Thermodynamic and transport properties of single crystalline RCoGe (R = Y, La-Nd, Sm-Tm)
Single crystals of RCoGe (R = Y, La-Nd, Sm-Tm) were grown using a self-flux method and were characterized by room-temperature powder x-ray diffraction; anisotropic, temperature and field dependent magnetization; temperature and field dependent, in-plane resistivity; and specific heat measurements. In this series, the majority of the moment-bearing members order antiferromagnetically; YCoGe and LaCoGe are non-moment-bearing. Ce is trivalent in CeCoGe at high temperatures, and exhibits an enhanced electronic specific heat coefficient due to Kondo effect at low temperatures. In addition, CeCoGe shows two low-temperature anomalies in temperature-dependent magnetization and specific heat measurements. Three members (R = Tb-Ho) have multiple phase transitions above 1.8 K. Eu appears to be divalent with total angular momentum L = 0. Both EuCoGe and GdCoGe manifest essentially isotropic paramagnetic properties consistent with J = S = 7/2. Clear magnetic anisotropy for rare-earth members with finite L was observed, with ErCoGe and TmCoGe manifesting planar anisotropy and the rest members manifesting axial anisotropy. The experimentally estimated crystal electric field (CEF) parameters B were calculated from the anisotropic paramagnetic and values and follow a trend that agrees well with theoretical predictions. The ordering temperatures, T, as well as the polycrystalline averaged paramagnetic Curie-Weiss temperature, , for the heavy rare-earth members deviate from the de Gennes scaling, as the magnitude of both are the highest for Tb, which is sometimes seen for extremely axial systems. Except for SmCoGe, metamagnetic transitions were observed at 1.8 K for all members that ordered antiferromagnetically.
keywords:Rare-earth compounds, Single crystals, Magnetization, Resistivity, Specific heat, Metamagnetic transition
The RTX (R = Y, La-Lu; T = transition metal; X = Si, Ge) ternary intermetallic family has been studied for decadesbook (). Most of RTX compounds crystallize in the ThCrSi tetragonal structureBan1 () (space group I4/mmm) with a single R ion site with a tetragonal point symmetry. Given that transition metals in this family, except for Mn, are non-moment-bearing, the magnetic properties of these compounds are mainly determined by rare earths’ local moment, the temperature dependent single ion anisotropy as well as the long range, indirect interactions (Ruderman-Kittel-Kasuya-Yosida (RKKY) type) between local moments via conduction electronsbook (). The competition between Fermi surface nesting (maxima in the generalized magnetic susceptibility)islam () and local moment anisotropy can lead to either incommensurate or commensurate magnetic propagation vectors, or sometimes multiple transitions from one to the other on cooling. Although detailed anisotropic studies of the RNiGe and RFeGe series have been madeRNi (); RFe (), studies of RCoGe compounds and their magnetic properties have primarily been done on polycrystalline samples with magnetic ordering temperature determined only down to 4.2 Kmccall1 (); mccall2 (); Pinto (). So far, only members with R = CeCefujii (); Cepaul (), PrPrvej (), NdCefujii (), EuEuHossain (); EuDio (), GdGdGood () and TbTbshigeoka1 (); Tbshigeoka (); Tbwiener () had been studied in single crystal form. The systematic growth and study of single crystals can address the issue of anisotropy and possible metamagnetic transitions in this series of compounds. It also allows for comparison to the aforementioned RNiGe and RFeGe series.
According to published literature, CeCoGe does not undergo any magnetic transitions and is reported to exhibit Kondo screening of the 4f moment. No consensus was reached on Ce’s valence stateCefujii (); Cepaul (); Cex (); takashi (). Neutron diffraction work on PrCoGe indicates a magnetic ordering at 28 K with a sinusoidally modulated incommensurate magnetic structure along c-axisPr (); PrHo (). In addition, at 2 K, well below its ordering temperature, two metamagnetic transitions were observed at 20 kOe and 100 kOePrvej (); Prvin (). NdCoGe has been reported to order antiferromagnetically at around 30 K and undergo a transition between different magnetic structures at 10 KCefujii (); NdEr (); Ndcp (); Ndandre (). Two metamagnetic transitions were observed at 30 kOe and 110 kOePrvin (). Temperature-dependent susceptibility and specific heat were measured on polycrystalline SmCoGeSm (), which indicate a magnetic transition at around 14 K. Single crystals of EuCoGe were synthesized using self flux method and characterized by transport measurements. A paramagnetic to antiferromagnetic transition temperature was determined to be 23 K and metamagnetic transition was observed at 2 KEuHossain (). Upon applying pressure above 3 GPa, Eu exhibit a continuous valence change from a high-temperature divalent state to a low-temperature trivalent stateEuDio (). GdCoGe is reported to order at around 40 Kmccall2 (); Gdnew (). A magnetic x-ray scattering studyGdGood () revealed that this compound orders antiferromagnetically with a temperature-dependent incommensurate wave vector associated with the Gd moments that primarily lie in the ab plane. Single crystals of TbCoGe, grown by tri-arc Czochralski method, showed successive metamagnetic transitions at low temperature with commensurate magnetic structure at low applied field and different incommensurate structures at higher fieldsTbshigeoka1 (); Tbshigeoka (). A neutron diffraction study on TbCoGe revealed an incommensurate to commensurate magnetic transition upon coolingTbneu (); Tbbuschow (); TbHo (). In both cases, the magnetic moments are parallel to the c-axis. Neutron studies on polycrystalline HoCoGePrHo (); TbHo () showed that it orders at 8 K with a ferromagnetic coupling within the plane and an antiferromagnetic coupling between planes. Another study on polycrystalline HoCoGe and DyCoGe claimed that they both experience an incommensurate to commensurate phase transition with Ho moments lying along c-axis while Dy moments deviate from c-axis in a temperature-dependent mannerDyHo (). Polycrystalline ErCoGe was reported to order antiferromagnetically at 4.2 K with Er moments perpendicular to the c-axisNdEr (); Ercp (). Polycrystalline TmCoGe was characterized to be ordering at 2.4 KTmGondek ().
In the present work, a systematic study of magnetic and electric properties of RCoGe single crystals, all grown out of high-temperature solutions rich in Ge and Co, is presented for R = Y, La-Nd, Sm-Tm. In addition, specific heat measurements provide further information about transition temperatures as well as qualitative insight into the low temperature degeneracy of the ground state. In this way, all of the studied members of the RCoGe series can be systematically compared and contrasted, having been grown and studied under the same conditions. After describing the experimental techniques used in crystal growth and characterization, experimental results will be presented starting with the non-moment-bearing R = Y and La members, combined, and then separately for the each of the other members. After the results section, discussions of trends along the series such as ordering temperature, Curie-Weiss temperature and also on CEF effect will be presented and followed by a brief conclusion.
Single crystals of RCoGe were grown using a self flux solution growth methodCanfield92 (); Canfield01 (); Canfieldeuro () where CoGe was used as the flux. Typical initial molar ratios of the three elements were R:Co:Ge = 6:47:47 or 8:46:46. The starting elements were added to a 2 ml alumina crucible and sealed in a quartz ampoule under a partial argon atmosphere. The ampoule was then heated up to 1250C and slowly cooled down to around 1100C, at which temperature the excess molten flux was decanted. Given that growth temperatures exceed 1200C, the pressure of the argon in the ampoule was adjusted so as to be as close to atmospheric pressure at 1250C as possible so as to mitigate problems associated with the softening of the silica. All crystals were plate-like with the c-axis perpendicular to the plate surface. Despite multiple attempts, crystals of R = Yb and Lu could not be grown.
The crystal structure was studied at room-temperature using a Rigaku Miniflex powder x-ray diffractometer (Cu K radiation). Samples were prepared by grinding single crystals into powders, which were then mounted and measured on a single crystal Si, zero-background, sample holder. A typical x-ray pattern is shown in Fig. 1 for GdCoGe. All major peaks are consistent with the RCoGe tetragonal structure; a minor amount of residual flux gives rise to small peaks associated with Co-Ge binary phases, which are indicated by arrows. Lattice parameters were inferred using GSAS softwareGSAS (); GUI (). Unit cell parameters are summarized in Table. 1, in which the uncertainty is about 0.2% for refined lattice parameters.
DC magnetization measurements were performed in a Quantum Design Magnetic Property Measurement System (MPMS), superconducting quantum interference device (SQUID) magnetometer (T = 1.8 - 350 K, H = 70 kOe). All samples were manually aligned to measure the magnetization along the desired axis.
Resistivity measurements were performed using a standard 4-probe, AC technique in a Quantum Design Physical Property Measurement System (PPMS) instrument (f = 17 Hz, I = 1 or 3 mA). For these measurements, samples were cut and polished into rectangular cuboid bars with approximate dimensions of 1.2 0.8 0.3 mm. Epotek-H20E silver epoxy was used to create contacts on all samples and Pt wires were placed such that the current was applied in the ab plane. Uncertainty in absolute resistivity due to the measurement of dimension and sample variation is about 20%.
Heat capacity was measured using the heat capacity option of a Quantum Design PPMS by using the relaxation method in the temperature range of 1.8 - 50 K. In the case of CeCoGe, a He cooling option was used for measurement down to 0.4 K.
Magnetic transition temperatures are inferred from the maximum of zero-field specific heat, d/dTfisherr () and d/dTfisherxt (), where is the polycrystalline averaged magnetic susceptibility calculated from the equation: = ( + 2)/3. Calculated is also used in obtaining the effective moment of magnetic rare earth ions in their high temperature paramagnetic state. For CeCoGe, PrCoGe, NdCoGe and SmCoGe, the polycrystalline magnetization of LaCoGe is subtracted from their polycrystalline magnetization in order to get a more accurate estimate of effective moment, because the temperature-independent magnetization is non-negligible compared with local moment contribution. For the rest of the members in RCoGe, given that their effective moments increase substantially, the influence of the temperature-independent magnetization is negligible and therefore ignored. Resistivity data was averaged between 3 neighbouring points before taking derivative to achieve better signal-to-noise ratio. The uncertainty in our determinations of the transition temperature was determined by the step width for the specific heat measurement and half width at half maximum for d/dT and d/dT. The error bars due to mass uncertainty and different ranges of linear fit is about 2% for effective moment and 15% for Curie-Weiss temperature, .
3.1 YCoGe, LaCoGe
YCoGe and LaCoGe bear no local moments due to the empty 4f-shells of Y and La. They manifest essentially temperature-independent magnetic susceptibility data, a combination of Pauli-like paramagnetic as well as Landau and core diamagnetic contributions, as shown in Fig. 2. The susceptibility of YCoGe, above 50 K, stays relatively constant with . The upturns at low temperature can be attributed to very small amount of paramagnetic impurities, most likely one of the rare earth ions with axial anisotropy (e.g. YTbCoGe with x 0.0001 would have a similar sized low-temperature Curie tail). For LaCoGe, although the upturn at low temperature is smaller than that in YCoGe, the magnetization does slowly increase with temperature. Compared with its low temperature value, at 300K, the magnetization has increased by nearly 30. In addition, the magnetic anisotropy for LaCoGe is smaller than that of YCoGe and of opposite sign with . The magnetic anisotropy in these two compounds, as well as the weak temperature-dependence of the magnetization is probably due to details of their band structure and Fermi surfaces, which affect the Pauli and Landau contributions to the total magnetization. Magnetic isotherms measured on YCoGe and LaCoGe at 1.85 K are approximately linear for both H and H. Slight curvature is consistent with small amounts of paramagnetic impurities.
The zero-field resistivity of YCoGe and LaCoGe show typical, metallic behavior, without any anomaly observed down to 1.8 K. The residual resistance ratios (RRR ) for YCoGe and LaCoGe are 2.7 and 5.0 respectively.
The temperature-dependent specific heat C data are similar for these two compounds. The estimated Debye temperatures are about 400 K for YCoGe and 370 K for LaCoGe. The relative value of two Debye temperatures roughly follows what would be predicted by Debye model with the different molecular masses associated with the change from Y to La. The linear coefficients of specific heat, , extracted from the plot of C/T versus T, are 10.4 mJ/mol K for YCoGe and 14.6 mJ/mol K for LaCoGe. In calculating the magnetic entropies of RCoGe magnetic members, although YCoGe and LaCoGe can provide an estimation of the non-magnetic specific heat, at a quantitative level, for this series, they do not allow for a detailed calculation, as the magnetic entropy of GdCoGe does not reach expected Rln8 upon ordering, indicating that this approximation is not ideal for this system. At a qualitative level, however, it is still interesting to get a sense of how CEF splitting reduces the free ion’s degeneracy for the members that manifest clear magnetic anisotropy. The specific heat of LaCoGe was used to approximate the non-magnetic contribution across the series.
Fig. 3 summarizes the thermodynamic and transport measurement results for CeCoGe. Temperature-dependent magnetization of CeCoGe measured at 1 kOe is anisotropic with . The inverse magnetic susceptibility shows a broad minimum at around 100 K, a maximum near 40 K and a lower temperature drop that is likely associated with an impurity tail, which is similar to earlier workCefujii (). Although the weak variation of magnetic susceptibility was explained by the Ce ion being in an intermediate valence stateCefujii (), given that the overall signal of magnetic susceptibility is small, evaluating the effective moment without taking the non-local-moment contribution into account may not be valid. The polycrystalline averaged susceptibility of LaCoGe was subtracted from that of CeCoGe in order to estimate the effective moment of Ce, as shown in the gray curve in Fig. 3(a). A value of 2.6 is inferred above 200 K, which is close to the theoretical value of Ce (2.5 ). Therefore, at high temperatures Ce is probably close to being in its trivalent state in CeCoGe. This interpretation is consistent with a near-edge x-ray absorption studyCex (). In H/M(T), there seems to exist a small kink at around 15 K. However, as it is not a typical feature for magnetic ordering and no clear feature was observed in other measurements, it is not clear at this stage what physical meaning it has.
The zero-field resistivity of CeCoGe shows little change for 100 - 300 K. A broad shoulder is observed at 100 K and is followed by a much stronger drop at lower temperatures. The RRR for CeCoGe is 3.6. At low temperature, its resistivity is proportional to T as shown in the inset of Fig. 3(b) with a slope A = 0.045 cm/K. Magnetic resistivity ( = - ) shows a broad maximum centered around 100 K.
The zero-field specific heat data measured down to 0.4 K is shown in Fig. 3(c). In the low temperature region, there is an anomaly in the C versus plot at around 2.3 K, which was not observed in previous He measurementstakashi (). However, no similar feature was observed in either resistivity or in magnetic susceptibility data. It may be because, at such a low temperature, neither resistivity nor magnetization measurements had high enough resolution to resolve the signatures associated with the feature seen in the specific heat. This feature may indicate some interesting physics that we do not yet understand and ultimately may merit further investigation. It is worth noting here that in the C versus T data, the feature was clearly seen albeit at the end of the measurement range (Fig. 3(c)).
The electronic specific heat, , of CeCoGe is 90-103 mJ/mol K in the range of 5-10 K, which is much larger than that of YCoGe and LaCoGe (see two estimates as red lines in Fig. 3(c)). This is consistent with a low temperature, Kondo screened state. In the perspective of entropy removal, the Kondo temperature T can be roughly estimated by T = R ln(N)/, where N is the degeneracy of the CEF split ground state being Kondo screened, and R is the ideal gas constant. T estimated in this way is about 60 K if N = 2 is used and 120 K if N = 4 is used, which, qualitatively, are consistent with the maximum observed in magnetic resistivity. The choice of degeneracy agrees with generalized Kadowaki-Woods relationkw (), in which CeCoGe lies in between N = 2 and N = 4. Numerical solution of Coqblin-Schrieffer modelRajan () can also be applied to fit magnetic susceptibility data of CeCoGe, yet it gives a much higher Kondo temperature (T 240 K). The discrepancy in T may come from a poor non-magnetic background subtraction.
The field-dependent magnetization measured at 1.85 K is anisotropic and increases linearly with field up to 70 kOe. Magnetoresistance measured at 1.8 K with Hc is weak, negative and appears to be non-linear in applied field.
The magnetic susceptibility of PrCoGe in Fig. 4(a) is also anisotropic with . A single transition is seen in the M/H(T) data at around 27 K. Since the magnetization is still increasing with decreasing temperature at the lowest temperature we could reach, the ordered state of PrCoGe may have a net ferromagnetic component and/or PrCoGe may have further, T 1.8 K, transitions as well. At high temperatures, Curie-Weiss behavior is clear with = -180 K, = -38 K and = -23 K. The effective moment obtained from its polycrystalline average in the paramagnetic state is 3.5 if the temperature-independent contribution represented by LaCoGe is subtracted, which is close to the theoretical prediction for free Pr ion (3.6 ). (Note: These values are compiled for all measured materials in Table 2 below)
The temperature-dependent, zero-field resistivity data (Fig. 4(b)) show a clear loss of spin-disorder scattering feature associated with the transition temperature obtained from magnetic susceptibility measurements. The RRR is 4.5.
In Fig. 4(c), the plots of d/dT as well as d/dT are shown in arbitrary units together with zero-field specific heat data. Features associated with an antiferromagnetic phase transition are consistent in all three measurements with the transition temperature inferred as 26.7 0.9 K. The specific heat data also reveal that there exists a broad shoulder around 8 K, which had been reported in an earlier studyPrvej (). This C(T) shoulder occurs at the same temperature range as the low-temperature upturn in the magnetic susceptibility and is probably associated with changes in the magnetic excitation spectrum. Estimated magnetic entropy indicates that the ordering moment comes from a pseudo-doublet ground state.
In Fig. 4(d), the magnetization isotherm measured at T = 1.85 K increases linearly when H(ab). For Hc, metamagnetic transitions were observed with magnetization showing step-like behavior with two well defined plateaus at 0.2 and 0.8 . This is consistent with observed metamagnetic transition at 20 kOePrvej (). Although we didn’t observe a clear magnetic hysteresis at 1.85 K, the first plateau at 0.2 probably represents a small ferromagnetic component in the intrinsic ordered state given the sharp increase of magnetization before the plateau and the linearity of magnetoresistance within the field range. Another metamagnetic transition at around 100 kOe was also reportedPrvej (), above which Pr is fully saturated. Magnetoresistance measured at 1.8 K with Hc shows consistent changes at the same critical fields, which was not well resolved in the above mentioned work.Prvej ()
The temperature-dependent magnetization of NdCoGe (Fig. 5(a)) is anisotropic with . There are two low temperature features in the M/H(T) data: a sharp feature, with a transition temperature at around 28 K and a broad feature near 9 K. Under higher applied fields, the two maxima were reported to gradually shift to lower temperatures with the second magnetic transition being almost smoothed out above 50 kOeCefujii (). A high temperature, Curie-Weiss fit to the polycrystalline averaged data suggests the effective moment to be 3.6 , which is the same as expected for Nd (3.6 ). The paramagnetic Curie-Weiss temperatures are = -50 K, = 11 K and = -19 K.
Fig. 5(b) shows the zero-field resistivity data of NdCoGe with RRR = 3.9. Only one transition was observed, which is close to the ordering temperature obtained above. A rather broad and smeared shoulder may correspond to a second magnetic transition. However, the feature in d/dT is too broad to offer any quantitative information.
The specific heat measurement also shows only one signature of phase transition, which confirms the above obtained ordering temperature. This is in agreement with reported specific heat measurementNdcp (). The transition temperature associated with the clear high-temperature feature is 27.9 0.9 K. Estimated magnetic entropy indicates that there is Rln4 entropy removed below the magnetic ordering temperature.
There have been discussions on the nature of the feature observed in temperature-dependent magnetization data at around 9 KCefujii (); NdEr (); Ndcp (); Ndandre (). It was speculated that the feature only emerges under certain finite applied fields. However, at 10 Oe, both the temperature and the relative size of two maxima in M/H(T) remain unchanged (not shown here). This feature perhaps originates from a change in magnon spectrum due to thermal depopulation of split CEF levels. If there really is a magnetic transition, then, in the perspective of specific heat measurement, the absence of a clear signature indicates that it is a transition that does not involve any significant amount of magnetic entropy.
The magnetization isotherms measured at 1.85 K (Fig. 5(d)) are anisotropic. When H(ab), the magnetization increases linearly with applied field whereas when Hc, a metamagnetic transition at around 17 kOe was observed and followed by a plateau at above 30 kOe. This is consistent with an early polycrystalline studyNdEr (). But in this case, the transition is much sharper with a better defined critical field. Another metamagnetic transition at about 110 kOe was reported for polycrystalline sample, above which the magnetization is approaching that of Nd’s saturated valuePrvin (). Magnetoresistance measured at 1.8 K with magnetic field parallel to c-axis shows a local maximum around the same critical field where metamagnetic transition was observed. After this, the resistivity increases linearly with applied field above 50 kOe.
As shown in Fig. 6(a), the temperature-dependent magnetization of SmCoGe is quite different from previous members. It is anisotropic but its anisotropy changes at around 75 K, below which . In addition, its inverse magnetic susceptibility does not follow Curie-Weiss behavior up to 300 K, but instead, shows a wide negative curvature and tends to saturate at room temperature. This behavior is commonly seen in Sm based compoundsRNi (); RSb2 (); RAgSb2 () and could come from thermal-population of Sm’s Hund’s rule excited states or a fluctuation of Sm’s valent state. A clear feature of an antiferromagnetic transition can be seen at around 17 K.
The temperature-dependent resistivity is showed in Fig. 6(b) with RRR = 4.3. A well pronounced signature of the loss of spin disorder scattering can be seen at the transition temperature.
The zero-field, temperature-dependent specific heat does not exhibit a typical shape, with a broad curvature sitting approximately 1 K below the transition temperature inferred at 16.5 0.2 K. The consistency of peak shape in C(T), d/dT and d/dT near the transition temperature may also be an indication of a cascade of closely spaced transitions that can not be well resolved by the present measurements. It is also possible that a specific type of incommensurate magnetic ordering structure leads to this broadened featureBlanco (). Magnetic entropy suggests that the ordered state evolves out of a CEF split, doublet state.
The magnetization isotherms (Fig. 6(d)) are linear with applied field up to 70 kOe with H(ab) yielding a slightly larger slope. The magnetoresistance also increases as applied field increases in a quadratic manner. No clear feature associated with a metamagnetic transition was observed.
Fig. 7 presents the measured data on EuCoGe. The temperature-dependent magnetization of EuCoGe is essentially isotropic above 50 K. In its high temperature paramagnetic state, a linear fit on inverse magnetic susceptibility gives = 10 K and = 7.7 , which suggests that Eu is in a divalent state. This is consistent with the anomalously large unit cell volume of EuCoGe shown in Table. 1 and Fig. 14 below. On the one hand, a positive Curie-Weiss temperature seems to indicate a ferromagnetic exchange interaction between Eu ions. On the other hand, a single transition temperature at 22.2 0.3 K was inferred from d, and the transition appears to be antiferromagnetic with the ordered moments being perpendicular to the crystallographic c-axis, given essentially temperature-independent below T for .
In Fig. 7(b), the zero-field resistivity with RRR = 4.5 also indicates a single transition at around 22 K. A clear decrease in the resistivity can be seen at the transition temperature. The zero-field temperature-dependent specific heat data, shown in Fig. 7(c), yield a consistent transition temperature. Combining three different measurements, the magnetic transition temperature of EuCoGe is 22.1 0.4 K. In a recent study on Eu-based intermetallic compound, EuNiGeJohnston (), a similar concomitance of a positive Curie-Weiss temperature and antiferromagnetic transition was observed and explained by a collinear A-type antiferromagnetic structure. Similarly, in the current case, given the anisotropy below T, it is possible that there exist a ferromagnetic interaction along c and an antiferromagnetic interaction within the ab plane, namely C-type antiferromagnetic structure. It will be interesting to study the magnetic structure of EuCoGe via magnetic x-ray scattering, since both Eu and Gd have similar ordered moment directions and yet different signs of (Data for GdCoGe will be shown in the next section). As zero CEF splitting for Eu Hund’s rule ground state multiplets would predict, the magnetic entropy calculated for this compound reaches Rln8 at the ordering temperature.
The magnetization isotherms of EuCoGe at T = 1.85 K are anisotropic. When Hc, the magnetization increases linearly with applied field. For H(ab), below 20 kOe, the magnetization increases linearly with applied field with a slightly smaller slope compare with that in Hc. At around 20 kOe, the magnetization in ab plane suddenly increases, after which it shows a weak negative curvature, similar to the earlier reported featuresEuHossain (). Magnetoresistance also increases at around 20 kOe and manifests a local maximum at around 25 kOe. It then decreases as applied field increases. At 80 kOe, the magnetoresistance manifests another sharp change in slope, which may indicate another metamagnetic transition. Further study on magnetization at higher field may help to clarify this point.
The temperature-dependent magnetization of GdCoGe, shown in Fig. 8(a), resembles that of EuCoGe. It is also isotropic as expected for a Hund’s rule ground state multiplet J with zero angular momentum. A high temperature Curie-Weiss fit on polycrystalline averaged H/M gives a negative = -32 K, which is consistent with simple antiferromagnetic ordering. The effective moment inferred is 8.1 , close to the the theoretical value of 7.9 /Gd. Only one transition at about 33 K was observed. The anisotropy on below T, as well as the magnetic x-ray scattering resultsGdGood () indicate that the ordered moments are in the basal, ab plane.
In Fig. 8(b), the temperature-dependent resistivity also shows a clear loss of spin-disorder scattering at the transition temperature. The RRR is 4.9.
The zero-field specific heat of GdCoGe (Fig. 8(c)) shows a clear signature of transition. Summarizing the data from (T), M/H(T) and C(T), the magnetic transition temperature of GdCoGe is 31.7 1.5 K, 33.2 1.8 K, 33.1 0.2 K respectively resulting in an average value of 32.6 2.4 K, which is smaller compared to earlier reports on polycrystalline materials: 37.5 KGdnew () and 40 Kmccall2 (), but fully consistent with the single crystal work reportedGdGood (). In addition, as can be seen in the magnetic specific heat of GdCoGe as well as in EuCoGe, there is a hump showing up at around 25 of their ordering temperatures. In studies of specific heat of Gd based compoundsBlanco (); Bouvier (), this phenomenon was observed to be common and was explained to arise naturally from mean field calculation for a (2J+1)-fold degenerate multiplets. Although the study was specifically focusing on Gd, it is not surprising that the specific heat of EuCoGe can be explained in the same way, as Eu is in its divalent state.
At 1.85 K, the field-dependent magnetization is similar to that of EuCoGe. When Hc, the magnetization is roughly linear in H whereas when H(ab), a metamagnetic transition occurs around 52 kOe. Although ab plane is not a well defined direction, 52 kOe, the field value found for GdCoGe, is more than double the value of 20 kOe found for EuCoGe. Although simple geometric arguments could give a factor of in critical field associated with in-plane orientation, so a factor of 2.5 makes the transition field in GdCoGe unambiguously higher than that in EuCoGe. Magnetoresistence measured at 1.8 K suddenly decreases at the critical field of the metamagnetic transition and increases both before and after the transition with different rates.
The temperature-dependent magnetization of TbCoGe is strongly anisotropic with (Fig. 9(a)). The sign of Curie-Weiss temperatures varies with the orientation: = -160 K, = 37 K and = -33 K. The value of effective moment is 9.9 , which is close to the theoretical value of Tb (9.7 ). Multiple transitions were observed, including two successive transitions at around 33 K and 29 K and a low temperature transition at 2.3 K. The ordering temperature is comparable with that of GdCoGe, which contradicts the prediction of simple de Gennes scaling. This will be expanded upon later, in the discussion section.
A clear loss of spin-disorder scattering can be seen in the zero-field resistivity measurement as shown in Fig. 9(b). RRR is 3.0 for this compound. The two higher temperature transitions seen in the magnetic susceptibility measurement are also clearly visible in the resistivity data, whereas no anomaly was observed at around 2.3 K.
The zero-field specific heat measurement is shown in Fig. 9(c) and its insets. There are four transitions at 33.3 K, 29.7 K, 28.8 K and 2.4 K. Two transitions show up in the temperature range around the second transition observed in M/H(T) data. It is possible that our magnetic susceptibility measurement simply does not resolve those two closely spaced transitions. An alternative scenario could be that those two transitions actually merge under a small finite applied field. To test this assumption, a temperature-dependent magnetization was measured at 200 Oe (not shown here). Even at this low field, no splitting of the transition is seen around the temperature range of interest. In Table. 2, the transition temperature inferred from C(T) will be used for the two middle neighbouring transitions. The magnetic phase diagram constructed for TbCoGe by Shigeoka et alTbshigeoka1 (); Tbshigeoka () indicates that, in zero applied field, there is only one magnetic phase below T. However, in the present study, up to 4 different phases are found above 1.8 K without applied field. The estimated magnetic entropy reached Rln2 at the ordering temperature.
The magnetization isotherms measured at 1.85 K show a metamagnetic transition with a step-like behavior when Hc. A plateau at about 4.5 /Tb was reached after the transition. In-plane field-dependent magnetization increases linearly with applied field. Magnetoresistance shows one more metamagnetic transition at around 80 kOe. Both metamagnetic transition fields are consistent with previously reported workTbshigeoka1 (); Tbshigeoka (); TbDy (). Another reported metamagnetic transition at 69 kOeTbshigeoka1 (); Tbshigeoka () was not clearly observed in our measurement, although the broad decrease in magnetoresistance above 70 kOe may actually reflect two metamagnetic transitions as reported.
The temperature-dependent magnetization of DyCoGe (Fig. 10(a)) is similar to that of TbCoGe. Two transitions at about 16 K and 14 K were observed. Curie-Weiss temperatures inferred in its paramagnetic state are = -80 K, = 28 K and = -16 K. The effective moment is 10.4 , which is close to the theoretical value for Dy (10.6 ).
The temperature-dependent, zero-field resistivity of DyCoGe has a RRR of 2.7. Two clear features can be seen in the inset of Fig. 10(b). Around the transition temperatures obtained above, there are very clear changes in slope.
The temperature-dependent specific heat of DyCoGe also shows two transitions. Together with the values obtained above, magnetic transition temperatures for DyCoGe are 16.0 0.7 K and 14.4 0.4 K (Fig. 10(c)). The estimated magnetic entropy at the ordering temperature is close to Rln4.
Clear features were observed in the magnetic isotherms measured at 1.85 K as shown in Fig. 10(d). For H(ab), a negative curvature was observed. For Hc, which is the easy axis, the magnetization shows sudden jumps between different, well-defined, plateaus at around 25 kOe and 40 kOe. Although it tends to saturate after about 50 kOe, the magnetization is still smaller than the expected value for saturated Dy (10.0 ). It is possible that the saturated moment is reduced due to CEF effectDyHo () or that there is another metamagnetic transition at fields higher than 90 kOe. An alternative explanation may be related to the deviation of local moments from c-axis at low temperature as reported by a neutron studyDyHo (). However, it is not obvious that the reported deviation would still exist under applied fields of up to 70 kOe. Magnetoresistance with Hc shows highly non-monotonic behavior that is consistent with magnetization isotherm data. First, it increases rapidly at the first critical field observed in magnetization isotherm measurement and then decreases even more sharply at the second transition field. Finally, the resistivity stays constant at higher fields. Metamagnetic transition critical fields in the present work are close to those reported in a previous study on polycrystalline samples, although the features found here are much sharperTbDy ().
Measurements made on HoCoGe are summarized in Fig. 11. It has a smaller magnetic anisotropy than TbCoGe or DyCoGe, yet still holds. Linear fits of the inverse susceptibilities gives: = -21 K, = 13 K and = -6.4 K. The effective moment is 10.6 , which is the same as the expected value of 10.6 for Ho ion. A single transition at 7.8 K was observed.
The temperature-dependent resistivity (Fig. 11(b)) decreases in the vicinity of the transition temperature, which is consistent with magnetic susceptibility measurement. The RRR is 2.3.
There are two features in zero-field specific heat measurement (Fig. 11(c)). The first one at 8.4 K is manifested by a change of slope and the second one, at 7.9 K, is associated with the local maximum in . The fact that there exists two closely spaced transitions is consistent with an early neutron studyDyHo (), albeit the exact transition temperatures are different. As these two transitions are very close in temperature, they are not clearly discernible in the derivatives of temperature-dependent magnetization and resistivity. In Table. 2, the ordering temperature is inferred from specific heat measurement. The magnetic entropy suggests that there may be a pseudo-triplet ground state below the ordering temperature.
Magnetization isotherms measured at 1.85 K are shown in Fig. 11(d). Comparing these data with those of DyCoGe, in HoCoGe, for Hc, the middle plateau is much narrower and for H(ab), the magnetization shows a positive curvature instead of the negative curvature found for DyCoGe. The metamagnetic transition fields for HoCoGe are also different: 15 kOe and 23 kOe. Similar to the case in DyCoGe, the saturated magnetization of HoCoGe is lower than the free ion value for Ho. Neutron studiesPrHo (); DyHo () suggest that the size of the Ho moment is probably reduced at low temperature. Therefore, according to the present measurement, the reduced saturation moment for Ho at 1.85 K is 8.9 /Ho. The magnetoresistance is cusp-like at both metamagnetic transitions and it stays fundamentally unchanged for applied fields along the c-axis above 30 kOe.
As shown in Fig. 12(a), in comparison to the previous local-moment-bearing rare earth members, the magnetic anisotropy is reversed in ErCoGe with . A high temperature linear fit on H/M(T) gives = 14 K, = -69 K and = -2.5 K. The effective magnetic moment yields 9.5 , which is close to the theoretical value for trivalent Er (9.6 ). Transition temperature inferred from d/dT is 4.2 0.6 K.
The temperature-dependent resistivity has a RRR of 1.9. It shows a weak, relatively smeared feature of the loss of spin-disorder scattering feature around the transition temperature. Nevertheless, in the plot of d/dT (Fig. 12(c)), the broad peak with a low signal-to-noise ratio makes it difficult to extract a clear signature of the transition temperature.
The low temperature specific heat data exhibit a well-defined shape, from which the transition temperature can be inferred to be 4.5 0.1 K. Estimated magnetic entropy indicates a doublet below the ordering temperature, which is in agreement with an earlier studyErcp ().
In magnetization isotherm measurements, for Hc, the magnetization increases linearly with applied field. When H(ab), the magnetization tends to saturate above 60 kOe with a moment size being around 8 /Er, which is smaller than its saturated value. In the lower field region, at around 9 kOe, the break in the slope of the in-plane magnetization increase seems to suggest a metamagnetic transition. This field corresponds to the observed change in slope of the magnetoresistance data. When conducting the experiment, special care was taken to ensure the direction of applied field is the same in magnetization isotherm and magnetoresistance measurement for the case of H(ab). In this way, the effect of possible magnetic in-plane anisotropy is avoided.
The temperature-dependent magnetic susceptibility of TmCoGe manifests an even larger planar anisotropy than in the case of ErCoGe (Fig. 13(a)). Just above T, , which indicates an extreme planar anisotropy. A low ordering temperature of 2.2 K can be clearly seen. The effective moment calculated from a linear fit on high temperature polycrystalline inverse susceptibility yields 7.4 , close to the theoretical value for Tm (7.6 ). The Curie-Weiss temperatures are: = 26 K, = -220 K and = -2.3 K. Features observed here are consistent with antiferromagnetic ordering demonstrated by a recent neutron scattering workTmGondek (). However, their claim of Tm moments being parallel to c-axis is clearly ruled out by our observations. It worth pointing out that their neutron diffraction patternTmGondek () actually demonstrated that the Tm magnetic moments have at least a significant perpendicular component to the c-axis with a well defined (001) Bragg peak emerging below the ordering temperature.
Fig. 13(b) shows the temperature-dependent resistivity data of TmCoGe. Its derivative (shown in Fig. 13(c)), similar to that of ErCoGe, does not allow for an accurate determination of transition temperature. In Table 2, the transition temperatures of ErCoGe and TmCoGe are based on C(T) and M/H(T) measurements.
The zero-field specific heat shows a salient feature with transition temperature inferred to be 2.2 0.1 K. Estimated magnetic entropy mostly comes from linearly extrapolated value in specific heat below 1.8 K, and the ground state may be a doublet.
Fig. 13(d) shows the magnetization isotherms of TmCoGe measured at 1.85 K. For Hc, the magnetization increases close to linearly with applied field below and above 20 kOe with slightly different slopes. For H(ab) there is a feature below 20 kOe that is most likely a metamagnetic transition, which is very broad due to T being only slightly above the measurement temperature. Magnetoresistance, which was carefully measured at 1.8 K with the external field applied in the same direction as the in-plane M(H) measurement, although noisy, shows a very broad positive curvature. The magnetic field where magnetoresistance starts to increase coincides approximately with the critical field of the metamagnetic transition, observed in c-direction. As mentioned above, the temperature of measurement is very close to the magnetic ordering temperature, possible metamagnetic transitions may be smeared by thermal excitation.
In the RCoGe series, YCoGe and LaCoGe exhibit roughly temperature-independent magnetic susceptibility as expected for metals without local moment and magnetic ordering. The slight anisotropy of their Pauli/Landau-based magnetic susceptibility can be explained by the anisotropy in their Fermi surface. Since the electron count should be the same for these two members, the reversal of magnetic anisotropy is probably due to the difference in lattice parameter, which can end up changing the Fermi surface geometry. The electronic heat capacity for each is about 2-3 mJ/(mol-atomic) K, which is common for metals.
From the perspective of structure, lanthanide contraction is expected when substituting one rare-earth ion for another in an isostructural series of compounds. Lattice parameters refined from powder x-ray diffraction are shown in Table 1 and unit cell volumes are shown in Fig. 14. There is a monotonic, almost linear contraction of unit cell volume with increasing atomic number across the trivalent lanthanides. EuCoGe exhibits a clear deviation from this trend, which is consistent with Eu being divalent instead of trivalent. As is often the case, unit cell volume of YCoGe is close to those of DyCoGe and HoCoGe.
|Compound||a (Å)||c (Å)||Volume (Å)|
In discussing magnetic properties, within the mean field theory, both polycrystalline Curie-Weiss temperatures and magnetic ordering temperatures are predicted to be proportional to the de Gennes factor dG (dG = (g-1)J(J+1)) if the effects of CEF splitting of the Hund’s rule ground state multiplet, J, are ignoredbook (). In practice, this proportionality is best seen for the heavy rare earth members (Gd-Tm). Fig. 15 shows the obtained ordering temperature, T, and polycrystalline Curie-Weiss temperature, , plotted against the dG factor. The ordering temperatures of heavy rare-earth members (Gd-Tm) do not follow the dG scaling. In particular, the ordering temperature of Tb is higher than, or at best comparable to, that of Gd, if experimental uncertainties are included. In the plot of the Curie-Weiss temperature, Tb also deviates from the predicted trend. An early study on polycrystalsmccall2 () did show a rough de Gennes scaling in T for members from Gd-Ho. The ordering temperatures inferred are close to those in the present study, except for GdCoGe, which is much higher. Yet, in their study, they also reported a higher magnitude of Curie-Weiss temperature for Tb than Gd. A similar breakdown of de Gennes scaling had been investigated in the series of RRhB compoundsNoakes (); Dunlap (). In that case, the peak of ordering temperatures in the de Gennes plot occurs at Dy instead of Gd. Theory had shown that with the CEF effect being taken into account, the ordering temperature can be enhanced to different extents according to the rare earth ion’s total angular momentum. When a strong easy c-axis anisotropy is present, Tb may become the new maximum in ordering temperatures. The deviation of from de Gennes scaling can be associated with the CEF effect as well. A breakdown of de Gennes scaling in a recent study on RNiBixiao () was also observed. However, it is still unclear why this breakdown is not a general observation for other rare earth intermetallic series with the same point symmetry and comparable single ion anisotropiesRNi (); RFe ().
|R||(K)||(K)||(K)||()||T (K)||T (K)||T (K)||T (K)||B (K)|
*: There also exists a feature at 8.6(2.9) K that may be associated with magnetic transition.
Except for Eu and Gd, all local moment bearing rare earth members in RCoGe exhibit magnetic anisotropy in their high temperature paramagnetic state. The CEF effect is identified as the leading reason for this anisotropy. Knowing that the rare earth ions in RCoGe possess a tetragonal point symmetry, if x, y and z-axis are chosen along conventional a, b and c-axis of the tetragonal structure, the CEF Hamiltonian can be expressed as followsCEFtet ():
where are the crystal field parameters and O are the Stevens operator equivalents. A are constants that reflect the strength of the CEF originating from the ions surrounding the central R ion. Although A may change slightly when progressing across the rare-earth series, due to lanthanide contraction, generally, it can be viewed as a constant for different rare-earth elements, as it will not affect the trend significantly. r is the expectation value of r for 4f electrons. are multiplicative factors which only need to be calculated once: ; and . Previous studieswang (); Boutron () showed that in a tetragonal symmetry, BO is the leading term characterizing crystal electric potential energy and consequently the anisotropic magnetic behavior. Experimentally, B can be determined from the high temperature anisotropic paramagnetic Curie-Weiss temperatureswang () by:
where J is the total angular momentum of Hund’s rule ground state for the specific rare-earth ion under study. This equation provides a way to determine B from the data listed in Table 2. The sign of B reflects whether the compound has an easy-axis or easy-plane anisotropy. In addition, as described before, B can also be theoretically calculated through:
If A is viewed as a constant, B can be calculated by adopting theoretical values of r Freeman ()and Hutchings (). As r is definite a positive number and is theoretically calculated, the easy magnetization direction still depends on the sign of , which can lead to different anisotropic propertiesRNi (); RFe (); RAgSb2 (); TbC (). Fig. 16 shows normalized experimental and theoretical values of B. Normalization was done to ensure both theoretical and experimental value of B for Tb are -1, which can help to factor out the influence of A not being taken into consideration. Fig. 16 plots the values inferred from our anisotropic values using Eqn.(2) as well as those calculated using Eqn.(3). Two data sets agree quite well which indicates that the anisotropy in this series compounds is indeed governed by the leading term of the CEF effect.
In order to see how much of the magnetic anisotropy the term captures for these materials, we can look at a very simplified Hamiltonian given by
where the second term is the Zeeman energy. Using this, we have calculated the paramagnetic susceptibility that would be obtained from such a Hamiltonian (see, for example work done by P. BoutronBoutron ()), where B determined from experimental Curie-Weiss temperatures is used. In Fig.4, 5 and 9-13, calculated magnetization curves were shown for RCoGe (R = Pr, Nd, Tb-Tm) in solid curves. As a first approximation, these curves capture the basic anisotropies and temperature-dependence. The discrepancies demonstrate that the influence of higher order crystal field parameters as well as RKKY interaction need to be considered so as to provide a more accurate physical interpretation for magnetic anisotropy, especially for members like PrCoGe and TmCoGe. Quantitatively, magnetic measurements on diluted magnetic rare earth ions in either YCoGe or LaCoGe would be needed to provide more detailed information about the CEF splitting and, as a result, provide a better understanding of the effects of the exchange interaction.
Comparing the RTGe (T = Fe, Co, Ni) series, for non-magnetic members, the electronic specific heats of YCoGe and LaCoGe are close to those obtained in RNiGeRNi (). Furthermore, as the magnetic susceptibilities of RCoGe (R = Y and La) are also close to their counterparts in Ni series, the density of states at the Fermi energy is likely to be similar for RCoGe and RNiGe. On the other hand, in RFeGeRFe (), the non-magnetic is nearly six times larger, which may be evidenced by a magnetic fluctuation on the Fe siteLuFe (). All three series exhibit generally the same magnetic anisotropy where the paramagnetic easy magnetization direction switch from axial (R = Pr, Nd, Tb-Ho) to planar (R = Er, Tm) following a positive A. The ordering temperatures of RTGe (T = Fe, Co, Ni) for heavy rare earth members shows a rough trend of T T TRNi (); RFe (); TbNi (). Given the enhanced magnetic susceptibility of RFeGe compared with the other two series, it is interesting to have, in fact, lower ordering temperature for RFeGe. All of CeTGe (T= Fe, Co and Ni) show Kondo lattice behavior with moderately enhanced valuesRNi (); CeFe (); CeNi (). Among these three compounds, CeCoGe has the highest Kondo temperature. Detailed band structure calculation may be helpful in illuminating the changes in these RTGe series as T is varied from Fe to Co to Ni.
In this work, single crystalline ternary compounds RCoGe (R = Y, La-Nd, Sm-Tm) were grown using a self-flux method and characterized by x-ray powder diffraction, temperature- and field-dependent magnetization, temperature- and field-dependent resistivity and zero-field specific heat measurements. Magnetic ordering temperatures were determined down to 1.8 K by dT/dT, d/dT and zero-field specific heat. All local-moment bearing rare-earth members, except for Ce, order antiferromagnetically above 2 K with the highest T value being 33.0 K (Tb) and the lowest being 2.2 K (Tm). YCoGe and LaCoGe are Pauli paramagnets. Ce is trivalent at high temperature in CeCoGe. Although it does not appear to order magnetically, it does show two weak anomalies at 15 K and 2.3 K, of which we are uncertain about the origin. An enhanced value, together with other transport measurements, is consistent with a Kondo screening effect with 90-103 mJ/mol K and T 100 K. More than one magnetic phase transition was observed in RCoGe (R = Tb-Ho). Magnetic anisotropies were observed for all members, except for Gd and Eu with half-filled 4f shells (L = 0). This anisotropy can be explained quite well by CEF theory, where crystal field parameter B is the leading term deciding the easy direction and the size of anisotropy. The de Gennes scaling does not hold for heavy rare-earth members, which may partially be explained by a strong CEF effect.
We would like to thank W. Jayasekara, H. Hodovanets, A. Thaler and Greg Dyer for useful discussions and experimental assistances. We would also like to thank A. Kreyssig for not only providing general discussion, but also providing key understanding about the existing TmCoGe scattering data and analysis. Work done at Ames Laboratory was supported by US Department of Energy, Basic Energy Sciences, Division of Materials Sciences and Engineering under Contract NO. DE-AC02-07CH111358. V.T. and X.L. would like to acknowledge support from AFOSR-MURI Grant No. FA9550-09-1-0603.
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