Kramers-Kronig relations for the wavenumber

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SUMMARY

The Kramers-Kronig (KK) relations can be applied to the complex wavenumber k(ω) = k'(ω) + i k"(ω) to derive the imaginary part k"(ω) from the real part k'(ω). According to Kristel Carolina Meza Fajardo's PhD thesis, the damping coefficient α(ω) can be calculated using the relationship between phase velocity V(ω) and the complex wavenumber. Additionally, the reference "Quantitative Seismology" by Aki & Richards provides a method to compute α(ω) using a principal value integral. However, successful application of KK requires a sufficiently large frequency domain and precise measurements, particularly around resonance points.

PREREQUISITES
  • Understanding of Kramers-Kronig relations
  • Familiarity with complex wavenumbers and damping coefficients
  • Knowledge of phase velocity and its relationship to wavenumber
  • Ability to perform principal value integrals
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  • Study the derivation and application of Kramers-Kronig relations in complex analysis
  • Learn about phase velocity calculations in wave propagation
  • Explore numerical methods for evaluating principal value integrals
  • Investigate resonance phenomena in wave mechanics and their implications for absorption peaks
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Researchers in wave physics, seismologists, and engineers involved in wave propagation analysis will benefit from this discussion, particularly those looking to apply Kramers-Kronig relations to complex wavenumber measurements.

big_gie
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Hi all,

I am wandering if I can apply the Kramers-Kronig (KK) relations to the complex wavenumber k(ω) = k'(ω) + i k"(ω). I have a measurement that easily gives me k'(ω) for a certain range of frequencies, but where k"(ω) is unreliable. I would like to use KK to find k" from k'.

According to Kristel Carolina Meza Fajardo's PhD thesis (located here: http://www.roseschool.it/files/get/id/4412 ), the damping coefficient α(ω) can be obtained from the phase velocity (section 3.4, page 34). Her equation (2.46) gives the relationship between the damping coefficient α(ω), the phase velocity V(ω) and the (complex) wavenumber k(ω) as:
\tilde{k}(\omega) = \frac{\omega}{V(\omega)} - i \alpha(\omega) \equiv k' + i k"​

From another reference (Quantitative Seismology, Aki & Richards, 2nd edition, 2002), the complex wavenumber is given by (Box 5.8, equation (1), page 167):
K = \frac{\omega}{c(\omega)} + i \alpha(\omega)​

Kramers-Kronig can be used to find the imaginary part from the real part of the wavenumber (Box 5.8, equation (10)):
\alpha(\omega) = \frac{-1}{\pi} P \int_{-\infty}^{\infty} \xi \left( \frac{1}{c(\xi)} - \frac{1}{c_{\infty}} \right) \frac{d\xi}{\xi - \omega}​
where P represents the principal value of the integral.

So I have two references telling me I can use KK to find \alpha(\omega) from \frac{\omega}{c(\omega)}.

One problem is obviously the integration over infinite domain. I have discrete measurements for some (positive) frequencies. How should I proceed?

But more importantly, can KK really apply to what I want? My ω axis is juste 2 \pi f where f is the measurement's frequency, it's not the x-axis of a Fourier transform...

Thanks for any hints!
 
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In principle this is possible.
However, you need to be able to calculate this integral!
This means a large-enough frequency domain of observation, and enough precision.
This is more likely to be possible around some "resonance" where the "index of refraction" varies quickly.
Then you will see the corresponding absorption peak.
I suggest you to experiment with the idea.
 

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