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In reflection seismology, the anelastic attenuation factor, often expressed as seismic quality factor or Q (which is inversely proportional to attenuation factor), quantifies the effects of anelastic attenuation on the seismic wavelet caused by fluid movement and grain boundary friction. As a seismic wave propagates through a medium, the elastic energy associated with the wave is gradually absorbed by the medium, eventually ending up as heat energy. This is known as absorption (or anelastic attenuation) and will eventually cause the total disappearance of the seismic wave.〔Toksoz, W.M., & Johnston, D.H. 1981. Seismic Wave Attenuation. SEG.〕 ==Quality factor, ''Q''== ''Q'' is defined as : where is the fraction of energy lost per cycle.〔Sheriff, R. E., Geldart, L. P., (1995), 2nd Edition. ''Exploration Seismology''. Cambridge University Press.〕 Its behaviour said to be dispersive because the rate of attenuation increases with frequency. The earth preferentially attenuates higher frequencies, resulting in the loss of signal resolution as the seismic wave propagates. Quantitative seismic attribute analysis of amplitude versus offset effects is complicated by anelastic attenuation because it is superimposed upon the AVO effects.〔Dasgupta, R., & Clark, R.A. (1998) Estimation of Q from surface seismic reflection data. ''Geophysics'' 63, 2120-2128〕 The rate of anelastic attenuation itself also contains additional information about the lithology and reservoir conditions such as porosity, saturation and pore pressure so it can be used as a useful reservoir characterization tool.〔Enhanced seismic Q compensation, Raji, W.O., Rietbrock, A. 2011. ''SEG Expanded Abstracts'' 30, 2737〕 Therefore, if ''Q'' can be accurately measured then it can be used for both compensation for the loss of information in the data and for seismic attribute analysis. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Anelastic attenuation factor」の詳細全文を読む スポンサード リンク
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