Possible Bicollinear Nematic State with Monoclinic Lattice Distortions in Iron Telluride Compounds
C. B. Bishop, J. Herbrych, E. Dagotto, A. Moreo

TL;DR
This paper proposes that iron telluride can host a bicollinear nematic state with monoclinic lattice distortions, stabilized by coupling between lattice strain and orbital order, observable above the temperature of full magnetic order.
Contribution
The study introduces a spin-fermion model with lattice coupling showing how a nematic state can emerge in FeTe, splitting the magnetic transition and stabilizing short-range order.
Findings
Monte Carlo simulations demonstrate transition splitting with increased coupling.
A monoclinic nematic phase with short-range order is stabilized.
The lattice distortion and nematicity occur above the magnetic ordering temperature.
Abstract
Iron telluride FeTe is known to display bicollinear magnetic order at low temperatures together with a monoclinic lattice distortion. Because the bicollinear order can involve two different wavevectors and , symmetry considerations allow for the possible stabilization of a nematic state with short-range bicollinear order coupled to monoclinic lattice distortions at a higher than the temperature where long-range bicollinear order fully develops. As a concrete example, the three-orbitals spin-fermion model for iron telluride is studied with an additional coupling between the monoclinic lattice strain and an orbital-nematic order parameter with symmetry. Monte Carlo simulations show that with increasing the first-order transition characteristic of FeTe splits and bicollinear nematicity is…
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Possible Bicollinear Nematic State with
Monoclinic Lattice Distortions in Iron Telluride Compounds
Christopher B. Bishop
Jacek Herbrych
Elbio Dagotto
Adriana Moreo
Department of Physics and Astronomy, University of Tennessee, Knoxville, TN 37966, USA
Materials Science and Technology Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, USA
Abstract
Iron telluride (FeTe) is known to display bicollinear magnetic order at low temperatures together with a monoclinic lattice distortion. Because the bicollinear order can involve two different wavevectors and , symmetry considerations allow for the possible stabilization of a nematic state with short-range bicollinear order coupled to monoclinic lattice distortions at a higher than the temperature where long-range bicollinear order fully develops. As a concrete example, the three-orbitals spin-fermion model for iron telluride is studied with an additional coupling between the monoclinic lattice strain and an orbital-nematic order parameter with symmetry. Monte Carlo simulations show that with increasing the first-order transition characteristic of FeTe splits and bicollinear nematicity is stabilized in a (narrow) temperature range. In this new regime the lattice is monoclinically distorted and short-range spin and orbital order breaks rotational invariance. A discussion of possible realizations of this exotic state is provided.
chalcogenides, bicollinear antiferromagnetism, nematicity, orbital-lattice coupling
pacs:
74.70.Xa, 71.10.Fd, 75.25.Dk
I Introduction
The theoretical understanding of high critical temperature superconductivity in iron compounds has evolved from its early qualitative developments based on Fermi surface nesting to more quantitative efforts incorporating the role of electronic correlations intro ; HKM ; kotliar ; dainat ; RMP2013 ; FCS . In particular, experts have focused on several complex regimes including electronic nematicity fisher2010 ; fisherother ; fernandes1 ; fernandes2 , an interesting state observed in several high critical temperature pnictide superconductors clarina ; rotundu ; kasahara ; zhou . Upon cooling, this nematic phase is reached at a temperature , concomitantly with a structural phase transition from a tetragonal to an orthorhombic lattice. Upon further cooling a magnetically ordered phase is stabilized at a lower temperature . The orthorhombic nematic phase between and exhibits a reduced symmetry under rotations from to . This is also observed in the magnetic and orbital degrees of freedom leading to nonzero magnetic and orbital “nematic” order parameters. Experimental investigations have shown that this nematic phase occurs in the parent compounds of the 1111 pnictides clarina . Since the orthorhombic lattice distortion huang is small ( and are the lattice parameters in the orthorhombic notation), it is often argued that the lattice plays the role of a “passenger” in the nematic transition which is believed to be driven by either the magnetic or orbital degrees of freedom. In addition, it is interesting to notice that the structural transition occurs simultaneously with the Néel temperature in several other iron-based materials. For example, members of the 122 family need to be electron doped, with the chemical replacement occurring directly on the FeAs planes, to develop the nematic phase rotundu ; kasahara ; zhou . Hole doping, or electron doping via chemical substitution away from the FeAs planes, fails to establish nematicity chenx ; saha .
In the chalcogenides, the parent compound FeTe exhibits an unexpected “bicollinear” magnetic state bao ; li ; CMR , shown in panels (a,b) of Fig. 1, whose coincides with the of a structural transition to a phase with a monoclinic lattice distortion, as shown in panel (d) of the same figure. This joint transition is strongly first order bao ; chen ; fobes . The reported lattice distortions in Fe1.076Te and Fe1.068Te are bao ( and are the low-temperature lattice parameters in the monoclinic notation). Replacing Te with Se the bicollinear magnetic order is eventually lost, the material becomes superconducting, and it develops an orthorhombic nematic phase above its superconducting critical temperature. In recent theoretical work, using a spin-fermion model we explained the bicollinear magnetic order using symmetry considerations as a consequence of the monoclinic distortion bistripes ; bnl2016 . Based on this reasoning, the role of the lattice in the case of FeTe appears more important than previously anticipated.
The aim of the present work is to argue that the pnictides and chalcogenides could potentially behave more symmetrically with regards to the presence of a nematic state. As expressed above, the pnictides either already have nematicity without doping, as in the 1111 compounds, or develop nematicity after doping as in the Co-doped 122 compounds. Based on symmetry arguments, the presence of a nematic regime is theoretically understood as follows. In these materials the magnetic ground state has wavevector , with staggered spins along the -axis and parallel spins along the -axis. However, the state should have the same energy by symmetry. In cases of two-fold degeneracy in the ground state, it was predicted that an Ising transition could occur upon cooling premi , with an order parameter that breaks lattice rotational invariance and involves only short-range magnetic correlations. Upon further cooling, the O(3) full symmetry breaking process is possible.
Our main observation here is that the bicollinear state shown in Fig. 1 (a) with wavevector has a partner, displayed in Fig. 1 (b), with identical energy but peaks . Then, the same Ising-O(3) rationale expressed above for the degeneracy can be repeated for bicollinear states: starting at high temperature both spin structure factors will start growing with equal strength upon cooling at the wavevectors and . By analogy with the pnictides, it is possible that at a critical nematic temperature an asymmetry develops such that , and then at a lower temperature , drops to zero while grows like the volume.
While no nematic phase with these characteristics has been reported yet in materials of the FeTe family with the bicollinear spin order, the present study provides computational evidence that there are Hamiltonians with spin- and orbital-lattice coupling that display this new nematic behavior if the couplings strengths are properly tuned. While our many-body tools do not allow us to predict what specific material may display this phenomenon, our symmetry arguments and concrete simulation results are offered as motivation for the experimental search for this exotic bicollinear-nematic state.
Previous numerical studies of spin-fermion models for pnictides with spin, orbital, and lattice degrees of freedom provided indications that the structural transition is due to the coupling between the lattice and spins shuhua13 . Thus, in these regards the lattice follows the spins. But the spin-lattice coupling leads to and, then, the establishment of a nematic phase with requires a more subtle mechanism. Investigations by our group have shown that the nematic regime can be achieved by the addition of an orbital-lattice coupling shuhua13 (or by the introduction of in-plane magnetic disorder, namely by replacing iron by non-magnetic atoms chris15 ; fernandes-dis ). Based on this previous research, here a coupling between the monoclinic lattice distortion and an orbital nematic parameter with symmetry will be added to the spin-fermion model that already has the spin-lattice coupling previously developed to study FeTe bistripes . It will be shown below that this addition generates the novel bicollinear nematic state. This is not an obvious result because the tight-binding term contains an intrinsic tendency towards collinear magnetic order that could have affected the fragile nematicity region that we are reporting here.
The publication is organized as follows. In Section II the model is described including the new term that must be incorporated in order to stabilize a bicollinear-nematic state. In Section III we provide an explanation of the numerical approach that allows for the parallelization of the Monte Carlo procedure and the concomitant use of clusters of reasonable size for our purposes. The main results showing the stabilization of the new nematic state are presented in Section IV. The discussion, including possible physical realizations, is in Section V, with brief conclusions in Section VI.
II Models
In the first subsection we will discuss a general model that addresses the interactions between electrons and the lattice for the case of monoclinic distortions. In the second subsection, the actual special case that was computationally investigated in this publication will be presented. Our effort aims to prove that there is at least one set of couplings for which, varying temperature, a bicollinear nematic state is stabilized. A more comprehensive analysis of phase diagrams varying the many couplings in the generic model would demand considerable computational resources and this task is left for future investigations.
II.1 Generic Model
The most general spin-fermion (SF) Hamiltonian discussed here is an extension of the purely electronic model previously introduced BNL ; shuhua , supplemented by additional couplings to the monoclinic lattice degrees of freedom shuhua13 ; chris ; igor :
[TABLE]
represents the three-orbitals (, , ) tight-binding Fe-Fe hopping of electrons, with the hopping amplitudes selected to reproduce photoemission data (see Eqs.(1-3) and Table 1 of three ). In the undoped-limit the average electronic density per iron and per orbital is set to =4/3 three and a chemical potential in chris controls its value. The on-site Hund interaction is =, where are the localized spins at site and are spins corresponding to orbital of the itinerant fermions at the same site. For computational simplicity, the localized spins are assumed classical and of norm one foot . contains the nearest neighbor (NN) and next-NN (NNN) Heisenberg interactions among the localized spins, with respective couplings and . As explained before shuhua13 ; shuhua , both NN and NNN could be active because of the geometry of the problem, where in each layer the Te atoms (or As, Se, P) are at the centers of iron plaquettes as seen from above. However, in our previous study of FeTe bistripes we observed that the experimental value of for FeTe could be obtained by simply setting . This is due to the fact that the intersite spin-spin couplings favor either checkerboard () or collinear () magnetic configurations and in order to obtain a bicollinear ground state it is necessary to use a larger value of the spin-lattice coupling which, in turn, increases intersite . is the lattice stiffness given by a Lennard-Jones potential to speed up convergence chris (full expression can be found in shuhua13 ).
Recently, an important novel term was introduced bistripes to describe FeTe properly. This term has the form = and it provides a coupling between the localized spins and the monoclinic lattice distortions kuo . The coupling constant strength is and the spin NNN nematic order parameter is defined as
[TABLE]
where indicates the four NNN sites to , with and representing unit vectors along the and axes, respectively. Note that has the value 2 (-2) in the perfect bicollinear states shown in Figs. 1 (a) and (b), respectively characterized by a peak at wavevectors and in the magnetic structure factor. is the lattice strain defined in terms of the Fe-Te distances as
[TABLE]
where (=1,…,4) is the distance between Fe at site and each of its four Te neighbors (see panel (c) of Fig. 1 and also Fig. S1, Suppl. Sec. of bistripes ). As in previous simulations, the Te atoms are allowed to move locally from their equilibrium position only along the and directions because the component of the position does not couple to the monoclinic distortion. It is important to notice that both and transform according to the representation of the symmetry group, which means that the spin-lattice term of the Hamiltonian transforms as as expected. As the spin-lattice coupling grows and induces a monoclinic distortion, develops a nonzero expectation value leading to the bicollinear spin state order as explained in bistripes .
The Hamiltonian described thus far bistripes leads to a first-order phase transition where both the monoclinic lattice and the bicollinear spin orders develop simultaneously. Thus, no bicollinear-nematic state was reported in bistripes . Based on previous investigations of pnictides using the spin-fermion model shuhua13 , it is natural to introduce a coupling between the lattice and the orbital degree of freedom to favor nematicity (note that adding this term does not imply immediately that the bicollinear nematic state will be stabilized because there are competing collinear tendencies in the tight-binding term; a specific calculation is thus needed, as presented below). For the new term, care with regards to the symmetry of the operators used is required. The monoclinic orbital-nematic order parameter is defined as
[TABLE]
where = (), and the orbital basis is related to the orbital basis by
[TABLE]
and
[TABLE]
Notice that the and axes point along nearest-neighbor irons, i.e. along the sides of the plaquette formed by four irons, while the axes point along next nearest-neighbor iron, i.e. along the diagonals of the iron plaquette. The and axis coincide and they are perpendicular to the plane formed by the iron layer.
The new term in the Hamiltonian that couples the orbital and lattice order parameters is given by
[TABLE]
Because the monoclinic lattice distortion transforms as the representation of , it must be coupled to an orbital order parameter that also transforms as which is why was constructed. This ensures that is invariant under the symmetry group.
II.2 Parameter Space Studied
Although the model described thus far is generic for the spin-fermion family of Hamiltonians, including Heisenberg couplings as well as lattice-spin and lattice-orbital terms, in practice we have setup to zero some of those couplings for simplicity. The reason is that we aim to prove computationally the existence of the novel proposed bicollinear nematic state at least in the most optimal region of parameter space. In practice, it would be impossible to establish the full phase diagram varying every single parameter in the complete model, but as experiments searching for the novel phase progress we can refine our analysis in future efforts.
was studied here with the same Monte Carlo (MC) procedure employed in shuhua13 , supplemented with the recently developed “Parallel Travelling Cluster Approximation (PTCA)” PTCA described in the next section. The particular values for the couplings eV, , and were chosen because they provide K for bistripes , which is the transition temperature experimentally observed in FeTe (note then that the Heisenberg couplings are neglected in this first exploratory study, for simplicity). The coupling strength is the dimensionless version of the spin-lattice coupling, employing eV as the bandwidth of the tight-binding term and as the constant that appears in shuhua13 . Since these couplings were discussed extensively before, in the present effort we will instead focus on a careful description of the new dimensionless monoclinic orbital-lattice coupling and its effects.
During the simulation the Te atoms are allowed to move locally away from their equilibrium positions within the - plane. The Fe atoms can move globally via a monoclinic distortion where the angle between two orthogonal Fe-Fe bonds is allowed to change globally to with the four angles in the iron plaquette adding to , so that the next angle in the plaquette becomes , with as a small angle (see Fig. 1 (d)). In addition, the localized spins and atomic displacements that determine the value of the local lattice distortion bistripes (see Fig. 1 (c)) are evaluated via a standard Monte Carlo procedure.
III Methods: the Parallel Traveling Cluster Approximation
To access the lattice sizes needed to study the existence of a monoclinic nematic phase we implemented the Parallel Traveling Cluster Approximation (PTCA) PTCA which is a parallelization improvement over the traveling cluster approximation (TCA) previously introduced tca . PTCA allows parallelization in order to use multiple CPU cores and by this procedure we can reach lattices as large as . To perform a Monte Carlo update of one of the local variables – either the localized spin at the iron site or the local distortion of the Fe-Te bonds joining the Fe atom at site with its four Te neighbors – an traveling cluster is constructed around site and the Hamiltonian is diagonalized only inside that cluster to decide whether the update is accepted. The algorithm is parallelized by dividing the lattice into four quadrants with sites, one per different CPU core. Then, each CPU generates traveling clusters around the sites belonging to its quadrant, see Fig. 2 for an illustration, and these clusters are then simultaneously diagonalized.
To update the global monoclinic lattice distortion given by the angles in the rhombus formed by the four irons shown in Fig. 1 (d) an extra new modification in the PTCA was introduced. The sites lattice was divided into 16 clusters with sites each as shown in Fig. 3. Each of four CPU cores was devoted to diagonalize four of the clusters as indicated in the figure. The same update is proposed in all the clusters which are simultaneously diagonalized. Then, all the eigenvalues are collected in one of the cores in order to calculate the probability of the Monte Carlo update and decide whether the update is accepted or rejected.
For thermalization typically 5,000 Monte Carlo steps were used, while 10,000 to 25,000 steps were performed in between measurements for each set of parameters and temperatures. The spin-spin correlation functions in real space were measured and the magnetic structure factor was calculated via their Fourier transform. Notice that in the bicollinear state the magnetic structure factor diverges for or . The Néel temperature is obtained from the magnetic susceptibility given by
[TABLE]
where and is the number of lattice sites. We also calculated the numerical derivative of with respect to temperature to double-check the value of . The monoclinic structural transition temperature, , was obtained by calculating the structural susceptibility given by
[TABLE]
where and is the deviation from 90o of the angle of the lattice plaquette as shown in Fig. 1 (d) bistripes . was also obtained from the numerical derivative of as a function of temperature and from monitoring the behavior of the spin-nematic and orbital-nematic order parameters, and respectively, introduced in the previous section and their associated susceptibilities.
IV Results
As explained before, in previous work bistripes we found that the magneto-structural transition experimentally observed in FeTe, with K, was reproduced by setting eV and , and by dropping the Heisenberg couplings i.e. using . In the present study for simplicity we keep fixed the values of all these parameters while we only vary the orbital-lattice coupling to investigate whether a nematic phase can be stabilized in a range of temperature. Future work will address what occurs in other portions of parameter space, such as with finite Heisenberg couplings [some partial results are already available (to be shown in future publications) and all indicates that the bicollinear nematic state is still present at large even including nonzero and ].
IV.1 Special case
Similarly as with the behavior reported before for the spin-fermion model in the case of the pnictides with spin order shuhua13 , in the bicollinear case studied here it was also observed that the novel bicollinear nematic region becomes stable by increasing the value of the orbital-lattice coupling. This is not obvious because of competing collinear tendencies, as already explained. Another similarity with the case of the collinear state shuhua13 is that the addition of the orbital-lattice coupling turns the first order magnetic transition into a second order one. The temperature width of nematicity remains narrow, as in many previous investigations, and robust values of are required. Nevertheless, this is sufficient to demonstrate the matter-of-principle existence of the bicollinear-nematic state discussed in this publication. For clarity, first let us address in detail the largest value of the coupling that we studied which was .
In Fig. 4 the magnetic susceptibility versus temperature is shown. A clear maximum at K indicates the magnetic transition to the bicollinear state with long-range order. The monoclinic lattice susceptibility is also shown. Interestingly, this quantity has a sharp peak at a clearly larger temperature K where the structural transition from tetragonal to monoclinic takes place, indicating that a bicollinear-nematic state does indeed occur.
In Fig. 5 the magnetic structure factor at wavevector is displayed. The from the susceptibility, shown with a dashed line, should occur when the rate of increase of the order parameter is maximized. This has been verified by performing a spline fit of the points obtained from the Monte Carlo simulation and taking the numerical derivative. The monoclinic lattice order parameter is also presented in Fig. 5. The structural transition temperature is displayed with a dashed line as well. We also verified that the maximum in the lattice susceptibility from Fig. 4 coincides with the maximum rate of change in the lattice order parameter via a spline fit of the Monte Carlo data.
In between the two transition temperatures and , a nematic phase is stabilized. In this phase both short-range orbital and spin nematic order develop as it can be seen in Fig. 6, where in panel (a) the susceptibilities associated with various order parameters are presented. It can be observed that the orbital-nematic and spin-nematic susceptibilities have maxima at as does the structural susceptibility. This confirms the presence of a monoclinic nematic phase characterized by orbital-nematic and spin-nematic orders. These properties are also reflected in the behavior of the respective order parameters shown in panel (b) of the figure.
Performing spline fits of the order parameters and taking numerical derivatives, the critical temperatures obtained from the susceptibilities were reproduced. It is important to notice that the lattice distortions are quantitatively similar to those reported in FeTe experiments while, as shown in Fig. 6 (b), the orbital and spin nematic order parameters develop values an order of magnitude larger. Thus, the strength of the orbital-lattice coupling used still leads to small lattice distortions but appears to generate robust magnetic and orbital short-range order inducing substantial anisotropic effects in these observables.
IV.2 Special case
As the value of the orbital-lattice coupling is reduced the separation between the magnetic and the structural transitions decreases. In panel (a) of Fig. 7 the magnetic and structural susceptibilities at obtained from Monte Carlo simulations are presented. In this case K while K. The orbital- and spin-nematic order parameters also have a maximum susceptibility at (not shown for simplicity). The magnetic and structural order parameters are shown in panel (b) of Fig. 7 and their qualitative behavior is in agreement with panel (a). The indicated transition temperatures have been obtained from numerical fits of the order parameters and their derivatives as described in the previous subsection. This case is close to the limit of our numerical accuracy. In principle, it is possible that simulations using larger systems and with far more statistics may unveil a very narrow bicollinear nematic state even for small values of . However, for our qualitative purposes simply showing the stability of the new proposed phase in any range of is sufficient.
IV.3 Phase Diagram
The phase diagram obtained as a function of the orbital-lattice coupling and temperature is presented in Fig. 8. It can be seen that the region with nematicity can be stabilized at robust values of the orbital-lattice coupling. While a very narrow nematic phase may exist at smaller values of this coupling, numerically we have been able to resolve the separation between the two critical temperatures only for . As described in the previous sections, the separation between and monotonically increases with .
V Discussion and Possible Physical Realizations
Our results have illustrated the possible existence of a nematic phase involving bicollinear short-range order, using as explicit example a computational study of the spin-fermion model incorporating the lattice distortions corresponding to the iron telluride family. Previous investigations bistripes showed that the addition to the electronic spin-fermion model for pnictides of a coupling between a spin-nematic order parameter with symmetry and the monoclinic distortions of the iron lattice does induce the low-temperature monoclinic and spin bicollinear state experimentally observed in FeTe. That result was remarkable because the spin-fermion model contains a tight-binding term that favors the and collinear states that arise from the nesting of the Fermi surface in weak coupling. However, the spin-lattice interaction, when sufficiently strong, can overcome these tendencies and stabilize the monoclinic bicollinear state.
Here, we have included an additional orbital-lattice term with coupling strength , involving the monoclinic lattice strain coupled to an orbital order parameter with symmetry. By this procedure we have shown that a novel nematic phase characterized by the breakdown of the lattice rotational symmetry between the two possible diagonal directions of the spin bicollinear state can be induced. In this new nematic phase, short-range spin- and orbital-nematic order develop accompanied by a lattice monoclinic distortion.
The model Hamiltonian studied here only allows us to show explicitly, as a matter of principle, that indeed the bicollinear-nematic state described above does occur in computational studies once all of the many degrees of freedom and couplings are properly incorporated. But it is difficult to predict on what specific material this subtle state will be realized in practice, thus we can only discuss some scenarios qualitatively. The possible splitting of and by electron doping was raised in fernandes1 . However, spin-fermion model studies including doping but not quenched disorder (i.e. in the “clean” limit) did not detect such a split, at least in the doping range studied (Fig. 2 of chris15 ). Another generic qualitative observation is that in the pnictides nematicity is observed for the 1111 compounds even in the undoped limit clarina . Thus, to find the nematic phase discussed here it may be necessary to synthesize materials with intercalated FeTe planes.
However, in our opinion the most likely scenario to stabilize the proposed bicollinear-nematic regime in variations of the FeTe compound is by the chemical replacement of iron by other transition metal elements, thus simultaneously modifying the electronic density as well as the amount of quenched disorder. In pnictides, replacing Fe by Co, Ni, or Cu indeed leads to a wide nematic region. Our previous computational investigations using the spin-fermion model with doping and disorder chris15 clearly showed that indeed by this procedure a nematic temperature range can be induced even in cases where and coincide in a first-order transition for the undoped parent compound, as in the 122 family. Disorder plays a more important role than doping in this split chris15 , as observed experimentally as well nni . To our knowledge the experimental investigations of (Fe,)Te, with another transition metal element, are very limited. We are aware of three main lines of investigations and conclusions:
(i) Copper doping of FeTe was studied in FTCu ; FTCu2 for two Cu concentrations using single crystals. For the case Fe1.06Cu0.04Te the presence of strain was detected at 41 K upon cooling FTCu . At lower temperatures approximately 36 K nearly-commensurate long-range bicollinear magnetic order occurs. The presence of two transitions seems in agreement with our prediction of bicollinear nematicity. However, in FTCu it was argued that between 36 K and 41 K the lattice distortion could be orthorhombic as in pnictides. The possible competition with orthorhombic tendencies was theoretically addressed and reported in bistripes . This competition adds an extra complication to the detection of the here predicted bicollinear-nematic state. For the case FeCu0.1Te only cluster glass behavior was found below 22 K, presumably due to disorder FTCu . Note that this glassy state could be nematic.
(ii) The case of Ni doping was reported for the compounds Fe1.1-xNixTe with , and FTNi . Magnetization studies show that decreases with increasing up to 0.04, while for a possible spin glass transition was reported. In fact, neutron diffraction at found neither structural nor magnetic transitions at low temperatures. Since this study focused on long-range magnetic order, the presence of bicollinear nematicity is still possible.
(iii) Cobalt doping has also been recently studied via single crystals of Fe1+y-xCoxTe with and FTCo . In the range up to the antiferromagnetic transition systematically decreases. For and larger the long-range order transition disappears.
As a partial summary, the available experimental literature on (Fe,)Te does not conclusively show neither the presence nor absence of bicollinear-nematicity, and more work is needed to clarify this matter now in the light of our present study. For example, in the context of pnictides the pioneering studies of Ba(Fe1-xCox)2As2 fisher2010 reported the resistivities vs. temperature along the and axes, highlighting their different behavior and substantial differences particularly below . Similar careful studies in the (Fe,)Te context must be performed but focusing on the temperature evolution of the resistivities along and perpendicular to the main spin diagonals in the bicollinear state, as already performed for FeTe reverse1 ; reverse2 . In addition, recent inelastic neutron scattering studies of nematicity in BaFe1.935Ni0.065As2 dai-Ni focused on the temperature dependence of the intensity of the peaks at and , reporting their split at with cooling, followed by a collapse to zero of the intensity at . Similar studies for -doped FeTe (=Cu,Ni,Co) should be carried for the temperature dependence of the neutron intensities corresponding to the and wavevectors.
We also would like to point out that our work confirms that magnetoelastic effects tend to estabilize the bicollinear state while in the absence of this kind of coupling plaquette or orthogonal double stripe order could be stabilized, which may be the case in FeTe with excess iron ducatman ; ducatman2 . In addition, in a recent publication gzhang a double-stage nematic bond-ordering above the bicollinear state was proposed, but this effect would be difficult to study numerically due to the narrow range of the nematic phase.
VI Conclusions
In this publication, based on simple symmetry observations and a concrete model Hamiltonian numerical simulation, we have argued that the exotic bicollinear state known to be stable in FeTe admits a possible nematic state above the antiferromagnetic critical temperature. In other words, as discussed in the previous section, via chemical substitution it is conceivable that a split of the first-order transition of FeTe could be generated. Upon cooling, this would induce first a , where the monoclinic distortion is stabilized and short-range spin and orbital order develops breaking the lattice rotational invariance, and second a at a lower temperature, where long-range bicollinear order is fully stabilized. Experimentally finding this new exotic state not only would confirm the theoretical prediction outlined here, but it would allow us to investigate to what extend nematic fluctuations are needed to induce superconductivity.
Acknowledgments
C.B. was supported by the National Science Foundation, under Grant No. DMR-1404375. E.D., J.H., and A.M. were supported by the US Department of Energy, Office of Basic Energy Sciences, Materials Sciences and Engineering Division.
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