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Distributed Acoustic Sensing in Geophysics


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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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      1.2.1. DAS Optimization for Seismic Applications

      Distributed fiber sensors measure physical parameters of an external environment continuously through the integration properties of light traveling along a lengthy optical path. This is quite different from point sensors, such as geophones, which make an inertial measurement of ground speed at fixed positions (SEAFOM, 2018). The DAS records a local strain rate, which can be converted into particle velocity to allow direct comparison with geophone data. Following Jousset et al. (2018), we can approximately represent DAS signal A(z, t) via ground displacement u(z, t), where FS is the DAS sampling frequency and L0 is the gauge length.

      If FS → ∞, L0 → 0, then the DAS signal can be presented in a double differential form: