Consider a statistical mechanical system (say the 1D Ising model) on a finite lattice of size N, and call the corresponding partition function (as a function of, say, real temperature and real magnetic field) Z(N)(t,h), where t is temperature and h - the magnetic field.
The partition function Z is analytic (in finite volume N) and doesn't admit any zeros. However, as soon as one passes to complex field h (or temperature, but let's consider complex field here), Z admits zeros on the unit circle S1 in C.
Call the set of zeros ZN, where N emphasizes finite lattice of size N. It is in general a nontrivial problem to decide whether the sequence of sets {ZN}N∈N accumulates on some set in S1, and if it does, to describe the topology of this limit set, which we'll call Z.
Now, suppose that for a given system we proved that there does indeed exist a nonempty set Z such that ZN→Z as N→∞ (in some sense - say in Hausdorff metric).
Is there a natural measure μ defined on Z that has physical meaning? If so, what sort of properties of this measure are physically relevant (say, relating to phase transitions)?
In my mind this is quite a natural question, because it translates into "Is there a natural way to measure the set where the system develops critical behavior?"
For example, one candidate would be the Hausdorff dimension. But I am interested more in something that would measure the density of zeros in a natural way (such as, for example, the density of states measure for quantum Hamiltonians).
EDIT: I know, of course, that the 1D Ising model is exactly solvable when interaction strength and magnetic field are constant. Here I implicitly assume that interaction (nearest neighbor, to keep it simple) and/or the magnetic field depend on lattice sites.
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