Print Email Facebook Twitter Flow Properties in Saturated Soils from Differing Behaviour of Dispersive Seismic Velocity and Attenuation Title Flow Properties in Saturated Soils from Differing Behaviour of Dispersive Seismic Velocity and Attenuation Author Ghose, R. Zhubayev, A. Faculty Civil Engineering and Geosciences Department Geoscience & Engineering Date 2012-06-04 Abstract A careful look into the pertinent models of poroelasticity reveals that in water-saturated sediments or soils, the seismic (P and S wave) velocity dispersion and attenuation in the low field-seismic frequency band (20-200 Hz) have a contrasting behaviour in the porosity-permeability domain.Taking advantage of this nearly orthogonal behaviour, a new approach has been proposed, which leads to unique estimates of both porosity and permeability simultaneously. Through realistic numerical tests, the effect of maximum frequency content in data and the integration of P and S waves on the accuracy and robustness of the estimates are demonstrated. To reference this document use: http://resolver.tudelft.nl/uuid:3f5867c0-ff68-447e-968a-216301f91698 ISBN 978-90-73834-27-9 Source 74th EAGE Conference & Exhibition incorporating SPE EUROPEC 2012, Copenhagen, Denmark, 4-7 June 2012 Part of collection Institutional Repository Document type conference paper Rights (c) 2012 The Author(s) Files PDF 285340.pdf 474 KB Close viewer /islandora/object/uuid:3f5867c0-ff68-447e-968a-216301f91698/datastream/OBJ/view