Significance
Iron loses its ferromagnetism under pressure, but it retains weaker local magnetic moments without long-range order. Its longitudinal spin fluctuations develop around a “smectic” pattern of alternating magnetic and nonmagnetic bilayers. This unique magnetic state has implications for the cores of small rocky planets and superconductivity in high-pressure iron.
Keywords: iron, high pressure, magnetism, superconductivity
Abstract
Using X-ray emission spectroscopy, we find appreciable local magnetic moments until 30 GPa to 40 GPa in the high-pressure phase of iron; however, no magnetic order is detected with neutron powder diffraction down to 1.8 K, contrary to previous predictions. Our first-principles calculations reveal a “spin-smectic” state lower in energy than previous results. This state forms antiferromagnetic bilayers separated by null spin bilayers, which allows a complete relaxation of the inherent frustration of antiferromagnetism on a hexagonal close-packed lattice. The magnetic bilayers are likely orientationally disordered, owing to the soft interlayer excitations and the near-degeneracy with other smectic phases. This possible lack of long-range correlation agrees with the null results from neutron powder diffraction. An orientationally disordered, spin-smectic state resolves previously perceived contradictions in high-pressure iron and could be integral to explaining its puzzling superconductivity.
Iron is well known since antiquity for its unique magnetic properties and continues to captivate scientists to this day. The study of iron and its alloys has many applications, including steel production and geophysics. Regarding the latter, the application of hydrostatic pressure induces a phase transition from the body-centered cubic (bcc) structure of -iron to the hexagonal close-packed (hcp) structure of -iron (Fig. 1). Iron is being studied at increasingly high pressures and temperatures, since it and its alloys compose the majority of Earth’s core (1). Nonetheless, the relatively low-pressure, low-temperature region of -iron has remained a mystery for decades. The ferromagnetism (fm) found in -iron disappears during the transition (2–4); however, the magnetic state of -iron is controversial. This became increasingly relevant after reports of unconventional superconductivity in this pressure range (5).
Fig. 1.
Schematic phase diagram of iron. The ambient ferromagnetic bcc phase (bcc-fm) is shown in purple. The high-pressure form -iron, which forms an hcp structure, is shown in blue/green for magnetic phases (hcp-m) and white for nonmagnetic phases (hcp-nm). Our calculations predict that the disordered moments (blue) form a spin-smectic state (green) below a critical temperature , which may be related to -iron’s superconductivity ( dome shown).
K X-ray emission spectroscopy (XES) recently found a local magnetic moment (4) in -iron; however, magnetic order is undetected down to 30 mK using Mössbauer spectroscopy (6). Conversely, Raman spectroscopy observes mode splitting until 40 GPa (7), possibly from symmetry breaking by magnetic order. Density functional theory (DFT) calculations have predicted a collinear antiferromagnetic (afm) ground state, afmII, composed of alternating magnetization along the hcp -axis (8) (Fig. 2, Right) which was consistent with null Mössbauer spectroscopy results and Raman mode splitting. However, recent DFT calculations also predict an afmII state in the Fe92Ni8 alloy, but with a substantial hyperfine magnetic field unlike in pure iron, yet synchrotron Mössbauer spectroscopy still detects no magnetism (9). Furthermore, low-temperature Raman spectroscopy discovered that the splitting disappears, contrary to expectations for magnetic order (10).
Fig. 2.
(Left) Orbital-resolved local polarization of the afmII and imIII phase. The occupation number of the majority () and minority () has been computed by integrating the locally projected DoS up to the Fermi level. (Right) Magnetic moment arrangements in the afmII and im phases with the magnetic unit cell shaded in red. White and black arrows are moments belonging, respectively, to the upper and lower -plane, and circles are zero moments.
In this work, we performed K XES with considerably higher statistics, a different analysis technique, and a better pressure transmitting medium than past results (4, 11, 12). We confirmed that -iron has an intrinsic local moment (4) and discovered that it decreases toward zero at 30 GPa to 40 GPa, which is the same pressure range where its superconductivity disappears. We searched for possible ordering of these moments, using neutron powder diffraction (NPD) at record high-pressure and low-temperature conditions (13), and found no magnetic order down to 1.8 K. The upper limit on the magnetic moment for afmII is 5 times smaller than theoretical estimates for the afmII configuration.
We searched for new magnetic phases in -iron using DFT and found spin-intensity-modulated (im) phases (Fig. 2, Right) lower in energy than the afmII phase in the pressure range where local magnetic moments are experimentally detected. We show that spin-intensity modulation is favored by the lattice frustration and the large spin degeneracy of iron sites in the hcp geometry. In order to account for this modulation, we derive an extended Heisenberg model from first principles, where spins are allowed to vary in both direction (transverse fluctuations) and magnitude (longitudinal fluctuations). Below a critical temperature (of about 55 K at 20 GPa), the finite-temperature solution of this model—sampled by classical Monte Carlo (MC)—consists of spatially separated afm bilayers, found also by our DFT calculations at zero temperature (imIII phase). This is a “spin-smectic” arrangement, since the longitudinal fluctuations break the lattice translation symmetry much in the same way a liquid crystal in the smectic phase breaks the translation invariance of a given direction (14). The spin-smectic arrangement perfectly cancels the spin frustration in the hcp afm lattice. While every bilayer is antiferromagnetically ordered, the orientational order between bilayers crucially depends on the spin coupling beyond nearest neighbors. We found the next-nearest-neighbors (interlayer) coupling to drop from 2 meV/ to 0.2 meV/ in the 20- to 35-GPa pressure range. The combined effect of the spin-flip softness due to a progressively weaker interlayer coupling, together with the proximity with other smectic phases, could lead to fluctuations destroying long-range order. This picture is consistent with our XES and neutron powder diffraction results, as well as previous experimental findings.
Intrinsic Magnetic Moment
Hard X-ray photon-in photon-out spectroscopy is well suited to investigate magnetism in 3d transition metal compounds under high pressure (15, 16). In particular, K XES is an established probe of magnetism in iron (4, 11, 12) and iron-based compounds (17–20). K () fluorescence has an intense mainline (K) and a weaker, low-energy satellite region (K), as shown in our spectra in Fig. 3. This splitting is primarily due to the exchange interaction between the core hole and the majority spin of the incomplete shell in the final state (21). Therefore, K spectroscopy probes the unpaired spin occupation, in other words, the spin angular momentum. In the case of iron, this corresponds approximately to the local magnetic moment magnitude, since the orbital angular momentum is essentially quenched.
Fig. 3.
Pressure dependence of K emission spectra of iron. The spectra have been aligned and normalized to the K mainline. All of the spectra measured between 4 K and 583 K are shown, since there is no temperature dependence (see text and Fig. 4 for details). (Inset) Zoom of the K satellite region after subtracting a high-pressure reference and binning the data.
We performed K XES on iron over a large range of pressures (0 GPa to 51.5 GPa) and temperatures (4 K to 583 K) using an argon pressure-transmitting medium. Numerous isothermal runs were performed with a monotonically increasing pressure. The spectra are shown in Fig. 3 after alignment and normalization to the K mainline ( eV). The relative change in satellite intensity is determined by subtracting a polynomial fit of the highest pressure point (51.5 GPa, 300 K) in the K region and integrating the intensity of the resultant difference spectrum (Fig. 3, Inset).
The pressure dependence of the K integrated intensity is shown in Fig. 4. The satellite intensity decline at 15 GPa corresponds to the transition, in agreement with X-ray diffraction (22, 23) and Mössbauer spectroscopy (24) using an argon pressure-transmitting medium. The use of a more hydrostatic pressure-transmitting medium, coupled with increased statistics and a different analysis technique, shows this transition and the intensity after this transition significantly better than previous XES measurements (4). The transition pressure from previous studies, using an argon pressure medium, supports that the signal above 18 GPa is intrinsic to the -iron phase rather than due to a minority -iron phase. The lack of temperature dependence around 20 GPa supports its intrinsic nature, since we would expect a larger K XES signal from more -iron impurities at lower temperatures due to the increased transition width (25). Furthermore, a signal due to exclusively -iron impurities implies unphysical values, e.g., 35% (10%) -iron at 20 GPa (30 GPa). Therefore, we find an intrinsic local magnetic moment in -iron that persists until 30 GPa to 40 GPa. This is, coincidentally, the pressure region above which superconductivity disappears in -iron. The pressure dependence of the magnetic moment from our first-principles calculations shows a remarkable similarity to our results (Fig. 4, Inset): a linear decrease in -iron, a sharp drop across the transition, and, finally, a linear decrease in -iron with a larger slope. Our calculations predict a null moment above 70 GPa, which is at a higher pressure than found by XES measurements; nonetheless, a naive linear mapping of the K integrated intensity to magnetic moment (right scale of Fig. 4) gives 0.74 at 20 GPa, which agrees remarkably well with 0.77 calculated for afmII. This magnetic moment also agrees fairly well with our new spin-im phases discussed below, in particular, imIII, which predicts 0.54 at 20 GPa.
Fig. 4.
Pressure dependence of the K integrated intensity expressed with respect to a high-pressure reference. The right scale is a linear mapping of K intensity to magnetic moment using 2.22 at ambient pressure. The gray dashed lines are guides for the eye. (Inset) Pressure dependence of the average magnetic moment per site found with our DFT calculations. The transition pressure from a tangent construction is shown as a vertical dashed line.
Spin-Smectic State
The ground-state determination of -iron has proven to be a difficult goal, since the hcp frustration for antiferromagnetism produces a broad range of spin arrangements in a narrow energy window (27–29). By means of extensive DFT calculations from first principles at T 0 K, we searched for the lowest energy state by perturbing the afmII spin arrangement, the previous best candidate to describe the -iron magnetic phase. Our main finding is that the modulation of the magnetic moment intensity favors the breaking of the afmII symmetry, as reported in Fig. 5.
Fig. 5.
(Left) Energy vs. volume per atom for the different phases of iron from DFT calculations at T 0 K: fm (bcc only), paramagnetic (pm), afm, im, and noncollinear (ncl); see text for details. The hcp–afmII curve is fitted with a Vinet equation of state (26) to determine the pressure used in Right and shown in Inset. (Right) Energy difference between the im and afmII phases as a function of pressure at T 0 K.
We found 3 different im phases, referred to as imI, imII, and imIII (Fig. 2, Right). The system is more stable when the magnetic moments’ amplitudes are site-dependent—all 3 im phases have a lower energy than afmII from 20 GPa to 60 GPa (Fig. 5, Right). The imIII phase is the most extreme case, with its alternating magnetic and nonmagnetic bilayers, and has a lower energy than afmII at all pressures above the transition. We refer to this distinct arrangement as “spin-smectic,” in analogy with the smectic phase in liquid crystals, since it also breaks lattice translation invariance. This mechanism is driven by magnetic frustration, yielding the imIII phase as the lowest energy state. Indeed, the im spin patterns can be obtained as local minima or saddle points by considering an isolated tetrahedron, the hcp frustration unit (30, 31), and minimizing the energy at fixed absolute magnetization. Another way of lowering the frustration is to develop noncollinear phases, which are expected in -iron (27). We searched for noncollinear phases in our ab initio investigation. The most stable one is reported in Fig. 5 as hcp–ncl and in SI Appendix, Fig. S4. It is still higher in energy than afmII, suggesting that longitudinal smectic fluctuations are the optimal spin arrangement in the frustrated hcp–iron lattice.
In Fig. 2, Left, we compare the local spin polarization of the afmII and imIII phases at 19 GPa (their average local magnetic moment is, instead, reported in Fig. 4, Inset) The homogeneous distribution of spin polarization among the orbitals in imIII signals a very weak crystal-field splitting and a large on-site spin degeneracy. This leads to enhanced spin-intensity modulations dictated by the intersite exchange interaction. Thus, we can map the DFT energies onto a generalized Heisenberg model, where the classical spins are allowed to change in both amplitude and direction (32–34), to account for both transverse and longitudinal spin fluctuations. In this down-folding procedure, we assumed a perfect hcp lattice for the model, since the DFT spin arrangement does not show any anisotropy, due to a nearly ideal hcp ratio.
We find that the afm nearest-neighbor Heisenberg model is able to capture the key DFT features, that is, the instability toward spin-intensity modulated phases, and their ab initio energy ordering () in the 20 GPa to 30 GPa region. However, in order to properly take into account the magnetic itinerancy of the system, we extended this simple model, including local, nearest-neighbor, and next-nearest-neighbor interactions up to the fourth order in the magnetic moment. Our extended model is able to not only capture the energy hierarchy of the DFT collinear and noncollinear phases but also reproduce their average magnetic moment. The fitting procedure and the evolution of the coefficients as a function of pressure are reported in SI Appendix, Fig. S5, Table S1, and section 3.
We investigated the finite-temperature behavior of magnetism in -iron by performing classical MC simulations of our generalized Heisenberg model. We observe a first-order phase transition with the critical temperature dropping from 55 K at 20 GPa to 15 K at 35 GPa. We warn, however, that the computed critical temperature is not to be considered in a stringent quantitative way, due to the open issue of phase space sampling in the case of longitudinal fluctuations (35, 36); however, its pressure dependence yields the predicted scaling behavior (Fig. 1).
For , the system acquires a spin arrangement of imIII type, which consists of antiferromagnetically ordered bilayers, interleaved with null magnetic moment bilayers (Fig. 2 and Fig. 6, Left). This particular smectic pattern completely removes the afm frustration generated by the nearest-neighbors interaction in the hcp lattice, since each spin is left with 4 nonzero neighbors of opposite orientation. We note that the DFT energy is minimized by such an arrangement, supporting the validity of our spin model. Once the smectic order has set in after the transition, the interlayer interaction in the extended Heisenberg model is mediated by the next-nearest-neighbors coupling, whose intensity decreases with pressure faster than . We remark that, in case of a vanishing coupling, the resulting smectic arrangement cannot be detected by neutron scattering, because of its lack of interlayer ordering.
Fig. 6.
(Middle) MC energy per spin as a function of the temperature at GPa. (Left) A representative snapshot of the smectic phase taken at , the ordered bilayers lying on the plane. (Right) A snapshot of the paramagnetic phase at . The temperature ramp has been performed by cooling the system from a disordered state in thermal equilibrium. For each temperature, the canonical distribution has been sampled by proposing lattice updates for each of the 128 random walkers.
Unobserved Static Magnetic Order
We investigated possible magnetic ordering in -iron using neutron powder diffraction. This technique is particularly suited to measuring afm structures, since their supercells imply detecting certain magnetic reflections away from the nuclear reflections and toward lower scattering angles where the magnetic form factor is greatest. Using the techniques described in ref. 13, we measured -iron above 20 GPa and down to 1.8 K. We see a complete transition during a quasi-isothermal pressure ramp to 18.5 GPa, and a slight pressure increase to 20.2 GPa upon cooling to 1.8 K.
The low- range of the diffraction pattern at 20.2 GPa/1.8 K is shown in Fig. 7 as gray error bars. The whole-pattern Rietveld refinement with -iron and diamond is shown as a black line. All of the nuclear reflections in this region are actually weak secondary reflections of the sample and sintered diamond anvils due to contamination (0.2%). The 2 large peaks around and are diamond (111) and (220) secondary reflections. Secondary reflections from -iron are found at (100), (002), (101), (102), and (110). No magnetic peaks are clearly visible in -iron. The difference pattern with a high-temperature reference (18.5 GPa/260 K) is shown as the blue line. There are no hints of magnetic order appearing from 260 K to 1.8 K, and the background features are temperature-independent.
Fig. 7.
Neutron powder diffraction pattern of -iron at 20.2 GPa/1.8 K performed with = 1.3-Å neutrons. The diffraction patterns (gray errors bars) are shown with their Rietveld refinement (black line), where all visible peaks are due to secondary reflections from contamination. The magenta and red ticks indicate reflections from diamond and -iron, respectively. Simulated diffraction patterns are shown for afmII (orange) and imIII (green-blue) using an average magnetic moment per site of 0.15 (solid line) and 0.3 (dashed line). The binned difference pattern with an 18.5 GPa/260 K reference is shown below using the same scale.
We simulated magnetic diffraction patterns for afmII and imIII with the goal of establishing the upper limits of their magnetic moments consistent with the diffraction pattern. The upper limits are expressed as the average ordered magnetic moment per site. For afmII, this corresponds to the same spin intensity at each site; however, for imIII, this corresponds to half the spin intensity of the nonzero sites, since the other sites have zero spin. The upper limit at 20.2 GPa/1.8 K is estimated to be 0.15 for both afmII and imIII, and their simulations are shown as solid colored lines. Simulations with twice the upper limit (0.3 ) are shown as dashed colored lines to give a sense of scale.
The upper limit on the magnetic moment of the afmII phase is 5 times less than 0.77 predicted by DFT. The measurement was performed at 1.8 K, well below the predicted ordering temperature of 75 K at 21 GPa for afmII (9) and 69 K at 16 GPa for an incommensurate afm structure (29). Furthermore, there is no noticeable change with temperature (1.8 K to 260 K) in the diffraction pattern. Therefore, if -iron hosts afmII long-range magnetic order, then its moment is in very strong disagreement with our estimate from both XES and DFT.
The imIII phase is also undetected by NPD and has an upper limit more than 3 times less than 0.54 predicted by DFT. We computed an ordering temperature of 55 K at 20 GPa for the spin-smectic, imIII-like state (Fig. 1 and SI Appendix). Like afmII, our NPD results are also incompatible with a fully ordered imIII state (albeit less so); however, they are compatible with an imIII-like state without interlayer ordering.
Discussion
We have found evidence of local magnetic moments without any long-range magnetic order in -iron. Previous DFT calculations predicted that the afmII configuration is the ground state of -iron (8). Using neutron powder diffraction, we give an upper bound on the afmII moment more than 5 times less than computed with DFT for afmII or estimated from our experimental XES results. These results are consistent with other reports against long-range afmII order (9, 10).
Our DFT calculations found spin-im phases which are lower in energy than the afmII state. Among these, the imIII state achieves the lowest energy by coping with the afm frustration of the hcp lattice with its smectic bilayer structure, where each atom in the afm bilayers is antiferromagnetically coupled to 4 nearest neighbors. DFT—and consequently derived spin models—tends to overestimate spin order in iron-based materials with significant itinerancy (37); therefore, a similar effect is also expected in -iron. Nevertheless, we found that the ferromagnetic interlayer coupling between the afm bilayers weakens rapidly with pressure, leading to stronger spin fluctuations around an imIII-like smectic pattern.
The smectic spin fluctuations which prevent long-range order can also be triggered by the im phases near-degeneracy, in a scenario similar to the one proposed to explain nematicity in FeSe (38). Both scenarios are compatible with our null neutron powder diffraction results. As well, an imIII-like state could be undetectable by Mössbauer spectroscopy if the dynamics of the bilayers is faster than the 100-ns timescale of Mössbauer spectroscopy. Ferromagnetic spin fluctuations are favored by transport measurements which report non-Fermi liquid behavior with dependence in this pressure region (39, 40). Spin fluctuations are also inferred from local-density approximation (LDA) + dynamical mean-field theory (DMFT) calculations due to an underestimation of resistivity, since spatial nonlocal spin correlations cannot be captured within this framework. Moreover, the LDA + DMFT paramagnetic equation of state remarkably matches the experimental one above 40 GPa, but shows an appreciable divergence precisely in the 15- to 40-GPa region (41).
We have shown, with XES, that the local magnetic moment in -iron disappears at 30 GPa to 40 GPa. The temperature below which resistivity measurements find a dependence is known as , and it also approaches zero in this pressure range (40). This is also the pressure where LDA + DMFT infers that spin fluctuations no longer play an important role (41). An anomalous Debye sound velocity, ratio (42), and Mössbauer center shift around 40 GPa have also been reported and were attributed to an electronic topological transition (43). However, X-ray diffraction results recently found no evidence of this electronic topological transition (25), and the most likely origin is the loss of magnetism we find in this study. The disappearance of magnetism around 30 GPa to 40 GPa in -iron means it does not play an important geophysical role on Earth (44); however, it could still play a role on smaller rocky planets such as Mercury and exoplanets. Furthermore, measurements of -iron below 40 GPa should not be extrapolated to higher pressures, due to the effects of magnetism in this low-pressure region. The calculated magnetic moments in imIII only disappear above 70 GPa (Fig. 4, Inset), which is higher than the experimental results discussed above. This discrepancy between experiment and calculations is likely due to the well-known overestimation of magnetic moments when using mean-field calculations such as DFT.
The disappearance of superconductivity (5, 40) coincides with the 30- to 40-GPa region discussed above and warrants speculation about its connection with the spin-smectic state (Fig. 1). The role of spin fluctuations was discussed shortly after the discovery of superconductivity in -iron, because of the failure of conventional phonon-mediated Bardeen–Cooper–Schrieffer theory (45–47). These attempts were quickly abandoned, since they required complicated competition between many interactions and were unable to replicate the relatively small pressure range. We believe that this line of inquiry should be revisited in the context of a spin-smectic state. Furthermore, previous studies used DFT calculations as input which predicts the disappearance of magnetism at higher pressures than we experimentally report here.
Conclusions
We have used K XES to reveal the existence of an intrinsic local magnetic moment in -iron. Our neutron powder diffraction results found no magnetic order and gave upper limits which suggest that the previously proposed ground state, afmII, does not order. Our DFT calculations found spin-im phases lower in energy than the afmII phase. This spin-intensity modulation reduces the effective frustration with a perfect cancellation found in the imIII arrangement, which also is the lowest energy state in the 15- to 35-GPa pressure range. Based on these results, we derived an extended afm Heisenberg Hamiltonian which correctly reproduces the DFT energy and magnetization hierarchy. MC simulations showed that the im-type arrangements survive at low temperature, suggesting that the long-range magnetic order is hampered by spin-smectic fluctuations in the low-temperature range. The spin-smectic state is compatible with our experimental findings but is also particularly elusive to detection. Muon spectroscopy would be very informative, and our results are motivation to push the current pressure limitations of this technique, which are currently an order of magnitude too small (48).
Materials and Methods
Neutron diffraction data of this work are available on the Institut Laue-Langevin DataCite (http://dx.doi.org/10.5291/ILL-DATA.5-31-2443) (49). All other data are available on the CNRS cloud (https://mycore.core-cloud.net/index.php/s/7sMWJtRZ6aqA3nB). XES was performed on GALAXIES at SOLEIL (50, 51) using 1-m Rowland circle in transmission geometry with Si(531) analyzer with a 30 80 beam of 9 keV. The 5-m-thick Fe foils loaded in Rh gasket of DAC with argon and ruby or :Sm2+. NPD was performed (49) on D20 (52) at Institute Laue-Langevin (ILL) using the technique reported in ref. 13. Rietveld refinement and simulations were performed with fullprof (53) using Fe3+ magnetic form factor. DFT used pw.x code of Quantum ESPRESSO (54) in the projector augmented wave scheme (55) with and electrons in valence and using the generalized gradient approximation with the Perdew–Burke–Ernzerhof functional (56). Plane wave (density) cutoff was set to 100 Ry (400 Ry). The Brillouin zone was integrated on mesh (8-atom unit cell) with 0.25-mRy Gaussian broadening. The Vinet equation of state (26) has been used to determine the pressure in the -phase, with the best-fit parameters , GPa, and . MC was used to study our generalized Heisenberg model (SI Appendix). We adopted a multiwalker approach, running 128 independent MC samplings per temperature in parallel, each of them performing lattice sweeps. To assess the convergence of thermodynamical averages, we performed finite-size scaling up to hcp unit cells.
Supplementary Material
Acknowledgments
We are very grateful to T. Strässle for his precious help with NPD experiments and critical reading of this manuscript. We acknowledge G. Morard for lending us an iron foil and a diamond pair, J.-P. Itié for two diamond pairs and advice, and A. Shukla for useful discussions. DFT and MC calculations benefited from computer resources made available by the Grand Équipement National de Calcul Intensif (GENCI) allocation under project no. A0050906493. Beamtime was from SOLEIL (project nos. 20130318 and 20120694) and ILL. B.W.L. and T.G. were supported by the French state funds managed by the Agence Nationale de la Recherche (ANR) within the “Investissements d’Avenir” program under reference ANR-11-IDEX-0004-02, and within the framework of the Cluster of Excellence Materials, Interfaces, Surfaces, Environment (MATISSE) led by Sorbonne Université.
Footnotes
The authors declare no conflict of interest.
This article is a PNAS Direct Submission.
Data deposition: Neutron diffraction data of this work are available on the Institut Laue-Langevin DataCite (http://dx.doi.org/10.5291/ILL-DATA.5-31-2443). All other data are available on the CNRS cloud (https://mycore.core-cloud.net/index.php/s/7sMWJtRZ6aqA3nB).
This article contains supporting information online at www.pnas.org/lookup/suppl/doi:10.1073/pnas.1904575116/-/DCSupplemental.
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