TY - JOUR TI - Attenuation effects on the seismic response of a bottom-simulating reflector SP - 510 N1 - cited By 5 AV - none EP - 517 PB - Elsevier B.V. SN - 18755100 ID - scholars5950 KW - Dispersion (waves); Gas hydrates; Hydration; Models; Reflection KW - Attenuation; Bottom simulating reflector; Computer requirements; Hydrate bearing sediments; Poro-elasticity; Pseudospectral methods; Seismic interpretation; Velocity dispersion KW - Seismology N2 - Bottom simulation reflectors (BSR) are seismic events generally corresponding to a partially saturated layer with gas separating hydrate-bearing sediments from brine-saturated sediments. Seismic attenuation and velocity dispersion affects the waveform of the BSR event. In this work, we consider a 1D methodology to study the effects of seismic Q, velocity dispersion, layer thickness and properties and characteristics of the overburden on the reflection coefficients and waveform of such event. We describe the media by using a rock-physics model based on poroelasticity, calculate the reflection coefficient of the BSR layer of varying thickness and compute the waveforms with a full-wave pseudospectral method. The proposed rock-physics/modeling methodology is fast in terms of computer requirements and can be used to quantify the seismic properties and compute waveforms useful for seismic interpretation and inversion of quantities such as porosity, hydrate content, gas saturation, clay content and thickness of the BSR layer. We show that in many cases the interpretation can be counterintuitive and a proper rock-physics methodology is essential to reach valid conclusions about the influence of the different parameters on the wave properties. © 2015 Elsevier B.V. VL - 24 JF - Journal of Natural Gas Science and Engineering A1 - Qadrouh, A. A1 - Carcione, J.M. A1 - Salim, A.M. A1 - Harith, Z.Z.T. UR - https://www.scopus.com/inward/record.uri?eid=2-s2.0-84937215706&doi=10.1016%2fj.jngse.2015.04.011&partnerID=40&md5=95e8844f1018c9b8ded605f33c2fcd59 Y1 - 2015/// ER -