@article{10011,
  abstract     = {We propose a new weak solution concept for (two-phase) mean curvature flow which enjoys both (unconditional) existence and (weak-strong) uniqueness properties. These solutions are evolving varifolds, just as in Brakke's formulation, but are coupled to the phase volumes by a simple transport equation. First, we show that, in the exact same setup as in Ilmanen's proof [J. Differential Geom. 38, 417-461, (1993)], any limit point of solutions to the Allen-Cahn equation is a varifold solution in our sense. Second, we prove that any calibrated flow in the sense of Fischer et al. [arXiv:2003.05478] - and hence any classical solution to mean curvature flow-is unique in the class of our new varifold solutions. This is in sharp contrast to the case of Brakke flows, which a priori may disappear at any given time and are therefore fatally non-unique. Finally, we propose an extension of the solution concept to the multi-phase case which is at least guaranteed to satisfy a weak-strong uniqueness principle.},
  author       = {Hensel, Sebastian and Laux, Tim},
  issn         = {1945-743X},
  journal      = {Journal of Differential Geometry},
  keywords     = {Mean curvature flow, gradient flows, varifolds, weak solutions, weak-strong uniqueness, calibrated geometry, gradient-flow calibrations},
  pages        = {209--268},
  publisher    = {International Press},
  title        = {{A new varifold solution concept for mean curvature flow: Convergence of  the Allen-Cahn equation and weak-strong uniqueness}},
  doi          = {10.4310/jdg/1747065796},
  volume       = {130},
  year         = {2025},
}

@phdthesis{20563,
  abstract     = {The theory of optimal transport provides an elegant and powerful description of many evolution
equations as gradient flows. The primary objective of this thesis is to adapt and extend the
theory to deal with important equations that are not covered by the classical framework,
specifically boundary value problems and kinetic equations. Additionally, we establish new
results in periodic homogenization for discrete dynamical optimal transport and in quantization
of measures.
Section 1.1 serves as an invitation to the classical theory of optimal transport, including the
main definitions and a selection of well-established theorems. Sections 1.2-1.5 introduce the
main results of this thesis, outline the motivations, and review the current state of the art.
In Chapter 2, we consider the Fokker–Planck equation on a bounded set with positive Dirichlet
boundary conditions. We construct a time-discrete scheme involving a modification of the
Wasserstein distance and, under weak assumptions, prove its convergence to a solution of this
boundary value problem. In dimension 1, we show that this solution is a gradient flow in a
suitable space of measures.
Chapter 3 presents joint work with Giovanni Brigati and Jan Maas. We introduce a new theory
of optimal transport to describe and study particle systems at the mesoscopic scale. We prove
adapted versions of some fundamental theorems, including the Benamou–Brenier formula and
the identification of absolutely continuous curves of measures.
Chapter 4 presents joint work with Lorenzo Portinale. We prove convergence of dynamical
transportation functionals on periodic graphs in the large-scale limit when the cost functional
is asymptotically linear. Additionally, we show that discrete 1-Wasserstein distances converge
to 1-Wasserstein distances constructed from crystalline norms on R
d
.
Chapter 5 concerns optimal empirical quantization: the problem of approximating a measure
by the sum of n equally weighted Dirac deltas, so as to minimize the error in the p-Wasserstein
distance. Our main result is an analog of Zador’s theorem, providing asymptotic bounds for
the minimal error as n tends to infinity.
},
  author       = {Quattrocchi, Filippo},
  issn         = {2663-337X},
  keywords     = {optimal transport, kinetic equations, boundary value problems, quantization, gradient flows, homogenization},
  pages        = {240},
  publisher    = {Institute of Science and Technology Austria},
  title        = {{Optimal transport methods for kinetic equations, boundary value problems, and discretization of measures}},
  doi          = {10.15479/AT-ISTA-20563},
  year         = {2025},
}

@unpublished{20571,
  abstract     = {We prove the convergence of a modified Jordan--Kinderlehrer--Otto scheme to a solution to the Fokker--Planck equation in $\Omega \Subset \mathbb{R}^d$ with general, positive and temporally constant, Dirichlet boundary conditions. We work under mild assumptions on the domain, the drift, and the initial datum.   In the special case where $\Omega$ is an interval in $\mathbb{R}^1$, we prove that such a solution is a gradient flow -- curve of maximal slope -- within a suitable space of measures, endowed with a modified Wasserstein distance.
Our discrete scheme and modified distance draw inspiration from contributions by A. Figalli and N. Gigli [J. Math. Pures Appl. 94, (2010), pp. 107--130], and J. Morales [J. Math. Pures Appl. 112, (2018), pp. 41--88] on an optimal-transport approach to evolution equations with Dirichlet boundary conditions. Similarly to these works, we allow the mass to flow from/to the boundary $\partial \Omega$ throughout the evolution. However, our leading idea is to also keep track of the mass at the boundary by working with measures defined on the whole closure $\overline \Omega$. The driving functional is a modification of the classical relative entropy that also makes use of the information at the boundary. As an intermediate result, when $\Omega$ is an interval in $\mathbb{R}^1$, we find a formula for the descending slope of this geodesically nonconvex functional. },
  author       = {Quattrocchi, Filippo},
  booktitle    = {arXiv},
  keywords     = {gradient flows, Jordan–Kinderlehrer–Otto scheme, curves of maximal slope, optimal transport, Dirichlet boundary conditions, Fokker–Planck equation},
  title        = {{Variational structures for the Fokker-Planck equation with general Dirichlet boundary conditions}},
  doi          = {10.48550/arXiv.2403.07803},
  year         = {2024},
}

