A Higher Degree of Magnetic Symmetry Induced by Intercalation of Non-Magnetic Na into Quasi-Two-Dimensional Van Der Waals Gapped FeOCl

Abstract

A spiral spin arrangement with a magnetic unit cell 28 times the size of the nuclear one has been reported for Fe spins below T_N = 80 K in bilayered van der Waals gapped FeOCl. In this work, we employ neutron magnetic diffraction and ac magnetic susceptibility to reveal a much smaller magnetic unit cell only 4 times the size of the nuclear one for Fe spins below T_N = 119 K, upon intercalation of 27% non-magnetic Na ions into the van der Waals gaps of FeOCl. X-ray emission spectra and X-ray absorption edge spectra reveal a charge transfer from the intercalated Na ions to the Fe sites, which partially reduces the Fe³⁺ into Fe²⁺ ions. The reduction results in a significantly increased Fe-O-Fe bond angle, which strongly enhances the antiferromagnetic superexchange (AFMSE) coupling relative to the competing ferromagnetic direct exchange (FMDE) coupling between neighboring Fe ions, thereby driving to a higher degree of magnetic symmetry and a substantially higher Neel temperature for the Fe spins in Na_0.27FeOCl.

1. Introduction

Crystallographically layered compounds have recently received considerable attention owing to their distinctive physical properties arising from quasi-two-dimensional (Q2D) nature. The Q2D nature, resulting from the presence of van der Waals crystallographic gaps, renders this class of materials excellent hosts for accommodating guest molecules. Intercalation of organic or inorganic compounds into layered metal oxychlorides MOCl (where M represents Fe, Ti, V, Cr or In) has been extensively reported [1,2,3,4,5,6,7,8,9,10]. It is known that the interaction between the intercalated guest molecules and the inorganic host matrix is governed by charge transfer between them, which results in partial reduction in the matrix [11,12]. A strongly oxidizing host is the key to a stable intercalation, as it provides the driving force for optimal uptake of guest molecules. Among them, iron oxychloride FeOCl is one of the most promising materials for intercalations of a wide variety of molecules owing to its high oxidizing power [13,14,15]. Lithium-ion intercalated FeOCl has been used as a cathode for rechargeable lithium batteries [16,17,18,19].

Until recently, studies made on intercalated FeOCl are mainly focused on the electrochemical properties, but less on the magnetic characteristics. FeOCl crystallizes into an orthorhombic Pmmn symmetry at room temperature [20,21]. Two types of magnetic interactions are present in FeOCl: ferromagnetic (FM) Fe-Fe direct exchange (DE) coupling between the two neighboring Fe ions, and antiferromagnetic (AFM) Fe-O-Fe superexchange (SE) coupling mediated through the O ions located between the two neighboring Fe ions. In addition, the anisotropic Cl-Fe-O network gives rise to distinct magnetic interaction along each of the three crystallographic directions. The competition between the FMDE and AFMSE couplings in this anisotropic network leads to a complex Fe spins arrangement. A three-dimensional long-range ordering of the Fe spins in FeOCl develops below 80 K, forming a spiral magnetic structure that may be characterized by a propagation vector of (2/7, 1/2, 1/2) with respect to the nuclear unit cell [20,21]. Intercalation of 16% polyaniline (C₆H₄NH) into FeOCl reduces the magnetic structure into a two-dimensional one, demonstrating that the appearance of 16% polyaniline in the van der Waals gaps is sufficient to disrupt the interlayer magnetic interactions in FeOCl [21]. In this article, we report on the observations of a charge-transfer-induced Fe spin rearrangement accompanied by a substantial enhancement of the Neel temperature, triggered by intercalation of 27% non-magnetic Na into FeOCl, namely Na_0.27FeOCl, investigated using neutron diffraction, X-ray emission, and ac magnetic susceptibility measurements. Both antiferromagnetic and ferromagnetic couplings are clearly observed in Na_0.27FeOCl, with the Fe spins exhibiting a higher degree of magnetic symmetry than in pristine FeOCl. It is the transfer of electronic charges from the Na ions into the Fe ions that significantly strengthens the AFMSE coupling in Fe-O-Fe chains, leading to a simple antiferromagnetic spin arrangement along the crystallographic a-axis direction and a ferromagnetic arrangement along the crystallographic b-axis direction in Na_0.27FeOCl.

2. Materials and Methods

2.1. Sample Fabrication

The polycrystalline iron-oxychloride FeOCl was prepared by the chemical vapor transport technique [20], employing the following processes: (1) mixing high-purity Fe₂O₃ and FeCl₃ powders with a mole ratio of 1:1.3 thoroughly before sealing in an evacuated glass tube; (2) heating the mixed powder at 380 °C for 48 h, followed by subsequent natural cooling to room temperature over 24 h; (3) washing the resultant product thoroughly using water-free acetone to remove the excess FeCl₃, before drying the wet powder at 60 °C under vacuum for 24 h. The grains in the resultant polycrystalline sample had a lamellar shape. The compound thus obtained was isolated from the atmospheric environment at all times to avoid hydration. Intercalation of Na into FeOCl was achieved by mixing 5.0 g (46.6 mmol) of FeOCl into 100 mL of 3% NaOH solution (75 mmol) in acetonitrile, followed by slow stirring at 120 rpm for 7 days. The shiny black microcrystalline product was then isolated by filtration, washed with acetone, and dried under vacuum.

2.2. Neutron Diffraction

Neutron powder diffraction measurements were conducted at ANSTO, using the cold neutron triple-axis spectrometer SIKA, employing pyrolytic graphite PG(002) crystals at both the monochromator and analyzer positions to select neutrons of wavelength λ = 2.359 Å, with PG filters placed before and after the sample positions to suppress higher-order wavelength contamination. For these measurements, ~10 g of the sample was loaded into a cylindrical vanadium can, which produces no detectable neutron diffraction peak. The sample temperature was controlled using a He-gas closed-cycle refrigerator.

2.3. X-Ray Emission Spectroscopy (XES) and X-Ray Absorption Edge Spectrum (XAS)

The X-ray emission spectrum was conducted at SPring-8, Japan Synchrotron Radiation Research Institite (Harima Science Garden City, Japan), using the Taiwan beamline BL12XU, employing a pair of Si(111) mirrors to define the energy of incident photons, a toroidal mirror to focus the beam into a spot size of 120 (horizontal) × 80 (vertical) μm² at the sample position, and a 1 m bent Si(531) crystal with a solid-state detector to analyze the Fe K_β (3p→1s) emission lines. The high-resolution X-ray absorption edge spectrum (XAS) was performed in the partial fluorescence yield (PFY) mode, by collecting the intensity at the maximum of the main peak of the Fe K_β emission line, when scanning the incident energy across the Fe K edge.

2.4. AC Magnetic Susceptibility

The alternating current (ac) magnetic susceptibility was measured using a Physical Property Measurement System, manufactured by Quantum Design (San Diego, CA, USA), employing the standard set up, with and without the presence of an applied magnetic field H_a. The magnetic response of the compound to the driving ac magnetic field was detected using two identical sensing coils connected in opposition. For these measurements, ~1 g of the sample was loaded into a non-magnetic cylindrical container. A pumped ⁴He cryostat was used to cool the sample and the lowest temperature achieved was 1.8 K.

3. Results

3.1. Crystalline Structure

It is known that FeOCl crystallizes into an orthorhombic Pmmn symmetry at room temperature [21]. The main focus in the structural study for the present Na-intercalated FeOCl is to determine the amount of Na ions that is intercalated into the crystallographic gaps and the changes in the gap separation. The neutron diffraction pattern taken at 130 K was analyzed using the General Structure Analysis System (GSAS) program [22], following the Rietveld profile refining method [23]. The refinements were carried out assuming an orthorhombic symmetry with a space group Pmmn and coherent scattering amplitudes of 0.954, 0.581, 0.958, and 0.363 × 10⁻¹² cm for Fe, O, Cl, and Na, respectively. All atom locations, occupation numbers, and lattice parameters were allowed to vary simultaneously. Figure 1 displays the observed (crosses) and fitted (solid lines) neutron diffraction patterns, taken at 130 K, with their differences plotted at the bottom. Apparently, the observed pattern may be described very well by the proposed orthorhombic Pmmn symmetry. All but Na sites are essentially fully occupied, with a Na composition of 0.27 to locate in the gap at (3/4, 1/4, −0.5870), giving chemical compositions of Na_0.27FeOCl for the compound (

Table 1. Refined structural parameters of Na_0.27FeOCl at 130 K. B_iso represents the isotropic temperature parameter with B_iso = π²<μ²>, where <μ²> is the mean square displacement.

Na0.27FeOCl at 130 K
Orthorhombic Pmmn space group (No. 59, Z = 2)
a = 3.0130(8) Å, b = 3.5605(9) Å, c = 11.351(7) Å
Atom	x	y	z	Multi	Biso (Å2)	Occupancy
Fe	0.75	0.25	0.0940(9)	2b	0.75(5)	1
O	0.25	0.25	−0.0337(7)	2a	0.88(7)	1.00(1)
Cl	0.25	0.25	0.2979(6)	2b	1.33(9)	0.99(2)
Na	0.75	0.25	−0.5870(4)	2b	0.03(1)	0.27(2)
Rp (%) = 22.7, Rwp (%) = 31.2, χ2 = 18.6
			Fe-O-Fe bond angle		Fe-Fe separation
Along a			131.5(5)		3.5526(9) Å
Along b			120.3(5)		3.1621(8) Å

). An axial lattice constant of c = 11.351 Å was obtained for the Na_0.27FeOCl at 130 K, which is 44% longer than the c = 7.9085 Å obtained for FeOCl at room temperature [21]. The crystalline structure of FeOCl may be viewed as a stacking of charge-neutral (Fe₂O₂Cl₂)_n lamellas, while the (Fe₂O₂Cl₂)_n lamellas consist of edge-sharing FeCl₂O₄ octahedrons, forming a bilayered Fe-O-Fe network, as shown in Figure 2. The Na ions connected to the Cl ions appear in the gap.

3.2. Charge Transfer

Two distinct peaks at 7045 and 7060 eV are clearly revealed in the X-ray emission spectra that link to the Fe-K_β line of FeOCl (solid line in Figure 3a) and Na_0.27FeOCl (dashed line in Figure 3a). These spectra were normalized in intensity to their maxima. The Fe-K_β spectral lines of FeOCl and Na_0.27FeOCl are nearly identical, showing that the high-spin state of Fe in FeOCl is retained upon intercalation of Na. The Fe-K_β line is known to be associated with the radiative 3p to 1s decays, following the creations of 1s core holes. Its spectral line shape is a direct result of the superimposition of two multiple groups originating from the exchange interaction between the 3p core-hole and the moment of the open 3d shell [24,25]. The two spectral lines observed correspond to the main K_β1,3 (3p to 1s) line at 7060 eV and the satellite line K_β on the lower photon-energy side at 7045 eV. The energy splitting between these two peaks is given by J × (2S + 1) and their intensity ratio by S/(S + 1), where J is the 3p − 3d exchange integral and S is the total spin of the 3d orbital [26]. The relative intensity and energy of the Fe-K_β structure therefore reflect directly the local magnetic moment. A slightly higher intensity of the satellite K_β line for the Na_0.27FeOCl than for the FeOCl (inset to Figure 3a) reveals that the intercalation of Na into FeOCl transfers charges to the Fe ions from apparently the Na ions. An alternation to the magnetic state of the Fe ions through reduction in the Fe³⁺ ions into Fe²⁺ ions can then be anticipated. A substantial shift in the spectral lines and intensities of the PFY-XAS spectra towards lower photon energies is clearly revealed for the Na-intercalated FeOCl, where both spectral lines of the Fe-K edge of Na_0.27FeOCl appear at slightly but noticeably lower photon energies than those of FeOCl (Figure 3b). The K edge of transition metals is known to contain both structural and electronic information [27]. No structural modification of the FeOCl bilayer was found upon Na intercalation, suggesting that the observed spectral modifications are mainly of electronic origin. The shift in the Fe-K edge spectrum towards lower-photon energies upon Na-intercalation agrees with the reduction in the Fe³⁺ sites expected from the shift in charge from Na sites to Fe sites.

3.3. Magnetic Transition

Direct comparisons between the temperature profiles of the in-phase component χ′ of the ac magnetic susceptibility of Na_0.27FeOCl (open circles) and FeOCl (open triangles) are shown in Figure 4a, where the solid lines indicate the results of fits of the data at high temperatures (>150 K) to Curie–Weiss law χ′ = C/(T − Cλ) where C is the Curies constant that proportional to the conduction electron density, and λ is the Weiss molecular field constant. The main features seen are: (1) a Curie constant of C = 0.144(2) emu-K/g-Oe was obtained from the fits for Na_0.27FeOCl, which is 12 times larger than the C = 0.012(1) emu-K/g-Oe for FeOCl, revealing that the intercalation of 27% Na into FeOCl giving rise to a 12 times increase for the conduction electron density; (2) negative values of λ = −965 g-Oe/emu was obtained for Na_0.27FeOCl and λ = −4500 g-Oe/emu for FeOCl, showing AFM couplings dominating over FM couplings in both compounds; (3) χ′(T) of both Na_0.27FeOCl and FeOCl depart from the Curie–Weiss behavior at low temperatures, indicating the appearance of magnetic correlations that link to the ordering of Fe spins; (4) χ′(T) of Na_0.27FeOCl departs from the Curie–Weiss behavior at T_N = 120 K, which is significantly higher than the T_N = 80 K for FeOCl; (5) the values of χ′ of Na_0.27FeOCl in the paramagnetic state are substantially higher than those of FeOCl at all temperatures studied, showing intercalation of Na gives rise to a higher conduction electron density for Na_0.27FeOCl [28]; (6) a peak appears in the χ′(T) of Na_0.27FeOCl, which shifts to a lower temperature at the appearance of an applied magnetic field (Figure 4b), revealing an antiferromagnetic character for the Fe ions in Na_0.27FeOCl; (7) χ′ of Na_0.27FeOCl and FeOCl increase on further cooling to lower temperatures in the magnetic state, showing the existence of a ferromagnetic component for both compounds. Remarkably, intercalation of 27% non-magnetic Na into FeOCl strongly enhances metallic character and largely strengthens the antiferromagnetic correlations between the Fe ions to increase T_N by as much as 50%.

3.4. Spin Arrangement

At a temperature well above any magnetic ordering temperature, the spins of the unpaired electrons scatter neutrons incoherently, so that the magnetic scattering appears as paramagnetic background in a powder diffraction pattern. When the magnetic correlations develop, as the temperature is reduced, the magnetic scattering develops into magnetic Bragg peaks. Figure 5 shows the magnetic diffraction pattern at 10 K, where the diffraction pattern taken at 130 K, serving as the non-magnetic background, has been subtracted to isolate the magnetic signals. This difference pattern reveals several resolution-limited peaks that developed as the temperature is reduced from 130 to 10 K, originated from the long range ordering of the Fe spins. These magnetic peaks can be indexed, based on the nuclear unit cell, with half-integer Miller’s indices for the basal a-axis and axial c-axis crystallographic directions but an integer for the basal b-axis crystallographic direction, revealing that the magnetic unit cell doubles the nuclear one along the a-axis and c-axis directions, but is the same along the b-axis direction. The spin configuration that fits best to the observed pattern is illustrated in Figure 6. This proposed magnetic structure may be viewed as consisting of ferromagnetic chains along the b-axis direction that are coupled antiferromagnetically along the a-axis direction, with the moments between the neighboring layers are mutually perpendicular. The solid curves in Figure 5 indicate the calculated diffraction pattern based on the proposed magnetic structure shown in Figure 6 with a magnetic moment of <μ_Z> = 3.62(3) μ_B at 10 K for the Fe spins. The calculated pattern agrees reasonably well with the observed one.

Intensities of the (1/2 0 1) (Figure 7a) and (1/2 0 3/2) (Figure 7b) magnetic peaks decrease progressively upon warming. They reveal typical order-parameter curves obtained on powdered samples to see thermal reductions in the magnetic order parameter (grey shaded regions in Figure 7) and intensity fluctuations near transition temperature (yellow shaded regions in Figure 7). It is known that magnetic intensity I_m is proportional to the square of magnetization M. The I_m(T) curve hence measures the thermal variations in the square of the magnetic order parameter M. The solid curves in Figure 7 indicate the results of the fits of the I_m in the grey shaded region to I_m = I_B + I₀{1 − (T/T_N)}^2β, where I_B is the background intensity, I₀ is the saturated magnetic intensity, T_N is the Neel temperature, and β is the critical exponent of the magnetic transition. The T_N and β obtained from the (1/2 0 1) and (1/2 0 3/2) magnetic intensities agree very well, giving T_N = 119(1) K and β = 0.25(4) for Na_0.27FeOCl. The T_N = 119(1) K obtained from magnetic intensities matches very well to the temperature at which χ′(T) departs from the Curie–Weiss behavior (Figure 4a). The T_N = 119(1) K obtained for Na_0.27FeOCl is 50% higher than the T_N = 80 K of FeOCl [21]. Remarkably, an intercalation of 27% non-magnetic Na into the van der Waals gaps of FeOCl largely strengthens the strength of magnetic interaction by as much as 50%. The β = 0.25 obtained for Na_0.27FeOCl is considerably smaller than the β = 0.34 of ferromagnetic Fe, revealing the appearance of a non-ferromagnetic magnetic component in Na_0.27FeOCl and the thermal reduction rate to the magnetic order parameter of AFM Na_0.27FeOCl is even smaller than the pure FM Fe.

4. Discussion

Intercalation reaction of 27% Na into the van der Waals gaps of FeOCl results in a 44% increase in the axial c-axis lattice constant, while no significant change is observed in the a- and b-axis lattice constants. A ferromagnetic Fe-Fe direct exchange coupling, together with an antiferromagnetic Fe-O-Fe superexchange coupling are present in Na_0.27FeOCl [29]. The moment directions of the neighboring spins along the a-axis direction in FeOCl have been found to be 2 × 360°/7 ≈ 102.85° apart [21]. Interaction of 27% Na into FeOCl results in a 27% enlarged Fe-O-Fe bond angle (from 103.5° to 131.5°) together with an 8% longer Fe-Fe separation (from 3.2992 Å to 3.5526 Å) along the a-axis direction, which give rise to a stronger antiferromagnetic coupling so that the neighboring spins along the a-axis direction in Na_0.27FeOCl becoming antiparallel. On the other hand, the Fe-O-Fe bond angle and the Fe-Fe bond length along the b-axis direction are smaller in Na_0.27FeOCl than in FeOCl, which results in a ferromagnetic arrangement of the Fe spins along the b-axis direction. The interbilayer magnetic coupling is dominated by the dipolar interaction, as the neighboring bilayers are bonded via van der Waals interactions. Apparently, the spiral magnetic structure of the Fe spins along the crystallographic a-axis direction in FeOCl reduces to a simple antiferromagnetic arrangement in Na_0.27FeOCl. On the other hand, the spiral three-dimensional magnetic structure for the Fe spins in FeOCl reduces into a two-dimensional one as 16% polyaniline (C₆H₄NH) is intercalated into FeOCl [21].

5. Conclusions

It is known that the magnetic structure of the Fe spins in layered iron oxychloride FeOCl is characterized by a propagation vector of (7/2 1/2 1/2) to reveal a spiral spin arrangement along the crystallographic a-axis direction from the appearance of strong competition between the AFMSE and FMDE couplings in the zig-zag Fe-O-Fe-O-Fe-O chains. Intercalation of Na into the van der Waals gaps provides additional electrons shifted into the Fe-sites, partially reducing the Fe³⁺ into Fe²⁺ that enlarges the Fe-O-Fe bond angle to a stronger AFMSE coupling but a weaker FMDE coupling. Apparently, a 27% Na-intercalation is enough to rearrange the spiral spin arrangement into a simple antiferromagnetic one in the crystallographic a-axis direction, and enhance the Neel temperature from 80 K for FeOCl into 119 K for Na_0.27FeOCl.