Skip to content
Transverse Field Ising Model

Transverse Field Ising Model

Introduction

The transverse field Ising model (TFIM) takes the classical Ising model — spins on a lattice coupled through their zz-components — and adds a magnetic field pointing perpendicular to that axis, along xx. This single addition turns a model that is secretly classical into a genuinely quantum-mechanical one, and makes the TFIM one of the simplest and most widely studied models of quantum magnetism and quantum phase transitions.

Why the ordinary quantum Ising model isn’t really quantum. Written with quantum spin operators, the “ordinary” Ising model with only a longitudinal coupling,

H0=Jzi,jSizSjz, H_0 = J_z \sum_{\langle i,j \rangle} S_i^z S_j^z ,

looks quantum mechanical, but is not, in any dynamical sense: every term of H0H_0 is built only from SzS^z operators, and SzS^z operators on different sites always commute with one another, so every term of the Hamiltonian commutes with every other. A sum of mutually commuting terms is automatically diagonal in the basis of classical spin configurations, so the eigenstates of H0H_0 are exactly the classical Ising configurations, with exactly the classical Ising energies — there is no tunneling between configurations, no superposition in the ground state, and no entanglement anywhere in the spectrum.

The transverse field changes everything. Adding a field along xx,

H=Jzi,jSizSjz+ΓiSix, H=J_{z} \sum_{\langle i,j \rangle} S_i^z S_j^z + \Gamma \sum_i S_i^x,

breaks this: SixS_i^x does not commute with SizS_i^z on the same site, so the two terms of HH can no longer be diagonalized simultaneously. Its eigenstates become genuine superpositions of classical spin configurations connected by single-spin flips (since SxS^x flips a spin between up and down), giving the model real quantum dynamics, ground-state entanglement, and, as discussed below, a genuine quantum phase transition — none of which is present at Γ=0\Gamma = 0.

Here, the first sum runs over pairs of nearest neighbors and Γ\Gamma is called the transverse field. In 1D, the system becomes critical at Γ/Jz=12\Gamma/J_z = \frac{1}{2} (see below). At Γ=0\Gamma = 0 the ground state reduces to the classical Ising ground state: antiferromagnetic for Jz>0J_z > 0 and ferromagnetic for Jz<0J_z < 0.

A testbed for quantum computing and quantum simulation. Because it is the simplest lattice model with both a classical limit and a tunable, non-commuting quantum term, the TFIM has become a standard benchmark well beyond condensed matter theory:

  • It is the natural target Hamiltonian for quantum annealers: the transverse field provides exactly the quantum tunneling between classical configurations that drives the annealing process (Kadowaki and Nishimori (1998)), and devices such as D-Wave’s quantum annealers are built around Ising-type Hamiltonians with a controllable transverse field.
  • It is one of the first nontrivial Hamiltonians realized on analog quantum simulators — arrays of Rydberg atoms, trapped ions, and superconducting-qubit devices — precisely because it is simple enough to engineer directly, yet rich enough to display a genuine quantum phase transition.
  • It is a standard first example in courses and textbooks introducing quantum algorithms: its two terms are exactly the two non-commuting building blocks (a diagonal “problem” Hamiltonian and a transverse-field “mixer” Hamiltonian) used in quantum annealing and the quantum approximate optimization algorithm (QAOA).

Physics of the model

A single spin already shows why order is destroyed. Before tackling the full lattice, it helps to look at a single spin in a transverse field, H=ΓSxH = \Gamma S^x. The eigenstates of SxS^x are the equal-weight superpositions ±x=12( ⁣± ⁣)|{\pm x}\rangle = \frac{1}{\sqrt{2}}(|\!\uparrow\rangle \pm |\!\downarrow\rangle), so whichever of these is the ground state (depending on the sign of Γ\Gamma), it has Sz=0\langle S^z \rangle = 0 exactly. A single spin in a transverse field can never point along zz, because SzS^z simply is not a conserved, sharply defined quantity once Γ0\Gamma \neq 0. This is the microscopic seed of everything that follows: switch on Γ\Gamma anywhere in the lattice and it constantly tries to randomize each spin’s zz-orientation, competing directly against the ordering tendency of JzJ_z.

Limiting cases. At Γ=0\Gamma = 0 the model reduces exactly to the classical Ising model discussed on the Ising Model page: the ground state is a classical antiferromagnetic or ferromagnetic pattern, doubly degenerate, since flipping every spin at once costs no energy. At Γ\Gamma \to \infty, the field term dominates completely and the ground state becomes a single, non-degenerate product state with every spin polarized along +x+x — a featureless quantum paramagnet with Siz=0\langle S_i^z \rangle = 0 on every site and no order of any kind. The interesting physics — the quantum phase transition described below — happens at intermediate Γ\Gamma, where neither limit is a good description and the two competing tendencies are of comparable strength.

Exact solution via the Jordan-Wigner transformation. What makes the 1D transverse field Ising model special, and such a popular first example to study, is that it can be solved exactly for any Γ\Gamma and JzJ_z, not just in the two limits above. The trick, due to Jordan and Wigner, is to rewrite the spin-1/2 operators as fermion creation and annihilation operators, each dressed with a nonlocal “string” built from all the spins that precede it along the chain — a bookkeeping device needed because fermions anticommute while spin operators on different sites commute. In terms of these fermions, the Hamiltonian turns out to be quadratic: a model of free fermions hopping and pairing on the lattice, with no interactions left between them at all. Any such quadratic fermionic Hamiltonian can be diagonalized exactly by a further change of variables (a Bogoliubov transformation), yielding an explicit single-particle dispersion relation ϵ(k)\epsilon(k) for the fermionic excitations as a function of Γ\Gamma and JzJ_z. This exact solution (Pfeuty (1970)) is what gives the precise critical ratio Γ/Jz=12\Gamma/J_z = \frac{1}{2} quoted above: it is exactly the point where the excitation gap minkϵ(k)\min_k \epsilon(k) closes, signaling the phase transition.

Domain walls and spin flips: two faces of the same excitation. The Jordan-Wigner fermions have a direct, physically intuitive interpretation in terms of the original spins. Deep in the ordered phase (ΓJz\Gamma \ll J_z), flipping a single spin relative to the ordered background does not create one defect but two domain walls — one on each side of the flipped spin — each separating a stretch of one magnetization sign from a stretch of the other; it is the transverse field that lets these domain walls subsequently hop along the chain, one lattice site at a time, and lets pairs of them be created or annihilated. Deep in the disordered phase (ΓJz\Gamma \gg J_z), the same fermionic quasiparticle is more naturally pictured instead as a single spin flipped away from the fully xx-polarized background. These are simply two limiting descriptions of one and the same particle-like excitation: its energy gap shrinks continuously as Γ\Gamma approaches Γc\Gamma_c from either side, and vanishes exactly at the transition, where the excitations become gapless and the low-energy physics turns scale-invariant.

A quantum model in dd dimensions is a classical model in d+1d+1 dimensions. More generally, in any number of spatial dimensions dd, the dd-dimensional quantum TFIM can be mapped onto a (d+1)(d+1)-dimensional classical Ising model. The extra dimension represents imaginary time: splitting the quantum-mechanical operator eβHe^{-\beta H} into many thin slices and inserting a complete set of classical spin configurations between each one (a Suzuki-Trotter decomposition) turns the quantum partition function into that of an ordinary classical Ising model living on a (d+1)(d+1)-dimensional lattice, with the transverse field controlling how strongly neighboring time slices are coupled to one another. This quantum-to-classical correspondence is both a conceptual bridge back to the purely classical Ising Model page, and the practical reason the quantum Monte Carlo methods described below work at all: they sample configurations of the equivalent classical model in one higher dimension, exactly as the classical Ising model’s own Monte Carlo methods sample classical spin configurations directly. At the 1D TFIM’s quantum critical point specifically, space and imaginary time in fact enter on a completely equal footing, so the transition there is equivalent to the ordinary 2D classical Ising model exactly at its critical point.

Phenomena

Quantum phase transitions vs. classical phase transitions. The classical Ising model’s phase transition is driven by temperature: raise TT high enough and thermal fluctuations always eventually destroy order, however strong the coupling JJ. The TFIM’s phase transition is fundamentally different in kind — it occurs at exactly T=0T=0, where there are no thermal fluctuations at all, and is driven instead purely by the strength of the transverse field Γ\Gamma, i.e. by quantum fluctuations of the kind introduced above. Formally, this shows up as a qualitative change in the character of the ground state itself as Γ\Gamma is tuned through Γc\Gamma_c — a phenomenon that only becomes truly sharp (mathematically non-analytic) in the limit of an infinite lattice, exactly as for the classical transition.

  • For Γ<Γc\Gamma < \Gamma_c, the system is in an ordered phase: the JzJ_z term wins, and the ground state spontaneously breaks the model’s Z2\mathbb{Z}_2 symmetry — the symmetry SizSizS_i^z \to -S_i^z on every site simultaneously, under which the Hamiltonian is invariant but an ordered state is not — to pick out one of the two possible ordered configurations.
  • For Γ>Γc\Gamma > \Gamma_c, the system is in a disordered phase: the field term wins, quantum fluctuations dominate throughout the lattice, and the Z2\mathbb{Z}_2 symmetry is restored, so Siz=0\langle S_i^z \rangle = 0 everywhere, just as for a single spin in a transverse field.

Order parameter and spontaneous symmetry breaking. The natural order parameter is the same one used for the classical Ising model, m=Sizm = \langle S_i^z \rangle: it vanishes throughout the disordered phase and grows continuously from zero as Γ\Gamma is lowered through Γc\Gamma_c — again a continuous (second-order) transition, just as in the classical model, but now as a function of Γ\Gamma rather than TT. There is a subtlety worth knowing if you plan to compute this numerically: on any finite lattice, the Z2\mathbb{Z}_2 symmetry cannot truly be broken, so the two ordered configurations mix into symmetric and antisymmetric combinations that form the ground state and the first excited state, split by an energy gap that shrinks exponentially fast as the lattice grows. Only in the thermodynamic limit does this splitting vanish completely and true symmetry breaking, with a genuinely nonzero order parameter, become possible. This finite-size splitting is directly visible in the low-lying spectra computed in the ED-04 tutorial below, and is a useful, very general diagnostic for spontaneous symmetry breaking in any finite-size numerical study.

Quantum criticality. Near Γc\Gamma_c, the correlation length ξ\xi — roughly, how far correlations between spins extend along the lattice — diverges as ξΓΓcν\xi \sim |\Gamma - \Gamma_c|^{-\nu}, exactly as for a classical continuous transition tuned by temperature. But because the transition is quantum, there is now also a correlation time that diverges in an analogous way, ξτξz\xi_\tau \sim \xi^{z}, characterized by a dynamical critical exponent zz that has no classical-transition analogue. The quantum-to-classical mapping above shows that the 1D TFIM’s quantum critical point is equivalent to the 2D classical Ising critical point, with space and imaginary time entering symmetrically; correspondingly this quantum critical point has z=1z=1, and shares the exact same critical exponents as the classical 2D Ising transition on the Ising Model page — for instance ν=1\nu = 1 and η=1/4\eta = 1/4, the same value of η\eta extracted numerically in the MC-07 tutorial for the purely classical model.

Universality beyond the Ising model itself. Because it is the simplest model with a Z2\mathbb{Z}_2-symmetric ordered phase and a continuous quantum phase transition driven by a single tuning parameter, the TFIM’s universality class describes the low-energy physics of many other systems that look quite different microscopically — including certain structural (ferroelectric) phase transitions, quantum magnets with strong easy-axis anisotropy, and, more abstractly, any system whose relevant low-energy physics reduces to a single fluctuating two-state degree of freedom competing against an ordering interaction. This is exactly the same phenomenon of universality already introduced for the classical model, now extended across the quantum-classical correspondence.

Methods

The 1D transverse field Ising model is exactly solvable (Pfeuty (1970)). Beyond 1D, and for properties not accessible from the exact solution (such as finite-size spectra away from the thermodynamic limit), numerical methods are needed:

MethodStrengthsLimitationsApplications
ED — see sparsediagExact results for small systems; captures the full quantum spectrum, including entanglementLimited to small systems, since the Hilbert space grows as 2N2^NFinite-size spectra and critical/CFT data; benchmarking other methods
QMC — see Stochastic Series ExpansionHandles much larger systems; gives access to finite-temperature propertiesRequires a QMC code that supports an external field (e.g. dirloop_sse, not looper); statistical rather than systematic errorsPhase diagrams; finite-temperature properties; large 2D/3D systems

Two tutorials work through the critical transverse field Ising chain directly:


For an overview of the other models in ALPS, see Models in ALPS.