Lieb's square ice constant
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| Representations | |
|---|---|
| Decimal | 1.53960071783900203869106341467188… |
| Algebraic form | |

Lieb's square ice constant is a mathematical constant used in the field of combinatorics to approximately count Eulerian orientations of grid graphs. It was introduced by Elliott H. Lieb in 1967.[1] It is called the square ice constant because the orientations that it counts arise in statistical mechanics of crystalline structures as the states of an ice-type model on a square grid.
The value of Lieb's square ice constant is Based on this, the number of Eulerian orientations of an grid is where the term, an instance of little o notation, hides parts of the formula that tend to zero in the limit as grows.
An grid graph has vertices. When constructed with periodic boundary conditions (with edges that wrap around from left to right and from top to bottom) it has edges and is 4-regular, meaning that each vertex has exactly four neighbors. An orientation of this graph is an assignment of a direction to each edge. It is an Eulerian orientation if it gives each vertex exactly two incoming edges and exactly two outgoing edges. An Eulerian orientation can be constructed by orienting each row of the grid (including the wraparound edge) as a cycle, and each column as another cycle, but there are many more orientations that are not of this special form.
Denote the number of Eulerian orientations of this graph by . Then this number is approximately exponential in , with Lieb's square ice constant as the base of the exponential. More precisely, is Lieb's square ice constant.[2] Lieb used a transfer-matrix method to compute this exactly.[1]