
[HMSH15,HS12]. For the recurrence of 𝑝-walks, a process that interpolates between random and
rotor walks, see also [HLSH18]; a generalization of 𝑝-walks on higher dimensional lattices has been
considered in [Cha23], where the author investigates the recurrence and transience behaviour of the
process. On state spaces other than ℤ, where the simple random walk is recurrent, the behaviour
of random rotor walks is not completely understood.
Stabilization of i.i.d. sandpiles. A sandpile on a graph 𝐺is a function 𝜎:𝐺→ℕ0, where for 𝑥∈𝐺,
𝜎(𝑥) represents the number of grains of sand present at site 𝑥. The sandpile 𝜎is stable if for each
𝑥,𝜎(𝑥) is strictly less than the number of neighbours of 𝑥in 𝐺. If at some vertex 𝑥the sandpile
𝜎(𝑥) has some number of grains greater or equal to the number of neighbours of 𝑥, then 𝜎(𝑥) is
unstable and topples by sending one grain of sand to each of the neighbours. The toppling at 𝑥
can create other unstable vertices, and we say that 𝜎stabilizes if we can reach a stable sandpile
configuration containing only stable vertices by toppling each vertex finitely many times, and 𝜎is
then called stabilizable. If the heights (𝜎(𝑥))𝑥∈𝐺are independent and identically distributed (i.i.d.)
random variables, we refer to 𝜎as an i.i.d. sandpile. Conditions for sandpiles at critical density1on
ℤ2were investigated in [HJL19, Theorem 1], where it is shown that an i.i.d. sandpile with E[𝜎(0)]
slightly less than 3 cannot stabilize almost surely unless 𝜎(𝑥)≤3 with high probability. We are not
aware of state spaces other than ℤ𝑑where necessary and sufficient conditions for i.i.d. sandpiles to
stabilize are given.
Rotor walks and sandpiles. While both processes may be seen as approaches to distribute chips
and move particles on a graph, another relation between them may not be obvious at first sight.
Indeed, there is another natural relation between these two processes, in terms of group actions.
In particular, for any finite graph one can define a rotor-router group with elements being the set
of acyclic rotor configurations, where a configuration is called acyclic if the rotors do not form a
directed cycle. On the same graph, over the set of stable sandpile configurations, one can define
in a natural way a Markov chain, by adding one chip uniformly at random and stabilizing. The
set of recurrent states for this Markov chain is a group, with group operation given by pointwise
addition followed by stabilization. This group is called the sandpile group or the critical group and
it acts transitively on the rotor-router group. These two groups are also isomorphic; we refer to
[HLM+08] and the references there for a beautiful exposition and more details in this direction.
Our contribution. We consider rotor walks and i.i.d. sandpiles 𝜎on the doubly infinite Sierpin´ski
gasket graph 𝖲𝖦 with fixed vertex 𝑜= (0,0) as in Figure 1. Our motivation for looking at such
state spaces comes from physics, because Abelian sandpiles on Sierpin´ski gasket graphs have been
considered by physicists for more than 20 years ago in [DPV01,DV98,KUZMS96], where several
predictions and conjectures have been made. While the conjectures are still lacking mathematical
proofs, there has been some recent progress on the limit shape for the Abelian sandpile on 𝖲𝖦 in
[CKF20]. For recent results on the identity element of the sandpile group and bounds on the speed
of convergence to stationarity of the Abelian sandpile Markov chain on 𝖲𝖦 see [KSHW24]; for the
scaling limit of the identity element, see also [KSH24].
We denote by (𝑅𝑡)𝑡∈ℕthe rotor walk with random initial configuration of rotors on the doubly-
infinite Sierpin´ski gasket graph 𝖲𝖦. If at the beginning of the process, for each 𝑥∈𝖲𝖦, the rotor
at 𝑥is uniformly distributed on the neighbours of 𝑥, that is, it points to each of the neighbours
with the same probability, then we call (𝑅𝑡)𝑡∈ℕuniform rotor walk, shortly 𝖴𝖱𝖶. It is not known
1On ℤ𝑑, the authors of [FdBR05] consider the case of 2𝑑particles at a site as stable, hence a shift in their results,
and they prove that a necessary condition for an i.i.d. sandpile to stabilize is E[𝜎(0)] ≤2𝑑−1, but this condition is
not sufficient for stabilization.
2