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Azimi Q models : ウィキペディア英語版
Azimi Q models

The Azimi Q models used Mathematical Q models to explain how the earth responds to seismic waves. Because these models satisfies the Krämers-Krönig relations they should be preferable to the Kolsky model in seismic inverse Q filtering.
==Azimi's first model==

Azimi's first model 〔Azimi S.A.Kalinin A.V. Kalinin V.V and Pivovarov B.L.1968. Impulse and transient characteristics of media with linear and quadratic absorption laws. Izvestiya - Physics of the Solid Earth 2. p.88-93〕 (1968), which he proposed together with 〔Strick: The determination of Q, dynamic viscosity and transient creep curves from wave propagation measurements. Geophysical Journal of the Royal Astronomical Society 13, p.197-218〕 Strick (1967) has the attenuation proportional to |w|1-γ| and is:
: \alpha (w)=a_1|w|^ \quad (1.1)
The phase velocity is written:
: \frac = \frac +a_1|w|^ +cot(\frac) \quad (1.2)

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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