Diffraction in Inhomogeneous Media
Diffraction in Inhomogeneous Media
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On the o other hand, because the diffracted rays are congnient, we find on evaluating the limit in (l5), that (60) A^(P) - A^(P^)[n2-n2(x^, )]-^^ [n(P^) K (P^)]^/^ Since the diffracting surface is a plane on which n(x) is constant, the diffraction coefficients at P, and Q, are equal and a (f) is constant. Further- more all other quantities in (60) may be evaluated at Q-, the point of tangency of the limiting ray, instead of at P, . By combining (60) with (17), we find for A^(P) the result (61) ...A^(P) - A^(Q^)[n(Q^) K (Q^)]^/^ D2[n2-n2(x^)]-l>^ e^"^ b ''b^ To complete the calculation of u, we note that the phase change along the surface ray is Just (62) n(x^^) (y^ - Y^^).
Furtheimore, ^^(Qn) can be determined from (58). The phase along the diffracted rays can be obtained from (5) by using (62) and the phase of the incident field at Q- . In this way we find - 26 - X X.
(63) 0(P) = n(x^)y + ] f ♦ f [^^^-^^^^^j^^^ dx.
If for any point in the refraction shadow y
What to read after Diffraction in Inhomogeneous Media?
You can find similar books in the "Read Also" column, or choose other free books by Bernard D Seckler to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
On the o other hand, because the diffracted rays are congnient, we find on evaluating the limit in (l5), that (60) A^(P) - A^(P^)[n2-n2(x^, )]-^^ [n(P^) K (P^)]^/^ Since the diffracting surface is a plane on which n(x) is constant, the diffraction coefficients at P, and Q, are equal and a (f) is constant. Further- more all other quantities in (60) may be evaluated at Q-, the point of tangency of the limiting ray, instead of at P, . By combining (60) with (17), we find for A^(P) the result (61) ...A^(P) - A^(Q^)[n(Q^) K (Q^)]^/^ D2[n2-n2(x^)]-l>^ e^"^ b ''b^ To complete the calculation of u, we note that the phase change along the surface ray is Just (62) n(x^^) (y^ - Y^^).
Furtheimore, ^^(Qn) can be determined from (58). The phase along the diffracted rays can be obtained from (5) by using (62) and the phase of the incident field at Q- . In this way we find - 26 - X X.
(63) 0(P) = n(x^)y + ] f ♦ f [^^^-^^^^^j^^^ dx.
If for any point in the refraction shadow y
What to read after Diffraction in Inhomogeneous Media?
You can find similar books in the "Read Also" column, or choose other free books by Bernard D Seckler to read onlineMoreLess
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