Abstract
In this study, a Co2O3 addition from 0.28 to 0.44 wt% is added to the MnZn ferrites. The effects of Co2O3 on the soft magnetic properties and loss performance of the MnZn ferrites were investigated over a wide temperature range from 25 to 140 °C. Either the spinel crystal structure or microstructure of the MnZn ferrites is not greatly affected by the Co2O3 content. The saturation magnetic induction (Bs) shows a maximum of 528 mT at 0.36 wt% Co2O3 due to the slight increase in density. At room temperature, the initial permeability (µi) of the MnZn ferrite is enhanced to a maximum of 2692, which is associated with the minimum magnetic anisotropy (|K|) obtained at 0.36 wt% Co2O3. However, the DC resistivity of the MnZn ferrite is seen to decrease with increasing Co2O3 content. Due to the enhanced initial permeability, the minimum core loss of the MnZn ferrite is obtained at 0.36 wt% Co2O3 under various conditions from 100 kHz/200mT to 300 kHz/100mT.
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1 Introduction
With the development of the third-generation semiconductor such as GaN, both the voltage and power of the switched mode power supplies (SMPS) in electronic devices have been significantly increased [1]. The MnZn ferrites are often used as the core materials in the SMPS, due to their high saturation magnetic induction (Bs) and high initial permeability (µi). The high Bs allows for a high power density that matches the high voltage provided by the third-generation semiconductors [2]. A high Bs also results in a reduced size of magnetic core so that the device could be made smaller. The high µi facilitates the magnetization process so that a lower external magnetic field is required for the same magnetic induction.
The MnZn ferrites are known to have a composition of MO·Fe2O3 with a spinel crystal structure. The tetrahedral sites (A sites) and octahedral sites (B sites) are occupied by metallic ions such as Mn2+, Fe2+, and Fe3+. Instead of being directly coupled, the metallic ions with magnetic moments are coupled by the super-exchange interactions through the non-magnetic oxygen ions. And the magnetic moment per unit cell as well as the other magnetic and electrical properties are mainly determined by the interaction between the magnetic ions [3]. By modifying the ions distributed in A sites and B sites, the soft magnetic properties of the MnZn ferrites can be greatly affected. For example, to enhance the initial permeability of the MnZn ferrite, a Fe-rich composition is often adopted so that Fe2+ ions are induced to the B sites, resulting in a reduced intrinsic magnetocrystalline anisotropy constant (K1). Moreover, the sintering process of a Fe-rich MnZn ferrite involves a protective atmosphere with a low oxygen partial pressure to maintain a high ratio of Fe2+: Fe3+ [4,5,6,7,8].
The improvement in soft magnetic properties of MnZn ferrites can also be achieved by using additives. Sintering aids such as Bi2O3 [9,10,11,12], MoO3 [13,14,15], and V2O5 [7, 16, 17] can be used to promote densification and grain growth through liquification during the sintering process. The enhanced sintering process results in a lower porosity and a larger average grain size, which are beneficial for domain wall movement in the magnetization process, leading to a higher initial permeability [3, 18,19,20]. Other research shows that additives such as barium titanate (BTO) and barium strontium titanate (BST) can reduce the average grain size of the MnZn ferrites and enhance the overall resistivity, resulting in significant reduction in the eddy current loss [8, 21]. Apart from additives that improves the magnetic properties only through modification of the microstructure, some metallic oxides contain ions that could enter the spinel lattices of the MnZn ferrite and affect its magnetic properties intrinsically. In this study, the effect of Co2O3 doping on the soft magnetic properties and power loss of MnZn ferrites are investigated over a wide temperature range of 25–40 °C.
2 Materials and methods
The MnZn ferrites with a Co2O3 addition from 0.28 to 0.44 wt% were prepared using the conventional ceramic method. Raw materials of Mn3O4, ZnO, and Fe2O3 with an analytical grade were weighed according to the stoichiometric composition of Mn0.71Zn0.22Fe2.07O4. The raw materials were mixed and milled in a planetary mill at 241 rpm for 2 h with steel balls and deionized water. The mass ratio of powder:water:ball was 2:3:6. The milled powder mixture was then dried in an oven at 90 °C. Then the mixture was pre-sintered at 900 °C in air for 2 h. After that, Co2O3 with an analytical grade was added to the mixture from 0.28 to 0.44 wt%. The mixture was ball-milled the second time at 241 rpm/min for 3 h. The powder mixture was dried again and mixed with 12.5 wt% of polyvinyl alcohol (PVA) and granulated. The granular powder was then pressed under a pressure of 98 MPa into green bodies in the shapes of disc and chip. The green body was sintered at 1250 °C under a nitrogen atmosphere with an oxygen pressure of 3.1% for 7 h.
The crystal structure of the sintered ferrites was characterized using a MAXima XRD-7000 X-ray diffractometer (XRD). The radiation source is Cu K-alpha. The microstructure of the sintered ferrite was characterized using the JEOL JSM-6490LV scanning electron microscope (SEM) on the fractured surface of the sample. The density of the sample was measured using the Archimedean method. The initial permeability and the DC-resistivity was measured using the TongHui TH2826 LCR meter. The magnetization curve of the sample was obtained using the LakeShore 8694 vibrating sample magnetometer (VSM). The saturation magnetization at 1200 A/m and the core loss under various conditions were measured using the IWATSU SY-8232 B-H analyzer.
3 Results and discussions
Figure 1 shows the XRD spectrum of sintered MnZn ferrites with various amount of Co2O3 addition from 0.28 to 0.44 wt%. In reference to the standard PDF#74-2401 card, all the samples show a spinel structure without discernible sign of other crystal structure. Moreover, discernible peak splitting at higher angles (55°–70°) can be observed. This is due to the nature of K-alpha emission. As the K-alpha emission is composed of two spectral emissions, K-alpha1 (wavelength, λ = 1.54060 Å) and K-alpha2 (λ = 1.54443 Å), the latter of which have a slightly lower energy than the former, resulting in a difference in wavelength. For a given crystal structure, the relation between wavelength, λ, is shown in the Bragg’s law:
where n is the diffraction order, d is the interplane distance, and θ is the angle of diffraction. It is seen that peak position is directly affected by the wavelength. The mismatch of peak positions, as a result from the difference of λ between K-alpha1 and K-alpha2, cannot be seen at lower diffraction angles, but becomes more significant at higher angles.
Figure 2 shows the morphology as well as the grain size distribution of the MnZn ferrite at the selected area on the fractured surface. Closed pores are seen at the grain boundaries as well as the joint of the grains. Figure 2b shows a normal distribution of grain size for each sample. For MnZn ferrites with a Co2O3 addition from 0.28 to 0.44 wt%, an average grain size ranging from 8.1 to 9.1 μm is obtained with a standard deviation from 3.7 to 4.7 μm. It can be concluded that the Co2O3 addition from 0.28 to 0.44 wt% has no significant effect on the microstructure. Previous studies also show a minor influence of Co2O3 addition on the MnZn ferrites. This is natural because the Co3+ ions tend to diffuse into the spinel lattice without concentration difference between grains and the grain boundaries [22].
Figure 3 shows the density and the Bs of the MnZn ferrite with a Co2O3 content of 0.28–0.44 wt%. The density of the MnZn ferrites is seen to increase slightly from 4.76 g/cm3 to a maximum at 4.81 g/cm3 as the Co2O3 content is increased from 0.28 to 0.36 wt%, while the Bs is also seen to increase from 518 mT to a maximum at 528 mT. The trend of Bs changing with Co2O3 content corresponds to that of the density. By definition, Bs is proportional to both density and the saturation magnetization, Ms. Therefore, the consistency in Bs and density changing with Co2O3 content indicates that the influence of Co2O3 on the MnZn ferrite is minor. In the previous study by Yang and Wang [22], it is argued that Co2+ ions enter the octahedral sites (B-sites) of the spinel structure, replacing the Fe3+ and Fe2+ and resulting in promoted super-exchange interactions between A-sites and B-sites. The stronger super-exchange interaction between A-sites and B-sites should lead to higher net magnetic moment: M = MA–MB. As a result, both Ms and Bs are enhanced [22]. Yet, no further evidence was shown.
Figure 4a shows the B-H of the MnZn ferrites with various amount of Co2O3 additions. While all the samples show a narrow B-H loop, samples with a Co2O3 addition of 0.36 and 0.44 wt% have a wider B-H loop. Figure 4b shows the initial permeability changing with the Co2O3 content at 25 °C. The µi is seen to increase from 2412 to 2691 as the Co2O3 content is increased from 0.28 to 0.36 wt%, before decreasing to below 2000 as Co2O3 content is further increased to 0.44 wt%. The µi is determined by multiple factors, and can be described in the empirical relation:
where λs is the saturation magnetostriction, σ is the internal stress, δ is the domain wall thickness, β and d are the volume fraction and diameter of the impurities, respectively [23, 24]. As discussed above, the change of Ms in MnZn ferrites in this study is minor, so Ms is not considered as a primary factor causing the change in µi. Instead, the major reason could be the change in the magnetocrystalline anisotropy. According to previous study, the MnZn ferrite with a composition of Mn0.71Zn0.22Fe2.07O4 is known to possess a negative K1 value [25], and the addition of Co2O3 is known to induce Co2+ ions with a positive K1 to the spinel structure and compensate the negative K1 of the original composition [26,27,28]. The change of magnetocrystalline anisotropy is studied and discussed later in this study.
Figure 5 shows the temperature dependence of µi of the MnZn ferrites. Two peaks of the maximum µi (60–80 °C and around 230 °C) can be observed, corresponding to the compensation point of magnetocrystalline anisotropy constant (K1) as the temperature is increased [25, 26]. At both compensation temperatures, µi of the MnZn ferrites is seen to be reduced by the Co2O3 additions. Meanwhile, the first peak of µi shift towards the lower temperature range and are broadened as the Co2O3 addition exceeds 0.36 wt%. The peak broadening effect could also be explained by the positive magnetic anisotropy induced by Co2+ [26, 29, 30] as the temperature curve of the µi of MnZn ferrite become less steep. The broadened µi peak provides stability and consistency in the real-world application of MnZn ferrites where the operating temperature fluctuates.
Figure 6 shows the magnetization curve of the MnZn ferrites at room temperature obtained using the VSM. The minor fluctuation at the maximum magnetization is attributed to the change in sample density. According to the previous research, the absolute value of K1 can be determined using the law of approach to saturation [31, 32] described in the following:
where a and b are numerical factors representing the resistance of domain rotation, χ represents the paramagnetic susceptibility. While a represents the influence of inhomogeneous distribution of stress and impurity, b is directly associated with the influence of magnetic anisotropy (K):
Because the influence of a is often negligible, linear fitting can be applied to the M(H)−1/H2 curve. Since the samples were prepared in the shape of a sphere, a demagnetizing factor of 1/3 was applied to correct the magnetization curves before fitting the data [33]. The calculated results of |K| are shown Table 1. As the Co2O3 addition is increased from 0.28 to 0.36 wt%, |K| is reduced from 2.47 × 104 J/m3 to a minimum of 1.69 × 104 J/m3. This reduction in |K| can be attributed to the compensating effect of Co2+ ions brought to the negative value of K1 of the MnZn ferrites [26]. As the Co2O3 content exceeds 0.36 wt%, the value of K1 becomes positive and continue to increase, leading to the increase of the value of the overall magnetic anisotropy. The trend of |K| changing with Co2O3 content corresponds to that of µi shown in Fig. 4b, and the minimum of |K| explains for the maximum µi at 0.36 wt% Co2O3.
Figure 7a shows the DC resistivity (ρ) at room temperature. As the Co2O3 content is increased from 0.28 to 0.32 wt%, ρ of the MnZn ferrites is seen to increase slightly from 11.7 to 13.1 Ω m. However, as Co2O3 is further increased to 0.44 wt%, ρ starts to decrease monotonously to 8.2 Ω m. It is widely known that the relatively low resistivity of MnZn ferrites can be attributed to the hopping mechanism between Fe2+ and Fe3+ ions. According to the previous studies [22, 34], the Co3+ ions enter the spinel lattices and occupy the octahedral sites, where Fe2+ ions exist. The Co3+ and Fe2+ ions have the tendency to form Fe2+–Co3+ pairs:
With the electrons from Fe2+ ions constrained to the Co3+ ions, the electron hopping between Fe2+ and Fe3+ ions is therefore limited, leading to the increased resistivity seen at the 0.32 wt% Co2O3. However, the as the Co2O3 content further increases, the electron hopping between the Fe2+–Co3+ pairs becomes dominant. Therefore, the resistivity starts decreasing with increasing Co2O3 content. Figure 7b shows the temperature dependence of ρ of the MnZn ferrites with various Co2O3 content. As the temperature is increased from 25 to 140 °C, the resistivity of the MnZn ferrites is reduced. This is due to the semiconducting nature of the MnZn ferrites, where increased temperature thermally excites the electrons and enhances their mobility [35, 36]. Meanwhile, the relationship between ρ and Co2O3 content is relatively consistent.
Figure 8 (a) shows the Pcv of the MnZn ferrites at 100 kHz/200mT, 200 kHz/125mT, and 300 kHz/100mT. At the above operating conditions, the contribution of hysteresis loss (Ph) and eddy current loss (Pe) is comparable [21]. As the Co2O3 is increased from 0.28 to 0.36 wt%, Pcv at the three operating conditions is reduced to the minimum. The reduction in Pcv with the increasing Co2O3 content from 0.28 to 0.36 wt% can be attributed to the enhancement in µi (see Fig. 4a), as the Ph is known to decrease with increasing µi. However, as the Co2O3 content is further increased to 0.44 wt%, Pcv at the three operating conditions is dramatically increased. The increase of Pcv as Co2O3 content exceeds 0.36 wt% can be attributed to the increase of both Ph and Pe. The increase of Ph is due to the reduction of µi (shown in Fig. 4a) and the increase of Pe is due to the reduction of ρ (shown in Fig. 7a) Co2O3 content is increased from 0.36 to 0.44 wt%. Figure 8b–d show the temperature dependence of Pcv of MnZn ferrite with various Co2O3 content at 100 kHz/200mT, 200 kHz/125mT, and 300 kHz/100mT, respectively. As directly shown in Fig. 7b, the resistivity of the MnZn ferrites with various Co2O3 content dramatically decreases with increasing temperature. As a result, the eddy current loss of MnZn ferrites with various Co2O3 is raised by increasing temperature. However, as the temperature is increased from 25 °C to the region of 40 ~ 80 °C, Pcv of the MnZn ferrites is reduced. This is due to the reduction of Ph, which is a result of µi increasing to the maximum (shown in Fig. 5).
4 Conclusions
This study investigates the effects of Co2O3 addition on the soft magnetic properties and loss performance of the MnZn ferrites used for power applications in the frequency range of 100–300 kHz. The saturation magnetization and density of the MnZn ferrites are slightly affected by the Co2O3 doping. The initial permeability is seen to increase to a maximum of 2691 with a Co2O3 addition of 0.36 wt%. The enhancement in the initial permeability corresponds to the minimum magnetic anisotropy value of 16.85×103 J/m3, which is attributed to the compensation effect on magnetocrystalline anisotropy brought about by the Co2O3 addition. The DC resistivity of MnZn ferrites generally decreases with the increasing Co2O3 content. In terms of the loss performance, proper amount of Co2O3 doping at 0.36 wt% is seen to benefit the reduction of core loss, which is primarily the results of enhanced initial permeability. Due to the decreasing resistivity of MnZn ferrites with increasing temperature, the core loss generally increases as the temperature is increased from 25 to 140 °C. The minimum core loss appears in the temperature range of 40–80 °C, which corresponds to the temperature dependence of initial permeability.
Data availability
All data generated in this study are reflected in the figures embedded in the article and can be made available on reasonable request.
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Funding
This present work was financially supported by the National Natural Science Foundation of China under Grant No. 52002055, and 52172267, the Sichuan Science and Technology Planning Project [2021YJ0556], the Innovation Group Project of Sichuan Province [2022JDTD0018], and the Science and Technology Bureau of Longquanyi District of Chengdu under Application Basis R&D Project No. LQXKJ-KJXM-2022-05.
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BF: Conceptualization, Formal analysis and Writing—Review and editing. YY: Investigation, Methodology, Formal analysis and Writing—Original draft. ZL: Investigation, Formal analysis and Writing—Original draft, review and editing. ZY: Conceptualization, Supervision, Project administration, Methodology, Writing—Review and editing. CW: Funding acquisition and Writing—Review. KS: Writing—Review. XJ: Writing—Review. QL: Funding acquisition and Writing—Review. ZL: Writing—Review.
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Fu, B., Yi, Y., Li, Z. et al. Soft magnetic properties and loss performance of Co2O3-doped power MnZn ferrite at 100–300 kHz. J Mater Sci: Mater Electron 34, 1259 (2023). https://doi.org/10.1007/s10854-023-10639-9
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DOI: https://doi.org/10.1007/s10854-023-10639-9