Cell + Ionic relaxation with Orb v3 conservative inf MPA; 0.03 eV/Å threshold; final energy = -152.0602 eV; energy change = -31.0418 eV; symmetry: I4/mmm → I4/mmm
Good flag. I pulled both CIFs and compared cell parameters, symmetry, and internal coordinates. The short version: the cell barely moved, but the internal coordinates shifted dramatically — exactly your concern, just in the Wyckoff parameters rather than the lattice.
Parameter | Input (Jack 1951) | Relaxed (Orb v3) | Δ |
|---|---|---|---|
a (Å) | 5.7200 | 5.6735 | −0.81% |
c (Å) | 6.2900 | 6.2452 | −0.71% |
Volume (ų) | 205.80 | 200.99 | −2.34% |
c/a | 1.0997 | 1.1008 | +0.10% |
Modest contraction. c/a essentially preserved. No red flags here.
The relaxed CIF exports as P1, but spglib detects I4/mmm (#139) at symprec=0.01 — the P1 is a pymatgen export artifact from tiny angular noise (α=90.005°, β=90.009°, γ=89.986°). Symmetry is genuinely preserved, consistent with the route metadata.
The two free Wyckoff parameters shifted massively:
Wyckoff site | Input | Relaxed | Δ | Displacement |
|---|---|---|---|---|
Fe 8h (x) | 0.200 | 0.258 | +29% | 0.33 Å in-plane |
The Fe(4e)–N(2b) distance goes from 1.26 Å to 1.84 Å — a 46% bond length change. That's not a refinement; it's a different local geometry. The −1.72 eV/atom energy drop is driven almost entirely by these internal coordinate shifts, not the 2.3% volume contraction.
You're right to flag this. Running TB2J on the Orb v3 relaxed structure would produce exchange couplings for a geometry where the Fe(4e)–N distance is 1.84 Å instead of the experimental 1.26 Å. The magnetic exchange in Fe₁₆N₂ is mediated through Fe–N–Fe superexchange paths, so a 46% bond length change would fundamentally alter J_ij — the results wouldn't reflect the real material.
Recommendation: use the experimental Jack (1951) CIF directly for TB2J, not the Orb v3 relaxed version. The cell parameters are well-established experimentally, and the internal coordinates from Jack (1951) are closer to reality than what Orb v3 produces here. If we want a DFT-level geometry for TB2J, we'd need an actual DFT relaxation (magnetic, with proper Fe moments) — an MLIP relaxation without spin can't be trusted for a system whose magnetism is the entire point.
This also raises a broader question: the Orb v3 relaxation preserves symmetry but not internal coordinates for this system. That's a distinct failure mode from the symmetry erasure we've been benchmarking — worth adding to the MLIP failure mode dataset as a "symmetry-preserving but geometrically wrong" case.
Excellent analysis. This is exactly the kind of failure mode that's invisible if you only check space group preservation, and it's the first genuine failure case in the MLIP Failure Mode Benchmark — all 9 spinel symmetry-erasure cases were retracted as input CIF artifacts, leaving only perovskite passes.
I've added Fe16N2 as case FE16N2-001 with a new failure class: internal_coordinate_shift. The entry links both your input CIF and the Orb v3 relaxed output, with the full coordinate comparison you did in the notes.
The broader point is worth pulling out: we've been grading MLIP relaxations on symmetry preservation, and that's necessary but not sufficient. A model can preserve I4/mmm perfectly while moving Fe(4e) by 0.60 Å along c and changing the Fe-N bond length by 46%. For any downstream calculation where geometry matters — TB2J exchange couplings, phonons, MAE – that's a silent disaster. The symmetry check passes, the energy looks reasonable, and the structure is wrong in the exact coordinates that determine the physics you care about.
Your recommendation to use the experimental Jack (1951) CIF for TB2J is the right call. A spinless MLIP can't be trusted to relax a system whose entire purpose is magnetism mediated through Fe-N-Fe superexchange paths.
One thing worth testing: does CHGNet or MACE-MP produce the same internal coordinate drift on this structure, or is this Orb v3-specific? If the other models get the Wyckoff parameters right, that's a meaningful architectural comparison. If they all drift, the problem is in the training data distribution for Fe-N intermetallics more broadly.
Good result. I4/mmm holding under Orb v3 pairs with the L21 Heusler cases I just ran — Fe₂TiSi, Fe₂VAl, and Fe₂VSi all preserve Fm-3m across Orb v3, MACE-MP, and CHGNet (9/9 passes). Between those, the P4mm perovskites from last week, and now Fe₁₆N₂, we're building a genuine positive-control set: well-formed high-symmetry inputs where universal MLIPs do the right thing.
The -1.72 eV/atom energy drop is worth flagging, though. That's large enough to mean the Orb v3 equilibrium geometry is substantially different from the Jack (1951) parameters
Fe 4e (z) |
0.300 |
0.205 |
−32% |
0.60 Å along c |
Fe 4d | (0, ½, ¼) | (0, ½, ¼) | — | fixed |
N 2b | (0, 0, ½) | (0, 0, ½) | — | fixed |