Distributed Acoustic Sensing in Geophysics. Группа авторов

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equals ATAN StartFraction sigma-summation Underscript j equals 1 Overscript upper P Endscripts alpha Subscript j Baseline upper I Subscript j Baseline left-parenthesis z comma t right-parenthesis Over sigma-summation Underscript j equals 1 Overscript upper P Endscripts gamma Subscript j Baseline upper I Subscript j Baseline left-parenthesis z comma t right-parenthesis EndFraction"/>

      (1.16)upper V equals StartRoot Im upper Z squared plus Re upper Z squared EndRoot

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      1.1.4. DAS Dynamic Range Algorithms

      An acoustic algorithm (Equation 1.15) transforms the DAS intensity signal into a phase shift proportional to fiber elongation value; a question then is how large can this phase shift be? An algorithm based on such ambiguous function as ATAN(x) can give a result only inside a limited region. The classic approach to recover large phase changes is unwrapping: stitching together two consecutive points t and t + Δt from different branches of signal (Itoh, 1982):

      This unwrapping, or phase tracking, concept works only if the phase difference is inside two quadrants:

      So, the second order tracking algorithm can be obtained by differentiating the signal before unwrapping:

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