Introduction

As an ancient magnet, Fe3O4 has been used as compass with a history about 3000 years1. With more in-depth understanding of Fe3O4, its novel properties including half-metallicity and high Curie temperature of about 860 K have potential applications in spintronic devices2,3. At ambient conditions, the high-temperature phase Fe3O4 has a face-center cubic lattice with a symmetry. As a mixed-valence iron oxide with an inverse spinel lattice, Fe3O4 is formally written as FeA3+ [Fe2+Fe3+]BO44. Two FeB atoms have one spin-down t2g electron in 3d orbits5. Rapid hop of the electron between two neighbor FeB forms the conductive mechanism of Fe3O4.

In 1939, Verwey found that the conductivity of Fe3O4 drops about two orders by cooling down to 125 K6. The lattice symmetry transforms from cubic to monoclinic simultaneously. The first-order approximation given by Verwey is an order-disorder transition of charge distribution at FeB7. The lattice structure of low-temperature phase (LTP) Fe3O4 once puzzled us. Gradually, the lattice structure of LTP Fe3O4 was clarified by X-ray diffraction, Raman and infrared spectroscopy in recent thirty years1,8,9,10,11. Below TV, the lattice is a suppercell of (ac is the cubic lattice constant) with Cc symmetry. The charge ordering has been observed by Magnetic Compton scattering12, resonant multiwave X-ray diffraction13 and selected area electron diffraction14. With the P2/c1,3,15 or Cc space group16,17,18, some theoretical calculations on the charge-orbital distribution give the results that is consistent with the experiments, which describe the ionic distribution, complex charge-orbital ordering pattern and ferroelectricity.

Recently, Senn et al.18,19,20 proposed a new type of quasiparticle named as “trimeron” by both the experimental and theoretical results, where an anomalous shortage of the distance between Fe2+ and Fe3+ appears. The minority-spin t2g electron is delocalized in a polaron that is composed of one Fe2+ donor and two Fe3+ acceptors18,19,20. Owing to the weak interactions, trimeron can be regarded as an orbital molecule, where three Fe ions locally coupled within an orbital ordered solid state. The trimeron model provides a new idea for understanding the Verwey transition. However, the case at a lattice strain may be different. High quality Fe3O4 samples grown on SrTiO321 and Co2TiO422 have been investigated, where the transition temperature shows a significant difference of about 10 K. So the strain may play an important role in the transition of Fe3O4, which should be studied in details.

In perovskite oxides (ABO3), B site is at the center of O octahedra23 and covalently bonding with the nearest O atoms24. Some previous results show that the tilting or rotation of the O-octahedra has an influence on the band gap of perovskite24,25. It is well known that the change of bond angle or bond length modifies the crystal field and band structure. Borisevich et al.25 indicate that the enlarged Fe-O-Fe angle and a higher symmetry can reduce the band gap of BiFeO3. By doping a ion with a larger atomic radium at B-site, Jiang et al. successfully tuned the band gap in CaFeO326.

In order to investigate the strain effect on the charge-orbital ordering and electronic structure of LTP Fe3O4, the first-principles calculations are carried out on LTP Fe3O4 with P2/c and Cc. It is found that the orbital ordering and band structure of LTP Fe3O4 can be tuned by the external strain. The band gap of Fe3O4 with both two symmetries can be changed by a strain with a critical region, where the trimeron shows a complex relation with the external strain.

Calculational Details

The electronic structures of the LTP Fe3O4 with structure (I) P2/c1 and structure (II) Cc19 are calculated by using the potential projector augmented wave method in Vienna Ab initio Simulation Package27,28. The calculations are based on the generalized gradient approximation plus on-site Column interaction (GGA + U)29,30,31. The energy cutoff is 400 eV. The Monkhorst-Pack grid of k-points for structure (I) is 6 × 6 × 2 and that for structure (II) is 3 × 3 × 2. The on-site Column interaction parameter U = 4.5 eV and on-site exchange interaction parameter J = 0.89 eV for all the Fe ions are used in the two structures16. The lattice constants and atomic positions in the two structures are used as that in refs 1 and 19, respectively. The same parameters except for k-points of 3 × 3 × 3 are used to calculate the high-temperature phase (HTP) Fe3O4 with structure (III) symmetry.

The stress is defined by the change of lattice constants as S = (as − a)/a × 100%, where S, a and as represents the strain, lattice constant without and with strain, respectively. Biaxial lattice strain is applied by fixing the in-plane lattice constants (a and b) and relaxing z direction throughout the calculations. The tensile and compressive strains are defined as S > 0 or S < 0. In order to clarify the strain effects on the charge-orbital ordering, the structural optimization for structures (I) and (II) with lattice constants are carried out, where the atomic positions are fully relaxed. Then, the lattice strain is taken into considerations. The structure optimization will stop until the total energy change is less than 10−5 eV and the Hellman–Feynman forces of optimized structure fall below 10−2 eV/Å.

Results and Discussions

Electronic & lattice structure with P2/c symmetry

In Fig. 1, the unique equivalent site of FeB in structure (III) breaks into Fe(B1a), Fe(B1b), Fe(B2a), Fe(B2b), Fe(B3) and Fe(B4) in structure (I) as the symmetry reduces1,3. The coordinate system of monoclinic structure rotates by 135° around z axis3. Figure 2 shows the electronic structure of structure (I) and (III). HTP Fe3O4 shows a half metallic characteristic, where the spin-down states near Fermi level comes from the extra minority electron of FeB t2g orbits2,5. In Fig. 2(b), the band gap of structure (I) is opened by 0.51 eV at Fermi level, which is a bit larger than the spectroscopic 0.14 eV10. Figure 2(c) shows the partial DOS at different FeB sites. The minority electron of FeB is localized at Fe(B1a), Fe(B1b) and Fe(B4), which is consistent with previous results1,3,16. These results suggest that Fe(B1a), Fe(B1b) and Fe(B4) are Fe2+ and Fe(B2a), Fe(B2b) and Fe(B3) are Fe3+. In Table 1, the bond-valence sum (BVS) of FeB is in well agreement with DOS. Herewith, the BVS expression is , where R0 is the bond-valence parameter32. For Fe2+ and Fe3+, R0 is 1.734 and 1.759, respectively. Ri refers to the ith bond length and b is a constant of 0.37 Å32.

Figure 1: The lattice structure of Fe3O4 with P2/c symmetry.
figure 1

The equivalent atom sites of Fe ions have the same color. The monoclinic coordinate is rotated from cubic coordinate around z axis by 135°.

Figure 2
figure 2

The total DOS of Fe3O4 with (a) and (b) P2/c space group. The PDOS of different FeB sites in structure (I) projected on 3d orbits is shown in (c).

Table 1 The BVS calculation results of FeB in structure (I).

In order to investigate the strain effects, the strain of −5%, −2.5%, 0%, +2.5% and +5% are set. In Fig. 3, the orbit of spin-down t2g electron at Fe(B4) (B4t2g↓) is almost in the xy plane at S = −2.5%, 0%, +2.5% and +5%. At S = −5%, the B4t2g↓ orbit shows a different style from others. In Fig. 3(a) and (b), the charge density of B4t2g↓ are projected onto and (110) plan at S = 0% and −5%. At S = 0%, the charge density of B4t2g↓ plotted on both planes shows ellipsoidal shape. At S = −5%, the charge density of the electron plotted on (110) plane still shows ellipsoidal shape, but the charge density plotted on plane shows a flower shape. This phenomena manifests that the B4t2g↓ orbit lies in the plane at S = −5%. In order to figure out the critical strain, the electronic structure is also calculated at S = −3% and −4%. Figure 3(c) shows the B4t2g↓ charge density projected onto (100) plane with a strain from 0% to −5%. The B4t2g↓ orbit still lies in the xy plane until the strain decreases to −5%. Therefore, the compressive strain of −5% is the critical value for P2/c symmetry. Meanwhile, DOS of 3d orbits of Fe(B4) also shows the same change. In Fig. 3(d), at S = −5%, the B4t2g↓ orbit changes from dx2-y2 to dyz + dxz by comparing the DOS at S = 0%. Actually, the B4t2g↓ orbit changes from dxy to dyz in HTP Fe3O4 coordinate system because of the rotation of coordinate3.

Figure 3
figure 3

Charge density of B4t2g↓ plotted on and (110) planes in structure (I) with (a) 0% and (b) −5% lattice strain are shown, respectively. Charge density of B4t2g↓ plotted on (100) plane for 0%, −2.5%, −3%, −4% and −5% lattice strain are showing in (c). The atom shown in white square is Fe (B4). The PDOS of Fe(B4) plotted on 3d orbits with 0% strain (upper panel) and −5% (lower panel) are shown in (d).

Since the conductivity of Fe3O4 is related to FeBt2g↓ and BO6 distortion, it is necessary to investigate the O-octahedral distortion at different FeB sites. In Fig. 4(a), the band gap shows a positive correlation with the increased ΔV except for S = −5%. Herewith, ΔV is the average volume difference between Fe2+O6 and Fe3+O6, Eg is the energy gap near Fermi level. By linear fitting Eg at different strains, we get Eg = 0.946ΔV − 0.651, where Eg at a compressive strain of −5% is not included. Quantitatively, the volume of FeO6 shows the magnitude of its crystal field. Since Fe3+ has a stronger interaction with surrounded O2− than Fe2+, the volume of Fe3+ O6 is smaller than that of Fe2+O6, but the electrostatic potential is higher than that of Fe2+O6. The results mean that the larger volume difference is, the more energy is needed when the electron hopes between Fe2+ and Fe3+. Therefore, as the tensile strain increases, the gap becomes larger. Simultaneously, the competition between the band gap and thermal activation energy has a relation with the metal-insulator transition (MIT) temperature. Therefore, the MIT temperature of Fe3O4 could be tuned by external strain. At a compressive (tensile) strain, the band gap becomes narrow (wide) and the MIT temperature of Fe3O4 becomes lower (higher).

Figure 4
figure 4

(a) The band gap Eg with the average FeO6 volume difference at different strains. (b) The local structure of Fe(B4) under P2/c symmetry. (c) The band structure of structure (I) with −4% and −5% compressive strain in left and right panel, respectively.

However, the above demonstration on the relation between ΔV and Eg is not proper for the case at S = −5%. Therefore, the Fe-O bond length in FeO6 at FeB is further analyzed. Since the charge density of Fe(B4) shows an obvious change and all the Fe(B4) atoms are equivalent with the same ambient ionic conditions, in Fig. 4(b), Fe(B4) at 1c/8 height is selected as a candidate. O(17), O(21), O(25), O(29) and Fe(B4) are almost in horizontal plane and O(2)-Fe(B4)-O(14) is parallel to z axis. Table 2 lists the Fe(B4)-O distances at different strains. In the horizontal plane, at S ≥ −4%, the bond length of Fe(B4)-O(17) and Fe(B4)-O(21) are longer than that of Fe(B4)-O(25) and Fe(B4)-O(29). At S = −5%, the distances Fe(B4)-O(17) and Fe(B4)-O(29) become much longer. The bond lengths of Fe(B4)-O(21) and Fe(B4)-O(25) show an anomalous shortage, but the Fe-O bond length along z direction shows a sudden enlargement. At S = −5%, the length of O(2)-Fe(B4)-O(14) is about 0.15 Å longer than that at S = −4%. The above phenomenon shows that the strain can tune the mode of ionic distribution and crystal field. At a larger strain, the orbital ordering pattern becomes unstable. The outermost 3d electrons of Fe(B4) have a strong Column repulsive interaction with surrounded O2− in horizontal plane. Owing to the change of the distribution of 3d orbits, the electrostatic energy can be partially released along the O(25)-Fe(B4)-O(21) direction. O2− has been pushed away along z direction due to the electronic interaction. The Fe-O bond length distortion in horizontal plane also appears at Fe(B2) and Fe(B3). However, the Fe-O bond lengths at Fe(B1) do not change. Since the inversion centers and partial face centers are occupied by Fe(B1), the symmetry of Fe(B1) is higher than other FeB sites, where the ambience of Fe(B1) is more stable than other FeB sites. Therefore, the mode of ionic distribution does not change at Fe(B1).

Table 2 The bond lengths (Å) between Fe(B4) at 1c/8 and surrounded O2− in structure (I) with the strain changing from +5% to −5%.

In the band structure, the energy of spin-down conduction-band minimum at S = −5% is higher by about 0.28 eV than that at S = −4%. However, in Fig. 4(c), the valence-band maximum of FeB t2g↓ is still just below Fermi level. The compressive strain of −5% can change the structure of O-octahedra at FeB sites. Simultaneously, the Fe-O Column interaction can raise the conduction band energy. So, in Fig. 4(a), the band gap of structure (I) at S = −5% is larger by about 0.28 eV than that at S = −4%.

Furthermore, the nearest six Fe-Fe distances around different FeB sites are analyzed. Unlike Column’s law, the <Fe2+-Fe3+> distance shows an anomalous shortage, which is even less than the <Fe2+-Fe2+> distance at Fe(B1) without strain. The phenomenon is consistent with trimeron model. As the tensile strain is applied, the weak bond interaction between Fe3+-Fe2+-Fe3+ becomes tighter around Fe(B1). When the compressive strain is applied, the trimerons around Fe(B1) become weak. However, the distance between Fe(B4) and Fe(B3) becomes shorter than the Fe2+-Fe2+ distance around Fe(B4). So, a more complex structure of trimeron forms, which will be demonstrated in the next section.

Electronic & lattice structure with Cc symmetry

In Fig. 5, when the symmetry reduces to Cc space group, the LTP Fe3O4 lattice and the charge-orbital ordering pattern become more complex. The electronic structure of bulk without strain is firstly calculated. The band gap near Fermi level with and without structural optimization is about 1.0 and 0.7 eV, respectively. Figure 5(b) shows the total DOS of the optimized structure. The energy gap is larger than experimental result because the calculation is proceeded at 0 K. Then, the strain of −5%, −2.5%, +2.5% and +5% is applied to the Cc structure. Different from P2/c structure, the structure (II) is sensitive to tensile strain. So, we then calculated the electronic properties at S = +3% and +4% to figure out the critical value.

Figure 5
figure 5

(a) The lattice structure under Cc symmetry. (b) Total DOS of structure (II). (c) Charge density map of spin-down electrons plotted on (001) plane at 3c/8 (left column) and 7/8 c (right column) with different strains. Fe(B42) is shown in the white square.

Figure 5(c) shows the spin-down charge density at a height of 3c/8 and 7c/8 as a tensile strain increases from 0% to +5%. At S < +4%, the Fe(B42)t2g↓ orbit [marked with white square in Fig. 5(c)] lies in the (110) plane at 3c/8 and lies in the plane at 7c/8. When the tensile strain exceeds the critical value at S = +4% and +5%, the Fe(B42)t2g↓ orbit rotates into horizontal plane. Figure 5(a) shows the atom sites of Fe(B42), which is labeled in dark blue. In Fig. 6(a), at S = +4% and +5% the DOS of Fe(B42) shows that the orbits of those Fe atoms change from dyz + dxz to dx2-y2. The coordinate of structure (II) also rotates around z axis by 135° from cubic Fe3O4, which is consistent with structure (I). Therefore, the orbit actually changes from dxz to dxy at 3c/8, which changes from dyz to dxy at 7c/8 within cubic coordinate. In the inset of Fig. 6(a), by comparing the DOS at S = +4% and +5%, it is found that although the Fe(B42)t2g↓ orbit changes at S = +4%, it still has the residual states projected onto dyz. The residual states come from the out-of-plane slope of dx2-y2. Then, the relationship between ΔV and Eg in structure (II) is investigated. In Fig. 6, Eg shows a positive relation with the increased ΔV at S < +4%, which can be described as Eg = 0.370ΔV + 0.534. However, the linear fitting parameters both slope and intercept are quite different from structure (I) due to the different structure and charge-orbital ordering pattern.

Figure 6
figure 6

(a) PDOS of Fe(B42) plotted on 3d orbits with a strain of 0%, +4% and +5% at 3c/8 (left panel) and 7c/8 (right panel), respectively. The correspondent local magnifications are shown in the inset. (b) The dependency between the band gap Eg and the corresponding average FeO6 volume difference ΔV with different strains.

Since the orbital change at Fe(B42) is obvious, the Fe-O bond length and O-octahedra distortion at Fe(B42) are taken as an example, where Fe(85) (at 3c/8) is selected as a substitute for other equivalent Fe(B42) sites. Figure 7(a) shows the local structure of Fe(85). The O(77), O(90), O(109), O(122) and Fe(85) atoms are almost in horizontal plane. O(2)-Fe(85)-O(53) is almost parallel to z axis. Table 3 lists the Fe(85)-O bond lengths at different strains, revealing the reason for the orbital change at Fe(B42). The FeO6 distorts in horizontal plane at S = +4% and +5%. The two shortest bonds are along (110) direction and the two longest bonds are perpendicular to (110) direction. When +4% and +5% strain is applied, both the shortest and longest bond are coexistent in diagonals. The Fe-O bond length along z direction suddenly decreases by about 0.1 Å when the strain increases from +3% to +4%. The obvious Fe-O bond length distortion in xy plane also appears at Fe(B2b1), Fe(B31), Fe(B32), Fe(B34), Fe(B41), Fe(B43) and Fe(B44). Due to the tensile strain, the expansion of the equatorial plane of O-octahedra can release the electrostatic energy between the surrounded O2− and outside electron of Fe2+. Correspondingly, the Column interaction along z direction can also be weakened by the transformation of Fe(B42)t2g↓ orbit, so the Fe-O bond length along z direction becomes shorter. Since the equatorial face can further expansion at S = +5%, more electrostatic energy can be released, where the Fe(B42)t2g↓ orbit becomes more parallel to the xy plane. In the inset of Fig. 6(a), at S = +5%, the residual dyz states are less than that at S = +4%. In Fig. 7(b), the conduction-band minimum at S = +4% is lower than that at S = +3%, where the valence-band maximum is still just below Fermi level. As a result, the band gap becomes smaller as the strain increases.

Figure 7
figure 7

(a) The local structure of Fe(B42) under Cc symmetry. (b) The band structure under Cc symmetry with +3% and +4% compressive strain in left and right panel, respectively.

Table 3 The nearest Fe-O bond lengths at Fe(85) with different stresses in structure (II).

Furthermore, the model of trimeron presented by Senn et al.18,19,20 is also observed in our calculations. It is found that the distribution of trimeron can be affected by external strain. When the strain increases from 0% to +5%, the Fe-Fe distance along x and y axis changes faster than that along the face diagonal direction of FeB4O4. The Fe-Fe distance along diagonal direction even reduces with the increased strain at some FeB sites. The process of FeB4O4 distortion is compared with an ideal model of equivalent volume deformation in tetragonal system. Figure 8 shows the sketch map of this ideal model, where a, h and l each respect the in-plane, out-of plane crystal edges and face diagonal. Lattice with tensile and compressive strain are superscripted with and ′′, respectively. The volume of this tetragonal V = a2h, so h = V/a2 and the face diagonal . The different coefficient of l with respect to a is . At 0 < a < 3.367, . In our model, the case of 0 < a < 3 is considered. As a result, the length of face diagonal reduces with the increased lattice constant. So, the trimerons along x and y direction break down by the tensile strain, but the correlation of trimerons along the face diagonal are strengthened. When a compressive strain is applied, the Fe-Fe distance along x and y direction becomes short and the Fe-Fe distance along face diagonal elongates. The trimerons along x and y direction are strengthened, but the trimerons along the face diagonal directions break down due to the compressive strain.

Figure 8: The sketch map shows the ideal model of deformation with equivalent volume.
figure 8

The FeB4O4 models without strain, with tensile or compressive strain are colored with blue, grey and orange, respectively. a, h and l each respects the in plane, out of plane direction Fe-O bond length and the Fe-Fe distance along face diagonal direction. The length of a′ and a″ is (1 + 6%)a and (1 − 6%)a, respectively. The ratio of a, a′ and a″ is correspondent with the calculation results. The local structure of FeB4O4 is also shown in the lower right corner.

Conclusions

We have investigated the biaxial strain effects on the electronic structure of LTP Fe3O4 with P2/c and Cc space group by GGA + U method. When the strain on the two structures are below their critical region, the distortion of O-octahedra can change the electrical potential difference between the nearest ferric and ferrous ions. As a result, the band gap shows a positive linear correlation with the strain. The narrower or wider band gap implies a lower or higher transition temperature. When the strain is above the critical value namely S < −4% in structure (I), the orbit of Fe(B4)t2g↓ changes from dxy to dyz in HTP Fe3O4 coordinate and the energy of conduction-band minimum raises. In structure (II), at S ≥ +4%, the orbit of Fe(B42)t2g↓ changes from dyz to dxy in HTP Fe3O4 coordinate and the energy of conduction-band minimum reduces. The trimeron appears in both the structure (I) and (II). The distribution of trimeron can also be affected by strain. The trimerons along x and y axes get broken (strengthen) at a tensile (compressive) strain. However, the trimerons along face diagonal are broken (strengthened) at a compressive (tensile) strain. These results can be ascribed to the change of Fe-Fe distance when different strains are applied, which can be estimated by geometric calculations.

Additional Information

How to cite this article: Liu, X. et al. Biaxial strain effect induced electronic structure alternation and trimeron recombination in Fe3O4. Sci. Rep. 7, 43403; doi: 10.1038/srep43403 (2017).

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