Natural orbital networks
Abstract
Given a finite set T of maps on a finite ring R, we look at the finite simple graph G=(V,E) with vertex set V=R and edge set E=(a,b) | exists t in T, b=t(a), b not equal to a. An example is when R=Zn and T consists of a finite set of quadratic maps Ti(x)=x2+ai. Graphs defined like that have a surprisingly rich structure. This holds especially in an algebraic set-up when T is generated by polynomials on Zn. The characteristic path length L and the mean clustering coefficient C are interlinked by global-local quantity LC=-L/log(C) which often appears to have a limit for n to infinity like for two quadratic maps on a finite field Zp. We see that for one quadratic map x2+a, the probability to have connectedness goes to zero and for two quadratic maps, the probability goes to 1, for three different quadratic maps x2+a,x2+b,x2+c on Zp, we always appear to get a connected graph for all primes.
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