1. Introduction
Zirconium dioxide (ZrO
2), or zirconia, exhibits several remarkable properties, including high thermal resistance, hardness, transparency, a high refractive index, chemical stability, and a high melting point. These properties have led to its use in various applications such as coatings, catalysis, and even sensing [
1,
2,
3,
4,
5,
6,
7,
8,
9,
10,
11,
12,
13]. Doping zirconium dioxide with various impurities can impart new properties, expanding its range of applications. For example, zirconia ceramics doped with rare earth elements exhibit a wide range of luminescent features, making them suitable for use in light-emitting devices [
1,
2]. Additionally, doping ZrO
2 with copper enhances its catalytic properties, enabling the production of highly efficient catalysts [
5,
6,
7,
8].
The incorporation of sub-valent impurities into the structure of zirconium dioxide is a complex and poorly understood process due to two main reasons. The first reason is that the doping impurity, depending on the technology used for its introduction, can occupy different structural positions. It can either enter directly into the zirconium dioxide structure or localize on the surface of granules, thus forming various surface complexes. The second reason is that the inclusion of sub-valent impurities in the zirconium dioxide structure requires charge compensation, which can lead to significant restructuring of the oxide itself. Pure ZrO2 crystals typically have a monoclinic structure at room temperature. Upon heating to around 1460 °C, it transforms into the tetragonal phase and then into the cubic phase at higher temperatures. However, it becomes unstable upon cooling, undergoing reverse transformations from cubic to tetragonal to monoclinic phases.
For ZrO
2 powders, the same processes are observed, with the difference that phase transitions occur at lower temperatures and depend on the size of the powder granules. An exception is powdered with nanosized granules, where the stabilization of high-temperature phases at room temperature is possible due to surface energy. The introduction of sub-valent impurities, such as the frequently used yttrium, into the structure of zirconium dioxide stabilizes the tetragonal or cubic ZrO
2 phases at room temperature, depending on the concentration of the impurities [
14,
15,
16]. The stabilization of both phases is believed to be due to the formation of oxygen vacancies required for dopant charge compensation [
4,
17]. Therefore, knowledge of the localization of sub-valent impurities and the identification of associated defects is important for understanding the properties of doped zirconium dioxide. The use of the electron paramagnetic resonance method for this purpose has proven to be a powerful tool in the study of intrinsic and impurity defects in various solid-state materials.
As mentioned above, copper doping of zirconium dioxide is used to enhance its catalytic properties. This enhancement is believed to be due to the formation of complexes containing copper, oxygen, and hydrogen atoms on the surface of zirconium dioxide powder granules. Previous studies have shown that when zirconium dioxide powders and ceramics are doped with copper, the copper atoms can be incorporated into the ZrO
2 structure, as well as form various complexes on the surface. For example, paramagnetic centers Cu
Zr2+ have been detected in yttrium-stabilized ZrO
2 ceramics, along with aggregates of Cu atoms, CuO molecules, and crystalline CuO located on the surface of granules and/or between powder grains [
9,
11,
18,
19]. However, up to date, these studies were not systematic.
Therefore, the present work is devoted to the study of electron paramagnetic resonance (EPR) of paramagnetic centers associated with copper in zirconium oxide powders calcined at different temperatures. The dependence of the formation of these paramagnetic centers on the concentration of introduced copper and the effect of co-doping with yttrium were also investigated. To clarify the nature and/or model of paramagnetic centers, nuclear magnetic resonance (NMR) and Raman spectroscopy techniques were additionally used.
The identification of paramagnetic centers observed in the EPR spectrum will facilitate the development of a fast and non-destructive method to control Cu-doped ZrO2 materials. Additionally, this will open up opportunities to optimize technological parameters for creating effective catalysts, using only a small amount of the investigated powders required for EPR research.
2. Materials and Methods
A co-precipitation technique was applied to synthesize Cu-doped and (Cu,Y)-codoped ZrO
2 powders from ZrO(NO
3)
2·nH
2O, Y(NO
3)
3, and Cu(NO
3)
2 precursors. The Zr and Cu salts and Zr, Cu, and Y salts were taken in the required ratio to produce Cu-doped and (Cu,Y)-codoped ZrO
2 powders, respectively. The composition of the prepared powders is given in
Table 1.
More details about the preparation of the powders studied here can be found elsewhere [
4]. When the co-precipitation process was completed, the gel-like substance was dried at 80 °C for 48 h to remove water molecules and subsequently heated at 150 °C for 24 h to complete the process. The resulting sediments underwent further calcination at 400, 600, 800, and 1000 °C for 2 h in air and then slowly cooled in the furnace to room temperature. As a result, nano-sized powders with average particle sizes ranging from 8 to 15 nm were obtained, depending on the calcination temperature. More details on their structural characterization can be found in ref. [
4].
Electron paramagnetic resonance (EPR) measurements were carried out using an X-band Varian E12 (Varian, Palo Alto, CA, USA) and Bruker EPR ELEXSYS 580 (Bruker Corporation, Billerica, MA, USA) spectrometers at room temperature and at liquid nitrogen temperature. The powders studied were placed in a quartz tube with an internal diameter of 4 mm, where their EPR signals were recorded with unsaturated microwave power (2 mW). A 100 kHz modulation of the magnetic field with peak-to-peak amplitude modulation of 0.1 mT was applied. The signal of an MgO:Mn sample containing 3 × 1015 spins was used as a reference. The obtained EPR spectra were normalized to the intensity of the MgO:Mn reference signal, taking into account the mass of each studied powder. Spectra simulations were performed using the WINEPR Simfonia software package (Version 1.25).
Magic-angle spinning nuclear magnetic resonance (MAS NMR) spectra of powdered samples were recorded on a 400 MHz commercial Bruker Avance NMR spectrometer (Bruker Corporation, USA) in a magnetic field of 9.40 T, at room temperature and with a spinning frequency of 5 kHz. 1H MAS NMR spectra were acquired using a single pulse sequence with a recycle delay of 5 s. The spectra were referenced against the TMS, which was taken here as the zero for the chemical shift.
The powders were also studied by means of the Raman scattering method. To record the Raman spectra, an MDR-23 spectrometer (LOMO, St. Petersburg, Russia) equipped with a cooled CCD detector, iDus 420 Andor (London, UK), was used. A diode-pumped solid-state 457 nm laser was used as the excitation source. The laser power density on the sample surface was less than 103 W/cm2 to prevent structural transformation due to laser heating. Spectral calibration was performed using the peak position of a 520.6 cm−1 phonon peak of a silicon single crystal, with a peak width of approximately 4 cm−1.
3. Results and Discussion
Figure 1a shows the EPR signals from ZrO
2 samples alloyed with different Cu contents ranging from 0.1 to 8 mol.% and calcined at 400 °C. The spectra were normalized by mass and the intensity of the reference sample, permitting direct comparison of signal intensity across different samples. The total intensity of the EPR signal shows a direct correlation with the increase in Cu loading, as illustrated in
Figure 1a. This indicates that the observed EPR signal is caused by either copper ions themselves or by the associated defects formed when copper enters the powders.
In parallel, changes observed in the shape of the spectra indicate the appearance of an additional signal. A detailed analysis of the EPR spectra shows that the EPR spectrum of ZrO
2 powder doped with up to 1 mol.% CuO can be described using a single-curve model, denoted as signal A (see
Figure 1b). Such spectra exhibit the characteristic for Cu
2+ (3d
9) species hyperfine splitting into four lines, well resolved in the g
|| region, due to the hyperfine coupling between unpaired electron (S = 1/2) and Cu nucleus (I = 3/2). Hyperfine splitting A
⊥ is usually very small, and due to its line width, the spectrum shows no splitting at the g
⊥ region. This spectrum reveals that the Cu
2+ center is axial (g
|| > g
⊥ > g
e) and can be described by corresponding parameters g
⊥ = 2.063, g
|| = 2.340, and A
|| = 130 G. Its parameters are intermediate between Cu(OH)
42− with g
|| = 2.29 and Cu(H
2O)
42+ with g
|| = 2.42 [
20]. The highest concentration of these paramagnetic centers was observed in sample Cu-1, at 2 × 10
17 spins/cm
3.
To describe the EPR spectra of ZrO
2 samples doped with 5 mol.% and 8 mol.% CuO, an additional component with g ~ 2.17 (Signal B) was required. Its shape and position were somewhat different for ZrO
2 samples doped with 5 and 8 mol.% CuO. Since the intensity of signal B increases with rising Cu content, it can be assumed that this signal relates to copper-enriched areas, where adjacent Cu
2+ ions are coupled by strong dipole–dipole or exchange interactions. These may be heavily doped near-surface regions of granules, metallic copper, or/and CuO
x nanoclusters on the grain surface. Previously, copper clusters were reported to exhibit superparamagnetic behavior [
21].
The intensity of paramagnetic signals changes with the measurement temperature in accordance with the Curie–Weiss law. At the same time, the intensity of the superparamagnetic signal depends weakly on temperature. Therefore, comparison of EPR spectra of a sample recorded at different temperatures allows one to separate the paramagnetic and superparamagnetic components in the spectra.
Figure 2 compares the EPR spectra of ZrO
2 doped with 8 mol.% CuO recorded at 300 and 77 K. Both spectra are seen to exhibit a very weak signal at g ≈ 4, caused by an uncontrolled iron impurity in the quartz tube used to hold the studied powders. This signal is paramagnetic. Since it does not overlap with the signals from the ZrO
2 powder, normalizing the experimental spectra is convenient to clarify the nature of the EPR signals studied.
The intensities of signals A and that of iron were found to change synchronously with the measurement temperature, thus following the Curie–Weiss law, which indicates the paramagnetic nature of signal A. At the same time, the intensity of signal B increased slightly at lower temperatures, thus indicating its superparamagnetic nature [
22]. This finding allows for the unambiguous identification of signal B with copper-rich nanoclusters, such as metallic copper or CuO
x located on the surface of ZrO
2 powder granules.
The nature of signal A cannot be determined based on EPR data alone. Similar EPR spectra have been observed in ZrO
2 and other copper-doped oxides (TiO
2, ZnO, etc.), which was attributed to copper ions in Cu-related surface complexes. In those complexes, copper ions were proposed to be situated in tetragonally distorted octahedral fields of ligands such as H
2O, O
−, SO
42−, and OH
− [
23,
24]. The nature of this signal will be discussed in more detail after presenting the NMR data.
Calcination temperature was found to drastically influence the line shape of the EPR signal of Cu-ZrO
2 powders, as seen in
Figure 3a–c. Signal A is seen to decrease with calcination temperature and almost disappears at 800 °C. In the samples calcined at 1000 °C (see
Figure 3a–c, blue lines), a set of narrow lines of an irregular shape is observed in a wide range of magnetic fields. The small line width of this signal indicates a strictly regular crystallographic environment of the corresponding paramagnetic center, excluding the scattering of radio-spectroscopic parameters of the center. Previously, this signal was observed by Vorona and coworkers [
19] and was assigned to Cu
2+Zr in the monoclinic ZrO
2 lattice (denoted as Signal C). Its radio-spectroscopic parameters are S = 1/2, I = 3/2, g
x = 2.021, g
y = 2.026, g
z = 2.168, A
xx ~ 40 × 10
−4 cm
−1, A
yy ~ 35 × 10
−4 cm
−1, A
zz ~ 186 × 10
−4 cm
−1, A
xz ~ 10 × 10
−4 cm
−1, and A
yz ~ 5 × 10
−4 cm
−1 for the
63Cu isotope. This can be explained by the fact that part of the Cu
2+ ions, which appeared as a result of the destruction of surface complexes, is additionally incorporated into the bulk of nanocrystals.
An increase in copper loading up to 1 mol% leads to an increase in the intensity of signal A. Further increases in the alloying impurity loading do not cause a noticeable increase in the intensity of signal A. Additionally, at 5 mol% CuO, signal B appears (
Figure 3b), with its intensity increasing as copper loading increases up to 8 mol% (
Figure 3c). An increase in the calcination temperature results in a decrease in the intensity of signal A. At a calcination temperature of 1000 °C, both signals A and B disappear, and only signal C is observed in the EPR spectrum.
Yttrium is frequently used as a stabilizing dopant for the tetragonal and cubic phases of zirconium oxide because it can remain within the ZrO
2 host matrix up to 1400 °C [
17]. Therefore, understanding the influence of yttrium incorporation on copper-related paramagnetic centers in ZrO
2 materials is crucial. It is seen in
Figure 3d–i that Cu-Y co-doping leads to the appearance of signal C at a lower calcination temperature, more specifically, at 800 °C, if compared to Cu-doped ZrO
2 powders. For a series of samples with the same copper content, the maximum intensity of signal C was observed for samples doped with 3 mol.% of Y
2O
3. A possible explanation is that additional doping with yttrium, which has a diffusion coefficient several times larger than that of copper [
25], accelerates the formation of oxygen vacancies required for dopant charge compensation. This, in turn, facilitates the simultaneous diffusion of copper into lattice sites at lower calcination temperatures. However, a further increase in the yttrium content up to 10 mol.% Y
2O
3, will lead to a competition between yttrium and copper in the occupation of cation sites because of the larger amount of Y ions. Consequently, the initial increase in the amount of Cu
2+Zr with yttrium doping changes to a decrease once the critical yttrium content is reached. This is due to a complex interplay of factors affecting the structure and stability of the lattice. Most authors of studies on copper-doped oxides attribute EPR signals similar to the above-mentioned signal A to surface complexes of copper with H
2O or OH. To clarify this issue, the
1H MAS NMR technique was applied to the powders studied. As an example,
1H MAS NMR spectra of ZrO
2 powders doped with 0.1 mol.% CuO (the lowest impurity loading) and ZrO
2 co-doped with 8 mol.% CuO and 10 mol.% Y
2O
3 (the highest impurity loading) are shown in
Figure 4.
All powders annealed at 400 °C were found to exhibit
1H MAS NMR signals consisting of two components: an intense band at δ = 6.83 ppm and a weak band at δ = 5.53 ppm. The components at δ = 5.53 ppm were observed to dominate in the powders calcined at 600 °C, while this
1H NMR signal was not detected in the samples calcined at higher temperatures (≥800 °C). Thus, the band at δ = 5.53 ppm was assigned to Zr-OH groups, while the band at 6.83 ppm is related to protons of H
2O molecules on the oxide surface [
26,
27,
28,
29]. The line width of both components was found to be strongly influenced by the number of protons involved in forming hydrogen bonds and decreased with increasing annealing temperature. The reduction in the contribution of the component at δ = 5.53 ppm observed at higher annealing temperatures indicates the escape of water molecules at 600 °C. This finding correlates with previously obtained IR spectroscopy data on the yield of adsorbed water and hydroxyl groups in ZrO
2 powders [
30]. The escape of water molecules is accompanied by a sharp decrease in signal A in the EPR spectra, which confirms the assignment of the signal to surface Cu
2+-(H
2O)
x complexes.
To confirm the model of the paramagnetic center responsible for the C signal, namely Cu
Zr2+ cation positions in the monoclinic ZrO
2, the same powders were studied using Raman shift spectroscopy.
Figure 5 presents Raman spectra of Cu-doped and (Cu,Y)-co-doped ZrO
2 powders calcined at 600 and 1000 °C. The number of phonon modes that appear in the Raman spectrum of ZrO
2 is known to be governed by its crystalline structure [
4,
31,
32]. Although the peak positions of some of them are nearly the same for different phases (for instance, the strong A
g mode at 476 and 475 cm
−1 for monoclinic and tetragonal phases, respectively), there are strong phonon modes specific only to monoclinic (A
g doublet at 183 cm
−1 and 193 cm
−1), tetragonal (B
1g mode at 155 cm
−1 and E
g mode at 257 cm
−1), and cubic (E
2g mode at 607 cm
−1) ZrO
2 phases [
31,
32]. Thus, these phonon modes are considered fingerprints for each crystalline phase and can be used to identify their contribution to the powder structure. As shown in
Figure 5a, all powders calcined at 1000 °C exhibit a characteristic A
g doublet at approximately 183 and 193 cm
−¹, indicating the dominant contribution of the monoclinic ZrO
2 phase. The corresponding EPR spectra show the C signal, with its intensity depending on the Cu and Y content, as seen in
Figure 3. Indeed, for the Cu-1-Y-3 powder, its contribution is lower and aligns with the presence of the tetragonal phase (revealed by the B
1g and E
g modes) in the Raman spectra (
Figure 5b). This finding corroborates the absence of the C signal in the EPR spectra of powders calcined at 600 °C (see
Figure 3) and demonstrates the dominant contribution of tetragonal ZrO
2 (see
Figure 5b).
This correlation of EPR and Raman shift spectra supports the proposed model of the paramagnetic center responsible for the C signal, namely the Cu2+Zr cation position in monoclinic ZrO2. Thus, the Cu-doped zirconium oxide powders studied in this work yielded three EPR signals that can be described using the following parameters: g⊥ = 2.063, g|| = 2.340, and A|| = 130 G (signal A), g ~ 2.17 (signal B), and gx = 2.021, gy = 2.026, gz = 2.168, Axx ~ 40 × 10−4 cm−1, Ayy ~ 35 × 10−4 cm−1, Azz ~ 186 × 10−4 cm−1, Axz ~ 10 × 10−4 cm−1, and Ayz ~ 5 × 10−4 cm−1 (signal C). They can be identified as surface Cu(H2O)x complexes, superparamagnetic Cu and/or CuOx nanoclusters at the grain boundaries, and Cu2+Zr in monoclinic ZrO2, respectively. Identification of the EPR signals enables tracing the formation of copper-related paramagnetic centers in Cu-doped zirconium dioxide powders produced under different process parameters.
Signal A was found to dominate in powders calcined at low temperatures (400 °C) and with low dopant concentrations (≤1 mol.% CuO). This indicates that, under these synthesis conditions, the copper alloying impurity ions were located on the surface of the zirconium dioxide powder grains, interacted with absorbed water, and formed surface Cu2+-(H2O)x complexes. At higher concentrations (5 and 8 mol.% CuO), the dopant atoms interacted with each other, forming superparamagnetic Cu or/and CuOx nanoclusters on the grain boundaries. When the calcination temperature was elevated to 600 °C, signal B became dominant in the EPR spectrum of Cu-doped ZrO2 powders. This implies the destruction of surface Cu2+-(H2O)x complexes at this temperature, which was confirmed by 1H NMR data on the release of adsorbed water. The copper ions liberated during this process drifted along the granule surface, beginning to interact with each other and forming superparamagnetic clusters on the grain boundaries. Increasing the calcination temperature to 1000 °C was observed to lead to the destruction of superparamagnetic clusters and the incorporation of copper ions into the zirconium dioxide structure as Cu2+Zr cationic substitutions.