Unified matrix-vector wave equation, reciprocity and representations

TL;DR

This paper develops a unified matrix-vector wave equation framework applicable to various wave phenomena in inhomogeneous media, deriving reciprocity theorems and representations that facilitate forward and inverse wave analysis.

Contribution

It introduces a comprehensive unified formalism for the matrix-vector wave equation across multiple wave types, including symmetry relations and reciprocity theorems.

Findings

Unified matrix-vector wave equation for diverse wave phenomena.

Derived reciprocity theorems based on symmetry properties.

Provided a unified wave field representation using Green's functions.

Abstract

The matrix-vector wave equation is a compact first-order differential equation. It was originally used for the analysis of elastodynamic plane waves in laterally invariant media. It has been extended by various authors for laterally varying media. Other authors derived a similar formalism for other wave phenomena. This paper starts with a unified formulation of the matrix-vector wave equation for 3D inhomogeneous, dissipative media. The wave vector, source vector and operator matrix are specified in the appendices for acoustic, quantum mechanical, electromagnetic, elastodynamic, poroelastodynamic, piezoelectric and seismoelectric waves. It is shown that the operator matrix obeys unified symmetry relations for all these wave phenomena. Next, unified matrix-vector reciprocity theorems of the convolution and correlation type are derived, utilising the symmetry properties of the operator matrix. These theorems formulate mathematical relations between two wave states in the same spatial domain. A unified wave field representation is obtained by replacing one of the states in the convolution-type reciprocity theorem by a Green's state. By replacing both states in the correlation-type reciprocity theorem by Green's states, a unified representation of the homogeneous Green's matrix is obtained. Applications of the unified reciprocity theorems and representations for forward and inverse wave problems are briefly indicated.