Cecilia
Granados-Miralles
*a,
Adrián
Quesada
a,
Matilde
Saura-Múzquiz‡
b,
Henrik L.
Andersen§
b,
José F.
Fernández
a and
Mogens
Christensen
b
aElectroceramics Department, Instituto de Cerámica y Vidrio, CSIC, Kelsen 5, ES 28049 Madrid, Spain. E-mail: c.granados.miralles@icv.csic.es
bCenter for Materials Crystallography, Department of Chemistry and iNANO, Aarhus University, Langelandsgade 140, DK 8000 Aarhus, Denmark
First published on 28th February 2020
CoFe2O4/Co–Fe magnetic composites are usually prepared through partial reduction of CoFe2O4, which often yields monoxides (i.e., FeO, CoO) as secondary phases. Since these compounds are paramagnetic at ambient conditions, the presence of a small amount of monoxide is generally downplayed in the literature, and the possible effects on the magnetic properties are simply ignored. However, the present study shows that even a low concentration of monoxide results in decoupling of the soft and hard magnetic phases, which inevitably leads to a deterioration of the magnetic properties. Additionally, it is confirmed that a partial reduction of CoFe2O4 is a suitable method to produce CoFe2O4/Co–Fe nanocomposites, provided that the treatment is well controlled with respect to duration, temperature and flow of reductant. A monoxide-free nanocomposite was produced and its magnetic properties evaluated both at room and low temperature. Our model system exemplifies the potential of exchange-coupling (and decoupling) as a tool to tune the magnetic properties of a material within a relatively wide range of values, thus widening its spectrum of potential applications.
The actual application determines the required magnetic properties. Very often, the stability and longevity of the devices rely on a strong resistance to demagnetization (i.e. hard magnetic material, with large coercivity, Hc). Other times, the crucial parameter that ensures compliance with the specific task is the ability of the material to become magnetized up to a high value (i.e. high saturation magnetization, Ms). Most of the available materials show either a large Hc and a moderate Ms or vice versa.12 Consequently, if relatively high values of both Hc and Ms are necessary, fabrication of composite materials should be addressed. According to the exchange-spring theory, the Ms of a hard magnetic material can be enhanced by adding a controlled amount of a large-Ms material (generally soft), and the cost in Hc will be low provided that the two materials are effectively exchange-coupled.13
Ferrites are among the most used magnetic materials, owing to their good magnetic properties, chemical and mechanical stability, and the availability of elements they are based on. Especially interesting are the spinel ferrites (SFs), as they allow easy tunability of the magnetic properties with small changes on the chemical composition,14–16 thus increasing their versatility towards different applications. SFs have been widely used in the electronic industry, for high-density data storage and spintronic devices.17,18 Their utilization for biomedical applications has increased significantly over the last years, especially in the fields of drug delivery19 and biosensors.20,21 In addition to their applications as magnetic materials, it is worth mentioning that SFs are widely used for other purposes, e.g., as catalysts for very varied chemical processes,22,23 advanced battery electrodes,24,25 electrochemical supercapacitors in energy storage systems,26etc.
SFs have the general formula M2+(Fe3+)2O4, with M = Mg, Mn, Fe, Co, Ni, Cu, Zn.17 Out of all them, only Co-spinel shows hard magnetic properties, while the rest are soft magnetic species.27 Moreover, CoFe2O4 can be easily reduced to a Co–Fe alloy in the presence of a small concentration of H2 gas and moderate temperatures (≈300 °C).28 Both facts make this compound interesting, as an incomplete CoFe2O4 reduction directly leads to coexistence of hard (CoFe2O4) and soft (Co–Fe) magnetic phases. This is an excellent tool from the material science viewpoint, as it offers the potential to fine tuning the soft/hard magnetic behavior of the produced material by means of controlling the composite composition.
For the above reasons, numerous studies on the CoFe2O4 (hard)/Co–Fe (soft) composite are found in the literature, including composites prepared as powders,29 dense pellets,30 or thin films.31 Some works have set the main focus on the preparation process (in situ studies),28,32 while others have taken care of an in-depth structural characterization of the produced composites using spectroscopic techniques such as Raman33 or Mössbauer spectroscopy.34,35 Others have put great efforts on studying the inter-particle coupling from different perspectives, both using transmission electron microscopy (TEM), and measuring δm curves (Henkel plots).35,36 Recently, micromagnetic calculations on these systems have also been reported.37 However, a successful exchange-coupling of these two magnetic phases has proven rather challenging to achieve, the reason behind it often remaining unclear. In the present work, the origin of magnetic decoupling in CoFe2O4/Co–Fe nanocomposites is addressed. Composites covering a range of compositions are prepared, and their crystalline and atomic structures are studied using high-resolution powder X-ray diffraction. Physical characterization of the magnetic properties is carried out both at room and low temperature, and coupling/decoupling of the system is evaluated in terms of the phases present in the sample and their average crystallite sizes.
Rietveld analysis of the PXRD data was performed using the FullProf Suite.39 In the Rietveld model, the oxides were described assuming a Co:Fe stoichiometry of 1:2 (i.e., CoFe2O4, Co0.33Fe0.67O) and a random distribution of the two cations among the equivalent crystallographic sites. The elemental composition of the alloy in the model varied depending on the sample. A detailed crystallographic description of all the Rietveld phases may be found on Tables S1–S5 in the ESI.†
Data were also collected on a NIST 660B LaB6 calibrant in the different experimental configurations, and these data were modelled (LeBail fit) to estimate the instrumental contribution to the peak broadening. The instrument contribution was deconvoluted from the samples data, and the remaining profile broadening, originating from the sample, was modelled as Lorentzian isotropic size-broadening using the Thompson–Cox–Hastings formulation of the pseudo-Voigt function.40
Prior to the measurements described above, the room temperature magnetization of the samples was measured in a smaller field range ±4 kOe (318 kA m−1) using a home-built VSM setup.41
Fig. 1 (a) Sample composition and (b) crystallite size of the constituent phases extracted from Rietveld analysis of the PXRD data measured on the starting material and the five different nanocomposites. The magnetic properties of the samples highlighted with a green/red/blue square are represented in Fig. 4 and 5 using the same color-code. |
Sample | CoFe2O4 | Co0.33Fe0.67O | Metallic alloy | ||||||||
---|---|---|---|---|---|---|---|---|---|---|---|
wt% | 〈D〉 (nm) | a (Å) | wt% | 〈D〉 (nm) | a (Å) | wt% | 〈D〉 (nm) | a (Å) | |||
Starting material | 100.0(3) | 14.4(1) | 8.3929(1) | — | — | — | — | — | — | — | |
{2h@300°C} | 63.8(3) | 21.5(1) | 8.3889(1) | 15.7(2) | 10.1(2) | 4.2695(2) | 20.5(1) | CoFe | 28.9(3) | 2.85645(4) | |
{4h@300°C} | 52.7(3) | 19.5(1) | 8.3886(1) | 8.5(2) | 8.3(3) | 4.2680(4) | 38.9(2) | CoFe | 26.0(2) | 2.85877(4) | |
{8h@300°C} | 19.1(4) | 10.6(3) | 8.3904(5) | — | — | — | 80.9(4) | CoFe | 30.4(2) | 2.86141(4) | |
{2h@400°C} | 56.1(4) | 52.9(4) | 8.38952(7) | 6.2(2) | 11.9(6) | 4.2860(4) | 37.8(7) | 16.9(3) | Co2Fe | 61(2) | 2.84639(3) |
20.8(3) | CoFe | 46.3(8) | 2.85434(3) | ||||||||
{2h@600°C} | — | — | — | — | — | — | 100(4) | 37(2) | CoFe | 64(2) | 2.85954(6) |
64(2) | Co2Fe3 | 139(5) | 2.86405(3) |
Fig. 2 (a) PXRD data and corresponding Rietveld model of the phases present in sample {2h@300°C}. (b) Selected 2θ-region of data and models for {2h@300°C}, (c) {4h@300°C}, and (d) {8h@300°C}. |
From the series of experiments at 300 °C with variable duration (2–8 h), it is clear that as time increases, the amount of CoFe2O4 decreases, at the expense of the appearance of reduced phases: a monoxide phase (Co0.33Fe0.67O) and a metallic alloy phase (CoFe). The monoxide seems to play the role of a reaction intermediate, as it disappears as the reduction advances. Thus, while 2 and 4 h at 300 °C produced composites with 16.1(2)% and 8.6(3)% monoxide, respectively, a monoxide-free composite with an 80.9(4)% metallic content was obtained after 8 h. Fig. 2(b–d) show selected 2θ-regions of the PXRD data and models corresponding to these three samples. The distinct Rietveld phases are highlighted to illustrate the appearance/disappearance of the different phases as dwell time increases.
At 300 °C, the growth of the soft phase crystallites remains relatively controlled (≤30.4(2) nm) regardless of the dwell time. Increasing the treatment temperature accelerates the reduction process,28 thus, 2 h at 400 °C led to lower CoFe2O4 content than 2 h at 300 °C. The monoxide content also decreased substantially at 400 °C. At 600 °C, 2 hours were sufficient to completely reduce the starting material to pure metallic phases. However, increasing the temperature entails a significant growth of the alloy crystallites.
Fig. 3(a) shows the evolution of the most intense reflections of the alloy phase as a function of the reduction temperature. While the diffraction data collected for the {2h@300°C} nanocomposite can be modelled with a single metallic phase (CoFe), at least two metallic phases are clearly present in the {2h@400°C} and {2h@600°C} samples. The refined unit cell parameters for the individual phases are displayed in Table 1 and plotted in Fig. 3(b) as a function of the treatment temperature. The dissimilar distribution of cell parameters suggests different elemental compositions of the alloys. Unfortunately, the Co:Fe ratio could not be extracted from the refinements, because Co and Fe are next-neighbors in the periodic table and therefore, practically indistinguishable using X-rays (see ESI in ref. 28).
The unit cell dimensions of Co–Fe alloys increase with an increasing Fe content.42 This allows an estimate of the elemental composition based on the lattice parameter. The empirical chemical compositions shown in Table 1 and Fig. 3 were assessed by substituting the refined unit cell parameters in the equation obtained by Ohnuma et al. for ordered body-centered-cubic (bcc) structures.42 For the mildest reduction, {2h@300°C}, the calculated alloy composition is CoFe. This indicates surplus Co on the alloy, compared to the Co:Fe stoichiometry of 1:2 presumed for the starting spinel material. This observation is in agreement with previous in situ investigations on this system, where the reduced phases were observed to appear in a Co-rich form, to later incorporate Fe and evolve towards Co:Fe = 1:2.28 At the higher temperatures, CoFe coexists with other alloy phases, i.e., Co2Fe in {2h@400°C} and Co2Fe3 in {2h@600°C}, showing that the Fe-content increases as the temperature rises. A similar phase segregation may be occurring at 300 °C, although the effect remains hidden under the broader diffraction peaks derived from the smaller crystallite sizes at this temperature, and in that case, the refined unit cell parameter should be understood as the weighted average of all the phases present. The cell dimensions increase slightly with dwell time, again indicating a late incorporation of the Fe in the alloy structure.
The influence of the amount of H2 inside the furnace was also investigated (see Fig. S6 in the ESI†). The gas pressure was increased up to 100 and 300 mbar, and no significant changes were observed neither on the sample composition nor the crystallite sizes, compared to the experiments at 20 mbar. This suggests that, for the amounts of sample used here, an H2 excess is ensured even at the lowest pressure, and as long as there is enough H2 available, the gas pressure does not seem to have a major influence on the process.
To evaluate whether the crystallite size of the starting material plays a role, an additional time series of experiments were carried out at 300 °C using CoFe2O4 powders with an average size of 8.2(1) nm (see Fig. S7 in the ESI†). Comparing these results with those represented in Fig. 1 (mean size starting material 14.4(1) nm), it is concluded that the smaller the size of the starting CoFe2O4, the faster the reduction occurs, i.e., the shorter the time required to achieve a certain reduction stage.
Sample | M s (A m2 kg−1) | M r (A m2 kg−1) | H c (kA m−1)a | H c (kOe)a |
---|---|---|---|---|
a H c is given both in SI an CGS units to ease comparison with other works. | ||||
Starting material | 73.9(4) | 19.7(1) | 83(2) | 1.04(2) |
{2h@300°C} | 86.3(1) | 29.5(1) | 115(1) | 1.44(2) |
{4h@300°C} | 115.6(1) | 30.4(2) | 90(1) | 1.13(2) |
{8h@300°C} | 185.1(1) | 27.0(2) | 60.4(9) | 0.76(1) |
{2h@400°C} | 125.6(1) | 13.8(2) | 44.3(6) | 0.557(7) |
{2h@600°C} | 229.7(2) | 1.7(2) | 3.23(2) | 0.0406(2) |
In order to discriminate the influence of the temperature from the effect of the actual reduction process, a 2 h long treatment in vacuum at 400 °C was carried out. No significant changes were observed in the magnetic properties after this treatment (see solid, gray circles in Fig. 4). Therefore, in the following, the starting CoFe2O4 powders will continue to be used as reference to evaluate the magnetic properties of the nanocomposites.
M s follows the expected linear increase with the amount of alloy present in the sample. The trends exhibited by Mr and Hc are slightly more complex. A mild reduction, such as {2h@300°C} (in red color) yields a significant enhancement of both parameters; the composite with a 20.5(1) wt% alloy has a 50% higher Mr and a 39% larger Hc than the starting material. This is understood as a consequence of the temperature which causes a moderate growth of the CoFe2O4 nanoparticles, from 14.4(1) to 21.5(1) nm, and has very likely induced a betterment of the crystallinity as well.
As the alloy wt% increases, both Mr and Hc decrease, but the decrease is much more pronounced for the temperature series (circles) than for the time series (squares). For instance, the {4h@300°C} nanocomposite has a Mr = 30.4(2) A m2 kg−1 and a Hc = 90(1) kA m−1, and these parameters are reduced by more than half for the sample with approximately the same composition fabricated at 400 °C for 2 h (Mr = 13.8(2) A m2 kg−1, Hc = 44.3(6) kA m−1). Despite the similarity in composition between these two samples, the crystallite sizes of both hard and soft phases are much larger for the composite prepared at the higher temperature, which can explain the deterioration of the magnetic properties: (i) the 52.9(4) nm refined for the hard phase in {2h@400°C} is above the critical stable single-domain size (SSD) for CoFe2O4 (≈40 nm),44 which explains the collapse in Hc observed for this sample. (ii) The alloy also grows well beyond typical SSD values, and formation of domains in the soft phase eases spontaneous demagnetization of the hard when both phases are coupled.31
Fig. 5 (a) Low temperature magnetic hysteresis loops for selected samples and (b) corresponding first derivative normalized. The samples represented in green, red and blue color in this figure are highlighted with the same colors in Fig. 1 and 4. |
The number of reversal or switching events is readily revealed by the maxima in the first derivative curve of the magnetization data. First derivatives of the M–H data from all samples are displayed in Fig. 5(b). The starting material shows the single-step behavior expected for a pure phase, with a single switching field, Hsw, at ≈940 kA m−1. The same is observed for the fully-reduced sample {2h@600°C} but with a nearly zero Hsw. Note the shape of the peaks here is much more Lorentzian than for the starting material. This shape can result from the convolution of several independent contributions from distinct phases (rather than a single-phase), all of them having a very similar, nearly-null magnetic anisotropy. This is in agreement with the two bcc species with different Co:Fe ratios visible in the PXRD data.
Two very distinct Hsw are detected for {2h@300°C} (red), which is an indicative of weakly exchanged soft–hard interphases. On the contrary, {8h@300°C} (blue) presents a single-step reversal, which in this case is attributed to an effective of exchange-coupling between the soft and hard phases. Independent magnetization reversal of the magnetic phases is visible for {4h@300°C}, although the peak defined by the larger Hsw is much less intense compared to the 2 h experiment at the same temperature (red curve). The δM/δH curve for {2h@400°C} is maximized at a single Hsw value. However, the peaks here are not symmetric and the peak tails do not coincide, suggesting some degree of decoupling of the two magnetic phases.
To summarize, the only composite showing LT exchange-coupling behavior is the monoxide-free sample {8h@300°C} (blue color). We believe this observation is far from coincidental, considering the correlation between the monoxide concentration and the degree of decoupling shown by our data (see plots on the right from Fig. 5(b)). The present study demonstrates how avoiding the monoxide is imperative for producing effectively exchange-coupled CoFe2O4/Co–Fe nanocomposites. This observation is consistent with and may help explain previous literature on the subject. Several studies report decoupling at RT in monoxide-containing samples29,45–48 Some decoupled “monoxide-free” examples are also found.49–53 However, we consider it possible that the monoxide was overlooked in those works. The proximity in 2θ of the monoxide and the spinel Bragg positions (see Fig. 2) makes it difficult to separate the contribution from these two phases unless the PXRD data has high enough resolution and the subsequent data analysis is appropriate.
Based on a joint interpretation of the RT and LT magnetization data, we understand that our monoxide-free, exchange-coupled sample {8h@300°C} is far from reaching the best magnetic properties the CoFe2O4/Co–Fe system allows. Samples with a lower alloy content, such as {2h@300°C} and {4h@300°C}, appear significantly more promising, owing to their higher Mr and Hc values at RT (see Fig. 4), despite the presence of monoxide hindering the optimal magnetic performance of these samples. Therefore, we believe that monoxide-free composites with an alloy content ≲40 wt% may lead to effectively exchange-coupled CoFe2O4/Co–Fe composites with superior magnetic properties, and should thus be pursued in future work.
Once the chemistry behind the process is understood, partial reduction of CoFe2O4 is a very strong method for synthesizing CoFe2O4/Co–Fe nanocomposites with controlled magnetic properties. Adjusting each of the reduction parameters (temperature, time, partial H2 pressure, crystallite size of the starting CoFe2O4 powders) has a very specific impact on the composition and crystallite sizes of the obtained nanocomposite, which, in turn, directly determines its magnetic behavior. The present work reveals exchange-coupling to be an excellent tool to further expand the range within which the magnetic properties of spinel ferrites can be tuned, extending the scope of this family of compounds. The method described here using CoFe2O4/Co–Fe as an example may in principle be applicable to other ferrite systems, including hard hexaferrites or other spinel ferrites (soft), and allows multiple combinations of magnetic compounds.
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: 10.1039/c9qm00713j |
‡ Current address: School of Chemistry, University of Sydney, F11, NSW 2006 Sydney, Australia. |
§ Current address: School of Chemistry, UNSW Australia, NSW 2052 Sydney, Australia. |
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