Work done with:
Stefano Martiniani
As a resilience measure
Wiley, D. A., Strogatz, S. H., & Girvan, M. (2006). The size of the sync basin. Chaos: An Interdisciplinary Journal of Nonlinear Science, 16(1).
Menck, P. J., Heitzig, J., Marwan, N., & Kurths, J. (2013). How basin stability complements the linear-stability paradigm. Nature physics, 9(2), 89-92.
\(A\)
\(B\)
\(B\) is more stable
To calculate configurational entropy
Martiniani, S., Schrenk, K. J., Ramola, K., Chakraborty, B., & Frenkel, D. (2017). Numerical test of the Edwards conjecture shows that all packings are equally probable at jamming. Nature physics, 13(9), 848-851.
Casiulis et al. Papers in Physics 15 (2023): 150001-150001.
Basin Stability
Soft sphere packings
Wiley, D. A., Strogatz, S. H., & Girvan, M. (2006). The size of the sync basin. Chaos: An Interdisciplinary Journal of Nonlinear Science, 16(1).
Menck, P. J., Heitzig, J., Marwan, N., & Kurths, J. (2013). How basin stability complements the linear-stability paradigm. Nature physics, 9(2), 89-92.
Uses naive sampling.
Xu, N., Frenkel, D., & Liu, A. J. (2011). Direct determination of the size of basins of attraction of jammed solids. Physical Review Letters, 106(24), 245502.
Asenjo, Daniel, Fabien Paillusson, and Daan Frenkel. "Numerical calculation of granular entropy." Physical review letters 112.9 (2014): 098002.
Martiniani, S., Schrenk, K. J., Stevenson, J. D., Wales, D. J., & Frenkel, D. (2016). Structural analysis of high-dimensional basins of attraction. Physical Review E, 94(3), 031301.
Martiniani, S., Schrenk, K. J., Ramola, K., Chakraborty, B., & Frenkel, D. (2017). Numerical test of the Edwards conjecture shows that all packings are equally probable at jamming. Nature physics, 13(9), 848-851.
Uses optimizers.
Cousins, Ben, and Santosh Vempala. "Gaussian Cooling and O^*(n^3) Algorithms for Volume and Gaussian Volume." SIAM Journal on Computing 47.3 (2018): 1237-1273.
Algorithm for convex objects
$$Z(k) = \int_{\mathbb{R}^N}^{} \mathcal{O}(x) dx$$
Oracle (1 if inside basin. 0 if outside) defined by ODE solves
Volume
Kuramoto
Soft spheres
Gradient systems, No limit cycles, easy to identify attractors
Casiulis et al. Papers in Physics 15 (2023): 150001-150001.
$$Z(k) = \int_{\mathbb{R}^N}^{} \mathcal{O}(x) e^{- \frac{1}{2} k \left|x-x_{0}\right|^{2}} dx$$
Normalizing constant of probability distribution
Oracle (1 if inside basin. 0 if outside)
Gaussian centered around minimum
$$ F(k) = - log(Z_{k}) $$
"Free energy"
$$ F(0) - F(k_{\infty}) = \int_{0}^{k_{\infty}} \frac{\partial F}{\partial k} dk = \int_{k_{\infty}}^{0} \langle \left| x-x_{0}\right|^{2} \rangle_{k} dk$$
Log volume (unknown)
Gaussian normalizing constant
Brute force MC misses most of the volume!!
Reconstruct uniform samples from MC walkers at different distances, which can be used to constuct volumes
Casiulis et al. Papers in Physics 15 (2023): 150001-150001.
Replica exchange
Casiulis et al. Papers in Physics 15 (2023): 150001-150001.
$$\alpha_{\text{swap}} = \min\left(1, \exp\left(-\frac{k}{2}(\beta_k - \beta_l)(|x_l - x^*|^2 - |x_k - x^*|^2)\right)\right)$$
Swap acceptance criterion
Volume estimation is the hard part
$$ \dot{\theta}_j = \sin(\theta_{j+1} - \theta_j) + \sin(\theta_{j-1} - \theta_j)$$
$$\theta_j^* = \frac{2\pi q \, j}{N}, \quad \text{stable for } |q| < N/4$$
$$\log S_B(q) = \log \frac{V(q)}{|\mathbb{T}_n|} \approx C - k q^2$$
$$ \dot{\theta}_j = \sin(\theta_{j+1} - \theta_j) + \sin(\theta_{j-1} - \theta_j)$$
$$\theta_j^* = \frac{2\pi q \, j}{N}, \quad \text{stable for } |q| < N/4$$
$$\log S_B(q) = \log \frac{V(q)}{|\mathbb{T}_n|} \approx C - k q^2$$
using VolumeEstimation, CommonSolve
# Estimate the volume of a 5D unit hypercube (true volume = 1)
membership(x) = all(abs.(x) .<= 0.5)
prob = VolumeProblem(membership, 5)
sol = solve(prob)
sol.log_volume # ≈ 0.0 (log of 1)
sol.volume # ≈ 1.0using BasinVolumes
dim = 2
power = 0.5
offset = 1.0
# Gradient descent on a cosine potential with basins at integer lattice points
function neg_grad(u, p, t)
S = dim + offset - sum(cos.(2pi .* u))
-power .* S^(power - 1) .* (2pi) .* sin.(2pi .* u)
end
# Check convergence to the basin at the origin
basin_check(u) = sum(abs2, u) < 1e-6
prob = BasinVolumeProblem(neg_grad, nothing, basin_check, dim; x0=zeros(dim))
sol = solve(prob; n_rounds=8, n_chains=8)
sol.log_volume # log of the estimated basin volume
sol.volume # the estimated basin volumeStefano Martiniani
Mathias Casiulis
Martiniani Lab