Antiferromagnetism and the emergence of frustration in saw-tooth lattice chalcogenide olivines Mn$_2$SiS$_{4-x}$Se$_x$ ($x$ = 0 $\textendash$ 4)
H. Nhalil, R. Baral, B. O. Khamala, A. Cosio, S. R. Singamaneni, M., Fitta, D. Antonio, K. Gofryk, R. R. Zope, T. Baruah, B. Saparov, and H. S., Nair

TL;DR
This study investigates the magnetic properties of Mn-based olivine chalcogenides with a saw-tooth lattice, revealing antiferromagnetic behavior, spin fluctuations, and a transition from long-range to short-range magnetic order as selenium content increases.
Contribution
It provides detailed experimental and theoretical analysis of how selenium substitution affects magnetism and electronic structure in Mn$_2$SiS$_{4-x}$Se$_x$, highlighting the emergence of frustration and short-range order.
Findings
Transition temperature decreases with Se-content from 86K to 66K.
Presence of magnetic anomalies and irreversibilities at low temperatures.
Density functional theory indicates antiferromagnetic ground state with ferromagnetic in-plane coupling.
Abstract
The magnetism in the saw-tooth lattice of Mn in the olivine chalcogenides, MnSiSSe ( = 14) is studied in detail by analyzing their magnetization, specific heat and thermal conductivity properties and complemented with density functional theory calculations. The air-stable chalcogenides are antiferromagnets and show a linear trend in the transition temperature, as a function of Se-content () which shows a decrease from 86~K for {\mss} to 66~K for {\msse}. Additional new magnetic anomalies are revealed at low temperatures for all the compositions. Magnetization irreversibilities are also observed as a function of . The specific heat and the magnetic entropy indicate the presence of short-range spin fluctuations in MnSiSSe. A spin-flop antiferromagnetic phase transition in the presence of applied magnetic field is…
| (Å) | (Å) | ||||
|---|---|---|---|---|---|
| Mn2SiS4 | 12.692(9) | 7.435(3) | 5.941(3) | 3.94 | 2.89 |
| Mn2SiS3Se | 12.860(1) | 7.527(4) | 6.009(8) | 2.48 | 1.23 |
| Mn2SiS2Se2 | 13.000(3) | 7.605(6) | 6.076(5) | 2.31 | 1.42 |
| Mn2SiSSe3 | 13.150(8) | 7.690(9) | 6.156(1) | 1.78 | 1.35 |
| Mn2SiSe4 | 13.302(8) | 7.777(2) | 6.243(6) | 1.97 | 1.4 |
| (K) | (K) | (K) | (/Mn) | (K) | |||||
|---|---|---|---|---|---|---|---|---|---|
| Mn2SiS4 | 83.7 | 11.7 | 4.0(3) | 226 | 2.7 | 0.36 | 0.05 | ||
| Mn2SiS3Se | 81.9 | 11.7 | 4.07(2) | 221 | 2.7 | 0.36 | 0.05 | ||
| Mn2SiS2Se2 | 77.7 | 19 | 5 | 3.95(5) | 219 | 2.8 | 0.35 | 0.08 | 0.02 |
| Mn2SiSSe3 | 71.7 | 17 | 3.8 | 3.8(2) | 193 | 2.7 | 0.36 | 0.08 | 0.02 |
| Mn2SiSe4 | 65.5 | 13.7 | 5.9(4) | 336 | 5.2 | 0.19 | 0.04 |
| Composition | (eV) | (Å) | (Å) | /Mn () | /Mn () | (eV) |
| Mn2SiS4 | 0.0 | 12.46, 7.27, 5.87 | 12.69, 7.44, 5.94 | 4.04, -4.05 | 4.0 | 0.47 |
| 0.40 | 12.69, 7.44, 5.94 | 4.12, -4.16 | 0.64 | |||
| Mn2SiS3Se (a) | 0.34 | 12.726, 7.320, 5.892 | 12.860, 7.527, 6.009 | 4.03, -4.03 | 4.07 | |
| Mn2SiS3Se (b) | 0.35 | 12.530, 7.315, 6.013 | 4.04, -4.04 | 0.40 | ||
| Mn2SiS3Se (1) | 0.0 | 12.59, 7.35, 5.91 | 4.02, -4.02 | 0.32 | ||
| Mn2SiS3Se (2) | 0.02 | 12.583, 7.335, 5.942 | 4.02, -4.03 | |||
| Mn2SiS3Se (3) | 0.12 | 12.590, 7.34, 5.96 | 4.04, -4.02 | |||
| Mn2SiS3Se (4) | 0.10 | 12.603, 7.338, 5.915 | 4.02, -4.03 | |||
| Mn2SiS2Se2 | 0.0 | 12.538, 7.432, 5.893 | 13.00, 7.61, 6.08 | 3.97, -3.97 | 3.95 | |
| Mn2SiSSe3 | 0.0 | 12.75, 7.45, 5.92 | 13.150, 7.690, 6.156 | 3.92, -3.92 | 3.8 | 0.1 |
| Mn2SiSe4 | 0.0 | 13.30, 7.78, 6.24 | 4.12, -4.12 | 5.9 | 0.45 |
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Taxonomy
TopicsCrystal Structures and Properties · Iron-based superconductors research · Phase-change materials and chalcogenides
Antiferromagnetism and the emergence of frustration in saw-tooth lattice chalcogenide olivines Mn2SiS4-xSex ( = 0 4)
H. Nhalil
Department of Chemistry and Biochemistry, University of Oklahoma, 101 Stephenson Parkway, Norman, OK 73019, USA
R. Baral
Department of Physics, 500 W University Ave, University of Texas at El Paso, El Paso, TX 79968, USA
B. O. Khamala
Department of Physics, 500 W University Ave, University of Texas at El Paso, El Paso, TX 79968, USA
A. Cosio
Department of Physics, 500 W University Ave, University of Texas at El Paso, El Paso, TX 79968, USA
S. R. Singamaneni
Department of Physics, 500 W University Ave, University of Texas at El Paso, El Paso, TX 79968, USA
M. Fitta
The Henryk Niewodniczański Institute of Nuclear Physics -PAN, Department of Magnetic Materials and Nanostructures, ul. Radzikowskiego 152, 31-342 Kraków, Poland
D. Antonio
Idaho National Laboratory, Idaho Falls, ID 83415, USA
K. Gofryk
Idaho National Laboratory, Idaho Falls, ID 83415, USA
R. R. Zope
Department of Physics, 500 W University Ave, University of Texas at El Paso, El Paso, TX 79968, USA
T. Baruah
Department of Physics, 500 W University Ave, University of Texas at El Paso, El Paso, TX 79968, USA
B. Saparov
Department of Chemistry and Biochemistry, University of Oklahoma, 101 Stephenson Parkway, Norman, OK 73019, USA
H. S. Nair
Department of Physics, 500 W University Ave, University of Texas at El Paso, El Paso, TX 79968, USA
Abstract
The magnetism in the saw-tooth lattice of Mn in the olivine chalcogenides, Mn2SiS4-xSex ( = 14) is studied in detail by analyzing their magnetization, specific heat and thermal conductivity properties and complemented with density functional theory calculations. The air-stable chalcogenides are antiferromagnets and show a linear trend in the transition temperature, as a function of Se-content () which shows a decrease from 86 K for Mn2SiS4 to 66 K for Mn2SiSe4. Additional new magnetic anomalies are revealed at low temperatures for all the compositions. Magnetization irreversibilities are also observed as a function of . The specific heat and the magnetic entropy indicate the presence of short-range spin fluctuations in Mn2SiS4-xSex. A spin-flop antiferromagnetic phase transition in the presence of applied magnetic field is present in Mn2SiS4-xSex, where the critical field for the spin flop increases from = 0 towards 4 in a non-linear fashion. Density functional theory calculations show that an overall antiferromagnetic structure with ferromagnetic coupling of the spins in the -plane minimizes the total energy. The band structures calculated for Mn2SiS4 and Mn2SiSe4 reveal features near the band edges similar to those reported for Fe-based olivines suggested as thermoelectrics; however the experimentally determined thermal transport data do not support superior thermoelectric features. The transition from long-range magnetic order in Mn2SiS4 to short-range order and spin fluctuations in Mn2SiSe4 is explained using the variation of the Mn-Mn distances in the triangle units that constitutes the saw-tooth lattice upon progressive replacement of sulphur with selenium.
I introduction
Complex magnetic excitations from frustrated lattices of magnetic atoms is an attractive topic in quantum correlated systems. The saw-tooth antiferromagnetic chain has a frustrated topology of corner-sharing triangles of spins where the ground state of the spin-half saw-tooth chain is understood exactly Kubo (1993); Sen et al. (1996); Nakamura (1996). Variety of ground states are predicted for the saw-tooth lattice depending on the ratio of the exchange interaction strengths between the base-base and the base-vertex pairs Blundell and Núñez-Regueiro (2003); Ohanyan (2009); Bellucci and Ohanyan (2010); Hao et al. (2011); Chandra and Sen (2004). The saw-tooth systems attain importance in connection with the zero energy flat-band modes similar to the case of Kagome lattices Zhitomirsky (2004, 2005) and are valuable as potential materials for magnonics Wang et al. (2018). Experimental studies on saw-tooth lattices are limited in number; some examples are the delafossites, olivine and germanates Cava (1993); Le Bacq (2005); Lau (2006); White et al. (2012). In this connection, chalcogenide olivines have received less attention regarding the magnetism and magnetic excitations arising from their underlying saw-tooth lattice. The ( = Mn, Fe, Ni; = Si, Ge; = S, Se, Te, O) olivines, where the atoms form a saw-tooth lattice, are well-known semiconducting magnetic compounds which find applications in optoelectronics and magentic devices Fredrick and Prieto (2013); Furdyna and Kossut (1988). They have been recently computationally projected as suitable thermoelectric candidates owing to peculiar band structure features Gudelli et al. (2015). They crystallize in orthorhombic space group and have relatively small tetrahedral ions () and large octahedral ions (). Olivines have a spinel-like structure but uses one quadravalent and two divalent cations instead of two trivalent and one divalent cations. The sites consist of the two crystallographically independent sites ( and sites) and form a triangle-based saw-tooth chain structure through the edge-sharing bonds along the -axisHagemann et al. (2000). Due to this structural feature, the -site lattice is geometrically magnetically frustrated when it is occupied by magnetic ions Hagemann et al. (2000). The end-compounds of Mn2SiS4-xSex Mn2SiS4 and Mn2SiSe4 order antiferromagnetically below their Neél temperature, 83 K and 66 K, respectively Ohgushi and Ueda (2005); Lamarche et al. (1994a); Jobic et al. (1995); Bodenan et al. (1996). Mn2SiS4 belongs to the class of anisotropic uniaxial antiferromagnets but with anomalous magnetic features near the spin-flop transition Ohgushi and Ueda (2005). A weak ferromagnetic interaction exists in a narrow temperature window between 83 K and 86 K, while displaying uniaxial anisotropy with the -direction as the easy axis. The origin of weak ferromagnetism (WF) and the unusual temperature dependence of spin-flop critical field is unclear in olivines despite the microscopic origin of WF which is supported by neutron scattering experiments Lamarche et al. (1994b). At 4.2 K a collinear ferromagnetic arrangement of the Mn spins at the two distinct crystallographic positions, (a site with inversion) and (mirror), was observed along the axis. As the temperature increases to 83 K, the orientation of the spins turns in the plane. At 83 K, both the and the spins reorient along the axis but with some canting in the plane. It is in the very small temperature range of 8386 K, spins at two different crystallographic positions display weak ferromagnetism. The paramagnetic to antiferromagnetic transition has been identified as belonging to the Heisenberg universality class and the weak ferromagnetic transition as first order with a latent heat 0.01 J/mol Junod et al. (1995). A very low value of magnetic entropy, about 5 of ln(2 + 1), is found to be released at the antiferromagnetic transition, indicating that the spin entropy is not completely removed at the . Experimental support for the short-range spin fluctuations come from the fact that purely magnetic intensity was observed in neutron diffraction data up to 140 K Lamarche et al. (1994b).
On the other end of the composition series of Mn2SiS4-xSex is the case of Mn2SiSe4, which has the magnetic easy axis along crystallographic -direction of the orthorhombic cell Bodenan et al. (1996). In the case of Mn2SiSe4, the average magnetic structure remains in a configuration intermediate to a ferrimagnet and an antiferromagent for most of the region. Though both Mn2SiS4 and Mn2SiSe4 are reported to show similar magnitude of magnetization, Mn2SiSe4 displays pronounced field and temperature cycling dependencies in magnetic susceptibility Bodenan et al. (1996). The temperature range spanned by the magnetization maximum (between 66 K and 17 K, almost 50 K) is much wider compared to that of Mn2SiS4 (between 86 K and 83 K, approximately 3 K) Jobic et al. (1995); Bodenan et al. (1996). The broadness of the transition in magnetic susceptibility of Mn2SiSe4 and the hysteresis-like effects already suggests strongly competing interactions leading to a frustrated magnetic state. An interesting aspect of the olivines that has recently received attention is related to thermoelectricity. Quasi-flat band edges near the valence and conduction bands were predicted using density functional theory calculations in the case of Fe2Ga ( = S, Se, Te) Gudelli et al. (2015). This theoretical investigation was preceded by experiments that showed nano-structured Fe2GeS4 is a photovoltaic material Park et al. (2015); Fredrick and Prieto (2013). Experimental studies have shown that Fe2SiS4 and Fe2GeS4 possess significant thermopower Platt (2010).
In the present paper we undertake a detailed experimental study of magnetism in Mn2SiS4-xSex. Our research is motivated by the prospect of understanding the role of magnetic frustration in the saw-tooth lattice of Mn in the series of olivines as the transition metal environment is altered from sulfur-rich to selenium-rich. A detailed magnetic and thermal property investigation of Mn2SiS4-xSex ( = 0, 1, 2, 3, 4) solid solutions is undertaken and is complemented with density functional theory calculations.
II Methods
II.1 Experimental techniques
Elemental Mn, Si, S and Se (99.99, Aldrich) were used as reactants to synthesize Mn2SiS4-xSex, = 04. Stoichiometric amount of these elements were weighed and mixed properly using a mortar and pestle before pelleting and loading into a 10 mm diameter quartz ampule in a N2-filled glove box. The quartz tubes were flame-sealed under a dynamic vacuum with pressure less than 10*-3* mTorr. The reaction mixtures were heated at 1000*∘C for 24 hours then cooled to room temperature at a rate of 100∘C/h. To improve the phase purity and crystallinity, samples were re-ground, pelleted and annealed under identical conditions as necessary. Room temperature powder X-ray diffraction (PXRD) measurements were performed on a Rigaku MiniFlex600 instrument with a D/tex detector using a Ni-filtered Cu- radiation (: 1.540562 ; : 1.544398 ). X-ray data collection experiments were performed at room temperature in the 10-70∘* (2) range, with a step size of 0.02*∘. Data analysis was performed using Rigaku PDXL software package. The collected data were fitted using the decomposition method (Pawley fitting) embedded in the PDXL package. For air stability studies, powder samples of all three compositions were left in ambient air for a period of 6 weeks. PXRD measurements were regularly performed during this period using the conditions described above. The specific heat, , of the samples were measured using the heat pulse method in a commercial VersaLab, Physical Property Measurement System from Quantum Design. Tiny pellets of Mn2SiS4-xSex* of mass approximately 2-3 mg were used for the measurements. The sample was attached to the calorimeter puck using N Apiezon grease. The was measured in the temperature range 50 K300 K under 0 T and 3 T. The temperature and field-dependent magnetization measurements were performed in a SQUID Magnetic Property Measurement System. DC magnetization was measured in the temperature range 2300 K and isothermal magnetization at 2 K in the range 7 T to 7 T. The thermal conductivity was measured using the TTO option in a commercial DynaCool-9, Physical Property Measurement System from Quantum Design.
II.2 Computational methods
The density functional theory (DFT) calculations were carried out using the Vienna ab initio simulation package (VASP) Kresse and Hafner (1993); Furthmüller et al. (1994); Kresse and Furthmüller (1996a, b). The projector augmented wave (PAW) method was utilized for the electron-ion interaction Blöchl (1994); Kresse and Joubert (1999); Blöchl et al. (2003) with an energy cutoff of 470 eV for the plane-wave basis functions. The generalized gradient approximation to exchange-correlation functional by Perdew, Burke, and Ernzhofer Perdew et al. (1996) was used. A -centered (444) -point grid based on Monkhorst-Pack scheme Monkhorst and Pack (1976) was employed for initial structure optimization and later a finer grid of 61113 was used for further refinement. We have relaxed the structures until the Hellmann-Feynman forces on the ions were lower than 0.04 eV/Å. An initial spin moment of 5 to Mn ions were assigned and the spin moment was allowed to relax. We also used VESTA Momma and Izumi (2011) software package for generating the crystal structures.
III Results and Discussion
III.1 X ray diffraction and air stability
Powder X-ray diffraction (PXRD) patterns along with the Pawley fitting of Mn2SiS4-xSex ( = 04) compounds measured at room temperature are shown in Fig 2. The results of the structural analysis of the PXRD patterns are summarized in Table (1). All samples crystallize in the orthorhombic space group ( 62). The compounds, Mn2SiS3Se ( = 1), Mn2SiS2Se2 ( = 2), and Mn2SiSe4 ( = 4) were obtained as pure phase samples, whereas the Mn2SiS4 ( = 0) and Mn2SiSSe3 ( = 3) samples contained minor impurity phase of MnS quantified to be less than 2 wt.
Air stability of Mn2SiS4-xSex is very important feature while considering use in practical device applications. Being a non-oxide, many chalcogenide based materials are prone to degradation upon exposure to air and moisture Choudhury et al. (2007); Flanagan and Shim (2015); de Kergommeaux et al. (2012). Air stability of Mn2SiS4-xSex compounds were investigated for over a period of 6 weeks by keeping the powder sample exposed to the ambient atmosphere. PXRD was collected regularly during this period and analyzed. PXRD patterns of the as-synthesized samples and those of the samples after exposure to air for 6 weeks showed no appreciable differences (not shown). After 6-weeks exposure to air, no additional peaks or peak broadening was observed in any of the five compositions. We confirm that Mn2SiSe4 series have good air stability thereby establishing their potential for use in practical applications.
The important structural feature of the Mn2SiS4-xSex compounds from the perspective of magnetism is the saw-tooth like triangular arrangement of Mn lattice.Hagemann et al. (2000) Such a lattice forms the basis for a frustrated lattice depending on the different bond lengths or the exchange parameters related to the triangular motif building up the saw tooth. Mn has two crystallographically distinct positions in this structure, viz., and where there are four magnetic ions per cell with inversion symmetry and mirror symmetry respectively. Previous neutron powder diffraction studies on the = 0 compound in the temperature range 4.2 K300 K have shown that there is no structural change in the temperature range mentioned above. For all the Mn2SiS4-xSex compounds, we assume the olivine structure in the entire temperature range employed in the present study. The refined lattice parameters that we obtain in the present study for Mn2SiSe4 match well with the earlier report on the crystal structure.Fuhrmann and Pickardt (1989) Incidentally, a structural peculiarity that the Mn(1) octahedra being less distorted than the Mn(2) octahedra was mentioned in Ref[Fuhrmann and Pickardt, 1989]. Similarly the lattice parameters obtained for Mn2SiSe4 series in the present work also matches well with the reported values.Jobic et al. (1995)
III.2 Specific heat
The experimentally measured specific heat of Mn2SiS4-xSex ( = 04) are presented in Fig 3 (a) where the specific heat under 0 T and 3 T are plotted together. The parent composition, Mn2SiS4 reproduces the antiferromagnetic phase transition at 84 KOhgushi and Ueda (2005, 2006, 2007); Junod et al. (1995) which characterizes the paramagnetic-to- antiferromagnetic phase transition. It is reported that in the temperature range 83 K86 K, Mn2SiS4 displays WF; further, below 83 K it is an antiferromagnet. From the present data of Mn2SiS4, we identify the AF transition at 86.2 K by taking the derivative, . The WF transition reported at 83 K is less-conspicuous in our derivative plot (not shown). Under the application of 3 T magnetic field, no changes to the peak at is noticeable for any of the compositions = 0 to 4. This points towards strong AF nature of the underlying spin structure, up to atleast 3 T. Upon substituting S with Se, the transition temperature decreases from 86 K for = 0 to 66 K for = 4, Mn2SiSe4. The evolution of the as a function of is presented in the inset (b) of Fig 3.
In order to account for the phonon part of the specific heat of Mn2SiS4-xSex, an Einstein model-based curve fit was administered to the . Such a fit is demonstrated in Fig 3 (b) for the case of Mn2SiS4. In (b), the solid line represents the fit using the following expression:
[TABLE]
where, = and is the weight factor for each mode. The specific heat data in the temperature range, was used for the fit. We obtain the Einstein temperatures as = 744 K and = 128 K. The lattice part of the specific heat thus obtained was subtracted from the total specific heat to obtain the magnetic part, which is plotted in the inset of Fig 3 (a) for all the compositions of Mn2SiS4-xSex. The magnetic entropy, = is calculated and plotted in the inset of Fig 3 (b) for = 04. Though the Mn2SiS4-xSex compounds undergo a PM-AF second order phase transition, it can be seen that significantly low magnetic entropy is released at the . The Mn2+ with spin = 5/2 contributes ln(6) = 14.8 J/mol-K towards spin entropy. In the case of Mn2SiS4, only 14 of this value is released at the . This, in turn, suggests that the Mn2+ spins of Mn2SiS4-xSex, which form a two-dimensional saw-tooth-like triangular arrangement are indeed in a frustrated magnetic state. Hence significant short-range magnetic order is expected to coexist along with the prominent AF order. It is noted here that the specific heat analysis that we have performed is on the data limited to only 50 K. Hence a comprehensive estimation of the lattice specific heat including a Debye term and extending down to low temperature was not possible. This would have resulted in a deviation in the values of presented here. However, we obtain supporting values from the earlier reports on the specific heat analysis and magnetic entropy determination of Mn2SiS4.Junod et al. (1995)
III.3 Magnetization
The dc magnetic susceptibility, , of the Mn2SiSe4 series measured in an applied magnetic field of 500 Oe are presented in Fig 4 for = 0, 1, 4 in panel (a) and = 2, 3 in (b). Though the phase transition temperatures () identified in the specific heat data are reflected in magnetic susceptibility as well, a significant difference in the magnitude of magnetic susceptibility is observed for the two sets of compositions in the panels (a) and (b). The magnetic phase transition in the case of Mn2SiS4 occurs as a sharp anomalous peak at = 83.7 K and matches with the reported value. Junod et al. (1995); Lamarche et al. (1994b) Upon progressive replacement of S with Se, the peak at the phase transition is weakened, and eventually for Mn2SiSe4 a very broad feature is seen below 65 K. This observation also matches with the previous report of the magnetic behaviour of Mn2SiSe4.Jobic et al. (1995)
The inset of (a) shows the values estimated from the data by taking the derivative, d/dT. The derivative, as a function of temperature for = 04 are presented in the panels (c) to (g). The magnetic transition temperatures, s, thus estimated through the derivatives are collected in Table 2. From the magnetization data, we have been able to identify multiple magnetic anomalies at low temperatures for all the compositions in Mn2SiS4-xSex. For the = 0, 1 and 4 compositions, in addition to the , a low temperature anomaly is observed in the temperature range near 12 K (denoted as in the table). For the = 2 and 3 compositions, we observe two more anomalies and in addition to the . This points out that the magnetic structure and the low temperature magnetism of Mn2SiS4-xSex compounds are more complex than the PM-AFM-WF transitions that were reported earlier. Junod et al. (1995); Jobic et al. (1995); Ohgushi and Ueda (2005) The presence of -MnS found in two of the samples through x ray diffraction analysis does not influence the magnetism as -MnS has a magnetic transition at = 140 K but we do not observe any anomalies at this temperature in any of the compositions.
The effective paramagnetic moment, and the Curie-Weiss temperature, are estimated form the inverse magnetic susceptibility versus temperature data following a curve-fit to Curie-Weiss law. The insets (1) and (2) in panel (b) shows the representative Curie-Weiss fits administered on Mn2SiS4 and Mn2SiSe4 as red solid lines. The estimated parameters from the fit are collected in Table 2 for all the five compositions. Slightly diminished values of effective moment compared to the theoretical spin-only moment of Mn2+ in state, = 5.92 , is observed in all the compounds except for Mn2SiSe4. The Curie-Weiss temperature returns negative values which indicate that the overall magnetic interactions in these compounds are antiferromagnetic type. The frustration parameter, = , shows a value of nearly 2.7 for all the compositions except for Mn2SiSe4 for which a higher value of 5.2 is recovered. This indicates that the compound Mn2SiSe4 is significantly frustrated than the other compounds. The frustration in Mn2SiS4-xSex stems from the geometrical triangular saw-tooth like arrangement of Mn2+ spins. The value of obtained for Mn2SiS4 compares well with the value reported for this material earlierOhgushi and Ueda (2005). The magnetic frustration effect that is observed through the frustration index is supported by the structural feature of the triangular Mn arrangement (refer Fig 1) that makes up the saw-tooth like lattice. In the case of Mn2SiS4 which has = 2.7, the Mn-triangle has two equal distances, 3.97 Å and one 3.71 Å. However, in the case of Mn2SiSe4 which has a high value (5.2), the Mn-triangle has all equal distance, 2.84 Å.
The magnetic structure of the = 0 and 4 compounds, Mn2SiS4 and Mn2SiSe4 have been elucidated through neutron powder diffraction methods. Junod et al. (1995); Lamarche et al. (1994b); Bodenan et al. (1996) The neutron diffraction study of Mn2SiS4 confirmed the presence of olivine crystal structure in the whole temperature range of 4.2 K to 180 K. However, as noted previously, Mn in this structure occupies two distinct Wyckoff positions, and . At 4.2 K, the Mn moments in both the positions were found to be collinear with the -axis. At higher temperature, the magnetic moment on the site gradually rotates away from the -axis. Between 83-86 K, both the and moments tend to align along the -axis. However, the moments are subjected to canting in the - plane.
A similar case of tendency for canting of the spins was observed in Mn2SiSe4 as well. However, in this case clear signature of diffuse magnetic scattering was observed, especially for the peaks at 2 = 22*∘* and 48*∘*Bodenan et al. (1996). The magnetization of Mn2SiSe4 was then attributed to the short-range ferro or ferrimagnetic arrangement of canted spins. The spin correlations as a part of the diffuse magnetic scattering is seen to persist up to 102 K. The observation to diffuse magnetic scattering in Mn2SiSe4 from the previous studies support the frustrated magnetism observed through a high frustration index, , and also low magnetic entropy released at the .
Multiple magnetic phase transitions at low temperature were observed in Mn and Fe orthosilicate olivines. Kondo and Mlyahara (1966); Santoro et al. (1966) In Mn2SiS4-xSex compounds, more than one magnetic anomaly is observed for all the compositions below their (refer to Table 2). By employing a Weiss mean-field model, the magnetic transitions in the Mn and Fe orthosilicates were qualitatively understood based on the parameter which is the ratio of the two superexchange angles present in the spin structure of these magnets. The ratio compares to the ratio, . It was shown that in the special case where , there arises a new low temperature phase transition below and it is indicated by the low values of the ratio where is the low temperature transition. In Table 2, we have collected the ratios , and for the Mn2SiS4-xSex compositions. It is easily noted that the value of is relatively constant across the compositions, except for the highly frustrated composition, Mn2SiSe4. Also, the values of and are highly diminished compared to that of . This is in agreement with the simple Weiss-field approach where the calculated exchange energies supported the low temperature magnetic anomalies. The broadness of the magnetic anomalies below in the Mn2SiSe4 compositions point toward short-range magnetic order rather than a long-range magnetic order in to a new magnetic structure. The dc magnetic susceptibility of the Mn2SiS4-xSex series in zero field-cooled (ZFC) and field-cooled (FC) protocol in the presence of external magnetic field, = 500 Oe is presented in Fig 5 (a-e). The effect of an external magnetic fields 1 T, 3 T and 5 T upon the field-cooled magnetic susceptibility is shown in the panels (f-j) of the same figure. For the compositions = 0, 1, the ZFC and the FC arms show no bifurcation at all (a, b). The magnetic phase transition is evident as a strong anomaly thereby confirming the AFM transition. For the compositions = 2, 3, and 4 strong irreversibilities are observed in the magnetic response which is an indication of significant short-range magnetic correlations or spin glass-like features. Interestingly, the highly frustrated compound Mn2SiSe4 presents a ZFC/FC response where the ZFC and FC arms cross each other in the low temperature region. This crossing happens at 18 K. This feature resembles the case of negative magnetization observed in many other oxide systems.Kumar and Yusuf (2015); Bartolomé et al. (2002); Menyuk et al. (1960) In the case of the spinel compound Co2VO4, the negative magnetization was explained in terms of a ferrimagnetic structure ( = 158 K) and the resulting complex magnetism at low temperature. However, the presence of ferromagnetic clusters embedded in an AFM matrix also can display negative magnetization as evidenced in the case of the rare-earth manganite, NdMnO3±δ where the stoichiometry of the oxygens also seem to play a role.Bartolomé et al. (2002) In order to accurately determine the presence of ferromagnetic short-range ordered clusters, low temperature neutron diffraction experiments were undertaken. In the case of Mn2SiSe4, the magnetic structure that is proposed already point towards the presence of short-range ferro or ferrimagnetic arrangement of canted spins. The magnetization data presented in Fig 5 (e) supports the claim of short-range ferrimagnetic canted spins. However, a detailed low temperature neutron powder diffraction study can shed more light on the proposed magnetic features. It can be noted that the application of external magnetic fields up to 5 T does not produce appreciable enhancement of the magnetization in any of the Mn2SiS4-xSexcompositions (panels (f-j)).
The isothermal magnetization curves, , as a function of applied field in the range 7 T to +7 T at 2 K for Mn2SiS4-xSex = 0 4 are plotted together in Fig 6 (a). The curves represent typical antiferromagnetic response with no indication of magnetic hysteresis. At 2 K and 7 T, the maximum magnetic moment attained is about 0.77 f.u. for Mn2SiSe4Ṫhe lowest moment is attained for Mn2SiS4 which has a value of 0.55 f.u. One of the earliest work on the Mn-chalcogenide olivines was related to the spin-flop transition and the associated tricritical point in the phase diagram. Ohgushi and Ueda (2005) The field-induced spin-flop transitions are reproduced in all the compositions in the present series of Mn2SiSe4 ( = 04). The field-induced spin-flop transitions are clearly evidenced in the derivatives versus plotted in Fig 6 (b-d) which are shown for = 0, 2 and 4. The variation of the critical field for spin-flop as a function of the Se-content is presented in the inset of (a). The spin-flop transition in Mn2SiS4 single crystals along the crystallographic -axis is observed at a critical field of about 3 T. In the present case, our samples of polycrystalline Mn2SiS4 also display the spin-flop transition at a comparable field value of 2.7 T. It can be observed that the first decreases with the replacement of S with Se, until = 2. Beyond = 2, for = 3, 4 increases and reaches a maximum for Mn2SiSe4 which is in fact, the highly frustrated composition in this group. In order to correlate the crystal and the electronic structure of the Mn2SiS4-xSex and to explore the band structure peculiarities of the current compositions as compared to that observed in Fe-based olivines that are predicted thermoelectrics Gudelli et al. (2015), we now take a look at the results from density functional theory calculations.
III.4 Density functional theory and thermal conductivity
The magnetic structure of Mn2SiS4 and Mn2SiSe4 are reported in the antiferromagnetic structure through neutron diffraction studies Bodenan et al. (1996); Lamarche et al. (1994b).
The magnetic moments of Mn are proposed to lie in the direction; the spins in the plane are ferromagnetically coupled while the adjacent layers are coupled antiferromagnetic. We have performed the DFT calculations for the antiferromagnetic spin arrangement of the four different compositions in Mn2SiS4-xSex. The experimental crystal structure for Mn2SiS4, obtained from the room temperature structure determined in the present work, was used as the starting point to generate the initial structures for all the four compounds following a energy-minimization process. The crystal symmetry is found to be orthorhombic with six inequivalent positions, agreeing with the space group reported Fuhrmann and Pickardt (1989). The optimized lattice constants, spin magnetic moments, and the band gaps of these systems are summarized in Table 3 and presented along with the corresponding experimental values for easy comparison. The total energy with the optimized lattice constants is lower than that with experimental lattice constants by 0.4 eV. The calculated magnetic moments on the Mn atoms show antiferromagnetic spin ordering. The DFT-calculated magnetic structure was found to match the experimental structure reported through previous neutron diffraction experiments Lamarche et al. (1994b). The range of the calculated spin magnetic moments, , are presented in the table for the optimized structure. An agreement is found between the and the experimental values () obtained from magnetization results of the present work. The substitution of one S by Se leads to two structures with the formula unit of Mn2SiS3Se which are identified as structures (a) and (b) in Table 3. Similar substitution by two Se atoms also leads to two structures using the same set of inequivalent atom positions. Apart from these, we also tested mixed structures with random substitutional positions in a supercell which led to Mn2SiS3Se and Mn2SiS2Se2 based on atom count only. However, we find that some of these structures have lower energy than the structures that conform to the orthorhombic symmetry and therefore we include them in the results, identified as structures Mn2SiS3Se (1)-(4) in the Table 3. For the Mn2SiS2Se2 compound, substitution of inequivalent atoms leads to the lowest energy structure compared to random substitution and therefore we present only the lowest energy structure in the table. However, for this compound and for Mn2SiSSe3, random substitution can lead to low lying structures within 0.020.07 eV above the ground state.
The Mn2SiSe4 compound with experimental lattice parameters is the lowest energy structure. For all the five compounds studied, the antiferromagnetic phase is the stable magnetic phase. The trend of the spin moment of the mixed compounds compare excellently with the trend seen from experiment. With higher number of Se atoms in the mixed compound, the spin moment decreases. However, the spin moment of the Mn2SiSe4 from DFT is much smaller compared to that derived from experimental data. We find that there can be several local minima in the potential energy surface with slightly different lattice constants for this compound. In all cases however the spin moment is still smaller than the experimental value. The experimental spin moments are determined from magnetization data collected at elevated temperatures where lattice expansion can lead to reduced interactions between atoms. The DFT calculations are done without any temperature effect which may explain the difference between the DFT and experimental spin moments. Moreover, these calculations also do not take into account non-collinear spin moments.
The band structure of the two terminal compounds Mn2SiS4 and Mn2SiSe4 are shown in Fig 7 (a, b) respectively. The bandgap of Mn2SiS4 and Mn2SiSe4 was found to be 0.47 eV and 0.45 eV respectively. Both structures have a direct bandgap as indicated by the valence band maximum (VBM) and conduction band maximum (CBM) from the band structure plot. The band structures have flat bands from G-X crystallographic direction and similar to that of Gudelli et al. Gudelli et al. (2015) in their Fe2GeS4 and Fe2GeSe4 band structure plots. The corresponding total and projected density of states (DOS) for Mn2SiS4 and Mn2SiSe4 are represented in panels (c, d) of Fig 7. The DOS shows that the states near the Fermi level arise mainly from the Mn d-states and S/Se states. In both the system the Si states lie deeper in energy. The conduction band has contribution mainly from the Mn states. The band gap obtained in the present study differ from those reported for Mn2SiS4Davydova et al. (2018). However, the antiferromagnetic spin arrangement assumed in the work by Davydova et al seem to be different from the AFM structure that is obtained in the present work as well as in earlier neutron reports Lamarche et al. (1994b). An LDA + U approach was used by Davydova et al which influences the band gap since U can be adjusted to match the experimental band gap.
Motivated by the band structure features that we found in Mn2SiS4 and Mn2SiSe4 and from the reports on other thio-olivines that project these materials as potential candidates for thermoelectric applications, we measured the thermal conductivity, . Figure 7 (e, f) shows the for Mn2SiS4 and Mn2SiSe4 respectively. Both compounds show thermal conductivity that is reminiscent of semiconducting materials where phonons dominate the thermal transport Tritt (2005). At low temperatures the thermal conductivity rapidly increases with increasing temperature, forms a pronounced maximum centered below 50 K, and then decreases down to room temperature. The maximum in low temperatures occurs due to reduction of the thermal scattering at low temperatures, i.e., in the regime where the phonon mean free path becomes larger than the interatomic distances. For both compounds the magnetic phase transition appears only as a small kink in at the Néel temperature (marked by arrows in Fig 7 (e, f)). The band gap obtained for Mn2SiSe4 is slightly diminished compared to that os Mn2SiS4 and the former shows -type conductivity according to our Seebeck coefficient measurement (not shown).
As the Se-content is increased from = 0 to = 4, the sharp magnetic transition observed in Mn2SiS4 is replaced with a broad transition extending over a large temperature range below 65 K. The results of magnetization and the specific heat experiments point towards the emergence of short-range order stemming from enhanced magnetic frustration. In Fig 8 the Mn-Mn distances between the Mn atoms occupying the crystallographically distinct m1 and m2 positions are represented for Mn2SiS4, Mn2SiS2Se2 and Mn2SiSe4. The distances marked on the figure are obtained from the refined x-ray diffraction data which is cross-checked against the distances obtained from DFT.
It can be seen from the figure that the Mn-triangles that form the saw-tooth lattice are isosceles and the Mn-Mn distances between the atoms in the m1 chain (along ) increases with Se-content. In general, the distances in the Mn-triangle increases from Mn2SiS4 towards Mn2SiSe4. The Mn(m1)Mn(m1) distance along the -direction for Mn2SiS4 is 5.94 Å which increases to 6.24 Å for Mn2SiSe4. The Mn(m1)Mn(m1) distances also undergo a similar increase. From this, it is clear that the inter-layer distance between the saw-tooth layers increase towards Mn2SiSe4 and subsequently a weakening of the exchange interaction can result. These structural features associated with the saw-tooth triangles lead to the formation of spin clusters in Mn2SiS4-xSex with increased Se-content resulting in predominant short-range order.
IV Conclusions
The magnetism of chalcogenide olivine Mn2SiS4-xSex with a saw-tooth lattice for the Mn moments are studied in detail using magnetization, specific heat and first-principles density functional theory calculations. Progressive substitution of S using Se in Mn2SiS4 is seen to shift the antiferromagnetic transition temperature from 86 K to 66 K. Though an antiferromagnetic transition is clear, the magnetic entropy estimated from the analysis of specific heat reveals diminished values suggesting strong spin fluctuations present. Among the Mn2SiS4-xSex compositions studied, Mn2SiSe4 is the most frustrated. A non-linear trend in the evolution of the critical field for spin-flop is found across the compositions. Density functional theory calculations support the stable orthorhombic crystal structure across the series and confirms the antiferromagnetic structure for Mn2SiS4 and Mn2SiSe4. Quasi-flat-band features similar to that seen in Fe-based olivines are seen in the present case however, the experimental thermal transport results do not support features favourable for a good thermoelectric.
V Acknowledgements
HSN acknowledges the UTEP start-up fund and UT Rising-STAR in supporting this work. BS acknowledges the financial support for this work provided by the University of Oklahoma startup funds. DA and KG acknowledge support from DOE’s (Basic Energy Science) Early Career Research Program. RRZ and TB acknowledge support by Department of Energy Basic Energy Science through Grant Nos. DE‐SC0002168 and DE‐SC0006818. Support for computational time by the NSF’s XSEDE project through grant TG‐DMR090071 is gracefully acknowledged. AC and SRS acknowledge The University of Texas at El Paso (UTEP) Start-up fund and NSF-PREM Program (DMR—1205302). The part of the paper prepared by Dr. Singamaneni and co-author A. Cosio are funded under the Award No. 31310018M0019 from UTEP, Nuclear Regulatory Commission. The statements, findings, conclusions, and recommendations are those of the author(s) and do not necessarily reflect the view of the UTEP or The US Nuclear Regulatory Commission.
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