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Proceedings of the National Academy of Sciences of the United States of America logoLink to Proceedings of the National Academy of Sciences of the United States of America
. 2015 Jul 21;112(31):9568–9572. doi: 10.1073/pnas.1504164112

Fragile charge order in the nonsuperconducting ground state of the underdoped high-temperature superconductors

B S Tan a, N Harrison b, Z Zhu b, F Balakirev b, B J Ramshaw b, A Srivastava a, S A Sabok-Sayr c, B Dabrowski c, G G Lonzarich a, Suchitra E Sebastian a,1
PMCID: PMC4534212  PMID: 26199413

Significance

Results from quantum oscillation and spectroscopic measurements have suggested charge order as responsible for the creation of a nodal electron pocket in the YBa2Cu3O6+δ and HgBa2CuO4+δ families of underdoped cuprates. However, the situation in the pristine YBa2Cu4O8 family remains ambiguous. Our high-precision quantum oscillation measurements point to a very similar nodal electron pocket in the stoichiometric cuprate family YBa2Cu4O8, despite the nonobservation of charge order signatures in diffraction experiments. Our findings in YBa2Cu4O8 indicate Fermi surface reconstruction in the hole underdoped cuprates associated with the magnetic field enhancement of charge order, the fragile low-magnetic field character of which is reflected in the short correlation length reported in various materials families.

Keywords: superconductivity, strongly correlated electron systems, high-Tc cuprate superconductors, Fermi surface, charge order

Abstract

The normal state in the hole underdoped copper oxide superconductors has proven to be a source of mystery for decades. The measurement of a small Fermi surface by quantum oscillations on suppression of superconductivity by high applied magnetic fields, together with complementary spectroscopic measurements in the hole underdoped copper oxide superconductors, point to a nodal electron pocket from charge order in YBa2Cu3O6+δ. Here, we report quantum oscillation measurements in the closely related stoichiometric material YBa2Cu4O8, which reveals similar Fermi surface properties to YBa2Cu3O6+δ, despite the nonobservation of charge order signatures in the same spectroscopic techniques, such as X-ray diffraction, that revealed signatures of charge order in YBa2Cu3O6+δ. Fermi surface reconstruction in YBa2Cu4O8 is suggested to occur from magnetic field enhancement of charge order that is rendered fragile in zero magnetic fields because of its potential unconventional nature and/or its occurrence as a subsidiary to more robust underlying electronic correlations.


The normal state of the underdoped copper oxide superconductors has proven to be even more perplexing than the d-wave superconducting state in these materials. At high temperatures in zero magnetic fields, the normal state of the underdoped cuprates comprises an unconventional Fermi surface of truncated “Fermi arcs” in momentum space, which is referred to as the pseudogap state (1). At low temperatures in high magnetic fields, quantum oscillations reveal the nonsuperconducting ground state in various families of underdoped hole-doped copper oxide superconductors to comprise small Fermi surface pockets (215). These small Fermi pockets in YBa2Cu3O6+δ have been identified as nodal electron pockets (2, 3, 11, 16, 17) originating from Fermi surface reconstruction associated with charge order measured by X-ray diffraction (1820), ultrasound (21), nuclear magnetic resonance (22), and optical reflectometry (23). However, various aspects of the underlying charge order and the associated Fermi surface reconstruction remain obscure. A central question pertains to the origin of this charge order, curious features of which include a short correlation length in zero magnetic field that grows with increasing magnetic field and decreasing temperature (20). It is crucial to understand the nature of this ground-state order that is related to the high-temperature pseudogap state and delicately balanced with the superconducting ground state. Here, we shed light on the nature of this state by performing extended magnetic field, temperature, and tilt angle-resolved quantum oscillation experiments in the stoichiometric copper oxide superconductor YBa2Cu4O8 (24). This material with double CuO chains has fixed oxygen stoichiometry, making it a model system to study. YBa2Cu4O8 avoids disorder associated with the fractional oxygen stoichiometry in the YBa2Cu3O6+δ chains, which has been shown by microwave conductivity to be the dominant source of weak-limit (Born) scattering (25).

Intriguingly, we find magnetic field- and angle-dependent signatures of quantum oscillations in YBa2Cu4O8 (13, 14) that are very similar to those in YBa2Cu3O6+δ, indicating a similar nodal Fermi surface that arises from Fermi surface reconstruction by charge order with orthogonal wave vectors (16). However, the same X-ray diffraction measurements that show a Bragg peak characteristic of charge order in YBa2Cu3O6+δ for a range of hole dopings from 0.084p0.164 (19, 20, 26) have, thus far, not revealed a Bragg peak in the case of YBa2Cu4O8 (19). We suggest that charge order enhanced by applied magnetic fields reconstructs the Fermi surface in YBa2Cu4O8, whereas charge order is revealed even in zero magnetic fields in YBa2Cu3O6+δ because of pinning by increased disorder from oxygen vacancies.

Results

Fig. 1 shows quantum oscillations in contactless conductivity (27) measured up to 90 T in YBa2Cu4O8 and at different temperatures from 1.3 to 8.0 K. The extended magnetic field range and increased sensitivity compared with previous quantum oscillation experiments (13, 14) enable precision measurements of the quantum oscillation frequency spectrum and effective quasiparticle mass of YBa2Cu4O8.

Fig. 1.

Fig. 1.

(A) Quantum oscillations measured in the contactless resistivity of YBa2Cu4O8 for the magnetic field parallel to the c axis. (B) Fourier transform of the measured quantum oscillations at different temperatures. (C) Plot of quantum oscillation amplitude as a function of temperature (symbols) accompanied by a Lifshitz–Kosevich fit (red line).

Preliminary quantum oscillation measurements on YBa2Cu4O8 accessed two (13) to four (14) oscillation periods over a restricted magnetic field range for a magnetic field angle parallel to the crystalline c^ axis. A single quantum oscillation frequency of 660 ± 30 T was reported, whereas the scatter of the quantum oscillation amplitude as a function of temperature precluded a determination as to whether a Lifshitz–Kosevich form is obeyed or an accurate extraction of a quasiparticle effective mass. Our quantum oscillation measurements over an extended magnetic field range access more than seven oscillation periods, revealing for the first time, to our knowledge, a pronounced quantum oscillation beat structure characteristic of multiple frequencies, very similar to YBa2Cu3O6.56 (6, 9, 28), with a dominant frequency of 640 T. Our precision measurements of quantum oscillation amplitude as a function of temperature shown in Fig. 1 B and C further reveal a distinctive Lifshitz–Kosevich form, characteristic of Fermi Dirac statistics. A fit to the Lifshitz–Kosevich form yields a quasiparticle effective mass of 1.8 (1)me in YBa2Cu4O8, which is, in fact, very similar to that measured for YBa2Cu3O6.56.

Angular measurements as a function of tilt angle to the applied magnetic field are required to identify the origin of the multiple-frequency spectrum that we observe in YBa2Cu4O8. Fig. 2 shows the quantum oscillations in YBa2Cu4O8 measured up to a maximum tilt angle of θ56°. A few key features are notable. First, the beat pattern at the 0° tilt angle persists up to high tilt angles. Second, the prominent Yamaji amplitude resonance (29) expected at θ52° for a neck–belly warped Fermi surface in YBa2Cu4O8 is absent up to the measured high tilt angles. The absence of a prominent Yamaji angle in YBa2Cu4O8 enables us to rule out a Fermi surface where the observed frequency spread arises from a dominant neck and belly fundamental warping. Instead, both of the observed features are consistent with a quasi-2D Fermi surface, in which the multiple-frequency spectrum originates from a splitting of frequencies as opposed to a fundamental neck and belly warping. Such a quasi-2D Fermi surface is similar to that identified in YBa2Cu3O6+δ (16, 28).

Fig. 2.

Fig. 2.

Quantum oscillations (colors) measured in the contactless resistivity of YBa2Cu4O8 for different angles of inclination (θ) of the magnetic field to the c axis plotted as a function of 1Bcosθ. Simulated quantum oscillations (gray) of a bilayer split quasi-2D Fermi surface model shown in Fig. 4 (16) are shown for the parameters listed in Table 1. Inset shows a schematic of the crystal tilt angle to the magnetic field.

Another clue as to the origin of the observed quantum oscillations in YBa2Cu4O8 is obtained by inspecting the evolution of the amplitude and phase of the quantum oscillations as a function of tilt angle. Fig. 3B shows the cross-correlation function between the measured quantum oscillations in YBa2Cu4O8 and a phase-matched sinusoidal function with frequency 640 T, which is averaged over the indicated magnetic field range, referred to as the correlator. We find that the correlator is very similar to that previously measured for YBa2Cu3O6.56 (11, 16) and shown in Fig. 3A. The correlator for YBa2Cu4O8 reveals a zero crossing and phase inversion of the quantum oscillation amplitude, signaling a spin zero at a tilt angle of θ 48°. A spin zero feature arises on destructive interference between quantum oscillations from two spin channels at certain special angles. At these spin zero angles, the ratio of the Zeeman energy to the cyclotron energy—captured by the spin splitting factor Rs=cos[(π/2)m*g*/mecosθ]—crosses zero and inverts sign. Spin zero angles are located at

θsz=cos1[m*g*(2n+1)me], [1]

where n is an integer, g* is the effective g factor, assumed here to be isotropic for simplicity (see Methods and Table 1 for the more general case). me is the electron mass, and m* is the effective quasiparticle mass for B parallel to the crystalline c^ axis (30).

Fig. 3.

Fig. 3.

(A) Symbols represent the cross-correlation function between the measured quantum oscillations in YBa2Cu3O6.56 and a phase-matched sinusoidal function with frequency 534 T, which is averaged over the indicated magnetic field range. Reprinted from ref. 16. (B) Symbols represent the cross-correlation function between the measured quantum oscillations in YBa2Cu4O8 and a phase-matched sinusoidal function with frequency 640 T, which is averaged over the indicated experimental magnetic field range. Solid lines show the fits using the equation and parameters in Table 1.

Table 1.

Parameters used to simulate the oscillatory waveform for a quasi-2D split Fermi surface model shown in Fig. 4 represented by the equation Ψtwofoldj=16Nj[RMBRsRDRT]jcos(2πFj/Bcosθπ+ϕ)

Parameter Description YBa2Cu4O8 YBa2Cu3O6.56
F0 Quantum oscillation frequency 639 T 534 T
ΔFtwofold Staggered twofold warping frequency 15 T
ΔFsplit Bilayer splitting frequency 91 T 90 T
m* Quasiparticle effective mass 1.8 me (fixed) 1.6 me (fixed)
B0 Magnetic breakdown field 4.2 T 2.7 T
g* g-Factor 1 2.0 2.1
g* g-Factor 2 0.1 0.4
ξ g-Factor anisotropy 1 1.6 1.4
ξ g-Factor anisotropy 2 0.8 0.2
ϕ Phase −1.6c 0 (fixed)

Here, RMB is the magnetic breakdown amplitude reduction factor (defined in Methods), and Nj counts the number of instances that the same orbit is repeated within the magnetic breakdown network. RD is the Dingle damping factor, RT is the thermal damping factor, and Rs is the spin damping factor (defined in Methods). The tabulated values used to simulate the quantum oscillation waveform yield good agreement with experiment as a function of B and θ (Figs. 2 and 3). The effective mass is taken to be a fixed quantity, having been determined independently from temperature-dependent measurements (9). The parameters are the same for all of the orbits, except for those denoted by subscripts and ◇, which correspond to subsets of orbits as defined in the text. The values of gj* and ξj here represent parameters used for simulation rather than unique identifications. The parameters used for YBa2Cu3O6.56 shown for comparison are taken from ref. 16.

A value of m*g* can be extracted by the measurement of at least two spin zeros, given the two unknown quantities n and g*, as was done for YBa2Cu3O6.56 (16). To interpret the single spin zero observed at θfirstsz48° in YBa2Cu4O8, a comparison with YBa2Cu3O6.56 is instructive, in which case two spin zeros were observed at θfirstsz55° (10, 16) and θsecsz66° (16). Good agreement with experimental data is yielded by associating an index value of n=2 with the first spin zero, for parameters including anisotropic g-factors (see Methods) given in Table 1. Parameters for YBa2Cu4O8 are remarkably similar to those obtained in the case of YBa2Cu3O6.56 (16), and are in good agreement with experimental data (solid lines in Fig. 3).

Given the similarities that we find between YBa2Cu4O8 and YBa2Cu3O6+δ in terms of the measured multiple-quantum oscillation frequency spectrum, split quasi-2D Fermi surface, and spin zero angles revealed by the correlator, we compare the measured quantum oscillations in YBa2Cu4O8 with the Fermi surface model fit to the measured quantum oscillations in YBa2Cu3O6+δ (11, 16, 17). We consider a model in which cyclotron orbits are associated with a nodal bilayer split Fermi surface from charge ordering shown in Fig. 4. Here, the quantum oscillation frequency spread is associated with a splitting of the Fermi surface arising from tunneling between bilayers. Magnetic breakdown tunneling in the nodal region where the splitting is smallest can then give rise to a series of combination frequencies, which is discussed in refs. 16 and 28. Figs. 2 and 3 show that this model can simulate the angular and magnetic field dependence of the quantum oscillations measured in YBa2Cu4O8 reasonably well. The parameters used for the model simulation are, in fact, very similar to those used to simulate quantum oscillations measured in YBa2Cu3O6.56 (Table 1) (16). The small staggered twofold warping included in the case of YBa2Cu3O6.56 is not included for YBa2Cu4O8 given the restricted angular range over which quantum oscillations can be accessed and the likely weaker amplitude warping associated with a longer c axis. We note that there is some deviation from the model at a few of the highest angles. This deviation may be caused by additional lifting of degeneracy of frequency components from effects such as a distortion of the simple tetragonal crystal structure or other details of Fermi surface geometry beyond those considered in this model.

Fig. 4.

Fig. 4.

Brillouin zone cross-section showing a schematic of a nodal electron pocket created by charge ordering wave vectors Q1=2π(±δ1/a,0) and Q2=2π(0,±δ2/b) (11, 16, 17). A shows the two Fermi surface cross-sections of frequency F1=F02ΔFsplit and F6=F0+2ΔFsplit. The gap separating bonding and antibonding surfaces is expected to be smallest at the nodes (31). A cut through the kz=0 plane of the Brillouin zone shows the possible magnetic breakdown orbits (16, 28). B–D show the range of possible magnetic breakdown orbits (F2=F0ΔFsplit, F3=F0, F4=F0, and F5=F0+ΔFsplit) as listed in Table 1.

Discussion

Our findings, therefore, reveal closely similar quantum oscillation features in YBa2Cu4O8 compared with YBa2Cu3O6.56, showing (i) a similar quasiparticle effective mass from a Lifshitz–Kosevich fit to the amplitude dependence as a function of temperature, (ii) a spread of multiple frequencies, yielding a prominent beat structure, (iii) an angular dependence of quantum oscillation frequencies consistent with Fermi surface splitting accompanied by magnetic breakdown rather than fundamental neck and belly warping, and (iv) a similar value of m*g* from the angular dependence and spin zero observed in the correlator. The common Fermi surface features point to the same origin of Fermi surface reconstruction in YBa2Cu4O8 as in YBa2Cu3O6+δ, which is particularly relevant given the nonobservation of charge order signatures thus far in YBa2Cu4O8 (19). In the case of YBa2Cu3O6+δ, indications are that the electronic structure comprises a nodal electron pocket from Fermi surface reconstruction by a superstructure with orthogonal wave vectors Q1=2π(±δ1/a,0) and Q2=2π(0,±δ2/b) associated with charge order observed by X-ray diffraction and other experiments (where δ1δ20.3) (19, 20, 22).

An unusual aspect of the charge order measured in YBa2Cu3O6+δ is the short average correlation length, which has been measured to be of the order of 100Å in the basal plane and the order of 10Å along the c axis from X-ray diffraction measurements in a magnetic field of 17 T (20). The measured average correlation length in the basal plane is comparable with the cyclotron radius of 100200Å in the magnetic field range of 30100 T where quantum oscillations are measured (212). Moreover, given that the anisotropic Fermi velocity associated with the observed pocket has a magnitude along the c axis that is approximately two orders of magnitude lower than in the basal plane (28, 31, 32), the component of the cyclotron trajectory along the c axis is also well within the c-axis correlation length. The measured charge ordering wave vectors with finite correlation length measured up to 17 T are, therefore, consistent with the Fermi surface reconstruction observed by quantum oscillations in an applied magnetic field. We note that the correlation length inferred from X-ray diffraction experiments represents an average over all parts of the sample, thus representing a lower bound on the correlation length associated with the most highly ordered regions of the sample, which are accessed, for instance, by quantum oscillation measurements. It has remained unclear thus far whether the reported short correlation length is caused by the nucleation and pinning of charge order at impurity/defect sites or whether it is because of the disruptive effects of impurities/defects in an intrinsically long-range charge ordered state (33, 34).

Our findings in YBa2Cu4O8, where impurity pinning centers are reduced compared with YBa2Cu3O6+δ because of the fixed oxygen stoichiometry, suggest that charge order of inherently short correlation length arises in zero magnetic fields in YBa2Cu3O6+δ on account of impurity sites that act as pinning potential centers. Charge order in the well-known charge density wave material NbSe2 has, for instance, been shown to initially develop around impurities (35). In the case of YBa2Cu4O8, however, where such impurity pinning centers are reduced, applied magnetic fields are required to tilt the balance of energy scales, such that charge susceptibility is further enhanced, and charge order is revealed to reconstruct the Fermi surface.

Our findings point to a fragile form of charge order in the nonsuperconducting ground state of the underdoped cuprates, which is enhanced by applied magnetic fields to yield Fermi surface reconstruction. An interesting question pertains to the origin of such intrinsically fragile charge order. A contributing factor may be the potential unconventional character of the observed charge correlations (36). Furthermore, charge order may arise as a corollary to more robust correlations in the underdoped cuprates, such as underlying strong spin correlations (37). The interplay between these correlations may be manifested as other order parameters, such as Amperean order (38), pair density wave order (39), d-wave checkerboard order (40), and quadrupolar order (41, 42), which have also been proposed to appear in fluctuating form above the superconducting temperature.

Methods

Quantum oscillation simulations include conventional thermal, Dingle, and spin damping factors of the same form used for previous comparisons with quantum oscillations measured in the underdoped cuprates and other layered families of materials (30).

The thermal damping factor is given by

RT=XjsinhXj,

where Xj=2π2kBmθj*T/eB, kB is the Boltzmann factor, and T is the temperature; mθj*=mj*/cosθ (taken to be the same for all orbits, and the subscript j is dropped) is determined by the projection of B perpendicular to the planes (i.e., the projection parallel to the c^ axis in YBa2Cu3O6+x), and mj* refers to the value of mθj* when B is parallel to the crystalline c^ axis [taken to be a fixed quantity determined independently from temperature-dependent measurements (9)].

The Dingle damping factor is given by

RD=exp(ΛjBcosθ),

where Λj is a damping factor, which is taken to be the same for all orbits, enabling us to drop the subscript j (30).

The spin damping factor is given by

Rs=cos[π2(mθj*me)gθj*],

where the anisotropic effective g factor has the form gθj*=gj*cos2θ+1/ξjsin2θ. Here, gj* refers to the value of gθj* when B is parallel to the crystalline c^ axis, whereas ξj=(g*/g*)2 is the anisotropy in the spin susceptibility. Two sets of anistropic g factors are considered for subsets of the orbits defined below. Because of the multiple frequencies in the model and the restricted angular range measured, it is not possible to uniquely identify the g factors. The values of gj* and ξj here represent parameters used for the simulation.

A splitting of the Fermi surface arising from tunneling between bilayers leads to two starting frequencies that are denoted as F1=F02Fsplit and F6=F0+2Fsplit. Magnetic breakdown tunneling (in the nodal region where the splitting is smallest) gives rise to a series of combination frequencies F2,F3,F4,F5 as discussed in refs. 16 and 28. Only two sets of anisotropic g factors are considered: orbits F1, F2, F4, F5, and F6, which undergo both magnetic breakdown tunneling and reflection, are approximated to have the same g-factor g* with anisotropy ξ, whereas orbit F3, which shows only magnetic breakdown tunneling without reflection, is approximated to have a common g-factor g* with anisotropy ξ (16). The magnetic breakdown amplitude reduction factor is given by

RMB=(iP)lν(1P)lη,

in which lν and lη count the numbers of magnetic breakdown tunneling and Bragg reflection events en route around the orbit having transmitted amplitudes iP and 1P, respectively. The magnetic breakdown probability is given by P=exp(B0/Bcosθ), where B0 is the characteristic magnetic breakdown field (30).

Acknowledgments

We thank B. Keimer, S. A. Kivelson, M. le Tacon, P. A. Lee, C. Pépin, S. Sachdev, and T. Senthil for useful discussions. We also thank the National High Magnetic Field Laboratory personnel, including J. B. Betts, Y. Coulter, M. J. Gordon, C. H. Mielke, M. D. Pacheco, A. Parish, R. D. McDonald, D. Rickel, and D. Roybal, for experimental assistance. B.S.T., A.S., and S.E.S. acknowledge support from the Royal Society, the Winton Programme for the Physics of Sustainability, and the European Research Council (ERC) under European Union Seventh Framework Programme Grant FP/2007-2013/ERC Grant Agreement 337425. N.H., Z.Z., F.B., and B.J.R. acknowledge support for high-magnetic field experiments from US Department of Energy (DOE), Office of Science, Basic Energy Sciences (BES)-Materials Sciences and Engineering (MSE) Science of 100 Tesla Programme. G.G.L. acknowledges support from Engineering and Physical Sciences Research Council (EPSRC) Grant EP/K012894/1. Work at Northern Illinois University was supported by the Institute for Nanoscience, Engineering, and Technology. A portion of this work was performed at the National High Magnetic Field Laboratory, which is supported by National Science Foundation Cooperative Agreement DMR-0654118, the State of Florida, and the DOE.

Footnotes

The authors declare no conflict of interest.

This article is a PNAS Direct Submission.

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