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Filippov Sliding Dynamics of Cosmic Dust Atmospheric Entry: Survival Boundaries, Asymptotic Mass Loss, and Inverse Problem Limits

Md Shahrier Islam Arham, Prasun Panthi, Min Heo

Abstract

We develop a mathematically rigorous framework for modelling the atmospheric entry of micrometeoroids with radii $r_{0}\in[0.5,1000]μm$ at hypervelocity speeds $v_{0}\in[11.2,72]km/s$. The governing four-state ODE system coupling altitude, speed, temperature, and radius has a discontinuous right-hand side at the ablation threshold $T=T_{melt}$, making it a Filippov dynamical system. We prove three original results. First, the empirical survival boundary $r_{0}^{crit}\propto v_{0}^{-3}$ (known since Love & Brownlee 1991) is the sliding bifurcation locus of the Filippov system: the locus in parameter space where particle trajectories first touch the attracting sliding region on the switching surface. This gives the $v_{0}^{-3}$ scaling its first rigorous dynamical-systems derivation. Second, a matched perturbation expansion with small parameter $δ_ε=3Λρ_{0}H/(8Q^{*}ρ_{p}r_{0}\sin γ)$ yields a closed-form mass-loss formula with numerically confirmed $\mathcal{O}(δ_ε^{2})$ error bound. Third, the transfer matrix K mapping entry distributions to stratospheric surface outcomes has a null space in its surviving-particle submatrix $K_{surv}$ determined by the full-ablation manifold A. For iron and cometary compositions (high vo, large ro), A is non-empty and contains particles permanently invisible to stratospheric collectors regardless of sample size. Fate maps for silicate and iron compositions are validated against Love & Brownlee (1991). Global Sobol analysis confirms entry speed as the dominant parameter. A regularised nonnegative inversion demonstrates partial recovery of the pre-atmospheric flux distribution.

Filippov Sliding Dynamics of Cosmic Dust Atmospheric Entry: Survival Boundaries, Asymptotic Mass Loss, and Inverse Problem Limits

Abstract

We develop a mathematically rigorous framework for modelling the atmospheric entry of micrometeoroids with radii at hypervelocity speeds . The governing four-state ODE system coupling altitude, speed, temperature, and radius has a discontinuous right-hand side at the ablation threshold , making it a Filippov dynamical system. We prove three original results. First, the empirical survival boundary (known since Love & Brownlee 1991) is the sliding bifurcation locus of the Filippov system: the locus in parameter space where particle trajectories first touch the attracting sliding region on the switching surface. This gives the scaling its first rigorous dynamical-systems derivation. Second, a matched perturbation expansion with small parameter yields a closed-form mass-loss formula with numerically confirmed error bound. Third, the transfer matrix K mapping entry distributions to stratospheric surface outcomes has a null space in its surviving-particle submatrix determined by the full-ablation manifold A. For iron and cometary compositions (high vo, large ro), A is non-empty and contains particles permanently invisible to stratospheric collectors regardless of sample size. Fate maps for silicate and iron compositions are validated against Love & Brownlee (1991). Global Sobol analysis confirms entry speed as the dominant parameter. A regularised nonnegative inversion demonstrates partial recovery of the pre-atmospheric flux distribution.

Paper Structure

This paper contains 39 sections, 9 theorems, 43 equations, 6 figures, 6 tables.

Key Result

Theorem 3.1

On $\Omega \setminus \Sigma$, the vector field $\mathbf{f}$ defined by Eq. eq:full_system is locally Lipschitz. Therefore, for any initial condition $\mathbf{y}_0 \in \Omega \setminus \Sigma$, there exists a unique solution on some interval $[0, \tau)$.

Figures (6)

  • Figure 1: Global Sobol first-order ($S_i$) and total-order ($S_{Ti}$) indices for $T_{\max}$. Computed over $N = 8192$ Saltelli samples. The analytical high-temperature limit $(S_{v_0})^2 = 9/16 \approx 0.56$ (dashed line) exceeds the full-physics value $S_{v_0} = 0.31$, quantifying the variance carried by radiation and ablation feedback.
  • Figure 2: Fate map for silicate micrometeoroids as a function of entry speed $v_0$ and initial radius $r_0$ (vertical entry, $\gamma = 90^\circ$). Colours: blue --- unmelted survival; cyan --- scoriaceous; orange --- cosmic spherule; red --- complete ablation. The dashed curve is the analytical survival boundary $r_0^{\mathrm{crit}} \propto v_0^{-3}$ from Theorem \ref{['thm:filippov']}; the solid curve is the Filippov sliding locus $\partial\Sigma^s$ from which Theorem \ref{['thm:filippov']} is derived. The agreement between these two curves confirms that the survival boundary is the sliding bifurcation locus of the Filippov system.
  • Figure 3: Fate map for iron micrometeoroids. The upper-right quadrant (red) shows complete ablation for $v_0 > 50km\per s$ and $r_0 > 200µm$. This non-empty full-ablation set $\mathcal{A}$ corresponds to the kernel of $K_{\mathrm{surv}}$ characterised in Theorem \ref{['thm:nullspace']}.
  • Figure 4: Singular value spectrum of $K$ and $K_{\mathrm{surv}}$. The full transfer matrix has condition number $\kappa(K) \approx 3.5\times 10^{16}$ (near machine precision); the surviving-particle submatrix has $\kappa(K_{\mathrm{surv}}) \approx 1.4\times 10^2$, indicating moderate ill-posedness for the recoverable component.
  • Figure 5: L-curve for Tikhonov regularisation. The optimal regularisation parameter $\lambda^* = 7.2$ is at the corner of maximum curvature.
  • ...and 1 more figures

Theorems & Definitions (26)

  • Remark 2.5: Knudsen correction
  • Remark 2.6: Rocket term
  • Remark 2.9: Biot number
  • Theorem 3.1: Local Existence and Uniqueness
  • proof
  • Proposition 3.2: Carathéodory Extension
  • Remark 3.3: Sigmoid Regularisation
  • Theorem 4.1: Global Existence
  • proof
  • Lemma 5.1: Simplified Sliding Condition
  • ...and 16 more