7. Quantum-to-Classical Mapping#
In this final section, we introduce a general technique that essentially enables us to map any quantum lattice system in \(d\) dimensions to a classical partition function in \(d+1\) dimensions, up to some caveats that we will return to at the end of this section.
7.1. Suzuki-Trotter decomposition#
Remember that thermal expectation values are given by
with the thermal partition function \(Z(\beta)\) given by
The ground state physics is encoded in the limit \(\beta \to \infty\). Note that, if the system has a unique ground state, we can obtain the ground state \(\ket{\Psi_0}\) of a quantum system by starting from essentially a random state \(\ket{\Phi}\) and evolving it in imaginary time \(\tau = -\mathrm{i} t\) for sufficiently long
Expanding the initial state \(\ket{\phi}\) in the energy eigenbasis of \(\hat{H}\), we see that the only condition is that it is not orthogonal to the ground state (subspace). In addition, the ground state will be well approximated if \(\tau \Delta E \gg 1\), with \(\Delta E=E_1 - E_0\) the energy gap. This imaginary time evolution also forms the basic ingredient of several numerical algorithms for approximating ground states of quantum many body systems, often in combination with the Suzuki-Trotter decomposition which is introduced below.
Using this approach, the following expression for the ground state expectation value of on operator \(\hat{O}\) is obtained
This expression can be compared to the thermal expectation value with \(\beta = 2\tau\); the only difference is in the boundary conditions.
For a quantum many body system, taking the exponential is as hard as determining the full diagonalisation of the hamiltonian, which is impossible due to the exponentially large Hilbert space. If the hamiltonian is a sum of local terms, each of these terms can be exponentiated easily, but for arbitrary \(\tau\) there is no relation ship between \(\exp(-\tau \sum_{i} \hat{h}_i)\) and the individual \(\exp(-\tau \hat{h}_i)\), unless the different \(\hat{h}_i\) commute. However, for an infinitesimal time step \(\epsilon\), we can use to Baker-Campbell-Hausdorff formula (or better yet, the Zassenhaus formula) to obtain
This then leads to the Suzuki-Trotter decomposition
The product in the final expressions requires chosing a specific order, exactly because the terms \(\hat{h}_i\) and thus also the factors \(\mathrm{e}^{-\frac{\tau}{M} \hat{h}_i}\) do not commute. The approximation and error term are valid for arbitrary choices of ordering, but different orderings are not equivalent. Particular choices can be more suitable for particular purposes. Furthermore, note that splitting the time interval \([0,\tau]\) into small segments \(\epsilon = \tau/M\) is also the starting point for deriving a path integral representation of the quantum partition function. The next step is to insert a resolution of the identity in between the \(N\) different factors, where the labels of the basis will behave as classical degrees of freedom. For obtaining a path integral, the basis should be labeled by a number of continuous degrees of freedom, which can then become continuous functions of time in the limit \(\epsilon\to 0\). Here, instead, we will keep \(\epsilon\) small but finite, and use a discrete basis.
7.2. From quantum to statistical mechanics#
Let’s start with a quantum system in \(d=0\), i.e. a small number of spins, or in particular, a single spin, described by a hamiltonian
While we could in principle exponentiate \(\hat{H}\) directly as it is a \(2 \times 2\) matrix, we will treat it using the Suzuki-Trotter decomposition. Throughout the remainder of this section, we will use the \(\sigma^z\) basis, which we denote as \(\ket{1} = \ket{\uparrow}\) and \(\ket{-1} = \ket{\downarrow}\). Inserting resolutions of the identity, we write
with \(s_{M+1} = s_1\), \(M\epsilon =\beta\), and where
where the parameters in the last line are given by \(K= -\frac{1}{2}\log \tanh(\epsilon h_x)\), \(h = \epsilon h_z\) and \(f_0 =\frac{1}{2}\log[\cosh(\epsilon h_x)\sinh(\epsilon h_x)]\).
We thus obtain
the partition function of the one-dimensional classical Ising model with periodic boundary conditions. Indeed, \(\braket{s_{i}|\mathrm{e}^{-\epsilon H}|s_{i+1}}\) does exactly correspond to the transfer matrix, and diagonalising the transfer matrix is the most straightforward approach to solving the one-dimensional classical Ising model.
7.3. Higher dimensional generalisation#
We now apply the same approach to the Ising model with both transverse and longitudinal field in \(d\) dimensions, on a hypercubic lattice. We separate the hamiltonian in two parts according to
Note that \(\hat{H}_1\) and \(\hat{H}_2\) in itself contain commuting terms, but of course don’t mutually commute. We follow the same strategy, and will in every (imaginary) time step introduce a resolution of the identity using the tensor product \(\sigma^z\) basis. We now denote the basis at time step \(k\) as \(\ket{\{s_{i,k}\}}\), where \(i\) labels a site in the \(d\) dimensional lattice hosting the quantum degrees of freedom, and \(k\) labels points along the imaginary time axis, which emerges as a new dimension in the problem. We find
as \(\hat{H}_1\) is diagonal in this basis, and
with \(K_\perp = \log \tanh(\epsilon h_x)\) as before. Here, we have now ignored an overall proportionality factor, which is irrelevant when using the partition function to compute expectation values. With this, we find
with \(K_{\parallel} = \epsilon J\) and \(h = \epsilon h_z\). We thus find the partition function of the classical Ising model in \(d+1\) dimensions with anisotropic interaction strengths, periodic boundary condition in the imaginary time direction and a number of sites in the time direction given by \(M = \beta/\epsilon\). Hence, the ground state regime \(\beta\to \infty\) corresponds to the thermodynamic limit in this additional time direction of the corresponding classical system, so that there are many similarities (or actually, equivalences) between between quantum phenomena in \(d\) dimensions and classical phenomena in \(D=d+1\) dimensions. On the other hand, when the quantum system is at finite temperature \(\beta\), the additional dimension is finite and never in the thermodynamic limit. In that case, this extra dimension cannot cause new non-analyticities in the partition function and finite temperature quantum systems in \(d\) dimensions are very similar to classical systems in \(d\) dimensions.
This quantum to classical mapping can also be inverted. Taking a codimension \(1\) slice out of a \(D\)-dimensional classical partition function, one obtains a transfer matrix which can be interpreted as the exponential of a quantum hamiltonian acting on the Hilbert space of a \(d=D-1\) dimensional quantum system. Hence, methods for targetting quantum ground states in \(d\) dimensions can also be used to study problems in \((d+1)\)-dimensional classical statistical mechanics.
It is clear that the quantum to classical mapping is not specific to the quantum Ising model and can be applied to any hamiltonian. The path integral representation of the partition function fits within the same scheme, and only differs in the fact that the limit \(\epsilon\to 0\) is taken such that the additional dimension becomes continuous. This is particularly natural if also the spatial dimensions of the quantum dimension are continuous, i.e. if we have a quantum field theory. In this case, a \(D=d+1\) dimensional classical statistical field theory is obtained. For relativistic quantum field theories, where it is common practice to explicitly count the time dimension together with the space dimensions, imaginary time evolution leads to an action, which is equivalently a hamiltonian of a classical field theory in \(D=d+1\) spatial dimensions, with full Euclidean invariance.
One might thus wonder if there is anything new to be learned from studying quantum ground states. First of all, there is one important catch which we have overlooked so far. There is no guarantee that the above process yields a classical partition function with Boltzmann weights which are positive, or even real. While this may seem like a technical detail, it is of major importance. The quantum to classical mapping is the basis behind the Quantum Monte Carlo method, one the most successful numerical methods for studying quantum many body systems. One maps the quantum problem to a classical partition function and then uses one of the many flavours of Monte Carlo sampling. However, with non-positive Boltzmann weights, the interpretation of a probability distribution is lost and no efficient sampling procedure can be designed, as samples might annihilate each other. This is known as the sign problem.
Secondly, for many non-relativistic quantum systems, the anisotropy between the imaginary time direction and the spatial dimensions in the corresponding classical system cannot be ignored, even at the critical point. In those cases, critical correlations behave differently in the spatial and the time direction, which is characterised by a dynamical critical exponent \(z\). The case \(z=1\) corresponds to the case where the critical point has (emergent) rotation/Lorentz invariance between time and space.
A final reason to study quantum systems directly is that certain concepts are more natural in that setting. In particular, the last 15 years, ideas from quantum information theory, and in particular the concept of entanglement, have made their way into the standard toolbox to study and characterize quantum many body systems.