Abstract
Abstract
The inverse problem of recovering the potential q(x) in the damped wave equation
m
(
x
)
u
t
t
+
μ
(
x
)
u
t
=
r
(
x
)
u
x
x
+
q
(
x
)
u
, (x, t) ∈ Ω
T
≔ (0, ℓ) × (0, T) subject to the boundary conditions u(0, t) = ν(t), u(ℓ, t) = 0, from the Neumann boundary measured output f(t) ≔ r(0)u
x
(0, t), t ∈ (0, T] is studied. The approach proposed in this paper allows us to derive behavior of the direct problem solution in the subdomains defined by characteristics of the wave equation and along the characteristic lines, as well. Based on these results, a local existence theorem and the stability estimate are proved. The compactness and Lipschitz continuity of the Dirichlet-to-Neumann operator are derived. Fréchet differentiability of the Tikhonov functional is proved and an explicit gradient formula is derived by means of an appropriate adjoint problem. It is proved that this gradient is Lipschitz continuous.
Subject
Applied Mathematics,Computer Science Applications,Mathematical Physics,Signal Processing,Theoretical Computer Science
Reference11 articles.
1. On the inverse problem in the theory of propagation of seismic waves;Blagoveshensky;Problems Math. Phys.,1966
2. One-dimensional inverse problem for a second order hyperbolic equation;Blagoveshensky;Math. Questions Wave Propag. Theory,1969
Cited by
2 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献