TY - CONF
T1 - Effective medium model in shales and sandstones at multifrequency observations
AU - Pertiwi, R. N.
AU - Iacopini, D.
AU - Healy, D.
N1 - Publisher Copyright:
© 5th EAGE Workshop on Rock Physics - Advancements in Rock Physics: Embracing the Fourth Industry Revolution. All rights reserved.
PY - 2020
Y1 - 2020
N2 - This rock-physics investigation aims to understand the elastic response of shales and poorly-consolidated sands with special attention to the variations in textural expression including mineralogy, preferred clay alignment, and porosity; as well as non-textural parameters: stress state and fluid saturation. This research explores such elastic response to produce a deeper understanding in the frequency-related behavior through a modeling approach. Within this framework, two specific aspects are investigated: (i) the elastic modulus as a function of pressure variation, as well as silt- and fluid- inclusion in an anisotropic clay medium, that will consequently produce different clay preferred alignment and distinct anisotropic behaviour at different frequency regime; (ii) the elastic modulus as function of porosity and water-saturation in isotropic granular media, that also addresses frequency-velocity dispersion by acknowledging the microscopic component.
AB - This rock-physics investigation aims to understand the elastic response of shales and poorly-consolidated sands with special attention to the variations in textural expression including mineralogy, preferred clay alignment, and porosity; as well as non-textural parameters: stress state and fluid saturation. This research explores such elastic response to produce a deeper understanding in the frequency-related behavior through a modeling approach. Within this framework, two specific aspects are investigated: (i) the elastic modulus as a function of pressure variation, as well as silt- and fluid- inclusion in an anisotropic clay medium, that will consequently produce different clay preferred alignment and distinct anisotropic behaviour at different frequency regime; (ii) the elastic modulus as function of porosity and water-saturation in isotropic granular media, that also addresses frequency-velocity dispersion by acknowledging the microscopic component.
UR - http://www.scopus.com/inward/record.url?scp=85092655262&partnerID=8YFLogxK
U2 - 10.3997/2214-4609.2020603015
DO - 10.3997/2214-4609.2020603015
M3 - Unpublished paper
AN - SCOPUS:85092655262
SP - 1
EP - 5
T2 - 5th EAGE Workshop on Rock Physics
Y2 - 10 February 2020 through 12 February 2020
ER -