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pro vyhledávání: '"Pratap N. Sahay"'
Autor:
Pratap N. Sahay, Anton Z. Capri
Publikováno v:
Geofísica Internacional, Vol 33, Iss 4, Pp 541-545 (1994)
Construimos un con junto completo de ejes simétricos para el campo de desplazamientos dentro de una barra elástica, homogénea, isotrópica y semi-infinita con condiciones de frontera semi-rigidas sobre la superficie curva de la barra y condiciones
Externí odkaz:
https://doaj.org/article/8b6ba37787084b0da4b94af267fd3f36
Publikováno v:
Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences. 479
In the poroelasticity theory of de la Cruz and Spanos, fluid shearing within the viscous boundary layer, i.e. fluid vorticity, manifests as an independent process, namely the diffusive slow shear wave. Quantifying its impact on elastic wave propagati
Publikováno v:
GEOPHYSICS. 86:MR315-MR324
The shear motion in Newtonian fluids, that is, the fluid vorticity, represents an intrinsic loss mechanism governed by a diffusion equation. Its description involves the trace-free part of the fluid viscous stress tensor. This part is missing in the
Autor:
Tobias M. Müller, Pratap N. Sahay
Publikováno v:
GEOPHYSICS. 85:A13-A17
Injecting fluid in a borehole often has been observed to be causally related with seismicity. The standard explanation assumes that a stress perturbation spreads out and triggers rock failure. It has been suggested that this spreading is governed by
Publikováno v:
First International Meeting for Applied Geoscience & Energy Expanded Abstracts.
Autor:
Tobias M. Müller, Pratap N. Sahay
Publikováno v:
GEOPHYSICS. 84:W1-W20
Biot’s theory of linear poroelasticity dates back to the mid-20th century and is still currently the backbone for understanding deformation processes in fluid-saturated porous rocks with applications in geomechanics, hydrogeology, reservoir enginee
Autor:
Tobias M. Müller, Pratap N. Sahay
Publikováno v:
GEOPHYSICS. 81:L27-L33
Within the Biot poroelasticity theory, the effective pressure coefficient for the bulk volume of a fluid-saturated rock and the Biot coefficient are one and the same quantity. The effective pressure coefficient for the bulk volume is the change of co
Autor:
Tobias M. Müller, Pratap N. Sahay
Publikováno v:
Geophysical Prospecting. 64:1122-1134
Poroelastic modelling of micro-inhomogeneous rocks is of interest for applications in rock physics and geomechanics. Laboratory measurements from both communities indicate that the Biot poroelasticity framework is not adequate. For the case of a macr
Autor:
Pratap N. Sahay, Josue G. González
Publikováno v:
SEG Technical Program Expanded Abstracts 2018.
Autor:
Tobias M. Müller, Pratap N. Sahay
Publikováno v:
Poromechanics VI.