Published online by Cambridge University Press: 29 May 2025
The six-vertex model, or the square ice model, with domain wall boundary conditions (DWBC) has been introduced and solved for finite n by Korepin and Izergin. The solution is based on the Yang–Baxter equations and it represents the free energy in terms of an n × n Hankel determinant. Paul Zinn-Justin observed that the Izergin–Korepin formula can be expressed in terms of the partition function of a random matrix model with a nonpolynomial interaction. We use this observation to obtain the large n asymptotics of the six-vertex model with DWBC. The solution is based on the Riemann–Hilbert approach. In this paper we review asymptotic results obtained in different regions of the phase diagram.
1. Six-vertex model
The six-vertex model, or the model of two-dimensional ice, is stated on a square lattice with arrows on edges. The arrows obey the rule that at every vertex there are two arrows pointing in and two arrows pointing out. This rule is sometimes called the ice-rule. There are only six possible configurations of arrows at each vertex, hence the name of the model; see Figure 1.
We will consider the domain wall boundary conditions (DWBC), in which the arrows on the upper and lower boundaries point into the square, and the ones on the left and right boundaries point out. One possible configuration with DWBC on the 4 × 4 lattice is shown on Figure 2.
The name of the square ice comes from the two-dimensional arrangement of water molecules, H2O, with oxygen atoms at the vertices of the lattice and one hydrogen atom between each pair of adjacent oxygen atoms. We place an arrow in the direction from a hydrogen atom toward an oxygen atom if there is a bond between them. Thus, as we already noticed before, there are two in-bound and two out-bound arrows at each vertex.
Figure 1. The six arrow configurations allowed at a vertex.
Figure 2. An example of a 4 x 4 configuration (left) and the corresponding ice crystal (right).
For each possible vertex state we assign a weight wi, i =1, ...., 6, and define, as usual, the partition function, as a sum over all possible arrow configurations of the product of the vertex weights,
where Vn is the n × n set of vertices,σ (x)∈{1,...,6} is the vertex configuration of σ at vertex x according to Figure 1, and Ni (σ) is the number of vertices of type i in the configuration σ.
To save this book to your Kindle, first ensure no-reply@cambridge.org is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.
Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.
Find out more about the Kindle Personal Document Service.
To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.
To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.