Separation of Time Scales in Weakly Interacting Diffusions
Arch. Rational Mech. Anal. (2026) 250:33
Digital Object Identifier (DOI) https://doi.org/10.1007/s00205-026-02180-w
Separation of Time Scales in Weakly
Interacting Diffusions
Zachary P. Adams, Maximilian Engel & Rishabh S. Gvalani
Communicated by M. Hairer
Abstract
We study metastable behaviour in systems of weakly interacting Brownian particles with localised, attractive potentials which are smooth and globally bounded.
In this particular setting, numerical evidence suggests that the particles converge
on a short time scale to a “droplet state” which is metastable, i.e. persists on a much
longer time scale than the time scale of convergence, before eventually diffusing to
0. In this article, we provide rigorous evidence and a quantitative characterisation
of this separation of time scales. Working at the level of the empirical measure, we
show that (after quotienting out the motion of the centre of mass) the rate of convergence to the quasi-stationary distribution, which corresponds with the droplet state,
is O(1) as the inverse temperature β → ∞. Meanwhile the rate of leakage away
from its centre of mass is O(e−β ). Furthermore, the quasi-stationary distribution is
1
localised on a length scale of order O(β − 2 ). Our proofs rely on understanding the
large β-asymptotics of the first two eigenvalues of the generator, which we study
using techniques from semiclassical analysis. We thus provide a partial answer to a
question posed by Carrillo et al. (see Aggregation–diffusion equations: dynamics,
asymptotics, and singular limits. Active particles. Advances in theory, models, and
applications, modeling and simulation in science, engineering and technology, vol
2, pp 65–108, Birkhäuser/Springer, Cham, 2019, Section 3.2.2) in the microscopic
setting.
1. Introduction
Consider the following system of weakly interacting diffusions
dX ti = −
N
1
j
∇W X ti − X t dt + 2β −1 dBti ,
N
i=1
(1.1)
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N , N ∈ N, represent the positions of N exchangeable particles (or
where (X ti )i=1
agents or spins), taking values in some smooth manifold , W is a smooth even
N are N ininteraction potential with well-behaved growth properties, and (Bti )i=1
dependent Brownian motions.
Depending on the choice of the interaction potential W , the system in (1.1)
can exhibit a wide variety of interesting dynamical phenomena. We are particularly
interested in the case in which W is attractive (i.e. ∇W (x)·x 0), globally bounded,
and has smooth and globally bounded derivatives of all orders. In this situation the
pairwise attraction mediated by W competes with the diffusive behaviour produced
by the independent Brownian motions. This competition is most easily observed at
the level of the thermodynamic limit N → ∞ when is bounded. Consider the
empirical measure μtN of the system (1.1), which is defined as
μtN :=
N
1
δXi .
t
N
i=1
Then, assuming W is sufficiently well-behaved, it is well-known (see, for example,
[45]) that we have the estimate
1
sup E d22 μt , μtN ,
N
t∈[0,T ]
for any T < ∞, where d2 (·, ·) is the 2-Wasserstein distance and μt is the unique
distributional solution of the nonlocal parabolic PDE
∂t μt = β −1 μt + ∇ · (μt ∇W ∗ μt ) ,
(1.2)
often referred to as the McKean–Vlasov equation. The above PDE can exhibit the
phenomenon of phase transitions (see [14,18]): for β sufficiently small, Eq. (1.2) has
a unique steady state (in the space of probability measures) while for β sufficiently
large, Eq. (1.2) possesses multiple steady states. This switch between one and
multiple steady states for (1.2) is caused exactly by the aforementioned competition
between the diffusive behaviour produced by the Laplacian, which dominates in
the β 1 regime and the tendency to aggregate due to the nonlocal drift, which
prevails in the β 1 regime.
The Setting: Bounded Potential on Unbounded Domain
In this article, we are interested in the setting of = Rd . Since W and all its
derivatives are assumed to be bounded, solutions of (1.2) are not uniformly tight
and the equation has no steady states which are probability measures. A proof of
this can be found in [13, Theorem 3.1].
Even though (1.2) has no steady states, the competition between the diffusive
and attractive terms manifests itself in a different manner. Numerical experiments
(see [12, Figure 8]) suggest that if the potential W is sufficiently localised, β 1,
and the initial datum is well-prepared, then solutions of (1.2) appear to converge to
a localised droplet state and stay close to it for a very long time before eventually
Arch. Rational Mech. Anal. (2026) 250:33
Page 3 of 36 33
Fig. 1. A schematic depiction of dynamical metastability: the coloured paths represent trajectories of a dynamical system which can be divided into a regime of fast convergence
towards the slow submanifold M (red), and slow motion along M (blue)
converging to 0, as expected. Thus, there is a separation of time scales between
convergence to the droplet state and the eventual escape of mass to infinity and
convergence to 0. This separation is an instance of what is commonly referred to
as dynamical metastability, wherein solutions of a dissipative dynamical system
converge on a fast time scale to a submanifold of its state space, along which the
time evolution is slow. We refer the reader to Fig. 1, where we provide a simple
schematic sketch of this phenomenon, which has been studied in the context of other
equations as well, such as reaction–diffusion equations including the Allen–Cahn
equation (see [3,10,17,28,36]) or the Cahn–Hilliard equation (see [8,26,44]). We
also point the reader to [12, Section 3.2.2] for a more detailed discussion of this
phenomenon in the context of (1.2).
Absence of Invariant Probability Measure for The Particle System We are
studying this separation of time scales as it shows up in the corresponding particle
system. In analogy to the absence of steady states for the thermodynamic limit,
the particle system (1.1) does not have an invariant probability measure under our
assumptions. To see this, consider the Fokker–Planck equation associated to the
law ρt (x) dx of (1.1),
∂t ρt = β −1 ρt + ∇ · (ρt ∇ H N ),
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where the Hamiltonian H N : (Rd ) N → R is given by
H N (x) :=
N
1
W (xi − x j ).
2N
i, j=1
We define f t := ρt eβ HN and observe that it solves the following equation
∂t f t = β −1 f t − ∇ H N · ∇ f t
= β −1 eβ HN ∇ · (e−β HN ∇ f t ).
Multiplying by f t and integrating by parts against the measure e−β HN (x) dx, we
obtain the estimate
d
| f t |2 e−β HN (x) dx = −2β −1
|∇ f t |2 e−β HN (x) dx.
dt (Rd ) N
(Rd ) N
We now use the fact that W is globally bounded by some constant K < ∞ along with
the Nash inequality [35] to assert that there exists a constant C = C(N , d, K , β)
such that
N d+2
Nd
d
| f t |2 e−β HN (x) dx −C
| f t |2 e−β HN (x) dx
.
dt (Rd ) N
(Rd ) N
Appl (...truncated)