A Gallery of
Mathematical Research


Single-source sandpile on Z² · final configurations for 53 to 1,299,052 grains · drawn at the same size

Random walks with memory

A random walk with memory chooses each step using its own past, such as the sites or edges it has already visited, so its position alone is not a Markov chain. The basic questions are whether the walk is recurrent or transient, how far it travels in \(n\) steps, and the shape of the set of sites it visits.

Abelian sandpile

The abelian sandpile was introduced by Bak, Tang and Wiesenfeld as a model of self-organized criticality. A vertex of a graph holding at least as many grains as its degree topples, sending one grain along each of its edges, and the final configuration does not depend on the order of the topplings (Dhar). The basic questions concern the avalanches caused by adding one grain to a configuration in the stationary state, and the large-scale shape of the stable configuration produced by a large initial pile.

Quantitative homogenization

Homogenization describes the large-scale behavior of differential equations with random or periodic coefficients, and of the associated diffusions: on large scales they behave like equations with constant effective coefficients. Quantitative homogenization gives rates for this approximation. When the coefficients are unbounded or have long-range correlations, the effective coefficients can grow or decay with the scale, and the diffusion can be superdiffusive or subdiffusive.

Brownian motion in a log-correlated potentialAt weak disorder and in every dimension \(d\ge2\), a Brownian particle whose drift is the gradient of a log-correlated potential has a unique scaling limit, whose path law is singular with respect to every mixture of Brownian motions. Quantitative Einstein relationFor a reversible diffusion in a random environment under a small constant force \(\lambda e_1\), the asymptotic velocity divided by \(\lambda\) converges to \(\Sigma_X e_1\), where \(\Sigma_X\) is the effective diffusivity of the unforced diffusion; for almost every environment, the error is at most \(\lambda^{\beta^*}\) for all \(\lambda\) below a random threshold, with a deterministic exponent \(\beta^*(d)\in(0,1/4)\). Critical long-range random conductance walkAt the critical exponent, for almost every realization of the conductances, the random walk converges to Brownian motion under the anomalous \(\sqrt{t\log t}\) scaling, with an effective diffusivity determined by the mean conductance alone. Brownian motion in an incompressible random driftIn a critically-correlated incompressible random drift, a quenched invariance principle holds under the superdiffusive scaling \(\sqrt t\,(\log t)^{1/4}\); when the stream matrix has positive Hurst exponent \(\gamma\ll1\), for a typical realization of the environment the displacement variance at time \(t\) grows like \(t^{2/(2-\gamma)}\). Random walk on orthogonal tilingsUnder mild deterministic regularity assumptions, random walks on orthogonal tilings of \(\mathbb R^d\), with a canonical choice of conductances, converge to Brownian motion modulo time parameterization. Examples include Delaunay triangulations with vertices sampled from a \(d\)-dimensional Gaussian multiplicative chaos measure.

Internal DLA and divisible sandpile

Internal diffusion-limited aggregation (internal DLA) and the divisible sandpile are growth models in which particles or mass spread from a source, by random walk or by sharing excess mass equally with neighbors, until every site holds at most one unit. With \(n\) particles or mass \(n\) started at the origin of \(\mathbb Z^d\), both occupied sets, rescaled by \(n^{1/d}\), converge to the same Euclidean ball; the basic questions concern their fluctuations and their shapes on other graphs.

Discrete unique continuation

A harmonic function on \(\mathbb R^d\) that vanishes on a nonempty open set vanishes everywhere; this is the unique continuation property. Discrete unique continuation asks which quantitative forms of this property hold for discrete harmonic functions on graphs, for example whether a function that vanishes on most of a ball must vanish on a smaller ball. Such statements are used to prove Liouville theorems and to study Anderson localization.

Pareto peeling

Pareto hull peeling sorts a set of points in Euclidean space into layers by repeatedly removing the points on the boundary of the Pareto hull of the remaining points, generalizing convex hull peeling. The Pareto hull is defined from a norm; in the plane it is the convex hull when the unit ball of the norm is strictly convex.