2. Basic equations
Here we consider a generic stack of infinitely extended layers in the x1 and x3 directions. We use the axis conventions defined on 2. This is the coordinate system classically employed in surface wave models: the x2 axis is oriented downwards so as not to have to deal with negative coordinates when considering the substrate. Since we are interested in monochromatic plane wave propagation, we assume that all fields possess a spectral harmonic dependence in exp(jω (t - s<x<)), with s< the phase slowness along the corresponding axis and ω the pulsation, so that ω s< represents the wave vector along x<. We write the mechanical stress tensor Tij and the electrical displacement...
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Basic equations