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Large linear magnetoelectric effect and field-induced ferromagnetism and ferroelectricity in DyCrO4

All the magnetoelectric properties of scheelite-type DyCrO4 are characterized by temperature- and field-dependent magnetization, specific heat, permittivity, electric polarization, and neutron diffraction measurements. Upon application of a magnetic field within ±3 T, the nonpolar collinear antiferromagnetic structure leads to a large linear magnetoelectric effect with a considerable coupling coefficient. An applied electric field can induce the converse linear magnetoelectric effect, realizing magnetic field control of ferroelectricity and electric field control of magnetism. Furthermore, a higher magnetic field (>3 T) can cause a metamagnetic transition from the initially collinear antiferromagnetic structure to a canted structure, generating a large ferromagnetic magnetization up to 7.0 μB f.u.−1. Moreover, the new spin structure can break the space inversion symmetry, yielding ferroelectric polarization, which leads to coupling of ferromagnetism and ferroelectricity with a large ferromagnetic component. Researchers have isolated a material with remarkable electrical and magnetic properties that could simplify data manipulation in devices such as high-density memory platforms. Youwen Long from the Institute of Physics, Chinese Academy of Sciences in Beijing and colleagues report that synthesizing dysprosium chromate (DyCrO4) under high pressure conditions produces a crystal with internal dipoles that respond to both magnetic and electric fields. Experiments demonstrated that magnetic field ordering of dipoles caused the material to emit a new electric output. Conversely, electric field alignment generated a large magnetic response over a wide temperature range. This magnetic output could be boosted even further by tweaking the initial dipole alignment with strong magnets. The team attributed the unusual magnetic and electric field control mechanisms to electronic interactions between dysprosium and chromium ions. The scheelite-type DyCrO4 shows a large linear magnetoelectric effect (magnetic field induced electric polarization) as well as the converse effect (electric field induced magnetization) within ± 3 T. A higher magnetic field induces a metamagnetic transition from the initially collinear antiferromagnetic structure to a canted one, generating a giant ferromagnetic component by about 7 μB f.u.−1. The new spin structure can break the spatial inversion symmetry and yield spontaneous ferroelectric polarization, giving rise to the coupling of ferromagnetism and ferroelectricity in a single-phase material.


Introduction
The linear magnetoelectric (ME) effect and multiferroicity enable control of polarization P (magnetization M) by a magnetic (electric) field, which is beneficial for applications in spintronic devices, nonvolatile memories, high-sensitivity magnetic field sensors, etc [1][2][3][4][5] . In the linear ME effect, the induced electric polarization or magnetization is proportional to the applied magnetic field H or electric field E, which can be expressed as P = αH or μ 0 M = αE 6,7 , where α denotes the linear ME coefficient and μ 0 denotes the magnetic permeability of a vacuum. Since the first observation of the linear ME effect in Cr 2 O 3 in the 1960s 8,9 , the search for single-phase ME materials with larger α values has attracted much attention. The maximum α obtained for a nonpolar antiferromagnetic (AFM) structure is <40 ps m −1 usually 6 . It is important to obtain a larger and constant ME effect in wider temperature and/or magnetic field regions for potential applications.
In the 1990s, the term "multiferroics" was proposed to describe materials that simultaneously exhibit more than one ferroic order, such as ferromagnetism, ferroelectricity, and ferroelasticity, in a single phase 10 . Among the different multiferroics, the spin-ordering-induced ferroelectrics (i.e., ME multiferroics) attracted significant attention owing to the strong ME coupling [11][12][13][14][15] . Based on the magnetic space group, collinear ferromagnetic (FM) spin alignment cannot break the spatial inversion symmetry. Therefore, electric polarization in single-phase ME multiferroics is often induced by some peculiar AFM or canted AFM spin structures instead of collinear ferromagnetism 16 . Consequently, the magnetic moment is too small to be effectively controlled [17][18][19] . It is very challenging to obtain a material with strongly coupled FM-ferroelectric properties and a considerable magnetic moment.
DyCrO 4 has a rare Cr 5+ valence state. Under ambient conditions, it crystallizes into a zircon-type crystal structure with the space group of I4 1 /amd 20,21 . An FM phase transition with a large magnetocaloric effect occurs at approximately 23 K [22][23][24] . Moreover, the zircon-type structure is sensitive to external pressure. A pressureinduced irreversible structural phase transition toward a scheelite-type new phase with I4 1 /a symmetry has already been reported 25 . In contrast to the FM zircon phase, the scheelite phase exhibits a long-range AFM transition [26][27][28] . In this study, scheelite-type DyCrO 4 was prepared in a polycrystalline form by a high-pressure and moderatetemperature treatment method (see "Materials and methods" below). Based on the powder X-ray diffraction (XRD) and neutron diffraction results, there is no discernable impurity phase, such as the residual FM zircon phase, or decomposed DyCrO 3 perovskite phase (see Supplementary Figs. S1 and S2 for details). This compound has a nonpolar collinear AFM ground state with zero magnetic field. Within μ 0 H ≈ ±3 T, a large and almost constant linear ME effect is observed, enabling H control of P and E control of M. Under higher magnetic fields, a metamagnetic transition occurs and is accompanied by a large FM magnetization. Furthermore, the new spin structure can break the spatial inversion symmetry and thereby generate ferroelectric polarization. The presented DyCrO 4 paves the way for novel investigations on simultaneous direct and converse linear ME effects and FM-ferroelectrics with large magnetic moments.

Sample synthesis and XRD
To fabricate the scheelite-type DyCrO 4 sample, the zircon-type sample was prepared at ambient pressure as a precursor, as reported in a previous study 26 . The prepared zircon-type DyCrO 4 powders were pressed into a golden cylinder with a diameter of 4.0 mm and height of 3.0 mm. The cylinder was treated at 6-8 GPa and 700-750 K for 10-30 min on a cubic-anvil-type high-pressure apparatus using pyrophyllite as a pressure transmission medium. When the heating power was turned off, the pressure was slowly released. The crystal quality and structure were analyzed by powder XRD using a Huber diffractometer with Cu K α1 radiation at 40 kV and 30 mA. The XRD data were acquired at room temperature in the 2θ range of 10°-100°with steps of 0.005°and analyzed by Rietveld refinement using the GSAS software 29 .
Magnetic, specific heat, dielectric, and pyroelectric current measurements The magnetic susceptibility (χ) and magnetization (M) were measured using a magnetic property measurement system (Quantum Design, MPMS-3). Both zero fieldcooling (FC) and FC modes were employed for χ measurements at 0.01 T. The field-dependent M measurements were performed at different temperatures. The specific heat (C p ) and electrical properties were measured using a physical property measurement system (Quantum Design, PPMS-9T). The C p data were acquired during cooling in the range of 50-2 K with different magnetic fields. For the measurements of the relative dielectric constant ε r , dielectric loss tanδ, and pyroelectric current density (J), the specimens were fabricated as thin plates with a typical surface area of 1-2 mm 2 and a thickness of 0.2 mm. Silver electrodes were coated onto the two surfaces of the plate for electrical measurements. Different frequencies of 1 kHz, 10 kHz, 0.1 MHz, and 1 MHz were applied for the dielectric constant and dielectric loss measurements at selected magnetic fields in the range of 0-9 T with intervals of 1 T using an Agilent E4980A Precision LCR Meter while sweeping the temperature from 2 to 50 K with a heating rate of 2 K min −1 . The pyroelectric current was measured by a Keithley 6517B precise electrometer while sweeping the temperature from 2 to 50 K at a rate of 2 K min −1 . Before this measurement, the sample was poled from 50 to 2 K with a poling electric field of E pol = ±1.08 MV m −1 . Once the temperature was decreased to 2 K, E pol was switched off and J was measured as described above. The magneticfield-dependent current was measured while sweeping the magnetic field at a rate of 0.01 T s −1 . In these measurements, the PPMS was used to provide low-temperature and magnetic field environments. The electric polarization (P) was obtained by integrating J as a function of time. In addition, we measured the electric-field-induced magnetization using MPMS-3 with different electric fields produced by the Keithley 6517B electrometer. Before the measurement, the sample was cooled from 50 to 10 K at a rate of 2 K min −1 at E pol = 0.5 MV m −1 and μ 0 H = 4 T. Once the temperature was decreased to 10 K, both E pol and H were switched off, and then M was measured during heating from 10 to 26.5 K at fixed temperatures and selected electric fields.

Neutron diffraction measurements
The neutron powder diffraction (NPD) measurements were carried out using the constant-wavelength highresolution neutron powder diffractometer HB2A at Oak Ridge National Laboratory (ORNL). The temperature was controlled by a Lakeshore Bridge, while the magnetic field was generated by an Oxford-5 T superconducting magnet. The temperature-dependent diffraction profiles were measured at a wavelength of λ = 2.41 Å with the collimation out-high intensity mode. The overall powder mass was 1.3 g. To reduce the thickness to enable a neutron transmission rate of approximately 90%, the sample powders were spread out inside a 30 × 48 × 0.25 mm 3 sample holder; their thickness was approximately 0.15 mm. The empty space in the sample holder was filled with Fluorinert to help fix the powders under a low temperature. The data were measured at different magnetic fields of 0, 1, 3, and 4.3 T. The magnetic refinements were carried out by the Rietveld method with the FullProf program 30 .

Results and discussion
As shown in Fig. 1a, the scheelite-type DyCrO 4 with a space group of I4 1 /a consists of spatially isolated CrO 4 tetrahedra and edge-sharing DyO 8 dimers 20,26 . According to the space group, DyCrO 4 is centrosymmetric without spontaneous ferroelectric polarization in the crystal structure. With the decrease in temperature to T N = 24 K, both the magnetic susceptibility measured at 0.01 T and specific heat at zero field show an AFM phase transition (Fig. 1b). Moreover, the NPD results at zero field (Fig. S2) suggest a collinear AFM spin structure composed of Dy 3+ and Cr 5+ spin sublattices, as presented in Fig. 1a. The magnetic symmetry analysis illustrates that the collinear AFM structure of DyCrO 4 has a magnetic point group of 2′/m, where the two-fold rotation is along the c axis, whereas the mirror is perpendicular to the c axis. This magnetic point group gives the ME tensor α ME with the form shown in Eq. (1). Therefore, although the magnetic group is nonpolar, it allows nonzero linear ME components, such as α 13 (α 31 ) and α 23 (α 32 ). This implies that an external H parallel to the c axis induces P along the a/b axis or vice versa while maintaining the initial spin structure, which can in principle lead to a linear ME effect.
To demonstrate the linear ME effect in an experiment, we first measure the temperature dependences of the relative dielectric permittivity and dielectric loss at different magnetic fields with an H⊥E configuration, as shown in Fig. 1c, d. At μ 0 H = 0 T, no anomaly in permittivity is observed in the measured temperature range. In contrast, a moderate magnetic field can induce an apparent dielectric peak near T N . Moreover, with the increase in the magnetic field, the dielectric peak becomes sharper and gradually shifts toward lower temperatures (Fig. 1c).
On the other hand, at a fixed H, the dielectric peak is independent of the measurement frequency (Fig. S3). Analogous phenomena are observed in the dielectric loss with a maximum value <0.032 (Fig. 1d), indicating the intrinsic dielectric variations with the magnetic field. The dielectric measurements thus suggest H-induced P.
To probe the off-diagonal nonzero components of the ME tensor α ME of the polycrystalline sample, we employ an ME annealing procedure with an H⊥E configuration, as described in the "Materials and methods" section and reported in the literature 31,32 . In a polycrystalline sample with a random distribution of the grain orientation, such an ME annealing procedure can be used to choose one of the ME domains for each grain so that the macroscopic ) The temperature-dependent pyroelectric current was measured at the selected magnetic fields (Fig.  S4), and then the related polarization was obtained by integrating the pyroelectric current as a function of the time. Using this approach, no significant P is observed at μ 0 H = 0 T at temperatures down to 2 K, as shown in Fig. 1e. However, under an external H⊥E, electric polarization is induced. The onset temperature of the induced P is in close agreement with the position of the dielectric peak. Moreover, the sign of H-induced P can be reversed by reversing the poling electric field E pol while maintaining the magnitude of P, as shown in Fig. 1f and Fig. S4. These results confirm H-induced polarization in accordance with the nonzero off-diagonal components in α ME , which is expected from the AFM spin structure of DyCrO 4 . Compared with the H⊥E configuration, the induced P observed in our sample with an H//E configuration is considerably reduced (Fig. S5), consistent with the null value of the diagonal components of the ME tensor as presented in Eq. (1), although the detected P is not exactly zero due to the polycrystalline nature of the sample. As shown in Fig. 1e, f, at μ 0 H ≤ 3 T, the magnitude of Hinduced P increases with H and exhibits a broad maximum at approximately 15 K and then slightly decreases at lower temperatures. Moreover, if one looks at the pyroelectric current as presented in Fig. S4, the sign of the current measured at 2 and 3 T changes to be negative below approximately 15 K. This observation suggests that the Cr and Dy ions may have opposite contributions to the induced electric polarization <3 T. However, for μ 0 H ≥ 4 T, the sign of the pyroelectric current is always positive. Correspondingly, the polarization gradually saturates and does not vary with further cooling. The essentially different polarization behaviors at lower and higher fields mentioned above are related to different spin structures due to a field-induced metamagnetic transition, as shown later. The maximum P is observed in the range of 4-5 T, which may be attributed to the interaction between the Dy-4f and Cr-3d moments. Owing to the remarkable magnetic anisotropy, the applied magnetic field can change the magnetic state of Dy and thus affect the electric polarization. To elucidate the distinct polarization behaviors of these, we measured the magnetization as a function of the magnetic field at selected temperatures, as presented in Fig. 2a. Above T N , M exhibits a linear relationship with H owing to paramagnetism. Below T N , the linear magnetization behavior is also observed at lower fields owing to the collinear AFM ground state (see Fig. S6). However, with the increase in H above a critical value (H c ), which is determined by the derivative of M with respect to H, a metamagnetic transition occurs from the initial collinear AFM structure to a canted one. For example, at 2 K, the critical field is 3.1 T; a large magnetic moment up to 7.0 μ B f.u. −1 caused by the metamagnetic transition is observed at field up to 7 T.
Further, the magnetic field-dependent dielectric constants were measured at selected temperatures (Fig. S7) to characterize the magnetodielectric (MD) effect (Fig. 2b). The MD curves display significant increases around μ 0 H c due to the metamagnetic transition, suggesting a different polarization behavior between the cases below and above μ 0 H c . Moreover, the MD value at 20 K and 7 T reaches 11.4%, which is larger than the maximum MD value for the single-crystal multiferroic TbMnO 3 11 . The magneticfield-dependent polarization was also measured to  Figure  2c, e show the resulting P calculated from the corresponding ME current measurement results (Fig. S8) at 20 and 2 K, respectively. At 20 K, the polarization variation is close to linear within ±μ 0 H c reflecting the linear ME effect related to the collinear AFM; a sharp variation occurred around the critical field, above which the linear ME behavior was affected. The calculated linear ME coefficient α of DyCrO 4 at 20 K was approximately constant at 50 ps m −1 in the region within ±μ 0 H c (Fig. 2d). Usually, the linear ME effects observed in collinear AFM materials without spontaneous electric polarization are quite small. For example, for a Cr 2 O 3 single crystal, which is a prototype system for studies on the linear ME effect, the value of α is only approximately 2-4 ps m −1 33,34 . Co 4 Nb 2 O 9 35 and LiCoPO 4 36 exhibit larger linear ME effects, but the coupling coefficients are approximately 20-30 ps m −1 . Compared with those of most single-phase compounds with nonpolar collinear AFM spin structures, the α value for DyCrO 4 is one of the highest reported, even though our sample is polycrystalline. The TbPO 4 single crystal is an extraordinary example with an α value up to 730 ps m −1 but only below a lower AFM transition temperature of 2.38 K 7 . It is worth noting that a few ME multiferroics exhibit very large ME effects 19,[37][38][39][40][41] . However, they often only occur near the phase transition boundaries, while away from them, the ME effects are considerably reduced. In contrast, the ME coefficient of DyCrO 4 is relatively constant over the wide magnetic field range of −μ 0 H c to +μ 0 H c . At low temperatures (e.g., 2 K) (Fig. 2e, f), the linear ME behavior of DyCrO 4 is also observed. At this temperature, the maximum α is increased to approximately 110 ps m −1 at μ 0 H c . We will later discuss more about the different P-H behaviors observed at 20 and 2 K.
In addition, we investigate the electric field-induced magnetization M E , i.e., the so-called converse ME effect 2 . Figure 3a shows the temperature dependence of M E measured in different electric fields. Below T N , a considerable E-induced magnetization with magnitude tunable by the electric field is observed. Moreover, the sign of M E can be reversed upon application of an opposite measurement electric field. These features are very similar to those of the H-induced P, as shown in Fig. 1e, f. To further analyze the linear dependence of M E on the applied E, periodically varied electric fields (top panel in Fig. 3b) were used for M E measurements at 10 K and zero magnetic field. The middle and bottom panels in Fig. 3b present the obtained values of M E after ME cooling at μ 0 H = 4 T and E pol = 0.5 and −0.5 MV m −1 . The magnitude of M E periodically changes according to the periodic variation in the electric field. Furthermore, a linear relationship between M E and applied E is observed, as demonstrated in the inset of Fig. 3b, confirming the converse linear ME effect of DyCrO 4 . The converse ME coefficient derived from dM E /dE at 10 K is 26 ps m −1 , which is slightly smaller than the value obtained from the H-induced P at 20 K.
The spin structure was studied in detail by NPD to investigate the spin origin of the electric polarization (see Supplementary Information for detailed analysis of NPD data). Figure 4a shows the net spin diffraction patterns obtained at 2 K under different magnetic fields after subtraction of the nuclear contribution from the collected NPD patterns (Fig. S2). At zero magnetic field, the spin structure composed of Cr 5+ and Dy 3+ was determined to be k = (0, 0, 0) collinear AFM with spin moments parallel to the a axis of the crystal lattice (Fig. 1a), agreeing well with a previous study 28 . The refined magnetic moments of Cr 5+ and Dy 3+ at 2 K and 0 T are 1.0 ± 0.1 and 9.6 ± 0.5 μ B , respectively, as expected from the spin-only theoretical value for a 3d-Cr 5+ ion (1.0 μ B ) and obtained (1), allows the generation of an intrinsic linear ME effect. Since both Cr 5+ and Dy 3+ take part in the AFM ordering and only a single anomaly is observed in magnetic susceptibility and specific heat curves (see Fig. 1b and Fig. S9), the Cr 5+ and Dy 3+ ions should order simultaneously at T N = 24 K. We thus conclude that these two types of ions contribute to the large linear ME effect in DyCrO 4 . Upon the application of a magnetic field up to 4.3 T (>μ 0 H c ), the propagation vector remains unchanged k = (0, 0, 0). The most notable variation is that the intensity of the magnetic (002) reflection gradually decreases with the increase in H (Fig. 4a, b and Fig. S10). This change implies that the magnetic moments rotate toward the applied magnetic field, inducing canting of the collinear AFM structure, which yields a net FM moment. Considering the polycrystalline nature of the sample, it is difficult to exactly fit the magnetic peaks under a magnetic field, owing to the variable orientation of the magnetic field with respect to different magnetic domains. Constraining our analysis to the two existing magnetic states (i.e., collinear AFM structure determined at zero field and collinear FM structure with all of the moments parallel to a fixed axis such as the c axis), we can obtain the ratio between these two phases by fitting the scale factor while keeping the spin moments of Cr and Dy constant, as determined at 0 T. The results evaluated at 2 K are shown in Fig. 4c. The composition of the FM phase at 4.3 T is approximately 65 ± 5%, indicating the strong ferromagnetism originating from the canted AFM alignment. After the metamagnetic phase transition above the critical magnetic field, the canted spin structure can be composed of both Dy 3+ and Cr 5+ spin sublattices (Fig. 4d) or just the dominant Dy 3+ sublattice (Fig. 4e). In these two cases, the magnetic point group always changes from the initially nonpolar 2′/m to a polar m. This polar point group can break the space inversion symmetry and thereby cause spontaneous ferroelectric polarization, yielding field-induced ferromagnetism and ferroelectricity in the compound with strong coupling with each other. It is worth noting that magnetostriction may occur under a high field, but this effect on the lattice change should be very small 42 . Based on the above ME results, the presented DyCrO 4 is a rare material that simultaneously exhibits large direct and converse linear ME effects as well as fieldinduced ferromagnetism-ferroelectricity with a giant magnetic moment, making it distinct from other reported materials. For example, in the well-known type-II multiferroics such as TbMnO 3 11 , the polarization originates from the spiral AFM ordering, and thus this structure does not exhibit a considerable net magnetic moment. Moreover, the converse ME effect is not observed in this compound because the magnetic field can easily change the spin structure. In compounds with (weak) ferromagnetism and electric polarization such as EuTiO 3 and GdFeO 3 , although the polarization appears at a higher temperature (approximately 250 K in the EuTiO 3 thin film), the FM transition occurs at a significantly lower temperature (4.2 K in the EuTiO 3 thin film), indicating negligible ME coupling 43 . In contrast to the field-induced polarization, in the weakly FM GdFeO 3 , the magnetic field rapidly suppresses the polarization to zero at 2-3 T 44 . DyFeO 3 also has a field-induced ferroelectric state, but the accompanying magnetic moment is limited (<1.0 μ B f.u. −1 ) 45 .
Using the experimental data, a characteristic magnetic and electric phase diagram can be obtained for different temperatures and magnetic fields. As shown in Fig. 5, the solid circles (T c ) and triangles (T N ) represent the phase boundary between the spin/electric order and disorder for scheelite-type DyCrO 4 . The values of T c are determined from the dielectric peaks shown in Fig. 1c, while T N is determined from specific heat data (Fig. S9). Below T N and μ 0 H c , the compound has a nonpolar collinear AFM structure with a large linear ME effect. The α value of this phase is among the highest values for the single-phase ME materials with nonpolar collinear AFM structures. Moreover, the magnitude of α is almost constant in the wider magnetic field region of −μ 0 H c to +μ 0 H c . In addition, the converse linear ME effect is also observed in this magnetic field region. Furthermore, the metamagnetic phase transition changes the nonpolar AFM spin structure to the polar structure with a large FM magnetization. A strong ferromagnetism coupled with ferroelectricity thus develops below T c and above μ 0 H c . Note that, when the magnetic field increases to 9 T, the compound is located near the paramagnetic and paraelectric phases at 20 K, while the FM and ferroelectric phases set in at 2 K. This difference is the reason why H-induced P at 20 and 2 K displays different behaviors in high magnetic fields, as shown in Fig. 2c, e. The presented DyCrO 4 is a rare material, which simultaneously displays large direct and converse linear ME effects in the nonpolar collinear AFM phase and field-induced ferromagnetism and ferroelectricity with a large magnetic moment.