Roy (2008) Potential Theory in Applied Geophysics
Roy KK (2008) Potential Theory in Applied Geophysics. https://doi.org/10.1007/978-3-540-72334-9
Contents
1 Elements of Vector Analysis
1.1 Scalar&Vector
1.2 Properties of Vectors
1.3 Gradient of a Scalar
1.4 Divergence of a Vector
1.5 Surface Integral
1.6 Gauss’s Divergence Theorem
1.7 Line Integral
1.8 Curl of a Vector
1.9 Line Integral in a Plane (Stoke’s Theorem)
1.10 Successive Application of the Operator ∇
1.11 Important Relations in Vector Algebra
2 Introductory Remarks
2.1 Field of Force
2.2 Classification of Fields
- 2.2.1 Type A Classification
- 2.2.2 Type B Classification
- 2.2.3 Type C Classification
- 2.2.4 Type D Classification
- 2.2.5 Type E Classification
- 2.2.6 Type F Classification
- 2.2.7 Type G Classification
- 2.2.8 Type H Classification
- 2.2.9 Type I Classification
- 2.2.10 Type J Classification
- 2.2.11 Type K Classification
2.3 Concept of Potential
2.4 Field Mapping
2.5 Nature of a Solid Medium
2.6 Tensors
2.7 Boundary Value Problems
- 2.7.1 Dirichlet’s Problem
- 2.7.2 Neumann Problem
- 2.7.3 Mixed Problem
2.8 Dimension of a Problem and its Solvability
2.9 Equations
- 2.9.1 Differential Equations
- 2.9.2 Integral Equations
2.10 Domain of Geophysics in Potential Theory
3 Gravitational Potential and Field
3.1 Introduction
3.2 Newton’s Law of Gravitation
3.3 Gravity Field at a Point due to Number of Point Sources
3.4 Gravitational Field for a Large Body
3.5 Gravitational Field due to a Line Source
3.6 Gravitational Potential due to a Finite Line Source
3.7 Gravitational Attraction due to a Buried Cylinder
3.8 Gravitational Field due to a Plane Sheet
3.9 Gravitational Field due to a Circular Plate
3.10 Gravity Field at a Point Outside on the Axis of a Vertical Cylinder
3.11 Gravitational Potential at a Point due to a Spherical Body
3.12 Gravitational Attraction on the Surface due to a Buried Sphere
3.13 Gravitational Anomaly due to a Body of Trapezoidal Cross Section
- 3.13.1 Special Cases
3.14 Gravity Field of the Earth
- 3.14.1 Free Air Correction
- 3.14.2 Bouguer Correction
- 3.14.3 Terrain Correction
- 3.14.4 Latitude Correction
- 3.14.5 Tidal Correction
- 3.14.6 Isostatic Correction
3.15 Units
3.16 Basic Equation
4 Electrostatics
4.1 Introduction
4.2 Coulomb’s Law
4.3 Electrostatic Potential
4.4 Electrical Permittivity and Electrical Force Field
4.5 Electric Flux
4.6 Electric Displacement ψ and the Displacement Vector D
4.7 Gauss’s Theorem
4.8 Field due to an Electrostatic Dipole
4.9 Poisson and Laplace Equations
4.10 Electrostatic Energy
4.11 Boundary Conditions
4.12 Basic Equations in Electrostatic Field
5 Magnetostatics
5.1 Introduction
5.2 Coulomb’s Law
5.3 Magnetic Properties
- 5.3.1 Magnetic Dipole Moment
- 5.3.2 Intensity of Magnetisation
- 5.3.3 Magnetic Susceptibility (Induced Magnetism)
- 5.3.4 Ferromagnetic Paramagnetic and Diamagnetic Substances
5.4 Magnetic Induction B
5.5 Magnetic Field Intensity H
5.6 Faraday’s Law
5.7 Biot and Savart’s Law
5.8 Lorentz Force
5.9 Ampere’s Force Law
5.10 Magnetic Field on the Axis of a Magnetic Dipole
5.11 Magnetomotive Force (MMF)
5.12 Ampere’s Law
5.13 Div B = 0
5.14 Magnetic Vector Potential
5.15 Magnetic Scalar Potential
5.16 Poisson’s Relation
5.17 Magnetostatic Energy
5.18 Geomagnetic Field
- 5.18.1 Geomagnetic Field Variations
5.19 Application of Magnetic Field Measurement in Geophysics
5.20 Units
5.21 Basic Equations in Magnetostatics
6 Direct Current Flow Field
6.1 Introduction
6.2 Direct Current Flow
6.3 Differential form of the Ohm’s Law
6.4 Equation of Continuity
6.5 Anisotropy in Electrical Conductivity
6.6 Potential at a Point due to a Point Source
6.7 Potential for Line Electrode Configuration
- 6.7.1 Potential due to a Finite Line Electrode
6.8 Current Flow Inside the Earth
6.9 Refraction of Current Lines
6.10 Dipole Field
6.11 Basic Equations in Direct Current Flow Field
6.12 Units
7 Solution of Laplace Equation
7.1 Equations of Poisson and Laplace
7.2 Laplace Equation in Direct Current Flow Domain
7.3 Laplace Equation in Generalised Curvilinear Coordinates
7.4 Laplace Equation in Cartesian Coordinates
- 7.4.1 When Potential is a Function of Vertical Axis z i.e. φ=f(z)
- 7.4.2 When Potential is a Function of Both x and y i.e. φ=f(xy)
- 7.4.3 Solution of Boundary Value Problems in Cartisian Coordinates by the Method of Separation of Variables
7.5 Laplace Equation in Cylindrical Polar Coordinates
- 7.5.1 When Potentialisa Function of zi.e.φ=f(z)
- 7.5.2 When Potential is a Function of Azimuthal Angle Only i.e. φ = f(ψ)
- 7.5.3 When the Potential is a Function of Radial Distance i.e. Φ = f(ρ)
- 7.5.4 When Potential is a Function of Both ρ and ψ i.e. φ = f(ρ ψ)
- 7.5.5 When Potential is a Function of all the Three Coordinates i.e. φ=f(ρψz)
- 7.5.6 Bessel Equation and Bessel’s Functions
- 7.5.7 Modified Bessel’s Functions
- 7.5.8 Some Relation of Bessel’s Function
7.6 Solution of Laplace Equation in Spherical Polar Co-ordinates
- 7.6.1 When Potential is a Function of Radial Distance r i.e. φ=f(r)
- 7.6.2 When Potential is a Function of Polar Angle i.e. φ = f(θ)
- 7.6.3 When Potential is a Function of Azimuthal Angle i.e. φ = f(ψ)
- 7.6.4 When Potential is a Function of Both the Radial Distanceand Polar Angle i.e. φ=f(rθ)
- 7.6.5 Legender’s Equation and Legender’s polynomial
- 7.6.6 When Potential is a Function of all the Three Coordinates Viz Radial Distance Polar Angle and Azimuthal Angle i.e. φ = f(r θ ψ)
- 7.6.7 Associated Legendre Polynomial
7.7 Spherical Harmonics
- 7.7.1 Zonal Sectoral and Tesseral Harmonics
8 Direct Current Field Related Potential Problems
8.1 Layered Earth Problem in a Direct Current Domain
- 8.1.1 Cramer’s Rule
- 8.1.2 Two Layered Earth Model
- 8.1.3 Three Layered Earth Model
- 8.1.4 General Expressions for the Surface and Subsurface Kernels for an N-Layered Earth
- 8.1.5 Kernels in Different Layers for a Five Layered Earth
- 8.1.6 Potentials in Different Media
8.2 Potential due to a Point Source in a Borehole with Cylindrical Coaxial Boundaries
8.3 Potential for a Transitional Earth
- 8.3.1 Potential for a Medium Where Physical Property Varies Continuously with Distance
- 8.3.2 Potential for a Layered Earth with a Sandwitched Transitional Layer
- 8.3.3 Potential with Media Having Coaxial Cylindrical Symmetry with a Transitional Layer in Between
8.4 Geoelectrical Potential for a Dipping Interface
8.5 Geoelectrical Potentials for an Anisotropic Medium
- 8.5.1 General Nature of the Basic Equations
- 8.5.2 General Solution of Laplace Equation for an Anisotropic
9 Complex Variables and Conformal Transformation in Potential Theory
9.1 DefinitionofAnalyticFunction
9.2 Complex Functions and their Derivatives
9.3 Conformal Mapping
9.4 Transformations
- 9.4.1 Simple Transformations
9.5 Schwarz Christoffel Transformation
- 9.5.1 Introduction
- 9.5.2 Schwarz-Christoffel Transformation of the Interior of a Polygon
- 9.5.3 Determination of Unknown Constants
- 9.5.4 S-C Transformation Theorem
9.6 Geophysical Problems on S-C Transformation
- 9.6.1 Problem 1 Conformal Transformation for a Substratum of Finite Thickness
- 9.6.2 Problem 2 Telluric Field over a Vertical Basement Fault
- 9.6.3 Problem 3 Telluric Field and Apparent Resistivity Over an Anticline
- 9.6.4 Problem 4 Telluric Field Over a Faulted Basement (Horst)
9.7 Elliptic Integrals and Elliptic Functions
- 9.7.1 Legendre’s Equation
- 9.7.2 Complete Integrals
- 9.7.3 Elliptic Functions
- 9.7.4 Jacobi’s Zeta Function
- 9.7.5 Jacobi’s Theta Function
- 9.7.6 Jacobi’s Elliptic Integral of the Third Kind
10 Green’s Theorem in Potential Theory
10.1 Green’s First Identity
10.2 HarmonicFunction
10.3 Corollaries of Green’s Theorem
10.4 RegularFunction
10.5 Green’s Formula
10.6 Some Special Cases in Green’s Formula
10.7 Poisson’s Equation from Green’s Theorem
10.8 Gauss’s Theorem of Total Normal Induction in Gravity Field
10.9 Estimation of Mass in Gravity Field
10.10 Green’s Theorem for Analytical Continuation
10.11 Green’s Theorem for Two Dimensional Problems
10.12 Three to Two Dimensional Conversion
10.13 Green’s Equivalent Layers
10.14 Unique Surface Distribution
10.15 Vector Green’s Theorem
11 Electrical Images in Potential Theory
11.1 Introduction
11.2 Computation of Potential Using Images (Two Media)
11.3 Computation of Potential Using Images (for Three Media)
11.4 General Expressions for Potentials Using Images
11.5 Expressions for Potentials for Two Electrode Configuration
11.6 Expressions for Potentials for Three Electrode Configuration
11.7 Expression for Potentials for Seven Electrode Configurations
12 Electromagnetic Theory (Vector Potentials)
12.1 Introduction
12.2 Elementary Wavelet
12.3 Elliptic Polarisation of Electromagnetic Waves
12.4 Mutual Inductance
- 12.4.1 Mutual Inductance Between any Two Arbitrary Coils
- 12.4.2 Simple Mutual Inductance Model in Geophysics
12.5 Maxwell’s Equations
- 12.5.1 Integral form of Maxwell’s Equations
12.6 Helmholtz Electromagnetic Wave Equations
12.7 Hertz and Fitzerald Vectors
12.8 Boundary Conditions in Electromagnetics
- 12.8.1 Normal Component of the Magnetic Induction B is Continuous Across the Boundary in a Conductor
- 12.8.2 Normal Component of the Electric Displacement is Continuous Across the Boundary
- 12.8.3 Tangential Component of E is Continuous Across the Boundary
- 12.8.4 Tangential Component of H is Continuous Across the Boundary
- 12.8.5 Normal Component of the Current Density is Continuous Across the Boundary
- 12.8.6 Scalar Potentials are Continuous Across the Boundary
12.9 Poynting Vector
13 Electromagnetic Wave Propagation Problems Related to Geophysics
13.1 Plane Wave Propagation
- 13.1.1 Advancing Electromagnetic Wave
- 13.1.2 Plane Wave Incidence on the Surface of the Earth
13.2 Skin Depth
13.3 PerturbationCentroidFrequency
13.4 Magnetotelluric Response for a Layered Earth Model
13.5 Electromagnetic Field due to a Vertical Oscillating Electric Dipole
13.6 Electromagnetic Field due to an Oscillating Vertical Magnetic Dipole Placed on the Surface of the Earth
13.7 Electromagnetic Field due to an Oscillating Horizontal Magnetic Dipole Placed on the Surface of the Earth
13.8 Electromagnetic Field due to a Long Line Cable Placed in an Infinite and Homogenous Medium
13.9 Electromagnetic Field due to a Long Cable on the Surface of a Homogeneous Earth
13.10 Electromagnetic Induction due to an Infinite Cylinder in an Uniform Field
- 13.10.1 Effect of Change in Frequency on the Response Parameter
13.11 Electromagnetic Response due to a Sphere in the Field of a Vertically Oscillating Magnetic Dipole
13.12 Principle of Electrodynamic Similitude
14 Green’s Function
14.1 Introduction
14.2 Delta Function
14.3 Operators
14.4 Adjoint and Self Adjoint Operator
14.5 Definition of a Green’s Function
14.6 FreeSpaceGreen’sFunction
14.7 Green’s Function is a Potential due to a Charge of Unit Strength in Electrostatics
14.8 Green’s Function can Reduce the Number of unknowns to be Determined in a Potential Problem
14.9 Green’s Function has Some Relation with the Concept of Image in Potential Theory
14.10 Reciprocity Relation of Green’s Function
14.11 Green’s Function as a Kernel Function in an Integral Equation
14.12 Poisson’s Equation and Green’s Function
14.13 Problem1
14.14 Problem2
14.15 Problem3
14.16 Dyadics
15 Numerical Methods in Potential Theory
15.1 Introduction
15.2 Finite Difference Formulation/Direct Current Domain (Surface Geophysics)
- 15.2.1 Introduction
- 15.2.2 Formulation of the Problem
- 15.2.3 Boundary Conditions
- 15.2.4 StructureoftheFDBoundaryValueProblem
- 15.2.5 Inverse Fourier Cosine Transform
- 15.2.6 Calibration
15.3 Finite Difference Formulation Domain with Cylindrical Symmetry DC Field Borehole Geophysics
- 15.3.1 Introduction
- 15.3.2 Formulation of the Problem
- 15.3.3 Boundary Conditions
- 15.3.4 Grid Generation for Discretization
- 15.3.5 Finite Difference Equations
- 15.3.6 Current Density Factor q at the Source
- 15.3.7 Evaluation of the Potential
15.4 Finite Difference Formulation Plane Wave Electromagnetics Magnetotellurics
- 15.4.1 Boundary Conditions
15.5 Finite Element Formulation Direct Current Resistivity Domain
- 15.5.1 Introduction
- 15.5.2 Derivation of the Functional from Power Considerations
- 15.5.3 Equivalence between Poisson’s Equation and the Minimization of Power
- 15.5.4 Finite Element Formulation
- 15.5.5 Minimisation of the Power
15.6 3D Model
15.7 Finite Element Formulation Galerkin’s Approach Magnetotellurics
- 15.7.1 Introduction
- 15.7.2 Finite Element Formulation for Helmholtz Wave Equations
- 15.7.3 Element Equations
15.8 Finite Element Formulation Galerkin’s Approach Isoparametric Elements Magnetotellurics
- 15.8.1 Introduction
- 15.8.2 Finite Element Formulation
- 15.8.3 Shape Functions Using Natural Coordinates (ξ η)
- 15.8.4 Coordinate Transformation
15.9 Integral Equation Method
- 15.9.1 Introduction
- 15.9.2 Formulation of an Electromagnetic Boundary Value Problem
16 Analytical Continuation of Potential Field
16.1 Introduction
16.2 Downward Continuation by Harmonic Analysis of Gravity Field
16.3 Taylor’s Series Expansion and Finite Difference Approach for Downward Continuation
- 16.3.1 Approach A
- 16.3.2 Approach B
- 16.3.3 An Example of Analytical Continuation Based on Synthetic Data
16.4 Green’s Theorem and Integral Equations for Analytical Continuation
16.5 Analytical Continuation using Integral Equation and Taking Areal Averages
- 16.5.1 Upward Continuation of Potential Field
- 16.5.2 Downward Continuation of Potential Field (Peters Approach)
16.6 Upward and Downward Continuation using Integral Equation and Lagrange Interpolation Formula
16.7 Downward Continuation of Telluric Current Data
16.8 Upward and Downward Continuation of Electromagnetic Field Data
16.9 Downward Continuation of Electromagnetic Field
- 16.9.1 Downward Continuation of Hz
17 Inversion of Potential Field Data
17.1 Introduction
17.2 Wellposedand Illposed Problems
17.3 Tikhnov’s Regularisation
17.4 Abstract Spaces
- 17.4.1 N–Dimensional Vector Space
- 17.4.2 NormofaVector
- 17.4.3 Metric Space
- 17.4.4 Linear System
- 17.4.5 Normed Space
- 17.4.6 Linear Dependence and Independence
- 17.4.7 Inner Product Space
- 17.4.8 Hilbert Space
17.5 Some Properties of a Matrix
- 17.5.1 Rank of a Matrix
- 17.5.2 Eigen Values and EigenVectors
- 17.5.3 Properties of the Eigen Values
17.6 Lagrange Multiplier
17.7 Singular Value Decomposition (SVD)
17.8 LeastSquaresEstimator
17.9 Ridge Regression Estimator
17.10 Weighted Ridge Regression
17.11 Minimum Norm Algorithm for an Under Determined Problem
- 17.11.1 Norm
- 17.11.2 Minimum Norm Estimator
17.12 Bachus – Gilbert Inversion
- 17.12.1 Introduction
- 17.12.2 B-G Formulation
17.13 Stochastic Inversion
- 17.13.1 Introduction
- 17.13.2 Conjunction of the State of Information
- 17.13.3 Maximum Likelyhood Point
17.14 Occam’s Inversion
17.15 Global Optimization
- 17.15.1 Introduction
- 17.15.2 Monte Carlo Inversion
- 17.15.3 Simulated Annealing
- 17.15.4 Genetic Algorithm
17.16 Neural Network
- 17.16.1 Introduction
- 17.16.2 Optimization Problem
17.17 Joint Inversion