Frequency-dependent attenuation (1/Q) should be used as a seismic attribute to improve the accuracy of seismic methods and imaging of the subsurface. In rocks, 1/Q is highly sensitive to the presence
Data contains two forced-oscillation measurements in partially saturated sandstone with varying fluid viscosities (e.g., water, glycerin) at seismic frequencies (2~400 Hz)
These are the supplementary data files for a paper submitted to the Journal of Geophysical Research (JGR), "Effects of fluid saturation and viscosity on seismic dispersion characteristics in Berea san