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Stable determination of the nonlinear parameter in the non-diffusive Westervelt equation from the Dirichlet-to-Neumann map

Mike Wendels

Abstract

The Westervelt equation models the propagation of nonlinear acoustic waves in a regime well-suited for applications such as medical ultrasound imaging. In this work, we prove that the nonlinear parameter, as well as the sound speed, can be stably recovered from the Dirichlet-to-Neumann map associated with the non-diffusive Westervelt equation in (1+3)-dimensions. This result is essential for the feasibility of reconstruction methods. The Dirichlet-to-Neumann map encodes boundary measurements by associating a prescribed pressure profile on the boundary with the resulting pressure fluctuations. We prove stability provided the sound speed is a priori known to be close to a reference sound speed and under certain geometrical conditions. We also verify the result through numerical experiments.

Stable determination of the nonlinear parameter in the non-diffusive Westervelt equation from the Dirichlet-to-Neumann map

Abstract

The Westervelt equation models the propagation of nonlinear acoustic waves in a regime well-suited for applications such as medical ultrasound imaging. In this work, we prove that the nonlinear parameter, as well as the sound speed, can be stably recovered from the Dirichlet-to-Neumann map associated with the non-diffusive Westervelt equation in (1+3)-dimensions. This result is essential for the feasibility of reconstruction methods. The Dirichlet-to-Neumann map encodes boundary measurements by associating a prescribed pressure profile on the boundary with the resulting pressure fluctuations. We prove stability provided the sound speed is a priori known to be close to a reference sound speed and under certain geometrical conditions. We also verify the result through numerical experiments.

Paper Structure

This paper contains 18 sections, 14 theorems, 159 equations, 3 figures.

Key Result

Proposition 1.1

Let $\Omega \subset \mathbb{R}^3$ be a compact, connected domain with smooth boundary $\partial \Omega$, and let $\delta$ be such that inequality eq:DNdelta holds for all $f \in H_{0,\epsilon_0}^{s+3}(\Sigma)$. Suppose that $c, \beta_\ell \in \mathcal{C}^{\infty}(\Omega), \, c > 0$ with $\lVert\beta for any $q < l$, where $0 < \mu < 1$ is dependent on $s,l,q$.

Figures (3)

  • Figure 1: Sketch of the setting of uhlmann2016inverse to locally invert a weighted geodesic ray transform around some point $p \in \partial \Omega$ for which the boundary is locally strictly convex with respect to the metric.
  • Figure 2: A log-log plot of $\lVert D_{\nu} (\tilde{u}_1 - \tilde{u}_2)\rVert_{L^2(\Sigma)}$ with $f(t,x) = \frac{1}{10} e^{-t^{-2}}$ for $\beta_1,\beta_2 \in [10^{-4},1], \, c \equiv 1$ (left) and for $c_1,c_2 \in [1,1.8], \, \beta \equiv 0$ (right), where $\Omega = [-1,1]^3, \, \Sigma = [0,3.48] \times \partial \Omega, \, \Delta x = 2^{-4}, \, \Delta t = 0.03$. The results are restricted to limited values for $\beta_2,c_2$ for clarity of presentation.
  • Figure 3: A log-log plot of $\lVert D_{\nu} (\tilde{u}_1 - \tilde{u}_2)\rVert_{L^2(\Sigma)}$ with $f(t,x) = \frac{1}{10} e^{-t^{-2}}$ and $c_{\alpha}(x)$ as in equation \ref{['eq:c_herglotz']} for $\beta_1,\beta_2 \in [10^{-4},0.34], \, \alpha = \frac{3}{2}$ (left) and for $\alpha_1,\alpha_2 \in [1,\frac{3}{2}], \, \beta \equiv 0$ (right), where $\Omega = [-1,1]^3, \, \Sigma = [0,3.48] \times \partial \Omega, \, \Delta x = 2^{-4}, \, \Delta t = 0.03$. The results are restricted to limited values for $\beta_2,\alpha_2$ for clarity of presentation.

Theorems & Definitions (26)

  • Proposition 1.1
  • Theorem 1.1
  • Definition 2.1: stefanov2016boundary
  • Lemma 2.1: kachalov2001inverse,lassas2020uniqueness
  • Lemma 2.2: kachalov2001inverse
  • Corollary 2.1
  • Lemma 3.1
  • proof
  • Lemma 3.2
  • proof
  • ...and 16 more