Distributed Acoustic Sensing in Geophysics. Группа авторов

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href="#ulink_a09dbb4d-9b4f-5a15-a79a-b087d12a64a6">Equation 1.41) looks similar to that for standard fiber signal (Equation 1.27). If, say, L0 = LS, then, in Equation 1.41, the curly expression { } represents a chapeau function for linear spline interpolation (Unser, 1999), In other words, v(z) is sampled and linearly interpolated with LS period in Equation 1.41 without any smearing, as it was for the case of conventional fiber (Equation 1.27).

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      The spatial spectral response in the wavenumber domain Kz can be represented by Fourier transform :

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      Equation 1.43 also includes a gain that can be obtained from synthetic gauge length optimization. With this approach, low spectral frequencies

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