Open Access Article
Leonardo Tacconi
* and
Mauro Perfetti
*
Department of Chemistry “Ugo Schiff” & INSTM RU, Università degli Studi di Firenze, Via della Lastruccia 3, 50019, Sesto F.no, (FI), Italy. E-mail: leonardo.tacconi@unifi.it; mauro.perfetti@unifi.it
First published on 19th May 2026
Lanthanide complexes exhibiting marked easy-axis magnetic anisotropy are the main targets to achieve highly performant single molecule magnets, pseudo contact shift agents and rotating magnetic refrigerants. To experimentally map the magnetic anisotropy orientation and magnitude, a growing portfolio of experimental techniques is now available, including powder and single crystal magnetometry, cantilever torque magnetometry, and X-ray magnetic circular dichroism. While these methods provide complementary information, reference values for ideal systems are not always applied consistently, possibly introducing ambiguity in data interpretation. Here we present a unified and quantitative set of benchmark magnetic observables for trivalent lanthanide ions exhibiting ideal easy-axis anisotropy. For each ion we report: the orientation-dependent saturation magnetization and low-temperature magnetic susceptibility; the field-dependent maximum magnetic torque signal; and the angular- and field-dependent normalized XMCD response at the M4,5 edges. The resulting tables and figures provide a simple, ready-to-use reference framework for direct comparison with experimental measurements of lanthanide-based magnetic systems.
In molecular magnetism, this statement most frequently refers to the magnetic moment of a sample—the quantity measured in magnetometric studies.1 Traditionally, most measurements are performed on powder samples because of their simplicity and rapid data acquisition.2 However, in recent years powder magnetometry has increasingly been complemented or replaced by single crystal3 and torque4 magnetometry. In parallel, growing interest has emerged in probing magnetic molecules deposited on surfaces, typically via highly sensitive spectroscopic techniques such as X-ray magnetic circular dichroism (XMCD),5 largely motivated by potential applications in areas such as molecular memory storage6 and spintronics.7
While combining multiple experimental techniques provides complementary information, the reference values expected for ideal systems are not always applied consistently. As a result, the interpretation of experimental data can become ambiguous, particularly when comparing results obtained from different techniques. To our knowledge, no unified set of reference values encompassing the major experimental techniques has been established for lanthanide-based magnetic systems.
A target property to design and finely tune for achieving performant magnetic materials is the magnetic anisotropy, i.e. the spatial dependence of the magnetic response of the material. Among the anisotropy shapes that can be achieved, easy-axis magnetic anisotropy is surely the most targeted. Such anisotropy implies that the molecule can be easily magnetized when a magnetic field is applied along a certain direction (the easy axis) while when the field is along the perpendicular plane the magnetic moment is negligible. Thanks to the partially filled 4f orbitals, lanthanide-based molecular complexes are ideal for achieving highly performant single molecule magnets, pseudo contact shift agents and rotating magnetic coolants. A review on its role in boosting the properties of these materials has been recently published.8
Since easy-axis magnetic anisotropy is a well-established target, in this contribution we present a series of tables and graphs summarizing the values of key observables expected for ideal easy-axis lanthanide systems. To provide a simple, ready-to-use and transparent reference framework, we analyze the limiting case of a perfectly axial system (i.e. no mixing between states). Although real systems often deviate from this idealized limit, it represents the best-case scenario for many applications of lanthanide molecular magnets, and it has been achieved in single-molecule magnets,9–11 pseudo-contact shift agents,12,13 and rotating magnetocaloric materials.14,15 The values reported here therefore provide a convenient benchmark to estimate the deviation of experimental results from the ideal targeted behaviour.
Within this framework, the magnetic behaviour of lanthanide ions is determined by the energy of the |J, mJ〉 states in the CF potential generated by the surrounding ligands. In the simplest case, their ordering can be rationalized using an electrostatic model,21 in which the key quantity is the charge density asphericity of the |J, mJ〉 states—first derived by Sievers22 and later popularized by Rinehart and Long.23 In particular, the angular dependence of the charge density for a given |J, mJ〉 state can be expressed as
![]() | (1) |
![]() | (2) |
Since this work focuses on idealized benchmark systems, Fig. 1 highlights the polar plots of the largest and smallest mJ states’ electron density for each trivalent ion, corresponding to ideal easy-axis and easy-plane magnetic anisotropy, respectively. All |J, mJ〉 states are reported in Fig. S1. In the representation shown in Fig. 1 and Fig. S1, an isotropic contribution was subtracted from all surfaces to emphasize the anisotropic component of the charge density. Therefore, the plotted quantity should be understood as a visualization of the deviation from spherical symmetry rather than as the full charge density. Each row of Fig. 1 groups ions differing by seven 4f electrons, and thus sharing the same orbital angular momentum, highlighting the similarities in their electron densities.24 This arrangement reveals the pronounced evolution of orbital asphericity across the lanthanide series and its strong dependence on mJ, spanning from prolate to oblate shapes. These differences reflect the multipolar character of the 4f shell and anticipate the strongly anisotropic magnetic response of different |mJ| states.
![]() | ||
| Fig. 1 Asphericity of the |J, mJ〉 (mJ = ±J and 0 or ±1/2 for non-Kramers and Kramers ions, respectively) components of Ln(III), calculated using equations reported by Sievers.22 Each row of the Figure compares ions differing by 7 f-electrons. The red and blue trace always correspond to the maximum and minimum mJ, respectively. | ||
In general, oblate charge distributions are preferentially stabilized by an axial CF, whereas prolate charge distributions are stabilized by equatorial ligand arrangements. This electrostatic picture provides an intuitive link between orbital asphericity, and the CF Hamiltonian used to describe the energy level structure.21,23
The CF potential at the lanthanide centre is described by the CF Hamiltonian
![]() | (3) |
| Ô20 = 3Ĵz2 − J(J + 1). | (4) |
Under the sole action of this operator, the energy of each |J, mJ〉 state becomes
| E(|J, mJ〉) ∝ 3mJ2 − J(J + 1) | (5) |
This transparent ordering mechanism naturally defines the axial anisotropy regime, which forms the basis of the model adopted throughout this work. For each ion, the magnitude of B20 was adjusted such that the energy separation between the ground and first excited states is fixed at 300 cm−1. Such a gap assures that at T = 2 K, at which we simulate all the benchmark values, only the pure |±mJ〉 ground state (with |mJ| = J) is populated while keeping the overall CF splitting below the spin–orbit interaction, thereby preserving the hierarchy of energy scales characteristic of trivalent lanthanides. Moreover, this relatively large energy gap strongly suppresses the contribution of excited states to the magnetic behaviour also in terms of the field-induced mixing via the Zeeman interaction. The CF parameters employed and the corresponding energy schemes are provided in Table S1. Although idealized, this model yields benchmark values that are consistent with those reported for strongly axial lanthanide complexes,28–30 supporting its use as a practical reference for assessing how closely real systems approach the easy-axis limit.
Importantly, among the thirteen trivalent lanthanide ions, we exclude from our analysis Eu(III) and Gd(III) due to their specific electronic structures. According to Hund's rules, Eu(III) has a singlet ground term (J = 0), arising from the cancellation of the L = 3 and S = 3 angular momenta. Consequently, its magnetic behaviour is weak and dominated by temperature-independent paramagnetism (TIP). In contrast, Gd(III) has 7 f-electrons, leading to L = 0. Therefore, its ground state presents negligible magnetic anisotropy. Since the present work focuses on the role of magnetic anisotropy in determining magnetic behaviour, these two ions fall outside the scope of the analysis.
ĤZeeman = μBgJ ·Ĵ = μBgJ(BxĴx + ByĴy + BzĴz)
| (6) |
The orientation of the magnetic field relative to the magnetic anisotropy axis plays a central role in determining the magnetic response. When the magnetic field is applied along the z magnetic axis, it couples to Ĵz, which is diagonal in the |J, mJ〉 basis. In this configuration the magnetization is determined solely by the identity and thermal population of the CF levels. By contrast, a transverse magnetic field couples through Ĵx and Ĵy, which contain the ladder operators Ĵ± and therefore mix the ground state with excited states. The magnitude of this mixing is primarily governed by the energy separation between the ground and excited CF states. An example of the role of the energy gap on the magnetic response is provided in Fig. S2, where magnetization curves at T = 2 K for a Dy(III) ion are simulated for different energy separations. As shown in the figure, decreasing the energy gap leads to a progressive deviation from the ideal horizontal plateau at high fields, reflecting the increasing contribution of field-induced mixing with excited states, commonly associated with TIP.
For these reasons, the orientation-dependent saturation magnetization provides a direct experimental probe of the axial character of the ground state. In this work the saturation magnetization was simulated at 2 K and 7 T, conditions readily accessible with commercial magnetometers. Three configurations were considered: along the principal magnetic axis z, within the isotropic xy plane, and an orientational average over a powder sample. The resulting values are reported in Fig. 3.
As expected, the largest magnetization is obtained when the magnetic field is applied along the z axis. In this configuration the saturation is well described by
![]() | (7) |
For powder samples the measured magnetization corresponds to an orientational average over all possible directions of the magnetic field relative to the molecular anisotropy axes. The powder magnetization is therefore given by
![]() | (8) |
For uniaxial systems, where the xy plane is isotropic and the magnetization depends only on the polar angle θ, this equation simplifies to
![]() | (9) |
In practice, this integral is evaluated numerically by computing the magnetization at a discrete set of orientations distributed uniformly over a sphere. Lebedev quadrature35 provides an efficient spherical sampling scheme, yielding accurate powder averages with a relatively small number of orientations.36,37 However, increasing the number of grid points raises computational cost, which can become significant for field- and temperature-dependent simulations. A commonly used simplified alternative is the so-called “thirds” approximation,38,39 in which the powder magnetization is approximated as the arithmetic mean of the principal components:
![]() | (10) |
Fig. S4 shows that this approximation can yield substantially different results from a rigorous spherical average in the low-temperature, high-field regime. This discrepancy is further illustrated in Fig. S5, where the temperature- and field-dependent powder magnetization curves for an easy-axis Dy3+ centre are compared using both approaches. The “thirds” approximation systemically underestimates the powder magnetization, a direct consequence of the highly anisotropic magnetization tensor in the easy-axis regime. Its use in quantitative simulations of anisotropic powder samples should therefore be approached with caution.
It is worth noting that the powder saturation magnetization value alone is not a clear indication of the nature of the ground state doublet of the investigated sample. As a matter of fact, a powder saturation value of around 5µB for a Dy3+ ion can also be obtained for ground states with significantly different compositions, as evidenced in Fig. S6. This arises because powder magnetization measurements correspond to an orientational average over all possible directions of the applied magnetic field, which can shade the correct wavefunctions. In other words, different combinations of |mJ| components may lead to similar powder saturation values. For this reason, the saturation magnetization alone cannot be considered a definitive fingerprint of the ground state. What provides more reliable insight into the ground state composition is the field dependence of the magnetization, the comparison between single crystal magnetization values measured parallel and perpendicular to the principal magnetic axis, and the comparison with other experimental techniques.
![]() | (11) |
In experimental practice, however, susceptibility is commonly approximated by measuring the magnetic moment and dividing it by the applied field, yielding:
![]() | (12) |
These two expressions only coincide when the magnetization varies linearly with the applied magnetic field. This distinction is important, as deviations from linearity can lead to noticeable differences between simulated susceptibilities and experimentally reported values.
Magnetic susceptibility is most reported as the product χT as a function of temperature. At high temperatures, χT approaches the Curie constant expected for the free ion, which can be calculated directly from the quantum number J and gJ.
At low temperature and low magnetic field, however, the situation is markedly different. Under these conditions only the lowest CF level is significantly populated, and the magnetic response becomes dominated by the nature of the ground state. The resulting χT value therefore provides a hint regarding the ground state anisotropy. For this reason, calculations were performed under experimentally accessible conditions (T = 2 K, B = 0.1 T) for the three relevant configurations discussed above. The resulting values are summarized in Fig. 4.
![]() | ||
| Fig. 4 Expected χT values calculated for lanthanide ions with an easy-axis magnetic anisotropy. Eu3+ and Gd3+ have not been included due to their J = 0 and L = 0 ground state, respectively. | ||
As observed for magnetization data, the calculated χT values clearly reflect the strongly anisotropic nature of the easy-axis ground state. The xy-plane susceptibilities remain close to zero across the entire lanthanide series, whereas the axial susceptibilities are significantly larger due to the strong magnetic moment associated with the ground state |mJ| component.
The “thirds” approximation works well at these low field for light ions (Fig. S7). Nevertheless, a non-negligible discrepancy persists for late-series ions, where deviations up to approximately 5% are observed. These results highlight the intrinsic limitations of the approximation and further support the use of spherical averaging when quantitative simulations of anisotropic powder samples are required.
τ = × .
| (13) |
The amplitude, angular dependence and field evolution of the torque signal therefore provide direct information on both the strength and symmetry of the magnetic anisotropy.45 In addition, torque measurements allow the orientation of the principal magnetic axes to be determined, an aspect that is often difficult to extract from conventional magnetometry alone.46,47
Because the magnetic torque vanishes in isotropic systems, torque magnetometry is intrinsically a single-crystal technique. In a powder sample, the statistical distribution of crystallite orientations causes cancellation of the net torque signal. Despite this requirement, the technique remains experimentally convenient because it can be applied to small crystals over a wide temperature range (typically 2–300K) and its sensitivity to anisotropy is suitable also for poorly anisotropic samples.48
In the present work we focus on the low-temperature (2 K) regime and magnetic fields between 1 and 9 T. Under these conditions, the Zeeman interaction dominates and the torque signal reflects the ground state anisotropy. The maximum torque amplitude therefore provides a direct fingerprint of the ground state composition, complementing the saturation magnetization and χT values discussed above.
The simulated torque curves are reported in Fig. S8–S18. Their phase is consistent with easy-axis magnetic anisotropy, and the angles at which the torque vanishes correspond to configurations where the easy magnetization direction is either parallel or perpendicular to the applied field.
The maximum torque amplitudes as a function of applied magnetic field are summarized in Table 1 for all lanthanide ions considered. Across the series the torque increases monotonically with field. Particularly large torque values are predicted for Dy3+, Ho3+ and Er3+, reflecting their large |mJ| ground states and favourable (i.e. > 1) gJ factors. By contrast, Sm3+ displays significantly smaller torque values throughout the entire field range, consistent with its comparatively small gJ.
| τmax(N m mol−1) | |||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| Ce3+ | Pr3+ | Nd3+ | Pm3+ | Sm3+ | Tb3+ | Dy3+ | Ho3+ | Er3+ | Tm3+ | Yb3+ | |
| B = 1 T | 3.97 | 8.18 | 8.51 | 4.89 | 0.47 | 39.43 | 45.22 | 45.22 | 39.44 | 28.05 | 11.93 |
| B = 2 T | 13.35 | 24.68 | 25.49 | 15.99 | 1.84 | 91.33 | 102.80 | 102.81 | 91.37 | 68.27 | 33.69 |
| B = 3 T | 24.81 | 42.88 | 44.14 | 29.16 | 3.97 | 142.72 | 159.85 | 159.87 | 142.78 | 108.53 | 55.68 |
| B = 4 T | 36.93 | 61.33 | 63.03 | 42.88 | 6.70 | 193.71 | 216.49 | 216.52 | 193.79 | 148.34 | 79.72 |
| B = 5 T | 49.22 | 79.75 | 81.83 | 56.69 | 9.87 | 244.39 | 272.88 | 272.91 | 244.50 | 187.97 | 102.64 |
| B = 6 T | 61.58 | 98.08 | 100.59 | 70.53 | 13.35 | 295.16 | 328.81 | 328.84 | 295.31 | 227.61 | 125.47 |
| B = 7 T | 73.91 | 116.40 | 119.30 | 84.33 | 17.04 | 345.66 | 385.20 | 385.25 | 345.83 | 267.11 | 148.11 |
| B = 8 T | 86.19 | 134.67 | 138.01 | 98.08 | 20.86 | 361.49 | 440.86 | 440.93 | 396.38 | 306.30 | 170.89 |
| B = 9 T | 98.41 | 152.76 | 156.57 | 118.66 | 24.81 | 446.11 | 497.02 | 497.09 | 446.40 | 345.66 | 193.42 |
The high brilliance and energy tunability of synchrotron radiation enable XMCD measurements on extremely small amounts of material,52 making the technique particularly suitable for studying molecular magnetic systems deposited on surfaces, down to the monolayer regime.53–55 In this work XMCD spectra were simulated for all trivalent lanthanide ions at the M4,5 edges, corresponding to the 3d104fn → 3d94fn+1 electronic transitions. These edges are accessed using soft X-rays (≈ 800–1500 eV) and directly probe the 4f shell responsible for the magnetic properties of lanthanide ions.56 Because the absolute magnitude of the XMCD signal strongly depends on beamline-specific experimental factors, the simulated spectra have been normalized with respect to the isotropic absorption spectrum. Details of the normalization procedure is provided in Note S1.
XMCD spectra were simulated at 2 K under magnetic fields ranging from 0 to 6 T, considering field orientations spanning from the principal magnetic z axis (θ = 0°) to the transverse x axis (θ = 90°). The complete angular dependence of the XMCD signal at 6 T, together with the field dependence of the dichroic intensities at both the M4 and M5 edges, are reported in Fig. S19–S29. Maximum XMCD values at both edges for all ions and field conditions are summarized in Tables S2–S12.
Across the lanthanide series, early ions display a larger dichroic signal at the M4 edge, whereas from Tb3+ onwards the dominant contribution shifts to the M5 edge. Notably, Yb3+ exhibits no signal at the M4 edge, consistent with its nearly filled 4f13 configuration, which suppresses the dipole allowed 3d3/2 → 4f transition responsible for the M4 XMCD signal.57
Consistent with easy-axis magnetic anisotropy, the dichroic signal reaches its maximum when the magnetic field is aligned with the z axis (θ = 0°). In this configuration the XMCD intensity rapidly approaches saturation with increasing field, reflecting the stabilization of the highest |mJ| component as ground state. The maximum values obtained at the M5 edge with θ = 0° at selected magnetic fields are listed in Table 2. A notable feature is the sign change of the XMCD signal between early and late lanthanide series, from positive values for Ce3+–Sm3+ to negative value from Tb3+ onwards, reflecting the reversal of the spin–orbit coupling interaction sign.
| XMCDmax(%) | |||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| Ce3+ | Pr3+ | Nd3+ | Pm3+ | Sm3+ | Tb3+ | Dy3+ | Ho3+ | Er3+ | Tm3+ | Yb3+ | |
| B = 0.2 T | 8.06 | 16.81 | 6.79 | 6.54 | 2.77 | −98.90 | −111.89 | −115.56 | −107.52 | −87.58 | −52.48 |
| B = 0.6 T | 22.97 | 45.16 | 18.19 | 18.44 | 8.35 | −173.98 | −185.27 | −191.15 | −189.17 | −177.45 | −133.48 |
| B = 0.8 T | 29.37 | 55.36 | 22.25 | 23.40 | 10.96 | −180.76 | −188.61 | −196.38 | −196.46 | −190.88 | −158.25 |
| B = 1.0 T | 34.90 | 62.95 | 25.25 | 27.56 | 13.64 | −182.84 | −191.71 | −197.78 | −198.70 | −196.39 | −174.50 |
| B = 1.5 T | 45.00 | 73.54 | 29.38 | 34.80 | 20.23 | −183.74 | −192.20 | −198.29 | −199.66 | −200.00 | −193.02 |
| B = 3.0 T | 55.54 | 79.46 | 31.65 | 41.44 | 38.08 | −183.74 | −192.20 | −198.29 | −199.66 | −200.00 | −200.00 |
When the field is applied within the equatorial plane (θ = 90°), the XMCD signal is strongly reduced and increases approximately linearly with field. This behaviour mirrors the transverse magnetization response discussed above and arises from the same physical mechanism. The angular dependence of the XMCD intensity therefore constitutes a spectroscopic analogue of directional magnetization measurements and provides a direct fingerprint of the ground state anisotropy.
A practically relevant observation also emerges from this systematic analysis. The “thirds” approximation for powder magnetization averaging introduces systematic deviations in the low-temperature, high-field regime, a non-negligible error for strongly anisotropic systems. These results highlight the importance of performing rigorous spherical averaging when quantitative agreement between simulations and experiments is required.
The reference values presented here are ready-to-use. All simulations were performed under experimentally accessible conditions (T = 2 K, B = 7 T for magnetization, B = 0.1 T for χT; B = 1–9 T for torque; and B = 0–6 T for XMCD) and are intended to facilitate immediate comparison with experimental measurements. Beyond providing a practical framework for interpreting magnetic data, these benchmarks offer simple yet quantitative guidelines for evaluating if the ideal easy-axis anisotropy of a lanthanide complex has been experimentally achieved, and for guiding the design of functional molecular magnetic materials.
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