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Relationships between Root Mean Square Velocities, Average Velocities, and Coefficients of Heterogeneity

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Velocities in Reflection Seismology

Part of the book series: Seismology and Exploration Geophysics ((MAGE,volume 3))

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Abstract

As we saw in chapter 6:

  • the average vertical velocity is the time average of the instantaneous velocities v:

    $${V_M} = \frac{1}{T}\int_o^T {v(t)dt} $$

    or

    $${V_M} = \frac{1}{T}\sum\limits_{k = 1}^n {{v_k}{t_k}} $$
  • the root mean square velocity VRMS is the square root of the time average of the squares of the instantaneous velocities:

    $$V_{RMS}^2 = \frac{1}{T}\int_o^T {{v^2}(t)dt} $$

    or

    $$V_{RMS}^2 = \frac{1}{T}\sum\limits_{k = 1}^n {v_k^2(t){t_k}} $$

It is important to note that for a given depth, the values of VM and VRMS are independent by definition of the distribution function of the velocities vk.

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© 1985 Springer Science+Business Media Dordrecht

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Cordier, JP. (1985). Relationships between Root Mean Square Velocities, Average Velocities, and Coefficients of Heterogeneity. In: Velocities in Reflection Seismology. Seismology and Exploration Geophysics, vol 3. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-3641-1_8

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  • DOI: https://doi.org/10.1007/978-94-017-3641-1_8

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-90-481-8416-3

  • Online ISBN: 978-94-017-3641-1

  • eBook Packages: Springer Book Archive

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