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Stefano Picotti

Researcher at National Institute of Oceanography, India

Publications -  60
Citations -  1362

Stefano Picotti is an academic researcher from National Institute of Oceanography, India. The author has contributed to research in topics: Transverse isotropy & Attenuation. The author has an hindex of 18, co-authored 52 publications receiving 1095 citations.

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P-wave seismic attenuation by slow-wave diffusion: Effects of inhomogeneous rock properties

José M. Carcione, +1 more
- 22 May 2006 - 
TL;DR: In this paper, the authors investigated the amount of attenuation and velocity dispersion caused by different types of heterogeneities in the rock properties, namely, porosity, grain and frame moduli, permeability, and fluid properties.
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Physics and Seismic Modeling for Monitoring CO2 Storage

TL;DR: In this article, a new petro-elastical and numerical-simulation methodology is presented to compute synthetic seismograms for reservoirs subject to CO2 sequestration, where the gas properties are obtained from the van der Waals equation and the absorption of gas by oil and brine, as a function of the in situ pore pressure and temperature.
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Subglacial Lake Whillans — Seismic observations of a shallow active reservoir beneath a West Antarctic ice stream

TL;DR: Seismic and surface observations from Subglacial Lake Whillans (SLW), West Antarctica, reveal that this active lake forms a persistent, albeit fluctuating, reservoir beneath Whillan Ice Stream as mentioned in this paper.
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Angular and Frequency-Dependent Wave Velocity and Attenuation in Fractured Porous Media

TL;DR: In this article, the authors considered the theory for all propagation angles by obtaining the five complex and frequency-dependent stiffnesses of the equivalent transversely isotropic medium corresponding to a poroelastic medium containing planar fractures.
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Estimation of glacier thicknesses and basal properties using the horizontal-to-vertical component spectral ratio (HVSR) technique from passive seismic data

TL;DR: In this article, the authors applied the radio-echo sounding, geoelectric and active seismic methods, widely employed to image the earth interior, to verify the reliability of the HVSR technique in Alpine and Antarctic glacial environments.