T.
Scholz
and
R.
Dronskowski
*
Institute of Inorganic Chemistry, RWTH Aachen University, 52056 Aachen, Germany. E-mail: drons@HAL9000.ac.rwth-aachen.de; Fax: (+49) 241-80-92642
First published on 22nd November 2016
We present an experimental and theoretical study of the solid solution GexFe4−xNy (0 ≤ x ≤ 1). A two-step ammonolytic reaction gives access to the compounds with phase-pure quality. The GexFe4−xNy nitrides show a transition from an antiperovskite-like to a tetragonally distorted structure with increasing germanium concentration. Various experimental and theoretical methods evidence that the iron substitution by germanium exclusively takes place at the cubic Wyckoff position 1a. Despite the phase transition, one observes a Vegard-type decrease of the lattice parameter over the entire compositional range. In addition, the nitrides have a limited nitrogen capacity: incorporating germanium drastically reduces the nitrogen content in the cubic structure, but increases it again in the tetragonal structure. Combined HT-XRD and TG-DSC measurements evidence that the germanium-richest nitrides are highly expanding materials. They first show a transition to a cubic structure before they decompose by releasing nitrogen. Magnetic measurements reveal that the gradual germanium incorporation is accompanied by a drastic weakening of the ferromagnetic interactions leading to a frustrated iron spin system. Ge0.97Fe3.03N0.56 is identified as a canonical spin glass with the characteristic parameters Tg = 36.68(5) K, τ* = 10−13.8(2) s, zν = 7.2(1) and ΔTm/(Tm·Δlg
ω) = 0.012.
A recently developed two-step ammonolytic synthesis6 combining a high-temperature sintering reaction (1000–1200 °C) and a low-temperature nitriding step (300–800 °C) was proven to be the most effective method to yield ternary iron nitrides MxFe4−xN (M = Rh,6 Pd,7 Ga,8,9 In,10 Sn,11,12etc.) with phase-pure quality. To date, the nitrides can be divided into two groups with regard to their magnetic properties: upon substitution they either remain ferromagnetic, as is the case in transition-metal iron nitrides, or lose the long-range magnetic order resulting in a frustrated spin system. Candidates of the second class of compounds include Sn0.9Fe3.1N, the first ternary iron nitride spin glass,12 and Ga0.9Fe3.1N with a postulated “cluster magnetism”.9 Germanium's proximity to Sn in the periodic table suggests that the Ge-substituted nitride might be related to those frustrated magnetic systems as well.
GexFe4−xNy was first studied by Stadelmaier and Fraker in 1962.13 They applied a classical NH3/H2 ammonolytic reaction to Fe–Ge precursor alloys to synthesize the ternary phase, and they also reported a cubic antiperovskite-like structure (Pmm, Fig. 1(a)) as well as a tetragonally distorted structure (I4/mcm, Fig. 1(b)). The relationship between the two structures can clearly be seen when considering the cuboids of Ge atoms. The very centre of a cuboid is occupied by a nitrogen atom that is surrounded by an octahedron of iron atoms. In the tetragonal structure, these octahedra are then twisted against each other. In the cubic nitride, the Ge–Ge distances are equal and correspond to the lattice parameter a. In the tetragonal structure, however, there are short and long Ge–Ge distances. To compare both structures in the later discussion, we will refer to an equivalent parameter aeq expressing an average Ge–Ge distance in the tetragonal case. Furthermore, Stadelmaier and Fraker found, in contrast to γ′-Fe4N and many ternary iron nitrides, a limited nitrogen concentration.
In another study by Sankar et al., the magnetic properties of the daltonide phase GeFe3Ny were investigated.14 Depending on the nitrogen concentration they found either a cubic nitride with a ferromagnetic (FM) ground state or a tetragonal nitride, for which they claimed antiferromagnetic (AFM) properties with a Néel temperature of 80 K. Experience with Ga0.9Fe3.1N8,9 suggests that a frustrated magnetic ground state can be easily misinterpreted as antiferromagnetism which is why we decided to re-examine the magnetic properties of germanium-rich iron nitride.
In this article, we present a comprehensive study of the entire solid solution GexFe4−xNy (0 ≤ x ≤ 1) regarding their two-step ammonolytic synthesis from the oxides, the determination of their structures and composition, the stability at elevated temperatures and, finally, the magnetic characterisation. Extensive density-functional theory (DFT) calculations were utilised to guide the experiments and to validate the results.
The high-temperature X-ray diffraction of Ge0.97Fe3.03N0.56 in a 0.3 mm quartz capillary was performed using a G644 diffractometer with Cu Kα1 radiation (λ = 1.54059 Å) and a PSD detector (38° ≤ 2θ ≤ 52°, step rate 0.02° in 2θ) from room temperature to the maximum temperature of 720 °C with temperature steps ΔT = 20 K.
When studying the structure of ternary iron nitrides MxFe4−xN, the first question concerns the Wyckoff position at which the substitution of Fe by a metal or metalloid M takes place. The M atom can either substitute Fe exclusively on one or on both positions simultaneously (1a and/or 3c). This depends on the covalent or metallic radius and, furthermore, on the metal's affinity to the central nitrogen atom. Generally speaking, larger M atoms prefer the larger cuboctahedral 1a environment (an approximated sphere with r = 1.42 Å) over the smaller 3c position (1.28 Å).8 The metallic radius of Ge (rM = 1.37 Å) is larger than that of Fe (rM = 1.26 Å)23, but the covalent radius of Ge (rcov = 1.20 Å) is smaller than that of Fe (l.s., rcov = 1.32 Å).24 These very different radii make the decision difficult if not impossible, and we therefore calculated the Ge distribution over both Wyckoff positions in cubic and tetragonal GeFe3N. The Ge atoms can either occupy 1a or 3c resulting in ordered phases 1a(Ge)3c(Fe3)1b(N) and 1a(Fe)3c(GeFe2)1b(N) when applying the cubic nomenclature. Furthermore, they can be statistically disordered as given in 1a(Ge1/4Fe3/4)3c(Ge3/4Fe9/4)1b(N). From the energetic results in Table 1, it is all too obvious that the Ge atoms will exclusively occupy the larger corner position – that scenario is energetically favoured by an enormous 97 or 110 kJ mol−1 over the statistically disordered arrangement. Furthermore, the theoretical calculations predict a preferred formation of tetragonal over cubic GeFe3N by an also significant 28 kJ mol−1. This is in good agreement with the only experimental results on GeFe3Ny in the literature.13,14 Since cubic γ′-Fe4N and tetragonal GeFe3N are the end members of the GexFe4−xNy series, experiments will show at which composition the tetragonal distortion arises.
Atomic arrangement in the cubic nomenclature | Cubic GeFe3N | Tetragonal GeFe3N | ||
---|---|---|---|---|
ΔE (kJ mol−1) | a (Å) | ΔE (kJ mol−1) | a eq (Å) | |
1a(Ge)3c(Fe3)1b(N) | +28 | 3.83 | 0 | 3.75 |
1a(Ge1/4Fe3/4)3c(Ge3/4Fe9/4)1b(N) | +138 | 3.97 | +97 | 3.92 |
1a(Fe)3c(GeFe2)1b(N) | +171 | 3.96 | +122 | 3.89 |
Prior to synthesis, the compound's theoretical thermochemistry is also worth studying. Hence, we compare GeFe3N to the elements and nitrides that are the most likely competing phases in the reaction. It is important to note that the metal oxides (GeO2 and Fe2O3) are used as starting materials in the later synthesis, but it is correct to refer to elemental Ge and Fe in the theoretical sets of reactants because they are instantly formed through reduction in the hydrogen flow. Furthermore, these thermochemical calculations are restricted to an FM ordering. An AFM ordering is considered in the later sections, but the energy differences introduced by different magnetic states are very small (cf. Section 3.5.2).
Table 2 shows two possible reaction schemes assuming that GeFe3N may adopt both structures, the cubic and the tetragonal. The first reaction can be understood as the incorporation of Ge into ε-Fe3N, while the second one describes the substitution of Fe in γ′-Fe4N by Ge. Both reaction schemes are exothermic, showing that the ternary compound is preferred over the binary nitrides and that the synthesis should be feasible over a wide range of reaction temperatures. However, it is well known from the binary Fe–N system that γ′-Fe4N decomposes to ε-Fe3N1+x at elevated temperatures (680 °C).25 Since this temperature is comparable to the usual nitriding temperatures, special attention needs to be paid to ε-Fe3N1+x as a possible side phase.
ΔHR (kJ mol−1) | Cubic GeFe3N | Tetragonal GeFe3N |
---|---|---|
(1) Ge + ε-Fe3N → GeFe3N | −3.9 | −31.9 |
(2) Ge + γ′-Fe4N → GeFe3N + α-Fe | −12.4 | −40.4 |
ϑ (°C) | x int | x occ(Ge)R | y occ(N)G | a or Ge–Ge (Å) | R P (%) | R B (%) | M (g mol−1) | ρ (g cm−3) |
---|---|---|---|---|---|---|---|---|
650 | 0.25 | 0.247(3) | 0.87 | 3.7909(1) | 3.41 | 3.11 | 239.71 | 7.31 |
650 | 0.50 | 0.492(3) | 0.61 | 3.7811(1) | 4.49 | 5.24 | 240.19 | 7.38 |
650 | 0.75 | 0.731(3) | 0.34 | 3.7638(1) | 3.38 | 3.43 | 240.42 | 7.49 |
650 | 1.00 | 0.975(5) | 0.54 | 3.7306(3)/3.8156(5) | 3.40 | 8.59 | 247.32 | 7.73 |
700 | 0.25 | 0.249(3) | 0.88 | 3.7916(1) | 3.30 | 3.24 | 239.89 | 7.31 |
700 | 0.50 | 0.485(2) | 0.64 | 3.7823(1) | 3.48 | 4.34 | 240.49 | 7.38 |
700 | 0.75 | 0.761(3) | 0.44 | 3.7696(1) | 3.61 | 2.83 | 242.32 | 7.51 |
700 | 1.00 | 0.974(3) | 0.56 | 3.7345(3)/3.8197(5) | 3.85 | 9.52 | 247.58 | 7.76 |
To deduce the lattice parameters and the mixed occupations from these powder patterns, Rietveld refinements were carried out whose results are summarised in Table 3. The Rietveld refinements were only successful if a Ge occupation was considered at the cubic corner position (1a) or at the equivalent tetragonal position (4b). Thus, both experimental and theoretical (cf. Section 3.1) results clearly point towards this position. Also, the Rietveld results match the intended metal ratios very well so that a metal loss during the reaction can be ruled out. But how about the nitrogen content? It is well known that GexFe4−xNy has a limited nitrogen capacity (y ≪ 1)13,14 but the nitrogen content is not accessible from Rietveld refinements because site-occupation refinements of light elements are hardly reliable from powder XRD data. Therefore, we determined the nitrogen content gravimetrically for several identical reactions. We consider this approach legitimate because it gave a satisfactory result for the synthesis of γ′-Fe4N which has only a small phase width regarding the nitrogen content;25 in addition, the constant metal ratio has already been established. The nitrogen content of four different germanium iron nitrides, each synthesised at 650 °C and 700 °C (all from Table 3), is illustrated in the ternary phase diagram in Fig. 3. The nitrogen occupation varies between 88% and 34% and, as Stadelmeier and Fraker already suggested,13 it decreases with increasing Ge content for the cubic nitrides along a curve from binary γ′-Fe4N to intermetallic Fe3Ge. Interestingly, the nitrogen content increases again when the structure distorts tetragonally at the highest Ge content. The data further indicate that the higher nitriding temperature of 700 °C leads to slightly higher nitrogen contents in the sample, all else equal.
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Fig. 3 Excerpt from the Fe–Ge–N phase diagram with compounds GexFe4−xNy synthesised at nitriding temperatures of 650 °C (orange) and 700 °C (blue). The compositional and structural parameters of these eight compounds are listed in Table 3. |
For the nitrides GexFe4−xNy synthesised at 700 °C and 650 °C, the structural parameters are shown in Fig. 4(a) either as the cubic lattice parameter a or as the equivalent parameter aeq in the tetragonal case. Substituting Fe by Ge atoms leads to a Vegard-type decrease. Even though the nitrides richest in Ge, namely Ge0.97Fe3.03N0.56 (700 °C) and Ge0.98Fe3.02N0.54 (650 °C), exhibit a tetragonal structure and have a relatively high nitrogen content, the averaged Ge–Ge distances (aeq) perfectly fit the Vegard lines of each series. The nitrides synthesised at the lower nitriding temperature and, therefore, with the lower nitrogen content result in slightly smaller unit cells. Compared to the nitride γ′-Fe4N, the unit cell contraction is 3.0% (700 °C) or 3.3% (650 °C). We also note that the contraction throughout the series does not fit the larger metallic radius of Ge (cf. Section 3.1) but the smaller covalent radius of Ge. This clearly suggests the importance of covalent bonding in this series. The tetragonal lattice parameters of Ge0.97Fe3.03N0.56 (700 °C) and Ge0.98Fe3.02N0.54 (650 °C) are a = 5.2814(7) Å, c = 7.6394(10) Å and a = 5.2759(7) Å, c = 7.6311(10) Å, respectively. Similar lattice parameters were reported in the literature.13,14
In addition, theoretical lattice parameters were calculated assuming different magnetic ground states. Supercells were filled random-like with different ratios of Fe and Ge atoms on 1a, either preserving the cubic metric or allowing the tetragonal distortion of Fe atoms. For a given composition only the supercells with the lowest energy were included in the final analysis (Fig. 4(b)). We reiterate that in contrast to experiment, the nitrogen position was fully occupied in these supercells.
For a cubic FM model the lattice parameter a does not reproduce the entire Vegard-like behaviour of the experimental data but it fits to the shrinking of the unit cell up to Ge0.375Fe3.625N, especially since the DFT parameterisation (GGA) underestimates the bond length. For higher substitutions the lattice parameter a significantly increases and deviates from the experimental trend. The calculated non-linear behaviour was actually observed in GaxFe4−xN, and it was understood as a magnetic effect.8
Jumping to the highest substitutions, it is not at all surprising that a cubic FM model is an inadequate description for GeFe3N, and so tetragonally distorted FM and AFM supercells were calculated. Both tetragonal FM and AFM models result in similar splittings of the Ge–Ge distances that slightly overestimate the experimental splitting. Nevertheless, the averaged distances aeq in theory and experiment fit nicely. The energetically more favourable tetragonal model for GeFe3N arrives, not surprisingly, at a better structural description than the cubic model (cf. Section 3.1).
Experimentally, the phases with intermediate substitutional grades show a linear shrinking of the lattice parameter a that cannot be described by just one theoretical model. It can rather be understood as a transition from a cubic FM cell to a tetragonal cell with FM and AFM interactions (discussed in Section 3.5.2). It may also be the case that the transition to the tetragonal phase is gradual, starting early and leading to broad reflections and changes in magnetic interactions of Fe spins.
In addition to FM and AFM ground states, a cubic non-magnetic (NM) model was used. The calculations yield much smaller lattice parameters and an expanding Vegard-like behaviour from 3.67 Å for γ′-Fe4N to 3.74 Å for GeFe3N. Hence, these clearly do not reproduce the experimental results.
The high-temperature X-ray diffraction pattern in Fig. 5(a) reveals a transition from the tetragonal Ge0.97Fe3.03N0.56 to a cubic primitive cell by a simple distortion (comparable to Fig. 1) setting in between 560 °C and 640 °C. Structural parameters like the Ge–Ge distances and the volume per formula unit Vf.u. were deduced from the positions of the reflections (202), (004) and (220) and are shown in Fig. 5(b). Up to 480 °C the Ge–Ge distances and the volume of tetragonal Ge0.97Fe3.03N0.56 expand linearly. The corresponding thermal expansion coefficients α in different directions are around 21–25 × 10−6 K−1, the expansion in the ab plane being larger than that along the c axis (Table 4). Given these values, Ge0.97Fe3.03N0.56 belongs to the group of highly expanding materials.26 In comparison, γ′-Fe4N has a value of 7.6 × 10−6 K−127 and is a candidate of the intermediate group (2 × 10−6 K−1 ≤ α ≤ 8 × 10−6 K−1).26 Above 480 °C the shorter Ge–Ge distance, mirroring what happens in the ab plane, is shrinking while the larger Ge–Ge distance, along the c direction, is still expanding. At 560 °C, reflections of the cubic structure appear, and in the range up to 580 °C reflections of the tetragonal and the cubic structures were fitted side-by-side showing a smooth transition especially for the shorter Ge–Ge distance. The volume of the cubic structure is shrinking up to 640 °C, the temperature at which the transition is complete, and a subsequent thermal expansion is absent.
Direction | α (10−6 K−1) |
---|---|
Short Ge–Ge distance | 23.7(6) |
Tetragonal axis a | 24.3(7) |
Long Ge–Ge distance | 21.3(8) |
Tetragonal axis c | 21.7(7) |
Deduced from Vf.u. (averaged) | 22.5(4) |
The high-temperature behaviour of Ge0.97Fe3.03N0.56 hints at a nitrogen loss upon shrinkage of the shorter Ge–Ge distance at 480 °C and a subsequent transition to the cubic structure. Nitrogen-free Fe3Ge itself crystallizes in the space group Pmm (with a phase transition to a hexagonal structure at 700 °C).28
Although a thermogravimetric measurement showed a step in the mass loss curve from 480 °C to 640 °C, it was only −0.2%, not a sign of nitrogen loss. A more significant step of −3.8% is from 640 °C to 970 °C. This corresponds to the entire nitrogen in the sample. To conclude, the sample does not decompose ahead of the structural transition. Ge0.97Fe3.03N0.56 rather shows a transition from the tetragonal to the cubic structure and a subsequent loss of nitrogen with increasing temperature. This may be the reason why the capillary for the high-temperature X-ray diffraction broke above 720 °C and an examination at higher temperatures was impossible.
The molar DC susceptibilities of four different GexFe4−xNy nitrides were measured in the temperature range 2–400 K in field-cooled (FC) and zero-field-cooled (ZFC) modes (Fig. 6(a)–(d)). The course of the susceptibilities suggests that an increase in Fe substitution by Ge leads to FM compounds with decreasing Curie temperatures from above room temperature to about 160 K for Ge0.76Fe3.24N0.44. The nitride with the highest germanium concentration shows a pronounced maximum at low temperatures (ca. 30–40 K for Ge0.97Fe3.03N0.56). Atomic substitution affects the magnetic properties continuously so that intermediate substitutional degrees have broad susceptibility maxima.
We further note that FC and ZFC susceptibilities diverge at low temperatures especially for the lower probing field of B0 = 0.01 T. Such a divergence indicates a collective spin behaviour like spin-glass behaviour, mictomagnetism, superparamagnetism, etc.29 Ge-substituted γ′-Fe4N therefore belongs to the latter class of ternary nitrides mentioned above. This divergence is demonstrated by a nearly constant FC susceptibility value at low temperatures, whereas the ZFC susceptibility increases with increasing temperature, approaching the FC susceptibility. These are characteristic features of a spin glass in which the magnetic moments are figuratively frozen below the spin-freezing temperature in case of a FC measurement; this results in a constant value for the susceptibility. Without a magnetic field, frozen clusters of magnetic moments are orientated anisotropically at low temperatures. In a subsequent ZFC measurement, the energy supplied by increasing temperature enables the alignment of these clusters with respect to the external field to eventually reach magnetic saturation. The energy barrier for rotation can also be overcome by higher external magnetic fields so that FC and ZFC susceptibilities converge already at lower temperatures and the characteristic features of a spin glass can be suppressed (cf. B0 = 0.1 T measurements).
To further investigate the magnetic properties of GexFe4−xNy, hysteretic loops were recorded at 5 K which is below the maximum-susceptibility temperature (Fig. 6(e)). The hysteretic loops have S-shapes and small coercivities. Clearly, the magnetisation decreases with increasing Ge concentration. The hysteretic loop of Ge0.25Fe3.75N0.88 is saturated, whereas those phases with higher Ge concentration only approach the magnetic saturation within the range of the applied field (B0 = ±5 T). This unsaturated behaviour is typical for a magnetically frustrated system because full saturation is never attained in these systems even at the lowest temperatures and highest magnetic fields. Spin glasses lack long-range magnetic order, and the highly degenerate ground state prevents the external field from fully aligning the frozen moments into its directions.29 Nonetheless, the experimental saturated and unsaturated magnetisation at B0 = ±5 T shows a linear behaviour decreasing from 8.96 NAμB for γ′-Fe4N to 0.57 NAμB for Ge0.97Fe3.03N0.56 (Fig. 6(f)). Substituting Fe by Ge atoms obviously weakens the ferromagnetic coupling and even suggests a zero overall magnetisation for daltonide GeFe3Ny when assuming a linear trend over the entire substitutional range. Upon comparing experimental data with theoretical saturation moments, a cubic FM model fits best the range from γ′-Fe4N to Ge0.375Fe3.625N with the slight overestimation going back to the chosen GGA parametrisation. The unsaturated magnetisation of Ge0.97Fe3.03N0.56, however, agrees with a tetragonal FM or even better with an AFM model. This trend was already observed when comparing the experimental lattice parameter to theoretical ones.
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Fig. 7 (a) Energy difference between different AFM spin arrangements (A–G) and the FM ordering in tetragonally distorted GeFe3N. Primitive cells illustrate the different spin arrangements of Fe atoms in which empty and filled circles relate to opposite directions of spins. (b) A cell of GeFe3N with tetragonal distortion (deduced from a cubic 2 × 2 × 2 cell) contains three of these primitive iron sublattices, one undistorted (blue, Fe(4a)) and two distorted (green and orange, Fe(8h)). Note: the B*-type cell is constructed from two B-type sublattices with opposite spin alignments and one A-type sublattice. For a more detailed explanation of the concept see ref. 8. |
Fig. 7(a) shows the comparison of the energies of different AFM spin arrangements using the tetragonal FM model of GeFe3N as a reference. All AFM arrangements differ from each other by less than 6 kJ mol−1 and they even have about the same energy as the FM reference. More precisely, the FM model is more stable than all AFM cells (indicated by positive energy differences) but the amount of less than 2 kJ mol−1 for the D and F models more or less equals the DFT internal accuracy. Thus, the narrow energy distribution reflects the importance of AFM interactions in GexFe4−xNy with high Ge contents despite an overall FM ground state for the idealised composition.
A closer look at the different AFM arrangements A–G shows that the energetically most favourable D- and F-type cells exhibit an equivalent number of both FM and AFM interactions between the neighbouring iron atoms along all spatial directions. In contrast, the highest-energy G-type structure has predominantly AFM interactions, and the A-type cell with mainly FM interactions is also more unstable. It seems that in an AFM ordering neither FM nor AFM interactions alone are preferred, and indeed a well-balanced, or better said, a statistical arrangement of iron spins is favoured. These findings support the idea of a spin-glass behaviour in Ge-rich iron nitrides.
The frequency shift of the temperature Tm, which is particularly important for a magnetic glassy transition, can further be quantified as (ΔTm/Tm) per decade of the angular frequency ω as ΔTm/(Tm·Δlg
ω).29 The shift of Ge0.97Fe3.03N0.56 was estimated to be about 0.012, which falls in the range of known canonical spin glasses (0.005–0.018) and which is also close to the value of Sn0.9Fe3.1N (0.015).12 Both ternary iron nitrides can be distinguished from semiconducting and insulating spin glasses (0.06–0.08) and superparamagnets (0.3).29
All these experimental findings clearly show that the magnetic transition at low temperatures in the DC and real AC susceptibilities arises from a spin-glass freezing of the magnetic moments in the sample so that Ge0.97Fe3.03N0.56 is a canonical spin glass. The reason for the spin-glass behaviour of highly diluted iron nitrides is that FM and AFM exchange interactions of comparable size play important roles, as exemplified from first-principles calculations.
A two-step ammonolytic reaction gave access to GexFe4−xNy. The nitrides adopt an antiperovskite-like structure nearly throughout the compositional range for which the cubic lattice parameter continuously decreases with a Vegard-type behaviour. Only the nitrides richest in Ge have tetragonally distorted structures with, for example, lattice parameters a = 5.2814(7) Å and c = 7.6394(10) Å for Ge0.97Fe3.03N0.56. In experiment, germanium iron nitrides have a limited nitrogen capacity, and the nitrogen content decreases with increasing Ge incorporation for the cubic nitrides; the tetragonal nitrides have a significantly higher nitrogen concentration. Combined high-temperature XRD and TG-DSC experiments evidence that Ge0.97Fe3.03N0.56 is a highly expanding material and it first shows a transition to a cubic structure before it loses its already limited nitrogen.
DC susceptibility and saturation magnetisation of GexFe4−xNy compounds reveal a linear weakening of FM interactions with increasing Ge concentration. Theoretical investigations of different AFM orderings show that neither FM nor AFM Fe spin orientations alone are preferred; instead, a statistical arrangement is favoured. Combined DC and AC magnetometry confirms a magnetically frustrated ground state and a spin-glass behaviour of Ge0.97Fe3.03N0.56. The temperature dependence of the real component of the AC susceptibility at different frequencies classifies Ge0.97Fe3.03N0.56 as a canonical spin glass (Tg = 36.68(5) K, τ* = 10−13.8(2) s, zν = 7.2(1), and ΔTm/(Tm·Δlg
ω) = 0.012) with RKKY indirect-exchange interactions.
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