Distributed Acoustic Sensing in Geophysics. Группа авторов
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Название: Distributed Acoustic Sensing in Geophysics

Автор: Группа авторов

Издательство: John Wiley & Sons Limited

Жанр: Физика

Серия:

isbn: 9781119521778

isbn:

СКАЧАТЬ signal with a linearly increasing amplitude. It is visible that both algorithms can recover a significant phase range, but the second order tracking algorithm can deliver in excess of a 10 times larger dynamic range.

      1.1.5. DAS Signal Processing and Denoising

      In all phase‐detection schemes, the change in optical phase between the light scattered in two fiber segments is determined, meaning we are measuring the deterministic phase change between two random signals. The randomness of the amplitude of the scattered radiation imposes certain limitations on the accuracy of the sensor, through the introduction of phase flicker noise. The source of flicker noise is an ambiguity: when the fiber is stretched, the scattering coefficient varies, and can become zero. In this case, the differential phase detector generates a noise burst regardless of which optical setup is used. The amplitude of such noise increases with decreasing frequency (as is expected for flicker noise) when the phase difference is integrated into the displacement signal.

      From a quantum point of view, we need, for successive phase measurements, a number of interfering photon pairs scattered from points separated by the gauge length distance. In some “bad” points, there are no such pairs, as one point of scattering is faded. A natural way to handle this problem is to reject “bad” unpaired photons by controlling the visibility of the interference pattern. As a result, the shot noise can increase slightly as the price for the dramatic reduction of flicker noise. The rejection of fading points can be practically implemented by assigning a weighting factor to each measurement result and performing a weighted averaging.

      This averaging can be done over wavelength if a multi‐wavelength source is used. Alternatively, we can slightly sacrifice spatial resolution and solve the problem by denoising using weighted spatial averaging (Farhadiroushan et al., 2010). The maximum SNR is realized when the weighting factor of each channel is chosen to be inversely proportional to the mean square noise in that channel (Brennan, 1959), meaning the squared interference visibility, V2, can be used for the weighting factor as:

      (1.21)left pointing angle upper A left-parenthesis z right-parenthesis right pointing angle almost-equals StartFraction upper A left-parenthesis z right-parenthesis dot upper V squared left-parenthesis z right-parenthesis circled-times p left-parenthesis z right-parenthesis Over upper V squared left-parenthesis z right-parenthesis circled-times p left-parenthesis z right-parenthesis EndFraction

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      source is shown in the right panel of Figure 1.5.

      1.1.6. Time Integration of DAS Signal

      (1.22)integral Subscript t 1 Superscript t 2 Baseline left pointing angle upper A left-parenthesis z comma t right-parenthesis right pointing angle italic d t equals StartFraction 1 Over upper A 0 EndFraction tau left-parenthesis z right-parenthesis circled-times left-bracket u left-parenthesis z comma t 2 right-parenthesis minus u left-parenthesis z minus upper L 0 comma t 2 right-parenthesis right-bracket

      meaning a time integrated DAS signal can be considered as an output of a huge caliper that is measuring fiber elongation between two points with sub‐nanometer precision. This measuring principle is different from that of a geophone but is similar to an electromagnetic linear strain seismograph that can measure changes in distance between two points on the ground (Benioff, 1935).

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