Abstract
The medium is supposed to be such that its properties are everywhere a function of but one co-ordinate x, being of one uniform quality where x is less than a certain value x1, and of another uniform quality (in general, different from the first) where x exceeds a greater value xm-1; and the principal problem is the investigation of the reflection which in general ensues when plane waves in the first medium are incident upon the strati-fications. For the present we suppose the quality to be uniform through strata of finite thickness, the first transition occurring when x = x1, the second at x = x2, and the last at x = xm-1. The expressions for the waves in the various media in order may be taken to be ϕ1 = A1ei[ct + by - a1 (x - x1)] + B1ei[ct + by + a1 (x - x1)], ϕ2 = A2ei[ct + by - a2 (x - x1)] + B2ei[ct + by + a2 (x - x1)], ϕ3 = A3ei[ct + by - a3 (x - x2)] + B3ei[ct + by + a3 (x - x2)], and so on, the A's and B's denoting arbitrary constants. The first terms represent the waves travelling in the positive direction, the second those travelling in the negative direction; and our principal aim is the determination of the ratio B1/A1 imposed by the conditions of the problem, including the requirement that in the final medium there shall be no negative wave.
Cite
CITATION STYLE
Strutt, J. W. (1912). On the propagation of waves through a stratified medium, with special reference to the question of reflection. Proceedings of the Royal Society of London. Series A, Containing Papers of a Mathematical and Physical Character, 86(586), 207–226. https://doi.org/10.1098/rspa.1912.0014
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