The rock physics handbook : tools for seismic analysis in porous media

347 Pages·1998·14.259 MB·English

by  Mavko, Gary, Mukerji, Tapan, Dvorkin, Jack

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Copyrighted Materials
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THE ROCK PHYSICS
HANDBOOK
TOOLS FOR SEISMIC ANALYSIS
IN POROUS MEDIA
Gary Mavko Tapan Mukerji Jack Dvorkin
Stanford UniversiQ Stanford UniversiQ Stanford UniversiQ
CAMBRIDGE
UNIVERSITY PRESS
PUBLISHED BY THE PRESS SYNDICATE OF THE UNIVERSITY OF CAMBRIDGE
The Pitt Building, Trumpington Street, Cambridge, United Kingdom
CAMBRIDGE UNIVERSITY PRESS
The Edinburgh Building, Cambridge CB2 2RU, UK
40 West 20th Street, New York NY 10011-4211, USA
477 Williamstown Road, Port Melbourne, VIC 3207, Australia
Ruiz de Alarcon 13, 28014 Madrid, Spain
Dock House, The Waterfront, Cape Town 8001, South Africa
http://www.cambridge.org
0 Cambridge University Press
This book is in copyright. Subject to statutory exception
and to the provisions of relevant collective licensing agreements,
no reproduction of any part may take place without
the written permission of Cambridge University Press.
First published 1998
First paperback edition 2003
Typeset in Franklin Gothic Demi and Times Roman
A catalogue record for this book is available from the British Library
Library of Congress Cataloguing-in-Publication Data
Mavko, Gary, 1949-
The rock physics handbook : tools for seismic analysis in porous
media / Gary Mavko, Tapan Mukerji, Jack Dvorkin.
p. cm.
Includes index.
ISBN 0 521 62068 6 hardback
1. Rocks. 2. Geophysics. I. Mukerji, Tapan, 1965
11. Dvorkin, Jack. 1953- . 111. Title.
QE431.6.P6M38 1998
552’.06-DC21 97-36653
CIP
ISBN 0 521 62068 6 hardback
ISBN 0 521 54344 4 paperback
PREFACE
I believe that the greatest practical impact of rock physics during the next few
years will come not from new laboratory or theoretical discoveries but from mak-
ing decades of existing results accessible to those who need them. This is not
to say that rock physics is a finished subject. On the contrary, many aspects are
still poorly understood and even controversial. Yet, particularly in applied fields,
only a fraction of existing rock physics results are widely known. Our goal in
preparing The Rock Physics Handbook was to help disseminate this information
by distilling into a single volume part of the scattered and eclectic mass of knowl-
edge that can already be useful for the rock physics interpretation of seismic
data.
Our objective in preparing the handbook was to summarize in a convenient
form many of the commonly needed theoretical and empirical relations of rock
physics - those relations that we derive once every two years and then forget or
find ourselves searching for in piles of articles, somewhere in that shelf of books,
or on scraps of paper taped to the side of the filing cabinet.
Our approach was to present results, with a few of the key assumptions and
limitations, and almost never any derivations. Our intention was to create a quick
reference and not a textbook. Hence, we chose to encapsulate a broad range of
topics rather than give in-depth coverage of a few. Even so, there are many topics
that we have not addressed. We hope that the brevity of our discussions does not
give the impression that application of any rock physics result to real rocks is
free of pitfalls. We assume that the reader will be generally aware of the various
topics, and, if not, we provide a few references to the more complete descriptions
in books and journals.
ix
X P R E F A C E
The Rock Physics Handbook is presented in the form of seventy-six stand-
alone articles. We wanted the user to be able to go directly to the topic of interest
and to find all of the necessary information within a few pages without the need to
refer to previous chapters, as in a conventional textbook. As a result, an occasional
redundancy is evident in the explanatory text.
The handbook contains sections on wave propagation, AVO-AVOZ, effec-
tive media, elasticity and poroelasticity, and pore-fluid flow and diffusion, plus
overviews of dispersion mechanisms, fluid substitution, and Vp-Vs relations. The
book also presents empirical results derived from reservoir rocks, sediments, and
granular media, as well as tables of mineral data and an atlas of reservoir rock
properties. The emphasis throughout is primarily on seismic properties. We have
also included commonly used models and relations for electrical and dielectric
rock properties.
We believe that this book is complementary to other works. For in-depth
discussions of specific rock physics topics, we recommend Acoustics of Porous
Media by BourbiC, Coussy, and Zinszner; Introduction to the Physics of Rocks by
GuCguen and Palciauskas; Rock Physics and Phase Relations edited by Ahrens;
and Offset Dependent Rejectivity - Theory and Practice of AVO Analysis edited
by Castagna and Backus. For excellent collections and discussions of classic rock
physics papers we recommend Seismic and Acoustic Velocities in Resenloir Rocks,
Volumes 1 and 2 edited by Wang and Nur, Elastic Properties and Equations of
State edited by Shankland and Bass, and Seismic Wave Attenuation by Toksoz and
Johnston.
We wish to thank the faculty, students, and industrial affiliates of the Stanford
Rock Physics and Borehole Geophysics (SRB) project for many valuable com-
ments and insights. We found discussions with Zhijing Wang, Thierry Cadoret,
Ivar Brevik, Sue Raikes, Sverre Strandenes, Mike Batzle, and Jim Berryman par-
ticularly useful. Li Teng contributed the chapter on anisotropic AVOZ, and Ran
Bachrach contributed to the chapter on dielectric properties. Ranie Lynds helped
with the graphics and did a marvelous job of proofing and editing. Special thanks
are extended to Barbara Mavko for many useful comments on content and style.
And as always, we are indebted to Amos Nur, whose work, past and present, has
helped to make the field of rock physics what it is today.
We hope you will find this handbook useful.
Gary Mavko
CONTENTS
Preface page ix
PART 1: BASIC TOOLS 1
1.1 The Fourier Transform 1
1.2 The Hilbert Transform and Analytic Signal 8
1.3 Statistics and Linear Regression 10
1.4 Coordinate Transformations 14
PART 2: ELASTICITY AND HOOKE’S LAW 17
2.1 Elastic Moduli - Isotropic Form of Hooke’s Law 17
2.2 Anisotropic Form of Hooke’s Law 19
2.3 Thomsen’s Notation for Weak Elastic Anisotropy 25
2.4 Stress-Induced Anisotropy in Rocks 26
2.5 Strain Components and Equations of Motion in Cylindrical and
Spherical Coordinate Systems 32
2.6 Deformation of Inclusions and Cavities in Elastic Solids 34
2.7 Deformation of a Circular Hole - Borehole Stresses 45
2.8 Mohr’s Circles 48
PART 3: SEISMIC WAVE PROPAGATION 51
3.1 Seismic Velocities 51
3.2 Phase, Group, and Energy Velocities 54
vi C O N T E N T S
3.3 Impedance, Reflectivity, and Transmissivity 57
3.4 Reflectivity and AVO 60
3.5 AVOZ in Anisotropic Environments 65
3.6 Viscoelasticity and Q 70
3.7 Kramers-Kronig Relations Between Velocity Dispersion
and Q 75
3.8 Waves in Layered Media: Full-Waveform Synthetic Seismograms 77
3.9 Waves in Layered Media: Stratigraphic Filtering and
Velocity Dispersion 82
3.10 Waves in Layered Media: Frequency-Dependent Anisotropy
and Dispersion 86
3.11 Scale-Dependent Seismic Velocities in Heterogeneous Media 91
3.12 Scattering Attenuation 95
3.13 Waves in Cylindrical Rods - The Resonant Bar 100
PART 4: EFFECTIVE MEDIA 106
4.1 Hashin-Shtrikman Bounds 106
4.2 Voigt and Reuss Bounds 110
4.3 Wood’s Formula 112
4.4 Hill Average Moduli Estimate 114
4.5 Composite with Uniform Shear Modulus 115
4.6 Rock and Pore Compressibilities and Some Pitfalls 117
4.7 Kuster and Toksoz Formulation for Effective Moduli 121
4.8 Self-Consistent Approximations of Effective Moduli 123
4.9 Differential Effective Medium Model 129
4.10 Hudson’s Model for Cracked Media 133
4.11 Eshelby-Cheng Model for Cracked Anisotropic Media 140
4.12 Elastic Constants in Finely Layered Media Backus Average 142
-
PART 5: GRANULAR MEDIA 147
5.1 Packing of Spheres - Geometric Relations 147
5.2 Random Spherical Grain Packings - Contact Models and Effective
Moduli 149
5.3 Ordered Spherical Grain Packings Effective Moduli 160
-
PART 6: FLUID EFFECTS ON
WAVE PROPAGATION 162
6.1 Biot’s Velocity Relations 162
6.2 Geertsma-Smit Approximations of Biot’s Relations 166
6.3 Gassmann’s Relations 168
6.4 BAM - Marion’s Bounding Average Method 177
C O N T E N T S vii
6.5 Fluid Substitution in Anisotropic Rocks: Brown and
Korringa’s Relations 179
6.6 Generalized Gassmann’s Equations for Composite Porous Media 181
6.7 Mavko-Jizba Squirt Relations 184
6.8 Extension of Mavko-Jizba Squirt Relations for All Frequencies 186
6.9 BISQ 190
6.10 Anisotropic Squirt 192
6.11 Common Features of Fluid-Related Velocity Dispersion Mechanisms 197
6.12 Partial and Multiphase Saturations 202
6.13 Partial Saturation: White and Dutta-OdC Model for Velocity
Dispersion and Attenuation 207
6.14 Waves in Pure Viscous Fluid 212
6.15 Physical Properties of Gases and Fluids 2 14
PART 7: EMPIRICAL RELATIONS 22 1
7.1 Velocity-Porosity Models: Critical Porosity and Nur’s Modified
Voigt Average 22 1
7.2 Velocity-Porosity Models: Geertsma’s Empirical Relations
for Compressibility 225
7.3 Velocity-Porosity Models: Wyllie’s Time Average Equation 226
7.4 Velocity-Porosity Models: Raymer-Hunt-Gardner Relations 228
7.5 Velocity-Porosity-Clay Models: Han’s Empirical Relations for
Shaley Sandstones 23 1
7.6 Velocity-Porosity-Clay Models: Tosaya’s Empirical Relations for
Shaley Sandstones 233
7.7 Velocity-Porosity-Clay Models: Castagna’s Empirical Relations
for Velocities 234
7.8 Vp-Vs Relations 235
7.9 Velocity-Density Relations 250
PART 8: FLOW AND DIFFUSION 255
8.1 Darcy’s Law 255
8.2 Kozeny-Carman Relation for Flow 260
8.3 Viscous Flow 264
8.4 Capillary Forces 266
8.5 Diffusion and Filtration - Special Cases 268
PART 9: ELECTRICAL PROPERTIES 27 1
9.1 Bounds and Effective Medium Models 27 1
9.2 Velocity Dispersion and Attenuation 275
9.3 Empirical Relations 279
9.4 Electrical Conductivity in Porous Rocks 282
viii C O N T E N T S
PART 10: APPENDIXES 289
10.1 Typical Rock Properties 289
10.2 Conversions 30 4
10.3 Moduli and Density of Common Minerals 306
References 313
Index 325
PART 1
BASIC TOOLS
SYNOPSIS
The Fourier transform of f(x)i s defined as
J --x
The inverse Fourier transform is given by
EVENNESS AND ODDNESS
A function E(x) is even if E(x)= E(-x). A function O(x) is odd if O(x) =
- 0(-x).
The Fourier transform has the following properties for even and odd functions:
Even Functions. The Fourier transform of an even function is even. A real
even function transforms to a real even function. An imaginarq. even function
transforms to an imaginav even function.
1
2 B A S I C T O O L S
Odd Functions. The Fourier transform of an odd function is odd. A real odd
function transforms to an imaginary odd function. An imaginary odd function
transforms to a real odd function (i.e., the “realness” flips when the Fourier
transform of an odd function is taken).
real even (RE) -+ real even (RE)
imaginary even (IE) -+ imaginary even (IE)
real odd (RO) -+ imaginary odd (10)
imaginary odd (10) + real odd (RO)
Any function can be expressed in terms of its even and odd parts:
where
p1 )+
E(x) = f(-x>l
1
O(x)= ,[f(x) - f(-x>l
Then, for an arbitrary complex function we can summarize these relations as
(Bracewell, 1965)
+ + +
f(x) = re(x) i ie(x) ro(x) i io(x)
+ + +
F(s) = RE(s) i IE(s) RO(s) i IO(s)
As a consequence, a real function f(x) has a Fourier transform that is hermi-
tian, F(s) = F*(-s), where * refers to the complex conjugate.
For a more general complex function, f(x), we can tabulate some additional
properties (Bracewell, 1965):