magnetic, low-cost sorbents (Table 7).
| Adsorbent | Adsorbate | pH | Dose (g L−1) | Time (min) | C0 (mg L−1) | qmax (mg g−1) or % removal | Ref. |
|---|---|---|---|---|---|---|---|
| Fe1−xCoxFe2O4 | DR79 | 3 | 0.8 | 120 | 50 | 56.85 | Hau et al.1 |
| Fe3O4/CeO2 nanocomposite | Acid Black 210 | 7 | 1.0 | 120 | 50 | 90.5 | Gao et al.31 |
| Iron oxide/carbon composite | Congo Red | 7 | 0.2 | — | 10 | 45.8 | Singh et al.10 |
| CoFe1.9Sm0.02O4@CS-ECH | Orange II | 6 | 2.0 | 180 | 50 | 209.3 | Humelnicu et al.32 |
| SF-B-CoNiAl | Eriochrome Black T | 2 | 0.33 | 180 | 20 | 329.61 | Elkhider et al.33 |
| Methyl Orange | 4 | — | 180 | 20 | 219.56 | ||
| Barium hexaferrite nanoparticles | Congo Red | — | — | 20 | — | 124.7 | Mohammed et al.34 |
| Co0.5Mn0.5Fe2O4 nanoparticles | Congo Red | 2 | 2.5 | 120 | 150 | 58.3 | Zhang et al.35 |
| CoFe2O4 nanoparticles | Congo Red | 4 | 0.3 | 130 | 50 | 13.88 | Sidhaarth et al.36 |
| FZ6 | DR79 | 3 | 0.8 | 120 | 50 | 95.295 | This study |
| Adsorbent | pH | Dose (g L−1) | Time (min) | C0 of Cr(VI) (mg L−1) | qmax (mg g−1) | Ref. |
|---|---|---|---|---|---|---|
| Fe3O4/chitosan/polypyrrole (Fe3O4/CS/PPy) | 2 | 0.5 | 12 h | 100 | 193.23 | Yin et al.7 |
| (Fe3S4)-CTAB | 2 | 0.75 | 60 | 100 | 330.03 | Zhou et al.37 |
| Fe2O3–MnO2–SnO2 | 2 | 2.5 | 90 | 50 | 69.2 | Uddin et al.8 |
| NiFe2O4@AC | 2 | 0.1 | 720 | 150 | 72.62 | Zhang et al.38 |
| NiFe2O4 | 3 | 0.2 | 55 | 20 | 294.1 | Zandipak et al.39 |
| MnFe2O4 | 3 | 3 | 480 | 10 | 5.813 | Lu et al.9 |
| Mg0.2Zn0.8Fe2O4 | 30.49 | Tatarchuk et al.40 | ||||
| Fe3O4 | 4 | 2 | 90 | 0.001 | 8.67 | Zhang et al.41 |
| Magnetic nanobiosorbent from Aspergillus niger biomass | 5.8 | 3.72 | 11 | 23.4 | 92% | Daneshvar et al.42 |
| NiFe2O4 reflux synthesized | 3 | 2 | 120 | 25 | 65% | Padmavathy et al.43 |
| FZ6 | 3 | 0.8 | 90 | 20 | 62.063 | This study |
For Cr(VI), FZ6 achieves a Langmuir qmax of 62.06 mg g−1 at pH values of 3 (dose 0.8 g L−1, t = 90 min, C0 = 20 mg L−1). This performance is comparable to multi-oxide Fe2O3–MnO2–SnO2 (69.2 mg g−1) and NiFe2O4@AC (72.62 mg g−1),8 and significantly higher than MnFe2O4 (5.813 mg g−1),9 Fe3O4 (8.67 mg g−1),41 and Mg0.2Zn0.8Fe2O4 (30.49 mg g−1).40 Although some specialized adsorbents report much larger capacities such as (Fe3S4)-CTAB (330.03 mg g−1)37 or NiFe2O4 (294.1 mg g−1),39 these frequently require harsher acidity (pH values of 2), different doses, or long contact times (e.g., 720 min for NiFe2O4@AC.38 In contrast, FZ6 offers a balanced profile: moderate-to-high capacity at pH values of 3, short equilibrium time (∼90 min), and magnetic separability, while simultaneously functioning as a dual adsorbent for both an anionic dye and a metal oxyanion.
Supplementary information (SI): additional adsorption data, fitting plots, characterization results, and experimental details. See DOI: https://doi.org/10.1039/d5ra07081c.
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