Geoscience Reference
In-Depth Information
through the coulombic interaction. (2) The flow of pore
water with respect to the solid phase (formed by the
assemblage of grains) generates a source current density
due to the drag of the charge density, near the mineral
grain surface, contained in the pore water. This streaming
current depends on either the zeta potential,
of Colloid and Interface Science , 202 , 195
-
204, doi: 10.1006/
jcis.1998.5402.
Biot, M.A. (1962a) Generalized theory of acoustic propagation
in porous dissipative media. Journal of the Acoustical Society of
America , 34 ( 9 ), 1254
1264.
Biot, M.A. (1962b) Mechanics of deformation and acoustic
propagation in porous media. Journal of Applied Physics , 33 ( 4 ),
1482
-
,oran
effective charge density Q V . We established a bridge
between these two quantities. (3) The seismoelectric
response due to the flow of water relative to the mineral
framework is triggered by the propagation of seismic
waves and, possibly as discussed later in Chapter 5,by
the seismic source itself. We must therefore account for
three types of EM disturbances: those associated with
the seismic sources, the coseismoelectric effects associ-
ated with the propagation of the seismic waves, and
the seismoelectric conversion (also called interface
response) associated with the conversion of hydrome-
chanical to EM energy at macroscopic interfaces in the
investigated material. (4) The distribution of the resulting
electrical field is controlled not only by the source current
density (direction and magnitude) generated in the
porous material but also by the conductivity distribution
in the material. This conductivity is frequency dependent
(to some extent) and is characterized by both an inphase
component and a quadrature component. This implies
that the electrical field is not necessarily in phase with
the source current density. The frequency dependence
of the electrical conductivity is termed induced polariza-
tion in geophysics and is not captured by the theory
of Pride.
We have also discussed previously the main ingredients
that are necessary to set the stage for the introduction of
the seismoelectric method. Chapter 2 will be devoted to
the development of a seismoelectric theory in fully
water-saturated conditions. This requires discussion of
the equations describing the propagation of seismic waves
in porous media characterized by a linear elastic skeleton
(dynamic poroelasticity) and the Maxwell equations,
usually taken in their quasistatic forms.
ζ
1498.
Blau, L. & Statham, L. (1936) Method and apparatus for seismic
electric prospecting. Technical Report, 2054067, U.S. Patent
and Trademark Office (USPTO), Washington, DC.
Bolève, A., Crespy, A., Revil, A., Janod, F., & Mattiuzzo J.L.
(2007) Streaming potentials of granular media: Influence of
the Dukhin and Reynolds numbers. Journal of Geophysical
Research , 112 , B08204, doi:10.1029/2006JB004673.
Booth, F. & Enderby, J. (1952) On electrical effects due to sound
Waves in Colloidal Suspensions. Proceedings of the American
Physical Society , 208A ,32
-
42.
Börner, F.D. (1992) Complex conductivity measurements of
reservoir properties. Proceedings of the Third European Core
Analysis Symposium, Paris, 359
-
386.
Casagrande, L. (1983) Stabilization of soils by means of
electro-osmosis: State of art. Journal of Boston Society of Civil
Engineers , 69 ( 2 ), 255
-
302.
Chapman, D.L. (1913) A contribution to the theory of
electrocapillarity. Philosophical Magazine , 25 ( 6 ), 475
-
481.
Chittoori, B. & Puppala, A.J. (2011) Quantitative estimation of
clay mineralogy in fine-grained soils. Journal of Geotechnical
and Geoenvironmental Engineering , 137 ( 11 ), 997
-
-
1008, doi:
10.1061/(ASCE)GT.1943-5606.0000521.
Cicerone, D.S., Regazzoni, A.E., & Blesa, M.A. (1992)
Electrokinetic properties of the calcite/water interface in the
presence of magnesium and organic matter. Journal of Colloid
and Interface Science , 154 , 423
433.
Darcy, H. (1856) Les fontaines publiques de la Ville de Dijon ,
Dalmont, Paris.
Debye, P. (1933) A method for the determination of the mass
of electrolyte ions. Journal of Chemical Physics , 1 ,13
-
-
16.
Derouet, B. & Denizot, F. (1951) Comptes Rendus de l
'
Académie
des Sciences, Paris , 233 , 368.
Einstein, A. (1916) The foundations of the general theory of
relativity. Annalen der Physik , 354 ( 7 ), 769
-
822, doi:10.1002/
andp.19163540702.
Enderby, J.A. (1951) On electrical effects due to sound waves
in colloidal suspensions. Proceedings of the Royal Society, London ,
A207 , 329
342.
Fourie, F.D. (2003) Application of Electroseismic Techniques
to Geohydrological Investigations in Karoo Rocks, PhD Thesis,
University of the Free State, Bloemfontein, South Africa, 195 pp.
Frenkel, J. (1944) On the theory of seismic and seismoelectric
phenomena in a moist soil, Journal Physics (Soviet) , 8 ( 4 ),
230
-
References
Ahmad, M.U. (1969) A laboratory study of streaming potentials.
Geophysical Prospecting , 12 ( 1 ), 49
241.
Friborg, J. (1996) Experimental and theoretical investigations
into the streaming potential phenomenon with special
-
64.
Avena, M.J. & De Pauli, C.P. (1998) Proton adsorption and
electrokinetics of an Argentinean Montmorillonite. Journal
-
Search WWH ::




Custom Search