In time reversal acoustics, the array records the incoming signal, reverses each recorded time trace, and re-emits it through the same medium. This is phase conjugation in the frequency domain. For the time-harmonic wave convention , reversing a real time trace replaces its positive-frequency wave amplitude by its complex conjugate. The medium must remain unchanged between recording and re-emission.
Let and , with the chosen source and array normalizations incorporated into the Green function. Let be the array's aperture weight, equal to the indicator of its receiving region for an ideal uniform array. The recorded field is
By wave reciprocity, back-propagation has the same Green function with the source and receiver exchanged. Therefore the physically re-emitted, back-propagated wave amplitude is
If and multiplies by , then , where denotes the transpose without conjugation. Taking a final complex conjugate instead defines the adjoint reconstruction . This distinction prevents an erroneous conjugation in the time reversal operator.
For a localized Gaussian beam or acoustic point source in a homogeneous medium, a finite aperture admits a limited range of angles. The focal width is of order when denotes the aperture diameter. In a random medium, multiple scattering creates paths with a larger angular spread. Each reversed path retraces its route, and the paths interfere constructively at the source. This can produce a larger effective aperture in time reversal and a narrower focus, even though the unreversed field has a complicated speckle pattern.
This comparison concerns a homogeneous reference medium; a deterministic heterogeneous medium can also provide useful multipath propagation. Suitable scale limits or frequency and spatial averaging can make refocusing self-averaging. Such self-averaging is not automatic for every monochromatic source and every random realization. Wave absorption, changing medium parameters, unresolved paths or poor array coverage can spoil refocusing. With complete capture of the propagating modes and a lossless unitary operator , ideal adjoint reconstruction is already exact in either medium. Random scattering can improve finite-aperture wave focusing through angular diversity. See the regime-dependent analysis in Statistical stability in time reversal.
To first order in , replace by and use the known incident field in the outgoing integral. The Born approximation for scalar wave scattering gives
Both the contrast term and the internal-field correction are second order for fixed geometry in the perturbative regime established in part i.
Specify the data space before taking an adjoint operator. For example, let and , where is a bounded measurement surface separated from . Define the linear operator
For bounded incident field this is a Hilbert-Schmidt operator, hence a compact operator. The equation is , with . Other sampling geometries give corresponding data spaces and weights; the paper does not specify one. Using the usual complex inner products, its adjoint operator is
The complex conjugations are required by the adjoint operator identity, not by wave reciprocity alone.
The Landweber iteration starts from and applies gradient descent to :
Each step back-propagates the data residual. The Landweber relaxation parameter controls stability, and early stopping of Landweber iteration prevents small singular values from amplifying measurement errors. For an explicitly real-valued index contrast, use the real Hilbert space structure and replace by in this update. Additional sign or support constraints require corresponding projections; none are assumed here.