The use of nanoscale zero-valent iron (nZVI) to remove heavy metal ions like Ni2+ from groundwater has been extensively studied; however, the compositional transformation of the Ni2+ and Fe0 during the removal is not clearly comprehensible. This study provides an insight into the componential, structural, and morphological transformations of Ni2+ and Fe0 at a solid–liquid interface using various characterization devices. The underlying mechanism of transformation was investigated along with the toxicity/impact of the transformed products on the groundwater ecosystem. The results indicated that Fe0 is transformed into lath-like lepidocrocite (γ-FeOOH), twin-crystal goethite (α-FeOOH), and spherical magnetite (Fe3O4), while Ni2+ is converted into Fe0.7Ni0.3 alloy and Fe–Ni composite (trevorite – NiFe2O4) with a fold-fan morphology. The Fe0 transformation mechanism includes the redox of Fe0 with Ni2+, H2O, and dissolved oxygen, the combination of Fe2+ and OH produced by Fe0 corrosion to amorphous ferrihydrite, and the further mineralogical transformation to Fe oxides with the aid of Fe2+ adsorbed on ferrihydrite. The conversion of Ni2+ is accomplished by reduction by Fe0 and surface coordination with Fe oxides. Compared with Ni2+ and Fe0, the toxicity and bioavailability of the transformed products are significantly reduced, hence conducive to the application of zero-valent iron technology in groundwater remediation.

  • The experiments were carried out for the mechanism of Fe0 and Ni2+ transformation by nZVI.

  • Heavy metals in wastewater have a direct effect on the transformation rate of Fe0 to Fe2+.

  • Fe0 and Ni2+ transformed into lath-like lepidocrocite, twin-crystal goethite, spherical magnetite, Fe0.7Ni0.3 alloy, and NiFe2O4 after reaction.

  • The environmental toxicity of the transformed products was significantly lower than nZVI and Ni2+.

Nickel ion (Ni2+) is among the most prevalent heavy metal ions that are of concern to human and environmental health (Sprynskyy et al. 2006; Luo et al. 2015; Sachan & Lal 2017; Ahmad et al. 2019). The presence of Ni2+ in the environment through natural and anthropogenic processes makes water and soil unsafe for human consumption and crop cultivation, respectively (Torres-Caban et al. 2019; Hashem et al. 2020). Considering the potential damaging effects of Ni2+, it is important to ensure that the concentration of Ni2+ in environmental media meets the corresponding quality standards.

The removal of Ni2+ from the aquatic system such as groundwater has been achieved through the employment of various techniques such as adsorption (Tsai et al. 2015; Matern et al. 2018; Ong et al. 2018), membrane separation (Volchek et al. 1993; Tanhaei et al. 2014), ion exchange (Moghbeli et al. 2017), bioremediation (Francy et al. 2020; Singh & Mishra 2020), and nanotechnology (Matlochova et al. 2013; Rathor et al. 2017). Among these techniques, nanotechnology which involves the use of nanoscale zero-valent iron (nZVI) has proven effective in reducing Ni2+ (Matlochova et al. 2013; Ulucan-Altuntas et al. 2018; Gil-Díaz et al. 2020).

Extensive efforts have been made to elucidate the performance, influence factors, and mechanism of Ni2+ removal by nZVI. Furthermore, review articles such as Vardhan et al. (2019), Aziz et al. (2023) and Bilal et al. (2021) focused on the removal of toxic metals from aquatic systems by traditional methods, while suggesting methods of improving low cost adsorbents to ensure efficient removal of heavy metals. It is worth noting that there are few reports on the transformations of Fe0 in the aqueous system as compared to the traditional methods of removing toxic substances from water. For instance, Roh et al. (Filip et al. 2019; Gil-Díaz et al. 2020) investigated the conversion of Fe0 filing/foam in reactive iron barrier under varying conditions (alkalinity, pH) and types of contaminants (TCE, U-235, Tc) in the field and laboratory. Amorphous iron (hydr)oxides, intermediate products (green rusts), and hydrated forms of ferric oxides such as goethite (α–FeOOH), ichlorina (β–FeOOH), and lepidocrocite (γ–FeOOH) were identified as the main corrosion products of Fe0. The composition of the products varied with contaminant identities, iron types, and environmental media. Anang et al. (2021) examined the compositional evolution of nZVI in the ichlorination of 2,4-dichlorophenol by attapulgite-supported Fe/Ni nanoparticles. It was found that ferrihydrite was first formed, which later resulted in the formation of lepidocrocite, goethite, and magnetite. Sohn et al. (Su et al. 2014) employed nZVI to reduce nitrate in the solution that was deoxygenated by a N2 stream for 2 h before adding nZVI, and the results showed that Fe0 was transformed to crystalline magnetite. In addition, ageing of nZVI in static water under oxic and anoxic conditions has been reported (Liu et al. 2015, 2017). The main corrosion product of nZVI at oxic conditions for 72 h is γ–FeOOH, whereas a mixture of FeO, α–FeOOH and β–FeOOH is formed in anoxic water.

Even though the above studies have examined the transformation of Fe0 in static water or in the removal of chlorinated organics, radioactive elements and nutrient contaminants, no investigation has focused on the chemical transformation of Fe0 nanoparticles and Ni2+ during the removal. In particular, the changes in the composition and form of Ni2+ after removal, as well as the potential ecological effects of nZVI and Ni2+ transformation products on the environment have not been reported. This leaves a gap in the literature that needs to be filled. An evaluation on the componential, structural, and morphological transformations of Ni2+ and Fe0 at solid–liquid interface is critical in understanding their fate in the environment and the associated risks, and predicting the application potential of Fe0 nanomaterials in groundwater remediation.

In this study, various methods and devices characterizing material composition, morphology and structure, including scanning electron microscopy (SEM), transmission electron microscopy (TEM), specific surface area analyzer, X-ray diffraction (XRD), and X-ray photoelectron spectroscopy (XPS), are used to identify the transformation products of Ni2+ and Fe0 in nZVI during the removal of Ni2+ by nZVI and elucidate their physicochemical properties. The schematic description of the transformation process is presented. In addition, the implications of transformation of Ni2+ and Fe0 to groundwater remediation are discussed.

Chemicals and materials

The chemicals which included iron(II) sulfate heptahydrate (FeSO4•7H2O), sodium borohydride (NaBH4), and nickel sulfate (NiSO4•6H2O) were purchased from Tianli Chemical Reagent Company in Tianjin, China. All the chemicals were of analytical grade. Deionized water was used to prepare the chemical solutions.

Preparation of nZVI

The liquid phase reduction method was used to prepare the nZVI (Mukherjee et al. 2015; Hu & Li 2018). 50 mL of H2SO4 (0.01 mol/L) was added to 13.9 g of the FeSO4•7H2O before the synthesis. 40 mL of the resulting mixture was then pipetted into a three-necked round bottom flask and stirred mechanically for 5 min (200 rpm). 3.026 g of NaBH4 was mixed with 40 mL of de-ionized water and stirred before adding dropwise to the FeSO4•7H2O solution in the flask. The mixture was mechanically stirred under N2 atmosphere. The resulting mixture was allowed to sit and stir mechanically for 15 min after all the NaBH4 solution was used up. The as-prepared nZVI was vacuum-filtered and washed with deionized water. The material was then dried under vacuum at −30 °C for 14 h in a freeze dryer.

Batch experiments

The nZVI was used to remove Ni2+ in the solution in order to investigate the transformation of the Ni2+ and Fe0 after removal. At the initial stages, 0.1 g of the prepared nZVI was added to 200 mL of NiSO4 solution (concentration = 5 mmol/L; initial pH = 4.0 ± 0.1). Two millilitres (2 mL) of the mixture was sampled at pre-determined time intervals (5, 10, 20, 30, 45, 60, 90, and 120 min) and filtered through a 0.45-μm nitrocellulose membrane. The filtrate of the sampled mixture at pre-determined time intervals was measured to determine the removal efficiency by the nZVI. The batch experiments were performed in duplicate in order to ensure precision. The residue of the nZVI after reaction with Ni2+ was freeze dried at −30 °C for 14 h, before used in characterizing the morphological and structural transformations of the Ni2+ and Fe0 (Anang et al. 2021).

Analytical methods

The atomic absorption spectrometer (NOVAA-350 Analytic Jena, Germany) was used to analyze the concentration of Ni2+ after removal. The equipment was calibrated with commercial standards of Ni2+ in order to ensure the identification of Ni2+ in solution. Equation (1) is used to determine the removal efficiency of Ni2+.
(1)
where C0 = initial concentration of Ni2+ and Ct = concentration of Ni2+ at time t.

The concentration of Fe2+ in the solution with different reaction time was measured by spectrophotometry using phenanthroline as the chromogenic agent. The concentration of total iron was determined by an atomic absorption spectrometer. The difference between total iron concentration and Fe2+ concentration is the concentration of Fe3+.

The concentration of dissolved oxygen (DO) was analyzed by a JPSJ-606L dissolved oxygen meter (Shanghai Yidian Scientific Instruments Co. Ltd, China).

Material characterizations

The morphological characteristics of Ni2+ and Fe0 in nZVI before and after reaction (120 min) were analyzed using SEM (Nova 400 Nano, FEI, USA) and TEM (Tecnai G2 F30, S-Twin, FEI, USA). The crystalline structure of the pristine and reacted nZVI was characterized using an X-ray diffractometer (XRD) (D/MAX-2500, Rigaku Co, Japan) operated at 45 kV and 250 mA with Cu Kα. The material surface composition of pristine and reacted nZVI was analyzed with the aid of X-ray Photoelectron Spectrometer (XPS) (Escalab 250Xi, Thermo Fisher Scientific, USA) with a monochromatic Al Kα X-ray source. The binding energies of the samples were calibrated using the C1s peak at 284.8 eV. The specific surface area and pore parameters of nZVI before and after removal of Ni2+ were determined by a specific surface area analyzer (Micromeritics ASAP 2020, USA).

Removal of Ni2+ by nZVI

Figure 1 shows the removal of Ni2+ by nZVI within 120 min. It is observed that 16.2% of the Ni2+ was removed within 5 min. An increase in the removal efficiency of the Ni2+ was evident from 5 to 90 min (48.6%). A slight decline in removal was achieved at 120 min (46.4%), and could be attributed to desorption of the Ni2+. This could have occurred due to the competitive adsorption of H+ and Ni2+ in the solution when the reaction time was prolonged. The initial pH of 5-mmol/L Ni2+ solution in this study was set at 4 to make the final pH after the reaction less than the minimum pH (6.2) for Ni2+ to form Ni(OH)2 precipitation, in order to determine the real product of Ni2+ transformation. However, this resulted in a lower removal rate of Ni2+ by nZVI. The impact of selectivity by other heavy metal ions on the removal efficiency of Ni2+ is shown in Supplementary material, Figure S1.
Figure 1

Removal of Ni2+ by nZVI (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Figure 1

Removal of Ni2+ by nZVI (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Close modal

Compositional transformation of Ni2+ and Fe0 in nZVI

XRD analyses

The XRD spectra of the nZVI before and after reaction with Ni2+ are shown in Figure 2. The peaks at 44.7°, 65.0°, and 82.3° (JCPDS No 06-0696) are indicative of Fe0 in both the pristine and reacted nZVI spectra. The same peaks denote the presence of Fe0.7Ni0.3 (JCPDS No 03-1049) in the reacted nZVI spectrum. It is worth noting that Ni0 existed in the form of Fe–Ni alloy in this study, and not nickel metal. This may be caused by Fe0 at some sites on the nZVI surface reducing Ni2+ to Ni0, and Ni0 combining with Fe0 at other sites. The intensity of the Fe0 peaks in the reacted spectrum decreased drastically, thus, denoting transformation into Fe oxides and Fe–Ni composite. The peaks at 27.0°, 36.3°, 38.0°, and 60.2° denote lepidocrocite (JCPDS No 44-1415, formula: γ-FeOOH), while those at 21.2°, 34.6°, and 41.1° indicate goethite (JCPDS No. 81-0463, formula: α-FeOOH). Moreover, those at 35.4° and 62.5° (JCPDS No. 19-0629) denote the presence of magnetite (Fe3O4), and 35.6°, 57.3°, 63.0° (JCPDS No 44-1485) denote the presence of trevorite (NiFe2O4). Apparently, Fe0 is transformed into lepidocrocite, goethite, magnetite, and Fe–Ni oxide composites (NiFe2O4) by the reaction of nZVI with Ni2+. Moreover, by comparing the peak intensity of the three iron oxides it can be inferred that lepidocrocite is the predominant transformation product of Fe0. This result is consistent with recent studies on the conversion of nZVI ageing in oxygenated water (Liu et al. 2013; Pullin et al. 2017). For Ni2+, in addition to forming NiFe2O4 composite with iron oxides, it also reacts with Fe0 to form Fe–Ni alloy. To the best of our knowledge, the reaction of Ni2+ with nZVI to form these two transformation products is now being reported by this study. Therefore, other characterization techniques were employed for further confirmation.
Figure 2

XRD patterns of nZVI before and after reaction with Ni2+ (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Figure 2

XRD patterns of nZVI before and after reaction with Ni2+ (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Close modal

SEM analyses

Figure 3 shows the SEM images of unreacted and reacted nZVI. The morphology of the unreacted nZVI shows particle agglomeration which is the result of the electrostatic and magnetic properties of the Fe0 nanoparticles (Figure 3(a)) (Dalla Vecchia et al. 2009; Ahmed et al. 2017; Eljamal et al. 2020; Ken & Sinha 2020; Pasinszki & Krebsz 2020; Cheng et al. 2021). Some of the Fe0 nanoparticles were present after the reaction (Figure 3(b)). The core of most Fe0 nanoparticles was hollowed out, leaving behind a shell. However, Liu et al. (2013) indicated that the Fe oxide shell on the surface of nZVI would collapse with time. Therefore, the existence of the Fe oxide shell in this study may be due to the fact that Fe0.7Ni0.3 alloy enhanced the strength of the Fe oxide shell, which also proved the formation of Fe0.7Ni0.3. Nevertheless, the deposition of Fe0.7Ni0.3 on the surface of the Fe oxide shell made the morphology of Fe0.7Ni0.3 difficult to be recognized. The morphology in Figure 3(b) includes lath rods and twin-crystal rods which can be attributed to lepidocrocite (L) and goethite (G), respectively (Anang et al. 2021). The approximate spherical morphology that appears to be clustered is indicative of magnetite (M), whereas the plate-like morphology denotes trevorite (T).
Figure 3

SEM images of pristine nZVI (a) and reacted nZVI (b) (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Figure 3

SEM images of pristine nZVI (a) and reacted nZVI (b) (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Close modal

TEM analyses

The TEM images of pristine and reacted nZVI are shown in Figure 4. The dark core in the chain-like morphology is the Fe0 core (Figure 4(a)). The hollowed chain-like morphology in Figure 4(b) is attributable to the Fe oxide shell deposited with Fe0.7Ni0.3. The plate-like morphology identified in the SEM image is clearly presented as an open folding fan in Figure 4(b), indicating that trevorite is a fan-shaped crystal. Moreover, the characteristic morphology of lepidocrocite (lath-like crystals) and goethite (twin crystals) are clearly distinguished. Spherical magnetite appeared to emerge from lepidocrocite.
Figure 4

TEM images of pristine nZVI (a) and reacted nZVI (b) (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Figure 4

TEM images of pristine nZVI (a) and reacted nZVI (b) (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Close modal
The HR-TEM images of the nZVI after reaction with Ni2+ are shown in Figure 5. The interplanar spacing (d-spacing) further confirm the morphological characteristics outlined in the TEM images. The d-spacing values in Figure 5(b) (0.153, 0.208, and 0.247 nm) match well with the (002, 311, and 301) planes of orthorhombic structured lepidocrocite, thus suggesting that lath-like morphology in Figure 5(a) is attributed to lepidocrocite. Similarly, the d-spacing value (0.112, 0.128, and 0.242 nm) in Figure 5(c) demonstrates that the spherical particle attached to the hollowed chain is magnetite. The d-spacing value (0.117 nm) in Figure 5(c) matches the (211) plane of Fe0, indicating that Fe0 is present in the hollowed chain. The d-spacing values in Figure 5(e) and 5(f) confirm the trevorite and Fe0.7Ni0.3 morphologies in Figure 5(d), while the d-spacing values in Figure 5(h) and 5(i) verify the goethite morphology of twin-rod in Figure 5(g).
Figure 5

TEM (a, d, g) and HR-TEM images (b, c; e, f; and h, i) of nZVI reacted with Ni2+ (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Figure 5

TEM (a, d, g) and HR-TEM images (b, c; e, f; and h, i) of nZVI reacted with Ni2+ (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Close modal
The TEM-mapping in Figure 6 clearly depicts the elemental composition of the individual morphologies in Figure 5. It is observed that the laths in the upper left corner in Figure 6(a) are indeed characteristic of lepidocrocite due to the plentiful Fe (Figure 6(c)) and O (Figure 6(b)) elements in that region as opposed to Ni in Figure 6(d). Additionally, the hollow tube/chain of spheres contained more Fe and Ni elements as compared to the O elements. This further iterates the demonstration of Fe0.7Ni0.3 by the hollow chain of spheres. The morphology of the folding fan in Figure 6(e) contained Fe, Ni, and O elements (Figure 6(f)–6(g)). However, the O content at the bottom of Figure 6(f) which depicts the hollowed spheres was sparsely distributed as compared to those of Fe and Ni. This also confirms the presence of Ni0 as Fe0.7Ni0.3 composite metal. The twin rods in Figure 6(i) formed an apparent fan shape which is encysted by the red oval. More Fe and O elemental composition confirms the presence of FeOOH species (goethite). However, trevorite could have been present in the dark portions of the morphology in Figure 6(i). This assertion is due to the rich distribution of Ni in the identified parts.
Figure 6

TEM images (a, e, i) and TEM-mapping (b, c, d; f, g, h; and j, k, l) of nZVI reacted with Ni2+ (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Figure 6

TEM images (a, e, i) and TEM-mapping (b, c, d; f, g, h; and j, k, l) of nZVI reacted with Ni2+ (initial Ni2+ concentration = 5 mmol/L; nZVI dosage = 0.5 g/L; initial pH = 4.0 ± 0.1; final pH = 5.4 ± 0.1; temperature = 25 ± 1 °C).

Close modal

XPS analyses

Figure 7 shows the wide scan spectra of pristine and reacted nZVI, as well as narrow scan spectra depicting the Fe 2p, O 1s and Ni 2p regions. The intensity of the Fe 2p peaks after Ni2+ removal was higher than those of the pristine nZVI (Figure 7(b)). Similarly, the Fe2+ (∼715.1 and ∼728.0 eV) and Fe3+ (∼719.7 and ∼732.5 eV) peaks were higher in intensity with a decreased Fe0 peak (∼706.7 eV). The reduced Fe0 peak reiterates conversion into Fe2+ and Fe3+. The O 1s region shows the presence of metallic O (∼529.8 to ∼530 eV) and organic C–O (∼531.6 eV) (Figure 7(c)). The peak intensity of the O 1s region after the removal was higher. This confirmed the transformation of the Fe0 into more iron hydr(oxides). The Ni 2p3 (∼856.0 eV) and Ni 2p1 (∼873.7 eV) peaks indicated the presence of Ni2+ in the reacted nZVI, which indirectly proves the formation of trevorite (Ni2+Fe3+2O2−4). The peaks at ∼852.3 and ∼870.0 eV are characteristic of Ni0, iterating the existence of Fe0.7Ni0.3.
Figure 7

XPS wide scan spectra (a) and narrow scan spectra of Fe2p (b), O1s (c), and Ni2p (d) of nZVI reacted with Ni2+.

Figure 7

XPS wide scan spectra (a) and narrow scan spectra of Fe2p (b), O1s (c), and Ni2p (d) of nZVI reacted with Ni2+.

Close modal

Mechanism on transformation of Ni2+ and Fe0 in nZVI

The Fe0 in nZVI acted as the reducing agent (EFe2+/Fe = −0.44 V) during the removal, while Ni2+ served as the oxidizing agent (ENi2+/Ni = −0.23 V). The reaction products were Fe2+ and Ni0 (Equation (2)). Ni0 continued to react with Fe0 to form Fe0.7Ni0.3 alloy (Equation (3)). Ni deposited on the surface of nZVI played a de-passivating effect on the iron oxide shell, and acted as an electron acceptor to accelerate the corrosion of the anode (Fe0) of the Fe–Ni galvanic cell and the mineralogical change of Fe0. In addition, H2O and DO also underwent redox reactions with Fe0, resulting in the formation of Fe2+, hydroxyl ions (OH), and hydrogen (Equations (4) and (5)).
(2)
(3)
(4)
(5)
The formed Fe2+ (the change of Fe2+ concentration over time is shown in Figure 8) reacted with OH to produce Fe(OH)2, which was further oxidized by DO to form amorphous iron oxides such as ferrihydrite (Fe5O3(OH)9) (Equations (6)–(8)) (Liu et al. 2007; Aeppli et al. 2019). Subsequently, Fe5O3(OH)9 (represented by FhyOH) was converted to γ-FeOOH with the aid of Fe2+ attached to it (Equations (9) and (10)) (Manning et al. 2002; Boland et al. 2014). Moreover, γ-FeOOH transformed into thermodynamically stable α-FeOOH as the reaction proceeded (Equation (11)) (Pullin et al. 2017). Under acidic conditions, FhyOH + Fe2+ () also became converted to α-FeOOH, but the reaction rate was significantly lower (Equation (12)).
(6)
(7)
(8)
(9)
(10)
(11)
(12)
(13)
Figure 8

Changes in Fe2+ and Fe3+ concentrations during the reaction of nZVI with Ni2+.

Figure 8

Changes in Fe2+ and Fe3+ concentrations during the reaction of nZVI with Ni2+.

Close modal
Figure 9 shows the variation of DO concentration during the removal. It was found that the concentration of DO decreased from the initial 6.3 to <1 mg/L due to consumption in the reaction. Moreover, it can be observed from Figure 8 that Fe2+ concentration increased with time, reaching the maximum at 60 min (113.4 mg/L). A slight decrease was observed until the 120 min (102.1 mg/L) reaction time elapsed. Therefore, the later conversion was carried out under anaerobic conditions, and with the adsorption of Fe2+, γ-FeOOH was converted to magnetite (Fe3O4) (Equation (13)) (Tamaura et al. 1983; Huang et al. 2003). This explains the phenomenon that magnetite appears to be derived from γ-FeOOH in the TEM image of the reacted nZVI (Figure 4(b)). However, the conversion of γ-FeOOH to α-FeOOH and Fe3O4 occurs under specific conditions, thus, lepidocrocite is the primary conversion product of Fe0 in nZVI, while goethite and magnetite are secondary products.
Figure 9

Variation in DO concentration during the reaction of nZVI with Ni2+.

Figure 9

Variation in DO concentration during the reaction of nZVI with Ni2+.

Close modal
Another mechanism of Ni2+ transformation included the surface coordination of Ni2+ with lepidocrocite, goethite and magnetite (iron oxide represented by ≡FeOOH, where ≡ denotes the interface of the iron oxide) to form ≡FeOONi+ (Equation (14)) and (≡FeOO)2Ni (Equation (15)) (Stumm 1992). It is inferred that the occurrence of surface coordination will widen the crystals of twin-rod goethite and lath-like lepidocrocite. Widened crystals in the same plane eventually stick together to form Fe–Ni oxide composites, thus, demonstrating how the apparent fan-shaped morphology which is indicative of trevorite (NiFe2O4) formed. The TEM image of reacted nZVI (Figure 5(d)) shows that the framework of the fan is rod-like and the sector is thin crystal, which well confirms this inference.
(14)
(15)
The compositional transformation of the Ni2+ and Fe0 during the removal process is graphically demonstrated in Figure 10.
Figure 10

Schematic representation of the transformation of Ni2+ and compositional evolution of Fe0 in nZVI during Ni2+ removal.

Figure 10

Schematic representation of the transformation of Ni2+ and compositional evolution of Fe0 in nZVI during Ni2+ removal.

Close modal

Implications of the transformation of Ni2+ and Fe0 to groundwater remediation by nZVI

Researchers perceived that most of the toxicity of nZVI in cells and complete organisms comes from the production of reactive oxygen species (ROS), including free radicals such as hydroxyl radicals, superoxide anions, and non-radical hydrogen peroxide (Liu et al. 2013; Wu et al. 2014). ROS is produced in Fenton and Haber–Weiss reaction with Fe0 as the main initiator (Wang et al. 2012; Wu et al. 2014). However, Fe0 in nZVI undergoes a series of reactions with Ni2+, H2O, and DO during the removal of Ni2+ by nZVI, transforming into lepidocrocite, goethite, and magnetite with the depletion of Fe0. The reactivity of these iron oxides is relatively weak, and it is difficult to react and produce ROS. As a result, the impact on groundwater ecosystems will be significantly reduced. In addition, many researchers reported that iron oxides provide high affinity for heavy metal ions and organic pollutants, which exert certain positive effects on aquatic ecological environment. Kooner (1993) revealed that at neutral pH, although 50% of zinc was still available for transport, almost 100% of lead and copper got adsorbed onto the surface of goethite. Scott et al. (Fendorf et al. 1997) investigated chromate and arsenate retention mechanisms on goethite and it was found that three different surface complexes exist on goethite for both oxyanions. Zhang et al. (Zhang & Huang 2007) examined the adsorption of seven fluoroquinolone (FQ) antibacterial agents with goethite and the results showed that 50–76% of the added FQs were strongly adsorbed by goethite under experimental conditions. Sheydaei et al. (Sheydaei & Khataee 2015) indicated that γ-FeOOH can be effectively used as catalyst in successive ultrasonic/γ-FeOOH /H2O2 processes for decolorization of a textile wastewater containing Reactive Orange 29. Lin et al. (2012) reported the oxidative transformation of bisphenol A (BPA) by laboratory and synthetic commercial goethite, both of which are considered to be effective in inducing BPA conversion.

In addition, the magnetic attraction between nanoscale iron oxide is significantly lower than that of nZVI, resulting in weakened aggregation. Therefore, the specific surface area of iron oxides will be obviously increased compared to nZVI, which is favorable for iron oxides to remove/degrade contaminants through adsorption/catalysis. Table 1 shows the BET specific surface area and pore parameters for pristine nZVI and reacted nZVI. It can be seen that the BET specific surface area (46.67 m2·g−1) and pore volume (0.2283 cm3·g−1) of the iron oxides (reacted nZVI) are 5.3 times and 6.4 times of that of pristine nZVI (8.76 m2·g−1 and 0.0358 cm3·g−1), respectively.

Table 1

BET specific surface area and pore parameters of pristine nZVI and reacted nZVI

MaterialsSBET (m2·g−1)Smicro (m2·g−1)Sext (m2·g−1)Vtotal (cm3·g−1)Vmicro (cm3·g−1)Vmeso (cm3·g−1)Pore size (nm)
Pristine nZVI 8.76 1.53 7.22 0.0358 0.0008 0.0361 16.59 
Reacted nZVI 46.67 8.57 38.10 0.2283 0.0044 0.2294 18.21 
MaterialsSBET (m2·g−1)Smicro (m2·g−1)Sext (m2·g−1)Vtotal (cm3·g−1)Vmicro (cm3·g−1)Vmeso (cm3·g−1)Pore size (nm)
Pristine nZVI 8.76 1.53 7.22 0.0358 0.0008 0.0361 16.59 
Reacted nZVI 46.67 8.57 38.10 0.2283 0.0044 0.2294 18.21 

The transformation of Ni2+ will also have an impact on its fate and bioavailability in groundwater ecosystem, as the toxicity of heavy metals to fish and other aquatic organisms depends primarily on free (hydrated) metal ions (Stumm 1992). Fe0.7Ni0.3 alloy and trevorite, which are transformed during the removal of Ni2+ by nZVI, will exist in a colloidal or suspended state, and most of them will be quickly transferred onto the suspended solids or the sediments at the bottom of the groundwater, thus the impact on aquatic organisms is negligible.

From the above, in the process of using nZVI to remediate groundwater contaminated by Ni2+, not only Ni2+ can be removed, but also the toxicity and bioavailability of Fe oxides and Fe–Ni composites formed by transformation are significantly reduced compared with Ni2+ and Fe0. Other heavy metal ions and organic contaminants in groundwater can also be adsorbed/catalyzed by iron oxides. The findings suggest that nZVI is a promising environmentally friendly technology in groundwater remediation.

A clear insight into the compositional transformation of Ni2+ and Fe0 during Ni2+ removal by nZVI was established in this study. XRD patterns indicated that the reaction of Fe0 with Ni2+ resulted in the transformation of the Fe0 into lepidocrocite (γ-FeOOH), goethite (α-FeOOH), and magnetite (Fe3O4). The Ni2+ became converted into trevorite (NiFe2O4) and Ni0 which existed in the form of Fe0.7Ni0.3 alloy. The results were confirmed by the d-spacing values obtained from HR-TEM images and the elemental composition obtained from TEM-mapping. In addition, SEM and TEM images showed that the morphologies of lepidocrocite, goethite, magnetite, and trevorite were lath-like, twin-rod, spherical, and folding fan, respectively. The mechanism of Ni2+ transformation includes reduction to Ni0 due to the reducibility of the Fe0, and the surface coordination of Ni2+ with Fe oxides to form Fe–Ni composite. The conversion of Fe0 undergoes a series of reactions, mainly composed of the redox of Fe0 with Ni2+, H2O, and DO, the combination of Fe2+ and OH produced by Fe0 corrosion to amorphous ferrihydrite, and the further mineralogical transformation to Fe oxides with the aid of Fe2+ adsorbed on ferrihydrite. Compared with Fe0, the toxicity of Fe oxides to aquatic organisms decreased, the specific surface area increased, and the affinity for heavy metal ions and organic pollutants was higher. In addition, most of the Fe0.7Ni0.3 alloy and trevorite, which exist in the suspended or colloidal state, will be transferred to the suspended solids or the sediments at the bottom of groundwater. The findings indicate that the use of nZVI technology to remediate Ni2+-contaminated groundwater is environmentally friendly.

The authors would like to thank the Analytical and Testing Center, Wuhan University of Science and Technology for helpful contributions in the execution of this study.

The authors would like to express their gratitude to the Key Project of Natural Science Foundation of China (Grant No. 41230638), for the financial support. The support from the Open Fund of Hubei Key Laboratory for Efficient Utilization and Agglomeration of Metallurgic Mineral Resources from Wuhan University of Science and Technology (2017zy008) is duly acknowledged.

E.A. made substantial contribution to conception of the study, performed data analysis, investigation, synthesized material, curated data, and wrote the first draft. H.L. made substantial contribution to conception of the study, supervised the experiments, reviewed, and edited the manuscript. X.F. performed software edits, reviewed and edited the manuscript, and provided technical and material support.

All relevant data are included in the paper or its Supplementary Information.

The authors declare there is no conflict.

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Supplementary data