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Distributed Acoustic Sensing in Geophysics. Группа авторов
Читать онлайн.Название Distributed Acoustic Sensing in Geophysics
Год выпуска 0
isbn 9781119521778
Автор произведения Группа авторов
Жанр Физика
Издательство John Wiley & Sons Limited
Here, we present a real‐time PGC‐DAS system. Combined with characteristics of large dynamic range and high sensitivity of PGC demodulation algorithm (Wang et al., 2015), the proposed system provides an effective technical solution to distributed fiber acoustic sensing. The sensing distance could reach 10 km with the minimum sample interval of 0.4 m. Corresponding to the average phase noise of 5 × 10‐4 rad/√Hz, a strain sensitivity of 8.5 pε/√Hz was achieved with a spatial resolution of 10 m, as well as a frequency response range of 2 Hz to 1 kHz over 10 km sensing distance. A field trial of this PGC‐DAS system was performed to compare nodal geophones. Results show that seismic records have a high consistency between them, proving the feasibility of PGC‐DAS system in seismology.
4.2. PRINCIPLE
The principle of PGC‐DAS system is shown in Figure 4.1. A coherent input light pulse passes through a circulator into the sensing optical fiber. RB light enters into an unbalanced MI with FRMs at the ends. There is a phase modulator on one arm of MI and an optical delay LMI on the other arm. RB signal mixes with itself and is detected by one photoelectric detector (PD).
Intensity distribution of RB light is a type of Fourier transform of random permittivity fluctuations (Bao et al., 2016). Assume that the sensing fiber is composed of successive slices with a length of ΔL. Each slice contains M scattering centers, and polarization states between each scattering center are consistent. The interference field of backscattered light at distance Lm = mΔL can be expressed by (Park et al., 1998):
(4.1)
where E0 is electric field intensity of the incident light; Pm is polarization‐dependent coefficient ranging from 0 to 1; α is optical power attenuation coefficient; rk and φk are scattering coefficient and phase of the kth scattering center, respectively; ai and φi are reflectivity and phase of scattering unit, respectively; and β is propagation constant.
Figure 4.1 Principle of PGC‐DAS system with an unbalanced MI.
Then, scattering light enters into MI, and RB1 and RB2 separated by LMI interference due to the same optical path. The interference electrical field E(t) is written as:
(4.2)
With simplified coefficients A and B, the interference intensity is given by:
For PGC demodulation algorithm, a sinusoidal signal with a modulation frequency of ωc is loaded on one arm of MI. Therefore, an additional phase modulation C ⋅ cos (ωct) is introduced in