Magnetotransport properties in a noncentrosymmetric itinerant magnet Cr{}_{11}Ge{}_{19}

Magnetotransport properties in a noncentrosymmetric itinerant magnet CrGe

N. Jiang jiangnan@mail.ecc.u-tokyo.ac.jp    Y. Nii    R. Ishii    Z. Hiroi    Y. Onose Department of Basic Science, University of Tokyo 153-8902, Japan
Institute for Solid State Physics, University of Tokyo, Kashiwa, Chiba 277-8581, Japan
August 23, 2019
Abstract

We have investigated anomalous Hall effect and magnetoresistance in a noncentrosymmetric itinerant magnet CrGe. While the temperature- and magnetic-field-dependent anomalous Hall conductivity is just proportional to the magnetization above 30 K, it is more enhanced in the lower temperature region. The magnitude of negative magnetoresistance begins to increase toward low temperature around 30 K. The anisotropic magnetoresistance emerges at similar temperature. Because there is no anomaly in the temperature dependence of magnetization around 30 K, the origin of these observations in transport properties is ascribed to some electronic structure with the energy scale of 30 K. We speculate this is caused by the spin splitting due to breaking of spatial inversion symmetry.

pacs:

I Introduction

Recently, noncentrosymmetric magnets have been studied extensively, because noncollinear spin textures are emergent in real and momentum spaces. In this class of materials, there is the spatially uniform component of the Dzyaloshinsky-Moriya interaction, which produces, in some cases, real space spin textures as a result of competition with the exchange interaction. The skyrmion latticeMühlbauer et al. (2009); Yu et al. (2010) and the chiral soliton latticeTogawa et al. (2012) are examples of them. In particular, in skyrmion lattice, electrons acquire Berry’s phase due to the topological nature of spin structure, which gives rise to nontrivial Hall signal denoted as topological Hall effectNeubauer et al. (2009). In noncentrosymmetric metals and semiconductors, the electronic bands are spin splitted along the principal axis dependent on the momentum due to the spin orbit interaction. The examples are the Rashba and Dresselhaus effectsRashba (1960); Dresselhaus (1955). In the itinerant magnets without spatial inversion symmetry, the coexistence of spin orbit driven spin splitting and localized magnetic moments gives raise to novel magnetoelectric phenomena. For example, the spin dependent scattering caused by magnetic moments in a spin splitted band gives raise to large anisotropic magnetoresistance (AMR)Rushforth et al. (2007). The anomalous Hall effect induced by momentum space Berry phase is also anticipated in a exchange biased Rashba bandDugaev et al. (2005); Sinitsyn et al. (2005). The magnetic moment can be controlled by the spin orbit torque produced by the electric current in a spin splitted bandMihai Miron et al. (2010). Because these novel phenomena depend on the crystal and magnetic structures, further studies of various noncentrosymmetric magnets seem quite important for the deep understanding of related physics.

Here we study a noncentrosymmetric itinerant magnet CrGe with a space group Han et al. (2016); Ghimire et al. (2012); Zagryazhskii et al. (1968); Kolenda et al. (1980). It shows a magnetic transition below about 90 K. The magnetization curve below Curie temperature is consistent with the picture of anisotropic ferromagnet with the easy axis along -axis. The effect of breaking of inversion symmetry has not been reported so far. In this paper, we have investigated electric and magnetic properties in a single crystal of CrGe in order to exploit the effect of breaking of inversion symmetry. We observe enhancement of anomalous Hall conductivity and the magnitude and anisotropy of magnetoresistance around 30 K. We speculate these anomalies are caused by the spin splitting due to inversion symmetric breaking.

Ii Experimental Details

Single crystals of CrGe were prepared by the self flux method. Mixed powder of Cr and Ge with the ratio of 1:4 were loaded in a alumina crucible. The crucible was sealed together with zirconium getter in a silica tube under vacuum. The tube was placed in a Bridgman furnace and heated to 1100 C in 20 hours and kept for 60 hours. After cooled to 1000 C in 5 hours, the tube was moved toward low temperature region in temperature gradient ( 1-5 C/mm) at the rate of 0.5 mm per hour for 300 hours. The crystals with the dimensions of several millimeter were obtained. The single crystallinity was confirmed by Laue X-ray diffraction. Magnetization was measured in a quantum design magnetic property measurement system (MPMS). The longitudinal and Hall resistivities were measured by conventional four probe method in a superconducting magnet (Oxford instruments Spectromag).

Iii Results and Discussion

Figure 1: Temperature dependence of (a) magnetization at 0.1 T and 1.5 T for and , (b) saturation magnetic fields, and and (c) zero field resistivity for and . Inset in (b) shows magnetization curves for and at 10 K.

Figure 1 (a) shows the temperature dependence of the magnetization in magnetic fields of 0.1 T and 1.5 T for and . The magnetization begins to rapidly increase around 85 K, suggesting the ferromagnetic transition. The magnetization along -axis is larger than that along -plane at 0.1 T, being consistent with the previous studyHan et al. (2016). At 1.5 T, the anisotropy of magnetization becomes very small. In the inset of Fig. 1 (b), we show the magnetization curves for and at 10 K. The magnetization curves for and saturate around 1 T and 0.1 T, respectively. After saturation, the magnitudes for and are almost identical. Figure 1 (b) shows the temperature dependence of the saturation magnetic fields . for is larger than that for , and both increase almost linearly below . In Fig. 1 (c), we show the temperature dependence of resistivities measured with electric currents perpendicular and parallel to -axis ( and ). For both the configurations, the resistivity shows a clear kink structure at while the temperature dependence is small in the higher temperature region. Below , the resistivity decrease rapidly due to the suppression of magnetic fluctuation, and the anisotropy is enhanced. The residual resistivities for and were 1.5 and 3.3 cm, respectively, indicating the high quality of present crystals.

Figure 2: Magnetic field dependence of Hall resistivity at various temperatures.
Figure 3: (a) Temperature dependence of Hall conductivity (red dots) and magnetization (green dashed line) around 1.5 T. The inset shows potted against . The black dashed line shows the dependence expected in the case of coexistence of skew scattering and intrinsic mechanisms (see main text). (b) Temperature dependences of for and . (c) Temperature dependences of for and .

In Fig. 2, we show the magnetic field dependence of Hall resistivity at respective temperatures. While the Hall resistivity shows linear magnetic field dependence at 120 K, it tends to saturate in the high field and the lower temperature region. Below the spontaneous component of Hall resistivity emerges. It decreases with decreasing temperature from . The magnetic field dependence of Hall resistivity is quite similar to that of magnetization. In the low temperature and high field region, in which the magnetization is saturated, the Hall resistivity does not show large magnetic field dependence. These suggest the dominant contribution of anomalous component. In Fig. 3 (a), we plot the temperature dependence of the Hall conductivity around 1.5 T for . To be strict, we average the data between 0.3 T to 2.6 T in order to precisely estimate . The error bar represents the standard error. We also plot the temperature dependence of the magnetization at 1.5 T for comparison. Above 30 K, the temperature dependence of is parallel with that of magnetization. This is consistent with intrinsic anomalous Hall effectNagaosa et al. (2010). Nevertheless, becomes larger than that expected from the scaling behavior below 30 K. Such an enhancement of might be caused by the emergence of skew scattering contribution. If this is the case, should satisfy the relation of , where , and and are constantsTian et al. (2009). However, in the present case, does not follow this relation as shown in the inset of Fig. 3 (a) inset. As discussed below, the magnetoresistance also shows anomalies in similar temperature range.

Figure 4: (a), (b) Magnetic field dependence of magnetoresistance for (a) and (b) in the magnetic fields parallel and perpendicular to -axis at various temperatures.
Figure 5: (a) Magnetic field dependence of for and at 2 K, 5 K, and 10 K. (b) Magnetic field dependence of at 2K with various configurations of current and magnetic field. (c) Magnetic field dependence of for in the magnetic fields parallel and perpendicular to -axis at 10 K. Dashed line shows vertically shifted for . and indicate the estimated components of positive magnetoresistance and AMR. (d) at 7 T, at 7 T, and for plotted against .

We show the magnetic field dependence of magnetoresistance in magnetic fields parallel and perpendicular to -axis in Fig. 4 (a) for and in Fig. 4 (b) for . The magnetoresistance data was measured in the transverse configuration () except for the and configuration. In conventional itinerant ferromagnets, negative magnetoresistance is observed around due to spin scatteringMasuda et al. (1977). It usually decreases with decreasing temperature. Such a negative magnetoresistance is certainly observed around also in the present case. In this temperature range, the magnetoresistance is isotropic with respect to the magnetic field direction. With decreasing temperature from , the magnetoresistance decrease at first. However, below 30 K the magnetoresistance begins to increase again. The magnetoresistances for and become different at lower temperature for both the and configurations. The anisotropy is increased in the low field region and saturated around 1 T. These observations suggest that the resistivity depends on the direction of the magnetization, which is ascribed to anisotropic magnetoresistance induced by spin orbit interactionMcGuire and Potter (1975). Incidentally, the additional -dependent positive magnetoresistance is observed in the high field region at 10 K for and . The positive magnetoresistance steeply increases with decreasing temperature from 10 K as shown in Fig. 5 (a). In Fig. 5 (b) we show the magnetoresistance for various current and field configurations at 2 K. While the positive magnetoresistance was observed at 2 K in all the configuration, that for and is most enhanced.

Phenomenologically, the observed magnetoresistance is composed of three components as follows;

(1)

is positive magnetoresistance enhanced in the low temperature region mainly in the configuration of and . is negative magnetoresistance. This component seems isotropic. is anisotropic magnetoresistance dependent on the direction of magnetization. We estimate these components for the magnetoresistance above 10 K as illustrated in Figs. 5 (c). We assume the isotropy of and field independence above for . We also assume that data above 10 K is dominated by the component. Therefore can be estimated by the extrapolation of data above to zero field. The component is estimated as for subtracted by and . Below 5 K, we assume is negligible compared with the other components and is estimated by the linear extrapolation (see Fig. 5 (a)). The estimated at 7 T, at 7 T, and are plotted against in Fig. 5 (d). steeply increased roughly as , while the increase of and are not so significant. Such a positive magnetoresistance enhanced in the low resistive regime is usually ascribed to the orbital magnetoresistance. The orbital magnetoresistance is caused by Lorentz force and becomes significant when is large ( and are cyclotron frequency and relaxation time, respectively). The orbital magnetoresistance satisfies Kohler’s rule, in which magnetoresistance is scaled by . While the scaling behavior cannot be directly confirmed in this case because of coexistence of other type magnetoresistance, the power law dependence is consistent with the Kohler’s rule. On the other hand, the low temperature increase of and can not be ascribed to the orbital magnetoresistance, because the dependences are quite gradual compared with , and because the magnetic field dependences are different from that expected for orbital magnetoresistance ( in high field and 0).

Apart from orbital magnetoresistance, let us discuss the low temperature anomalies of magnetotransport properties. We show the temperature dependence of and in Fig. 3 (b) and (c). The data shown in this figure is estimated similarly to the case of . begins to increase with decreasing temperature below 30 K. Similar low temperature enhancements of AMR were reported for some itinerant ferromagnets, which is caused by the crossover of dominant scattering source from electron phonon type to impurity typevan Gorkom et al. (2001); Smit (1951). Because the impurity scattering induces the large AMR compared with electron phonon scattering, the magnitude of AMR is increased as the resistivity approaches the = 0 value. However, in our case the resistivity around the onset of AMR is much larger than the residual resistivity. Therefore, there should be another origin of temperature dependence. Around the onset temperature, begins to increase and the anomalous Hall conductivity is enhanced compared with magnetization. These three anomalies seem to have a common origin. The magnetization and the saturation magnetic fields does not show any anomaly around this temperature as shown in Figs. 1 (a) and (b). Therefore, the above mentioned transport anomalies should originate from some electronic structure with the energy scale of 30 K. Because CrGe is a noncentrosymmetric magnet, the spin splitting caused by spin orbit interaction seems the most plausible origin. As mentioned in introduction, in ferromagnets without inversion symmetry, anomalous Hall effect can be induced by the Berry curvature of spin splitted band. The anisotropic magnetoresistance can also be induced by spin dependent scattering by localized moment. The origin of negative magnetoresistance may be caused by the magnetic field induced change of spin splitted bands. However, at present, this scenario cannot be examined extensively because of the lack of the information regarding spin-splitted band structure. In order to confirm this scenario relativistic band calculation is needed.

Iv Summary

We have uncovered several magnetotransport anomalies below around 30 K. The negative magnetoresistance and anomalous Hall conductivity are largely enhanced in this temperature region. Anisotropic magnetoreisistance is also observed in a similar temperature region. We speculate these observations are caused by the spin splitting due to the breaking of spatial inversion symmetry. The investigation of relativistic energy band is indispensable for understanding of spin dependent transport properties in CrGe.

Acknowledgements.
This work was supported in part by Grants-in-Aid for scientific research (Grants no.17H05176, no.16H04008, and no.15K21622) for the Japan Society for the promotion of Science.

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