This document discusses how to determine the position of an orbiting body as a function of time for different orbit types. It introduces Kepler's equation, which relates the true anomaly to time through integrals that must be solved iteratively. For elliptical orbits, Kepler's equation leads to the definition of mean anomaly as a function of true anomaly. The mean anomaly is directly proportional to time through the mean motion. Eccentric anomaly is also introduced to simplify expressions relating true anomaly to time.
Is ellipse really a section of cone. The question intrigued me for 20 odd years after leaving high school. Finally got the proof on a cremation ground. Only thereafter I came to know of Dandelin spheres. But this proof uses only bare basics within the scope of high school course of Analytical geometry.
Kittel c. introduction to solid state physics 8 th edition - solution manualamnahnura
1. The document discusses crystallographic planes and directions in a cube, the Miller indices of planes with respect to primitive axes, and the spacing between dots projected onto different planes of a crystal structure.
2. Key concepts from crystallography such as Miller indices, primitive lattice vectors, reciprocal lattice vectors, and the first Brillouin zone are defined. Calculations of interplanar spacing and lattice parameters are shown for simple cubic and face-centered cubic lattices.
3. Binding energies, cohesive energies, and equilibrium properties are calculated and compared for body-centered cubic and face-centered cubic crystal structures. Approximations made in describing crystal binding using Madelung energies and pair potentials are
- The Gibbs method determines orbital elements from three position vectors of an object.
- It utilizes the fact that the position vectors must lie in the same orbital plane, defined by the angular momentum vector.
- Equations relating the position vectors and angular momentum allow solving for the angular momentum magnitude.
- Knowing the angular momentum vector and magnitude allows determining the velocities at the three observation times from the position vectors using basic orbital mechanics equations.
1. The document provides examples of converting between different units of measurement using metric prefixes like micro, pico, and nano. Conversions include kilometers to microns, centimeters to microns, and yards to microns.
2. Additional examples convert between inches and picas, points, and other units like grys and almudes which are used to measure volumes of grains.
3. Conversion factors are also provided for seconds, days, weeks, centuries and other units of time. Examples show converting between these different units of time.
Question answers Optical Fiber Communications 4th Edition by Keiserblackdance1
Scribd download slideshare Solution manual Optical Fiber Communications 4th Edition by Keiser Full Download link at https://findtestbanks.com/download/solution-manual-optical-fiber-communications-4th-edition-by-keiser/ instant download communication systems,fiber communications 4th,Gerd Keiser,optical fiber
This is downloadable version of Solution manual Optical Fiber Communications 4th Edition by Gerd Keiser
Instant download Optical Fiber Communications 4th Edition solutions after payment item
Solution manual Optical Fiber Communications 4th Edition by Gerd Keiser
Click link bellow to view sample chapter of Optical Fiber Communications 4th solutions
http://findtestbanks.com/wp-content/uploads/2017/06/Link-download-Solution-manual-Optical-Fiber-Communications-4th-Edition-by-Gerd-Keiser.pdf
The fou free solution and test banks list
1. The document provides examples of unit conversions using metric prefixes and other conversion factors. Calculations are shown for distances, areas, volumes, and time conversions between various units like kilometers, meters, centimeters, microseconds, seconds and years.
2. Geometric formulas are used to calculate properties of the Earth like circumference, surface area and volume. Examples of unit conversions involving length, area, volume, time and other units are also provided.
3. Examples involve calculating distances, areas, volumes, rotations, uncertainties and time differences between various measurement systems including metric, English, and other historical units. Careful application of conversion factors and significant figures is emphasized.
Differential geometry three dimensional spaceSolo Hermelin
This presentation describes the mathematics of curves and surfaces in a 3 dimensional (Euclidean) space.
The presentation is at an Undergraduate in Science (Math, Physics, Engineering) level.
Plee send comments and suggestions to improvements to solo.hermelin@gmail.com. Thanks/
More presentations can be found at my website http://www.solohermelin.com.
Is ellipse really a section of cone. The question intrigued me for 20 odd years after leaving high school. Finally got the proof on a cremation ground. Only thereafter I came to know of Dandelin spheres. But this proof uses only bare basics within the scope of high school course of Analytical geometry.
Kittel c. introduction to solid state physics 8 th edition - solution manualamnahnura
1. The document discusses crystallographic planes and directions in a cube, the Miller indices of planes with respect to primitive axes, and the spacing between dots projected onto different planes of a crystal structure.
2. Key concepts from crystallography such as Miller indices, primitive lattice vectors, reciprocal lattice vectors, and the first Brillouin zone are defined. Calculations of interplanar spacing and lattice parameters are shown for simple cubic and face-centered cubic lattices.
3. Binding energies, cohesive energies, and equilibrium properties are calculated and compared for body-centered cubic and face-centered cubic crystal structures. Approximations made in describing crystal binding using Madelung energies and pair potentials are
- The Gibbs method determines orbital elements from three position vectors of an object.
- It utilizes the fact that the position vectors must lie in the same orbital plane, defined by the angular momentum vector.
- Equations relating the position vectors and angular momentum allow solving for the angular momentum magnitude.
- Knowing the angular momentum vector and magnitude allows determining the velocities at the three observation times from the position vectors using basic orbital mechanics equations.
1. The document provides examples of converting between different units of measurement using metric prefixes like micro, pico, and nano. Conversions include kilometers to microns, centimeters to microns, and yards to microns.
2. Additional examples convert between inches and picas, points, and other units like grys and almudes which are used to measure volumes of grains.
3. Conversion factors are also provided for seconds, days, weeks, centuries and other units of time. Examples show converting between these different units of time.
Question answers Optical Fiber Communications 4th Edition by Keiserblackdance1
Scribd download slideshare Solution manual Optical Fiber Communications 4th Edition by Keiser Full Download link at https://findtestbanks.com/download/solution-manual-optical-fiber-communications-4th-edition-by-keiser/ instant download communication systems,fiber communications 4th,Gerd Keiser,optical fiber
This is downloadable version of Solution manual Optical Fiber Communications 4th Edition by Gerd Keiser
Instant download Optical Fiber Communications 4th Edition solutions after payment item
Solution manual Optical Fiber Communications 4th Edition by Gerd Keiser
Click link bellow to view sample chapter of Optical Fiber Communications 4th solutions
http://findtestbanks.com/wp-content/uploads/2017/06/Link-download-Solution-manual-Optical-Fiber-Communications-4th-Edition-by-Gerd-Keiser.pdf
The fou free solution and test banks list
1. The document provides examples of unit conversions using metric prefixes and other conversion factors. Calculations are shown for distances, areas, volumes, and time conversions between various units like kilometers, meters, centimeters, microseconds, seconds and years.
2. Geometric formulas are used to calculate properties of the Earth like circumference, surface area and volume. Examples of unit conversions involving length, area, volume, time and other units are also provided.
3. Examples involve calculating distances, areas, volumes, rotations, uncertainties and time differences between various measurement systems including metric, English, and other historical units. Careful application of conversion factors and significant figures is emphasized.
Differential geometry three dimensional spaceSolo Hermelin
This presentation describes the mathematics of curves and surfaces in a 3 dimensional (Euclidean) space.
The presentation is at an Undergraduate in Science (Math, Physics, Engineering) level.
Plee send comments and suggestions to improvements to solo.hermelin@gmail.com. Thanks/
More presentations can be found at my website http://www.solohermelin.com.
This document provides an overview of key concepts in vector calculus, including:
- Vector calculus concepts such as limits, continuity, derivatives, and integrals of vector functions.
- Operations on vectors like addition, subtraction, scalar multiplication.
- Vector products including the dot product and cross product.
- Applications of vector calculus like determining velocity, acceleration, and line, surface, and volume integrals.
- Parametric representations of curves using a parameter like time, and their relation to geometry.
This document provides an overview of quantum electrodynamics (QED). It begins by discussing cross sections and the scattering matrix, defining cross section as the effective size of target particles. It then derives an expression for cross section in terms of the transition rate and flux of incident particles. Next, it summarizes the derivation of the differential cross section and decay rate formulas in QED using relativistic quantum field theory and Feynman diagrams. It concludes by briefly reviewing the historical development of QED and the equivalence of the propagator approach and other formulations.
This document contains instructions and problems related to a physics exam on relativistic particles and superconducting magnets. It includes 4 problems:
1) Describing the motion of a relativistic particle subject to an attractive central force, including graphs of position vs time and momentum vs position.
2) Modeling a meson as two quarks with a central attractive force, and graphing their motion.
3) Transforming the motion graphs from problem 2 into a different reference frame moving at 0.6c.
4) Calculating the energy of a meson moving at 0.6c as observed in the lab frame.
The document provides answer sheets for the problems and specifies the
This document is the preface to the instructor's manual for Classical Dynamics of Particles and Systems by Stephen T. Thornton and Jerry B. Marion. It provides an overview of the contents of the manual, which contains solutions to the end-of-chapter problems from the textbook. The preface notes there are now 509 problems and the solutions range from straightforward to challenging. It stresses the solutions are only for instructors and should not be shared with students.
1) The document presents a wavelet collocation method for numerically solving nth order Volterra integro-differential equations. It expands the unknown function as a series of Chebyshev wavelets of the second kind with unknown coefficients.
2) It states and proves a uniform convergence theorem that establishes the convergence of approximating the solution using truncated Chebyshev wavelet series expansions.
3) The paper demonstrates the validity and applicability of the proposed method through some illustrative examples of solving integro-differential equations using the Chebyshev wavelet collocation approach.
1) Identical particles are particles that can be substituted for each other without changing the physical situation. The particle exchange operator P12 interchanges the coordinates of particles 1 and 2 and commutes with the Hamiltonian.
2) The eigenstates of the particle exchange operator P12 have eigenvalues of +1 or -1, corresponding to symmetric and antisymmetric wave functions respectively.
3) Pauli's principle states that systems of identical particles with half-integer spin obey Fermi-Dirac statistics and have antisymmetric wave functions, while those with integer spin obey Bose-Einstein statistics and have symmetric wave functions.
International Journal of Computational Engineering Research(IJCER)ijceronline
The document discusses using an elliptical curve as an alternative to compound or spiral curves for highway horizontal alignments. It provides equations to define an ellipse based on its major and minor axes and eccentricity. An approach is presented to determine the elliptical curve that satisfies design speed and radius requirements for a given highway design problem. Algorithms are provided to calculate chord lengths, deflection angles, and station points along the elliptical curve. An example problem applies the elliptical curve approach and compares results to equivalent circular and spiral-circular curves.
The document discusses the transformation of coordinates from rectangular to polar coordinates and vice versa. It provides definitions and examples of how to perform these transformations using trigonometric functions. It also explains how to perform translations and rotations of coordinate axes, providing examples of transforming equations under these changes of coordinates. Finally, it discusses representing a circle and parabola using polar coordinate equations.
This document summarizes the key steps and results of two problems involving symmetrical tops and rigid body rotation:
1) It shows that for a torque-free symmetrical top, the angular momentum vector rotates about the symmetry axis with a constant angular frequency, while the symmetry axis rotates about the fixed angular momentum vector with the same frequency. It derives an expression for the maximum separation of the Earth's rotation axis and angular momentum axis.
2) It derives expressions for the kinetic energy and angular momentum components of a uniform right circular cone rolling without slipping on a horizontal plane. It finds the principal moments of inertia and center of mass location of the cone.
The klein gordon field in two-dimensional rindler space-time 200920ver-displayfoxtrot jp R
- The author considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
- They define a two-dimensional action for the scalar field and derive from it the Klein-Gordon equation of motion in this background.
- The equation can be solved exactly using imaginary time. The solution is oscillatory with an angular frequency that corresponds to an integral number, suggesting quantization of the scalar field frequencies in this space-time.
The klein gordon field in two-dimensional rindler space-time 23052020-sqrdfoxtrot jp R
1) The document considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
2) It defines a two-dimensional action for the scalar field and obtains from it the Klein-Gordon equation of motion in the Rindler space-time.
3) The equation has an exact series solution that terminates at an integral number of terms, suggesting the scalar field frequencies correspond to integer values in imaginary time.
The klein gordon field in two-dimensional rindler space-time 04232020updtsfoxtrot jp R
1) The document considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
2) It defines a two-dimensional action for the scalar field and obtains from it the Klein-Gordon equation of motion in this background.
3) The equation has an exact series solution that terminates at an integral number of terms, suggesting the scalar field frequencies correspond to integer values in imaginary time.
The klein gordon field in two-dimensional rindler space-time -sqrdupdt41220foxtrot jp R
1) The document considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
2) It defines a two-dimensional action for the scalar field and obtains from it the Klein-Gordon equation of motion in the Rindler space-time.
3) The equation has an exact series solution that is oscillatory in imaginary time, with the oscillation frequency corresponding to an integral number related to the surface gravity of the space-time.
The klein gordon field in two-dimensional rindler space-time 16052020foxtrot jp R
1) The document considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
2) It defines a two-dimensional action for the scalar field and obtains from it the Klein-Gordon equation of motion in this background.
3) The equation has an exact series solution that terminates at an integral number of terms, suggesting the scalar field frequencies correspond to integer values in imaginary time.
Please show the whole code... Im very confused. Matlab code for ea.pdfarshiartpalace
Please show the whole code... I\'m very confused. Matlab code for earth orbit Using a software
package such as MATLAB, create a plot of an Earth orbit with a = 31, 800 km and e = 0.6 for 0
lessthanorequalto theta lessthanorequalto 2 pi. The origin of the plot should be Earth. Perigee
should be in the direction of the positive x axis (therta = 0). On this plot, you should label (by
hand) the semimajor axis, semiminor axis, radius of perigee, radius of apogee, and the
semiparameter (semilatus rectum) of the ellipse.
Solution
---------------------------------------------------------------------------------------------------------------------
-------------------------------------------------
Elliptic orbit:
%periapsis
rp = 500e3 + getradius(\'earth\');
%eccentricity
ec = .7;
%semimajor axis
a = getsemimajoraxis(rp,ec);
%apoapsis
ra = 2*a-rp;
%true anomaly
theta = [0:.1:360];
orbit = ellipse(theta,a,ec,\'earth\');
figure(1), plot(orbit.x,orbit.y); axis equal
Re = getradius(\'earth\');
x = Re*cosd(theta);
y = Re*sind(theta);
hold on
plot(x,y,\'color\',[0 1 1])
hold off
figure(2), plot(theta,orbit.V/1000)
xlabel(\'\\theta\'), ylabel(\'V (km/s)\')
%current time
c = clock;
%reset hour and second
c(4) = 12; %hour
c(5) = 0; %minute
c(6) = orbit.tau; %seconds
%ellapsed time
datetime(c)
%returns 14-Feb-2015 21:34:54, so it\'s about 9.5 hours later still on
%Monday
2
ans =
22-Feb-2015 21:34:54
-----------Elliptic orbit
%periapsis
rp = 500e3 + getradius(\'earth\');
%eccentricity
ec = .7;
%semimajor axis
a = getsemimajoraxis(rp,ec);
%apoapsis
ra = 2*a-rp;
%true anomaly
theta = [0:.1:360];
orbit = ellipse(theta,a,ec,\'earth\');
figure(1), plot(orbit.x,orbit.y); axis equal
Re = getradius(\'earth\');
x = Re*cosd(theta);
y = Re*sind(theta);
hold on
plot(x,y,\'color\',[0 1 1])
hold off
figure(2), plot(theta,orbit.V/1000)
xlabel(\'\\theta\'), ylabel(\'V (km/s)\')
%current time
c = clock;
%reset hour and second
c(4) = 12; %hour
c(5) = 0; %minute
c(6) = orbit.tau; %seconds
%ellapsed time
datetime(c)
%returns 14-Feb-2015 21:34:54, so it\'s about 9.5 hours later still on
%Monday
2
ans =
22-Feb-2015 21:34:54
3
The circular orbits at perigee and apogee are
7.6167 and 3.1997 km/s, respectively.
-----Parabolic orbit:
Sphere of influence is actually a chapter 5 concept, but is the distance at which the gravitational
forces
between two objects is equal. Thus,
While an approximation, if we just estimate this as the point between the sun and the earth
where
these forces balance, then if the orbital radius of Earth is , then
, and thus solution for r_E in gives
r_soi = getsphereofinfluence(\'earth\',\'sun\');
display([\'Radius from center of earth to sphere of influence is approximately \' num2str(r_soi)]);
%perifocal distance
rp = 500e3 + getradius(\'earth\');
%eccentricty
ec = 1; %always so for a a parabola
theta = -180:1:180;
orbit = parabola(theta,rp,\'earth\');
figure(3), plot(orbit.x,orbit.y); axis equal
Re = getradius(\'earth\');
x = Re*cosd(theta);
y = Re*sind(theta);
.
- The document describes the conjugate beam method for analyzing beams with varying rigidities.
- The method involves drawing an imaginary conjugate beam that is loaded based on the bending moments of the real beam.
- The slope and deflection of points on the real beam can then be determined from the shear and bending moment of the corresponding points on the conjugate beam.
- An example problem is worked out in detail to demonstrate calculating the slope and deflection at the end of a cantilever beam with varying moment of inertia along its length using the conjugate beam method.
The document discusses applications of integration, including calculating the length of a curve and surface area of solids obtained by rotating curves. It provides formulas for finding the arc length of a curve given by y=f(x), and surface area of solids obtained by rotating curves about the x- or y-axes. Examples are worked out applying these formulas to find the arc length of curves and surface area of rotated regions. The document also discusses evaluating triple integrals to find the volume of a three-dimensional region and using triple integrals to find the centroid of a volume.
The klein gordon field in two-dimensional rindler space-time 28072020ver-drft...foxtrot jp R
- The author considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
- They define an informal two-dimensional action for the scalar field and obtain from it the Klein-Gordon equation of motion in this background.
- The equation can be solved exactly using imaginary time. The solution is oscillatory with an angular frequency that corresponds to an integral number, suggesting quantization of the scalar field frequencies in this space-time.
The klein gordon field in two-dimensional rindler space-time 14072020foxtrot jp R
- The author considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
- They define an informal two-dimensional action for the scalar field and obtain from it the Klein-Gordon equation of motion in this background.
- The equation can be solved exactly using imaginary time. The solution is oscillatory with an angular frequency that corresponds to an integral number, suggesting quantization of the scalar field frequencies in this space-time.
This document discusses torsion and torsion of circular shafts. It introduces torsion, defines the assumptions made in analyzing torsion of circular shafts, and derives the equations for shear strain, stress, angle of twist, and torque-twist relationship. It provides the torsion formulas for solid and hollow circular shafts. Sample problems are included to demonstrate calculating shear stress, torque, and angle of twist in statically indeterminate torsion problems.
This document provides an overview of orbital perturbations and methods for modeling them. It introduces Cowell's method and Encke's method for numerically integrating the equations of motion with perturbations. It then discusses atmospheric drag as a perturbation, describing how drag causes orbits to decay over time. It provides the US Standard Atmosphere 1976 model for atmospheric density with altitude.
This document discusses coordinate systems for describing orbits in three dimensions. It introduces the geocentric equatorial frame, which uses a right-handed Cartesian coordinate system centered on Earth with axes defined by the vernal equinox and Earth's rotation. The state vector specifies an object's position and velocity in this frame using six components. Orbital elements also uniquely define orbits using six parameters and the location of the object. Coordinate transformations allow changing between the state vector and orbital element representations.
This document provides an overview of key concepts in vector calculus, including:
- Vector calculus concepts such as limits, continuity, derivatives, and integrals of vector functions.
- Operations on vectors like addition, subtraction, scalar multiplication.
- Vector products including the dot product and cross product.
- Applications of vector calculus like determining velocity, acceleration, and line, surface, and volume integrals.
- Parametric representations of curves using a parameter like time, and their relation to geometry.
This document provides an overview of quantum electrodynamics (QED). It begins by discussing cross sections and the scattering matrix, defining cross section as the effective size of target particles. It then derives an expression for cross section in terms of the transition rate and flux of incident particles. Next, it summarizes the derivation of the differential cross section and decay rate formulas in QED using relativistic quantum field theory and Feynman diagrams. It concludes by briefly reviewing the historical development of QED and the equivalence of the propagator approach and other formulations.
This document contains instructions and problems related to a physics exam on relativistic particles and superconducting magnets. It includes 4 problems:
1) Describing the motion of a relativistic particle subject to an attractive central force, including graphs of position vs time and momentum vs position.
2) Modeling a meson as two quarks with a central attractive force, and graphing their motion.
3) Transforming the motion graphs from problem 2 into a different reference frame moving at 0.6c.
4) Calculating the energy of a meson moving at 0.6c as observed in the lab frame.
The document provides answer sheets for the problems and specifies the
This document is the preface to the instructor's manual for Classical Dynamics of Particles and Systems by Stephen T. Thornton and Jerry B. Marion. It provides an overview of the contents of the manual, which contains solutions to the end-of-chapter problems from the textbook. The preface notes there are now 509 problems and the solutions range from straightforward to challenging. It stresses the solutions are only for instructors and should not be shared with students.
1) The document presents a wavelet collocation method for numerically solving nth order Volterra integro-differential equations. It expands the unknown function as a series of Chebyshev wavelets of the second kind with unknown coefficients.
2) It states and proves a uniform convergence theorem that establishes the convergence of approximating the solution using truncated Chebyshev wavelet series expansions.
3) The paper demonstrates the validity and applicability of the proposed method through some illustrative examples of solving integro-differential equations using the Chebyshev wavelet collocation approach.
1) Identical particles are particles that can be substituted for each other without changing the physical situation. The particle exchange operator P12 interchanges the coordinates of particles 1 and 2 and commutes with the Hamiltonian.
2) The eigenstates of the particle exchange operator P12 have eigenvalues of +1 or -1, corresponding to symmetric and antisymmetric wave functions respectively.
3) Pauli's principle states that systems of identical particles with half-integer spin obey Fermi-Dirac statistics and have antisymmetric wave functions, while those with integer spin obey Bose-Einstein statistics and have symmetric wave functions.
International Journal of Computational Engineering Research(IJCER)ijceronline
The document discusses using an elliptical curve as an alternative to compound or spiral curves for highway horizontal alignments. It provides equations to define an ellipse based on its major and minor axes and eccentricity. An approach is presented to determine the elliptical curve that satisfies design speed and radius requirements for a given highway design problem. Algorithms are provided to calculate chord lengths, deflection angles, and station points along the elliptical curve. An example problem applies the elliptical curve approach and compares results to equivalent circular and spiral-circular curves.
The document discusses the transformation of coordinates from rectangular to polar coordinates and vice versa. It provides definitions and examples of how to perform these transformations using trigonometric functions. It also explains how to perform translations and rotations of coordinate axes, providing examples of transforming equations under these changes of coordinates. Finally, it discusses representing a circle and parabola using polar coordinate equations.
This document summarizes the key steps and results of two problems involving symmetrical tops and rigid body rotation:
1) It shows that for a torque-free symmetrical top, the angular momentum vector rotates about the symmetry axis with a constant angular frequency, while the symmetry axis rotates about the fixed angular momentum vector with the same frequency. It derives an expression for the maximum separation of the Earth's rotation axis and angular momentum axis.
2) It derives expressions for the kinetic energy and angular momentum components of a uniform right circular cone rolling without slipping on a horizontal plane. It finds the principal moments of inertia and center of mass location of the cone.
The klein gordon field in two-dimensional rindler space-time 200920ver-displayfoxtrot jp R
- The author considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
- They define a two-dimensional action for the scalar field and derive from it the Klein-Gordon equation of motion in this background.
- The equation can be solved exactly using imaginary time. The solution is oscillatory with an angular frequency that corresponds to an integral number, suggesting quantization of the scalar field frequencies in this space-time.
The klein gordon field in two-dimensional rindler space-time 23052020-sqrdfoxtrot jp R
1) The document considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
2) It defines a two-dimensional action for the scalar field and obtains from it the Klein-Gordon equation of motion in the Rindler space-time.
3) The equation has an exact series solution that terminates at an integral number of terms, suggesting the scalar field frequencies correspond to integer values in imaginary time.
The klein gordon field in two-dimensional rindler space-time 04232020updtsfoxtrot jp R
1) The document considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
2) It defines a two-dimensional action for the scalar field and obtains from it the Klein-Gordon equation of motion in this background.
3) The equation has an exact series solution that terminates at an integral number of terms, suggesting the scalar field frequencies correspond to integer values in imaginary time.
The klein gordon field in two-dimensional rindler space-time -sqrdupdt41220foxtrot jp R
1) The document considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
2) It defines a two-dimensional action for the scalar field and obtains from it the Klein-Gordon equation of motion in the Rindler space-time.
3) The equation has an exact series solution that is oscillatory in imaginary time, with the oscillation frequency corresponding to an integral number related to the surface gravity of the space-time.
The klein gordon field in two-dimensional rindler space-time 16052020foxtrot jp R
1) The document considers a Klein-Gordon scalar field in a two-dimensional Rindler space-time background.
2) It defines a two-dimensional action for the scalar field and obtains from it the Klein-Gordon equation of motion in this background.
3) The equation has an exact series solution that terminates at an integral number of terms, suggesting the scalar field frequencies correspond to integer values in imaginary time.
Please show the whole code... Im very confused. Matlab code for ea.pdfarshiartpalace
Please show the whole code... I\'m very confused. Matlab code for earth orbit Using a software
package such as MATLAB, create a plot of an Earth orbit with a = 31, 800 km and e = 0.6 for 0
lessthanorequalto theta lessthanorequalto 2 pi. The origin of the plot should be Earth. Perigee
should be in the direction of the positive x axis (therta = 0). On this plot, you should label (by
hand) the semimajor axis, semiminor axis, radius of perigee, radius of apogee, and the
semiparameter (semilatus rectum) of the ellipse.
Solution
---------------------------------------------------------------------------------------------------------------------
-------------------------------------------------
Elliptic orbit:
%periapsis
rp = 500e3 + getradius(\'earth\');
%eccentricity
ec = .7;
%semimajor axis
a = getsemimajoraxis(rp,ec);
%apoapsis
ra = 2*a-rp;
%true anomaly
theta = [0:.1:360];
orbit = ellipse(theta,a,ec,\'earth\');
figure(1), plot(orbit.x,orbit.y); axis equal
Re = getradius(\'earth\');
x = Re*cosd(theta);
y = Re*sind(theta);
hold on
plot(x,y,\'color\',[0 1 1])
hold off
figure(2), plot(theta,orbit.V/1000)
xlabel(\'\\theta\'), ylabel(\'V (km/s)\')
%current time
c = clock;
%reset hour and second
c(4) = 12; %hour
c(5) = 0; %minute
c(6) = orbit.tau; %seconds
%ellapsed time
datetime(c)
%returns 14-Feb-2015 21:34:54, so it\'s about 9.5 hours later still on
%Monday
2
ans =
22-Feb-2015 21:34:54
-----------Elliptic orbit
%periapsis
rp = 500e3 + getradius(\'earth\');
%eccentricity
ec = .7;
%semimajor axis
a = getsemimajoraxis(rp,ec);
%apoapsis
ra = 2*a-rp;
%true anomaly
theta = [0:.1:360];
orbit = ellipse(theta,a,ec,\'earth\');
figure(1), plot(orbit.x,orbit.y); axis equal
Re = getradius(\'earth\');
x = Re*cosd(theta);
y = Re*sind(theta);
hold on
plot(x,y,\'color\',[0 1 1])
hold off
figure(2), plot(theta,orbit.V/1000)
xlabel(\'\\theta\'), ylabel(\'V (km/s)\')
%current time
c = clock;
%reset hour and second
c(4) = 12; %hour
c(5) = 0; %minute
c(6) = orbit.tau; %seconds
%ellapsed time
datetime(c)
%returns 14-Feb-2015 21:34:54, so it\'s about 9.5 hours later still on
%Monday
2
ans =
22-Feb-2015 21:34:54
3
The circular orbits at perigee and apogee are
7.6167 and 3.1997 km/s, respectively.
-----Parabolic orbit:
Sphere of influence is actually a chapter 5 concept, but is the distance at which the gravitational
forces
between two objects is equal. Thus,
While an approximation, if we just estimate this as the point between the sun and the earth
where
these forces balance, then if the orbital radius of Earth is , then
, and thus solution for r_E in gives
r_soi = getsphereofinfluence(\'earth\',\'sun\');
display([\'Radius from center of earth to sphere of influence is approximately \' num2str(r_soi)]);
%perifocal distance
rp = 500e3 + getradius(\'earth\');
%eccentricty
ec = 1; %always so for a a parabola
theta = -180:1:180;
orbit = parabola(theta,rp,\'earth\');
figure(3), plot(orbit.x,orbit.y); axis equal
Re = getradius(\'earth\');
x = Re*cosd(theta);
y = Re*sind(theta);
.
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1. Orbital Position as a Function
of Time
3
CHAPTER OUTLINE
3.1 Introduction ..................................................................................................................................145
3.2 Time since periapsis .....................................................................................................................145
3.3 Circular orbits (e [ 0)...................................................................................................................147
3.4 Elliptical orbits (e < 1)...................................................................................................................147
3.5 Parabolic trajectories (e [ 1)........................................................................................................163
3.6 Hyperbolic trajectories (e > 1)........................................................................................................165
3.7 Universal variables .......................................................................................................................173
Problems.............................................................................................................................................183
Section 3.2 .........................................................................................................................................183
Section 3.4 .........................................................................................................................................184
Section 3.5 .........................................................................................................................................186
Section 3.6 .........................................................................................................................................186
Section 3.7 .........................................................................................................................................186
3.1 Introduction
In Chapter 2, we found the relationship between position and true anomaly for the two-body problem.
The only place time appeared explicitly was in the expression for the period of an ellipse. Obtaining
position as a function of time is a simple matter for circular orbits. For elliptical, parabolic, and
hyperbolic paths, we are led to the various forms of Kepler’s equation relating position to time. These
transcendental equations must be solved iteratively using a procedure like Newton’s method, which is
presented and illustrated in this chapter.
The different forms of Kepler’s equation are combined into a single universal Kepler’s equation by
introducing universal variables. Implementation of this appealing notion is accompanied by the
introduction of an unfamiliar class of functions known as Stumpff functions. The universal variable
formulation is required for the Lambert and Gauss orbit determination algorithms in Chapter 5.
The road map of Appendix B may aid in grasping how the material presented here depends on that
of Chapter 2.
3.2 Time since periapsis
The orbit formula, r ¼ ðh2=mÞ=ð1 þ ecos qÞ, gives the position of body m2 in its orbit around m1 as a
function of the true anomaly. For many practical reasons, we need to be able to determine the position
CHAPTER
Orbital Mechanics for Engineering Students. http://dx.doi.org/10.1016/B978-0-08-097747-8.00003-7
Copyright Ó 2014 Elsevier Ltd. All rights reserved.
145
2. of m2 as a function of time. For elliptical orbits, we have a formula for the period T (Eqn (2.82)), but we
cannot yet calculate the time required to fly between any two true anomalies. The purpose of this
section is to come up with the formulas that allow us to do that calculation.
The one equation we have that relates true anomaly directly to time is Eqn (2.47), h ¼ r2 _
q, which
can be written as
dq
dt
¼
h
r2
Substituting r ¼ ðh2=mÞ=ð1 þ ecos qÞ we find, after separating variables,
m2
h3
dt ¼
dq
ð1 þ ecos qÞ2
Integrating both sides of this equation yields
m2
h3
t tp
¼
Zq
0
dw
ð1 þ e cos wÞ2
(3.1)
where the constant of integration tp is the time at periapsis passage, where by definition q ¼ 0. tp is
the sixth constant of the motion that was missing in Chapter 2. The origin of time is arbitrary. It is
convenient to measure time from periapsis passage, so we will usually set tp ¼ 0. In that case
we have
m2
h3
t ¼
Zq
0
dw
ð1 þ e cos wÞ2
(3.2)
The integral on the right may be found in any standard mathematical handbook, such as Beyer (1991),
in which we find
Z
dx
ða þ bcos xÞ2
¼
1
ða2 b2Þ
3=2
2atan1
ffiffiffiffiffiffiffiffiffiffiffi
a b
a þ b
r
tan
x
2
b
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
a2 b2
p
sin x
a þ bcos x
!
ðb aÞ (3.3)
Z
dx
ða þ bcos xÞ2
¼
1
a2
1
2
tan
x
2
þ
1
6
tan3 x
2
ðb ¼ aÞ (3.4)
Z
dx
ða þ bcos xÞ2
¼
1
ðb2 a2Þ3=2
2
6
4
b
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
b2 a2
p
sin x
a þ bcos x
aln
ffiffiffiffiffiffiffiffiffiffiffi
b þ a
p
þ
ffiffiffiffiffiffiffiffiffiffiffi
b a
p
tan x
2
ffiffiffiffiffiffiffiffiffiffiffi
b þ a
p
ffiffiffiffiffiffiffiffiffiffiffi
b a
p
tan x
2
!
3
7
5 ðb aÞ (3.5)
146 CHAPTER 3 Orbital Position as a Function of Time
3. 3.3 Circular orbits (e [ 0)
If e ¼ 0, the integral in Eqn (3.2) is simply
Z q
0
dw, which means
t ¼
h3
m2
q
Recall that for a circle (Eqn (2.62)), r ¼ h2
/m. Therefore h3 ¼ r
3
2m
3
2, so that
t ¼
r
3
2
ffiffiffi
m
p q
Finally, substituting the formula (Eqn (2.64)) for the period T of a circular orbit, T ¼ 2pr
3
2=
ffiffiffi
m
p
, yields
t ¼
q
2p
T
or
q ¼
2p
T
t
The reason that t is directly proportional to q in a circular orbit is simply that the angular velocity 2p/T
is constant. Therefore, the time Dt to fly through a true anomaly of Dq is (Dq/2p)T.
Because the circle is symmetric about any diameter, the apse linedand therefore the periapsisd
can be chosen arbitrarily.
C, F P
D
t = 0 Apse
line
r
FIGURE 3.1
Time since periapsis is directly proportional to true anomaly in a circular orbit.
3.4 Elliptical orbits (e 1)
Set a ¼ 1 and b ¼ e in Eqn (3.3) to obtain
Zq
0
dw
ð1 þ ecos wÞ2
¼
1
ð1 e2Þ
3
2
2tan1
ffiffiffiffiffiffiffiffiffiffiffi
1 e
1 þ e
r
tan
q
2
!
e
ffiffiffiffiffiffiffiffiffiffiffiffiffi
1 e2
p
sin q
1 þ ecos q
#
3.4 Elliptical orbits (e 1) 147
4. Therefore, Eqn (3.2) in this case becomes
m2
h3
t ¼
1
ð1 e2Þ
3
2
2tan1
ffiffiffiffiffiffiffiffiffiffiffi
1 e
1 þ e
r
tan
q
2
!
e
ffiffiffiffiffiffiffiffiffiffiffiffiffi
1 e2
p
sin q
1 þ ecos q
#
or
Me ¼ 2tan1
ffiffiffiffiffiffiffiffiffiffiffi
1 e
1 þ e
r
tan
q
2
!
e
ffiffiffiffiffiffiffiffiffiffiffiffiffi
1 e2
p
sin q
1 þ ecos q
(3.6)
where
Me ¼
m2
h3
1 e2
3
2
t (3.7)
Me is called the mean anomaly. The subscript e reminds us that this is for an ellipse and not for pa-
rabolas and hyperbolas, which have their own “mean anomaly” formulas. Equation (3.6) is plotted in
Figure 3.2. Observe that for all values of the eccentricity e, Me is a monotonically increasing function
of the true anomaly q.
From Eqn (2.82), the formula for the period T of an elliptical orbit, we have
m2ð1 e2Þ
3
2=h3 ¼ 2p=T, so that the mean anomaly can be written much more simply as
Me ¼
2p
T
t (3.8)
0
e = 0
e = 0.2
e = 0.5
e = 0.8
e = 0.9
Mean anomaly, Me
FIGURE 3.2
Mean anomaly vs true anomaly for ellipses of various eccentricities.
148 CHAPTER 3 Orbital Position as a Function of Time
5. The angular velocity of the position vector of an elliptical orbit is not constant, but since 2p radians are
swept out per period T, the ratio 2p/T is the average angular velocity, which is given the symbol n and
called the mean motion,
n ¼
2p
T
(3.9)
In terms of the mean motion, Eqn (3.5) can be written simpler still,
Me ¼ nt
The mean anomaly is the azimuth position (in radians) of a fictitious body moving around the ellipse at
the constant angular speed n. For a circular orbit, the mean anomaly Me and the true anomaly q are
identical.
It is convenient to simplify Eqn (3.6) by introducing an auxiliary angle E called the eccentric
anomaly, which is shown in Figure 3.3. This is done by circumscribing the ellipse with a concentric
auxiliary circle having a radius equal to the semimajor axis a of the ellipse. Let S be that point on the
ellipse whose true anomaly is q. Through point S we pass a perpendicular to the apse line, intersecting
the auxiliary circle at point Q and the apse line at point V. The angle between the apse line and the
radius drawn from the center of the circle to Q on its circumference is the eccentric anomaly E.
Observe that E lags q from periapsis P to apoapsis Að0 q 180Þ, whereas it leads q from A to P
ð180 q 360Þ.
To find E as a function of q, we first observe from Figure 3.3 that, in terms of the eccentric anomaly,
OV ¼ acos E, whereas in terms of the true anomaly, OV ¼ ae þ rcos q. Thus,
acos E ¼ ae þ rcos q
Q
F V P
E
S
r
a O
A
b
a
B
D
ae
FIGURE 3.3
Ellipse and the circumscribed auxiliary circle.
3.4 Elliptical orbits (e 1) 149
6. Using Eqn (2.72), r ¼ að1 e2Þ=ð1 þ ecos qÞ, we can write this as
acos E ¼ ae þ
a
1 e2
cos q
1 þ ecos q
Simplifying the right-hand side, we get
cos E ¼
e þ cos q
1 þ ecos q
(3.10a)
Solving this for cos q we obtain the inverse relation,
cos q ¼
e cos E
ecos E 1
(3.10b)
Substituting Eqn (3.10a) into the trigonometric identity sin2
E þ cos2
E ¼ 1 and solving for sin E
yields
sin E ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffi
1 e2
p
sin q
1 þ ecos q
(3.11)
Equation (3.10a) would be fine for obtaining E from q, except that, given a value of cos E between 1
and 1, there are two values of E between 0 and 360, as illustrated in Figure 3.4. The same comments
hold for Eqn (3.11). To resolve this quadrant ambiguity, we use the following trigonometric identity:
tan2 E
2
¼
sin2
E=2
cos2 E=2
¼
1 cos E
2
1 þ cos E
2
¼
1 cos E
1 þ cos E
(3.12)
From Eqn (3.10a)
1 cos E ¼
1 cos q
1 þ ecos q
ð1 eÞ and 1 þ cos E ¼
1 þ cos q
1 þ ecos q
ð1 þ eÞ
0
1
1
2 2
cos E
EI EIV
E
FIGURE 3.4
For 0 cos E 1, E can lie in the first or fourth quadrant. For 1 cos E 0, E can lie in the second or third
quadrant.
150 CHAPTER 3 Orbital Position as a Function of Time
7. Therefore,
tan2 E
2
¼
1 e
1 þ e
1 cos q
1 þ cos q
¼
1 e
1 þ e
tan2 q
2
where the last step required applying the trig identity in Eqn (3.12) to the term (1 cos q)/(1 þ cos q).
Finally, therefore, we obtain
tan
E
2
¼
ffiffiffiffiffiffiffiffiffiffiffi
1 e
1 þ e
r
tan
q
2
(3.13a)
or
E ¼ 2tan1
ffiffiffiffiffiffiffiffiffiffiffi
1 e
1 þ e
r
tan
q
2
!
(3.13b)
Observe from Figure 3.5 that for any value of tan (E/2), there is only one value of E between 0 and
360. There is no quadrant ambiguity.
Substituting Eqns (3.11) and (3.13b) into Eqn (3.6) yields Kepler’s equation,
Me ¼ E esin E (3.14)
This monotonically increasing relationship between mean anomaly and eccentric anomaly is plotted
for several values of eccentricity in Figure 3.6.
Given the true anomaly q, we calculate the eccentric anomaly E using Eqn (3.13). Substituting E
into Kepler’s formula, Eqn (3.14), yields the mean anomaly directly. From the mean anomaly and the
period T we find the time (since periapsis) from Eqn (3.5),
t ¼
Me
2p
T (3.15)
tan
E
2
E
0
FIGURE 3.5
For any value of tan (E/2), there is a corresponding unique value of e in the range 0 to 2p.
3.4 Elliptical orbits (e 1) 151
8. On the other hand, if we are given the time, then Eqn (3.15) yields the mean anomaly Me. Substituting
Me into Kepler’s equation, we get the following expression for the eccentric anomaly:
E esin E ¼ Me
We cannot solve this transcendental equation directly for E. A rough value of E might be read from
Figure 3.6. However, an accurate solution requires an iterative, “trial and error” procedure.
Newton’s method, or one of its variants, is one of the more common and efficient ways of finding
the root of a well-behaved function. To find a root of the equation f(x) ¼ 0 in Figure 3.7, we estimate it
to be xi and evaluate the function f(x) and its first derivative f 0(x) at that point. We then extend the
tangent to the curve at f(xi) until it intersects the x-axis at xiþ1, which becomes our updated estimate of
the root. The intercept xiþ1 is found by setting the slope of the tangent line equal to the slope of the
curve at xi, that is,
f0
ðxiÞ ¼
0 fðxiÞ
xiþ1 xi
from which we obtain
xiþ1 ¼ xi
fðxiÞ
f0ðxiÞ
(3.16)
The process is repeated, using xiþ1 to estimate xiþ2, and so on, until the root has been found to the
desired level of precision.
To apply Newton’s method to the solution of Kepler’s equation, we form the function
fðEÞ ¼ E esin E Me
0
Eccentric anomaly, E
Mean anomaly, Me
e = 0
e = 0.2
e = 0.4
e = 0.6
e = 0.8
e = 1.0
FIGURE 3.6
Plot of Kepler’s equation for an elliptical orbit.
152 CHAPTER 3 Orbital Position as a Function of Time
9. and seek the value of eccentric anomaly that makes f(E) ¼ 0. Since
f0
ðEÞ ¼ 1 ecos E
for this problem, Eqn (3.16) becomes
Eiþ1 ¼ Ei
Ei esin Ei Me
1 ecos Ei
(3.17)
n
ALGORITHM 3.1
Solve Kepler’s equation for the eccentric anomaly E given the eccentricity e and the mean anomaly
Me. See Appendix D.11 for the implementation of this algorithm in MATLAB.
1. Choose an initial estimate of the root E as follows (Prussing and Conway, 1993). If Me p, then
E ¼ Me þ e/2. If Me p, then E ¼ Me e/2. Remember that the angles E and Me are in radians.
(When using a hand held calculator, be sure that it is in the radian mode.)
2. At any given step, having obtained Ei from the previous step, calculate
fðEiÞ ¼ Ei esin Ei Me and f0
ðEiÞ ¼ 1 ecos Ei.
3. Calculate ratioi ¼ fðEiÞ=f0
ðEiÞ.
4. If jratioij exceeds the chosen tolerance (e.g., 108
), then calculate an updated value of E,
Eiþ1 ¼ Ei ratioi
Return to Step 2.
5. If jratioij is less than the tolerance, then accept Ei as the solution to within the chosen accuracy.
n
Root
x
f
xi+1
f(xi)
xi
Slope =
df
dx
f
x
=
d
dx
x
x=xi
FIGURE 3.7
Newton’s method for finding a root of f(x) ¼ 0.
3.4 Elliptical orbits (e 1) 153
10. EXAMPLE 3.1
A geocentric elliptical orbit has a perigee radius of 9600 km and an apogee radius of 21,000 km, as shown in
Figure 3.8. Calculate the time to fly from perigee P to a true anomaly of 120.
Solution
Before anything else, let us find the primary orbital parameters e and h. The eccentricity is readily obtained from
the perigee and apogee radii by means of Eqn (2.84),
e ¼
ra rp
ra þ rp
¼
21;000 9600
21;000 þ 9600
¼ 0:37255 (a)
We find the angular momentum using the orbit equation,
9600 ¼
h2
398;600
1
1 þ 0:37255 cosð0Þ
0 h ¼ 72;472 km2
=s
With h and e, the period of the orbit is obtained from Eqn (2.82),
T ¼
2p
m2
h
ffiffiffiffiffiffiffiffiffiffiffiffiffiffi
ffi
1 e2
p
3
¼
2p
398;6002
72; 472
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 0:372552
p
3
¼ 18;834 s (b)
Equation (3.13a) yields the eccentric anomaly from the true anomaly,
tan
E
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffi
1 e
1 þ e
r
tan
q
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 0:37255
1 þ 0:37255
r
tan
120
2
¼ 1:1711 0 E ¼ 1:7281 rad
Then Kepler’s equation, Eqn (3.14), is used to find the mean anomaly,
Me ¼ 1:7281 0:37255 sin 1:7281 ¼ 1:3601 rad
120°
Earth
21,000 km
9600 km
P
A
B
FIGURE 3.8
Geocentric elliptical orbit.
154 CHAPTER 3 Orbital Position as a Function of Time
11. Finally, the time follows from Eqn (3.12),
t ¼
Me
2p
T ¼
1:3601
2p
18;834 ¼ 4077s ð1:132 hÞ
EXAMPLE 3.2
In the previous example, find the true anomaly at three hours after perigee passage.
Solution
Since the time (10,800 s) is greater than one-half the period, the true anomaly must be greater than 180.
First, we use Eqn (3.12) to calculate the mean anomaly for t ¼ 10,800 s.
Me ¼ 2p
t
T
¼ 2p
10;800
18;830
¼ 3:6029 rad (a)
Kepler’s equation, E esin (E) ¼ Me (with all angles in radians), is then employed to find the eccentric anomaly.
This transcendental equation will be solved using Algorithm 3.1 with an error tolerance of 106
. Since Me p, a
good starting value for the iteration is E0 ¼ Me e/2 ¼ 3.4166. Executing the algorithm yields the following
steps:
Step 1:
E0 ¼ 3:4166
fðE0Þ ¼ 0:085124
f0
ðE0Þ ¼ 1:3585
ratio ¼
0:085124
1:3585
¼ 0:062658
jratioj 106
; so repeat:
Step 2:
E1 ¼ 3:4166 ð0:062658Þ ¼ 3:4793
fðE1Þ ¼ 0:0002134
f0
ðE1Þ ¼ 1:3515
ratio ¼
0:0002134
1:3515
¼ 1:5778 104
jratioj 106
; so repeat:
3.4 Elliptical orbits (e 1) 155
12. Step 3:
E2 ¼ 3:4793
1:5778 104
¼ 3:4794
fðE2Þ ¼ 1:5366 109
f0
ðE2Þ ¼ 1:3515
ratio ¼
1:5366 109
1:3515
1:137 109
jratioj 106
; so accept E ¼ 3:4794 as the solution:
Convergence to even more than the desired accuracy occurred after just two iterations. With this value of the
eccentric anomaly, the true anomaly is found from Eqn (3.13a) to be
tan
q
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffi
1 þ e
1 e
r
tan
E
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 þ 0:37255
1 0:37255
r
tan
3:4794
2
¼ 8:67210q ¼ 193:2
EXAMPLE 3.3
Let a satellite be in a 500 km by 5000 km orbit with its apse line parallel to the line from the earth to the sun, as
shown in Figure 3.9. Find the time that the satellite is in the earth’s shadow if: (a) the apogee is toward the sun and
(b) the perigee is toward the sun.
Solution
We start by using the given data to find the primary orbital parameters, e and h. The eccentricity is obtained from
Eqn (2.84),
e ¼
ra rp
ra þ rp
¼
ð6378 þ 5000Þ ð6378 þ 500Þ
ð6378 þ 5000Þ þ ð6378 þ 500Þ
¼ 0:24649 (a)
P
A
To the sun
a
b
c
d
r
Earth
RE
FIGURE 3.9
Satellite passing in and out of the earth’s shadow.
156 CHAPTER 3 Orbital Position as a Function of Time
13. The orbit equation can then be used to find the angular momentum
rp ¼
h2
m
1
1 þ ecosð0Þ
0 6878 ¼
h2
398;600
1
1 þ 0:24649
0 h ¼ 58;458km2
=s (b)
The semimajor axis may be found from Eqn (2.71),
a ¼
h2
m
1
1 e2
¼
58;4582
398;600
1
1 0:246492
¼ 9128 km (c)
or from the fact that a ¼ ðrp þ raÞ=2. The period of the orbit follows from Eqn (2.83),
T ¼
2p
ffiffiffi
m
p a3=2
¼
2p
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
398;600
p 91283=2
¼ 8679:1 s ð2:4109 hÞ (d)
(a) If the apogee is toward the sun, as in Figure 3.9, then the satellite is in earth’s shadow between points a and b
on its orbit. These are two of the four points of intersection of the orbit with the lines that are parallel to the
earthesun line and lie at a distance RE from the center of the earth. The true anomaly of b is therefore given by
sin q ¼ RE/r, where r is the radial position of the satellite. It follows that the radius of b is
r ¼
RE
sin q
(e)
From Eqn (2.72), we also have
r ¼
a
1 e2
1 þ ecos q
(f)
Substituting Eqn (e) into Eqn (f), collecting terms and simplifying yields an equation in q,
ecos q
1 e2
a
RE
sin q þ 1 ¼ 0 (g)
Substituting Eqns (a) and (c) together with RE ¼ 6378 km into Eqn (g) yields
0:24649cos q 1:3442sin q ¼ 1 (h)
This equation is of the form
A cos q þ B sin q ¼ C (i)
It has two roots, which are given by (see Exercise 3.9)
q ¼ tan1 B
A
cos1 C
A
cos
tan1 B
A
(j)
For the case at hand,
q ¼ tan1 1:3442
0:24649
cos1 1
0:24649
cos
tan1 1:3442
0:24649
¼ 79:607
137:03
3.4 Elliptical orbits (e 1) 157
14. That is
qb ¼ 57:423
qc ¼ 216:64 ðþ143:36Þ
(k)
For apogee toward the sun, the flight from perigee to point b will be in shadow. To find the time of flight from
perigee to point b, we first compute the eccentric anomaly of b using Eqn (3.13b):
Eb ¼ 2 tan1
ffiffiffiffiffiffiffiffiffiffiffiffi
1 e
1 þ e
r
tan
qb
2
!
¼ 2tan1
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 0:24649
1 þ 0:24649
r
tan
1:0022
2
!
¼ 0:80521 rad (l)
From this we find the mean anomaly using Kepler’s equation,
Me ¼ E esin E ¼ 0:80521 0:24649 sin 0:80521 ¼ 0:62749 rad (m)
Finally, Eqn (3.5) yields the time at b,
tb ¼
Me
2p
T ¼
0:62749
2p
8679:1 ¼ 866:77 s (n)
The total time in shadow, from a to b, during which the satellite passes through perigee, is
t ¼ 2tb ¼ 1734 s ð28:98 minÞ (o)
(b) If the perigee is toward the sun, then the satellite is in shadow near apogee, from point c (qc ¼ 143.36
)
to d on the orbit. Following the same procedure as above, we obtain (see Exercise 3.11),
Ec ¼ 2:3364 rad
Mc ¼ 2:1587 rad
tc ¼ 2981:8 s
(p)
The total time in shadow, from c to d, is
t ¼ T 2tc ¼ 8679:1 2$2891:8 ¼ 2716 s ð45:26 minÞ (q)
The time is longer than that given by Eqn (o) since the satellite travels slower near apogee.
We have observed that there is no closed-form solution for the eccentric anomaly E in Kepler’s
equation, E esin E ¼ Me. However, there exist infinite series solutions. One of these, due to Lagrange
(Battin, 1999), is a power series in the eccentricity e,
E ¼ Me þ
X
N
n¼1
anen
(3.18)
where the coefficient an is given by the somewhat intimidating expression
an ¼
1
2n1
X
floorðn=2Þ
k¼0
ð1Þk 1
ðn kÞ!k!
ðn 2kÞn1
sin½ðn 2kÞMe (3.19)
158 CHAPTER 3 Orbital Position as a Function of Time
15. Here, floor(x) means x rounded to the next lowest integer [e.g., floor(0.5) ¼ 0, floor(p) ¼ 3]. If e is
sufficiently small, then the Lagrange series converges. This means that by including enough terms in the
summation, we can obtain E to any desired degree of precision. Unfortunately, if e exceeds 0.6627434193,
the series diverges, which means taking more and more terms yields worse and worse results for some
values of M.
The limiting value for the eccentricity was discovered by the French mathematician Pierre-Simone
Laplace (1749–1827) and is called the Laplace limit.
In practice, we must truncate the Lagrange series to a finite number of terms N, so that
E ¼ Me þ
X
N
n¼1
anen
(3.20)
For example, setting N ¼ 3 and calculating each an by means of Eqn (3.19) leads to
E ¼ Me þ esin Me þ
e2
2
sin2 Me þ
e3
8
ð3sin3 Me sin MeÞ (3.21)
For small values of the eccentricity e, this yields good agreement with the exact solution of Kepler’s
equation (plotted in Figure 3.6). However, as we approach the Laplace limit, the accuracy degrades
unless more terms of the series are included. Figure 3.10 shows that for an eccentricity of 0.65, just
below the Laplace limit, Eqn (3.21) (N ¼ 3) yields a solution that oscillates around the exact solution
but is fairly close to it everywhere. Setting N ¼ 10 in Eqn (3.20) produces a curve that, at the given
Eccentric anomaly, E
e = 0.65
Exact and N = 10
N = 3
Mean
anomaly,
M
e
π
FIGURE 3.10
Comparison of the exact solution of Kepler’s equation with the truncated Lagrange series solution (N ¼ 3 and
N ¼ 10) for an eccentricity of 0.65.
3.4 Elliptical orbits (e 1) 159
16. scale, is indistinguishable from the exact solution. On the other hand, for an eccentricity of 0.90, far
above the Laplace limit, Figure 3.11 reveals that Eqn (3.21) is a poor approximation to the exact
solution, and using N ¼ 10 makes matters even worse.
Another infinite series for E (Battin, 1999) is given by
E ¼ Me þ
X
N
n¼1
2
n
JnðneÞsin n Me (3.22)
where the coefficients Jn are Bessel functions of the first kind, defined by the infinite series
JnðxÞ ¼
X
N
k¼0
ð1Þk
k!ðn þ kÞ!
x
2
nþ2k
(3.23)
J1 through J5 are plotted in Figure 3.12. Clearly, they are oscillatory in appearance and tend toward
zero with increasing x.
It turns out that, unlike the Lagrange series, the Bessel function series solution converges for all
values of the eccentricity less than 1. Figure 3.13 shows how the truncated Bessel series solutions
E ¼ Me þ
X
N
n¼1
2
n
JnðneÞsin n Me (3.24)
Exact
N = 10
N = 3
Eccentric anomaly, E
0
e = 0.9
Mean
anomaly,
M
e
FIGURE 3.11
Comparison of the exact solution of Kepler’s equation with the truncated Lagrange series solution (N ¼ 3 and
N ¼ 10) for an eccentricity of 0.90.
160 CHAPTER 3 Orbital Position as a Function of Time
17. FIGURE 3.12
Bessel functions of the first kind.
Eccentric anomaly, E
0
e = 0.99
Exact
N = 3
N = 10
Mean
anomaly,
M
e
FIGURE 3.13
Comparison of the exact solution of Kepler’s equation with the truncated Bessel series solution (N ¼ 3 and
N ¼ 10) for an eccentricity of 0.99.
3.4 Elliptical orbits (e 1) 161
18. for N ¼ 3 and N ¼ 10 compare to the exact solution of Kepler’s equation for the very large elliptical
eccentricity of e ¼ 0.99. It can be seen that the case N ¼ 3 yields a poor approximation for all but a few
values of Me. Increasing the number of terms in the series to N ¼ 10 obviously improves the
approximation, and adding even more terms will make the truncated series solution indistinguishable
from the exact solution at the given scale.
Observe that we can combine Eqn (3.10) and Eqn (2.72) as follows to obtain the orbit equation for
the ellipse in terms of the eccentric anomaly:
r ¼
a
1 e2
1 þ ecos q
¼
a
1 e2
1 þ e
e cos E
ecos E 1
From this it is easy to see that
r ¼ að1 ecos EÞ (3.25)
In Eqn (2.86), we defined the true-anomaly-averaged radius rq of an elliptical orbit. Alternatively, the
time-averaged radius rt of an elliptical orbit is defined as
rt ¼
1
T
ZT
0
rdt (3.26)
According to Eqns (3.12) and (3.14),
t ¼
T
2p
ðE esin EÞ
Therefore,
dt ¼
T
2p
ð1 ecos EÞdE
On using this relationship to change the variable of integration from t to E and substituting Eqn (3.25),
Eqn (3.26) becomes
rt ¼
1
T
Z
2p
0
½að1 ecos EÞ
T
2p
ð1 ecos EÞ dE
¼
a
2p
Z
2p
0
ð1 ecos EÞ2
dE
¼
a
2p
Z
2p
0
1 2ecos E þ e2
cos2
E
dE
¼
a
2p
2p 0 þ e2
p
162 CHAPTER 3 Orbital Position as a Function of Time
19. so that
rt ¼ a
1 þ
e2
2
Time-averaged radius of an elliptical orbit (3.27)
Comparing this result with Eqn (2.87) reveals, as we should have expected, that rt rq. In fact,
combining Eqn (2.87) and Eqn (3.27) yields
rq ¼ a
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
3 2
rt
a
r
(3.28)
3.5 Parabolic trajectories (e [ 1)
For the parabola, Eqn (3.2) becomes
m2
h3
t ¼
Zq
0
dw
ð1 þ cos wÞ2
(3.29)
Setting a ¼ b ¼ 1 in Eqn (3.4) yields
Zq
0
dw
ð1 þ cos wÞ2
¼
1
2
tan
q
2
þ
1
6
tan3 q
2
Therefore, Eqn (3.29) may be written as
Mp ¼
1
2
tan
q
2
þ
1
6
tan3 q
2
(3.30)
where
Mp ¼
m2t
h3
(3.31)
Mp is dimensionless, and it may be thought of as the “mean anomaly” for the parabola. Equation (3.30)
is plotted in Figure 3.14. Equation (3.30) is also known as Barker’s equation.
Given the true anomaly q, we find the time directly from Eqns (3.30) and (3.31). If time is the given
variable, then we must solve the cubic equation
1
6
tan
q
2
3
þ
1
2
tan
q
2
Mp ¼ 0
which has but one real root, namely,
tan
q
2
¼
3Mp þ
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
ffi
3Mp
2
þ 1
q 1
3
3Mp þ
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
ffi
3Mp
2
þ 1
q
1
3
(3.32)
3.5 Parabolic trajectories (e ¼ 1) 163
20. EXAMPLE 3.4
A geocentric parabola has a perigee velocity of 10 km/s. How far is the satellite from the center of the earth
six hours after perigee passage?
Solution
The first step is to find the orbital parameters e and h. Of course we know that e ¼ 1. To get the angular momentum,
we can use the given perigee speed and Eqn (2.80) (the energy equation) to find the perigee radius,
rp ¼
2m
v2
p
¼
2$398;600
102
¼ 7972 km
It follows from Eqn (2.31) that the angular momentum is
h ¼ rpvp ¼ 7972$10 ¼ 79;720 km2
=s
We can now calculate the parabolic mean anomaly by means of Eqn (3.31),
Mp ¼
m2t
h3
¼
398;6002$ð6$3600Þ
79;7203
¼ 6:7737 rad
Therefore, 3Mp ¼ 20.321 rad, which, when substituted into Eqn (3.32), yields the true anomaly,
tan
q
2
¼
20:321 þ
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
20:3212 þ 1
p 1
3
20:321 þ
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
20:3212 þ 1
p 1
3
¼ 3:1481 0 q ¼ 144:75
Finally, we substitute the true anomaly into the orbit equation to find the radius,
r ¼
79;7202
398;600
1
1 þ cos ð144:75
Þ
¼ 86;899 km
2
Mean
anomaly,
M
p
2
FIGURE 3.14
Graph of Eqn (3.30).
164 CHAPTER 3 Orbital Position as a Function of Time
21. 3.6 Hyperbolic trajectories (e 1)
Setting a ¼ 1 and b ¼ e in Eqn (3.5) yields
Zq
0
dw
ð1 þ ecos wÞ2
¼
1
e2 1
esin q
1 þ ecos q
1
ffiffiffiffiffiffiffiffiffiffiffiffiffi
e2 1
p ln
ffiffiffiffiffiffiffiffiffiffiffi
e þ 1
p
þ
ffiffiffiffiffiffiffiffiffiffiffi
e 1
p
tanðq=2Þ
ffiffiffiffiffiffiffiffiffiffiffi
e þ 1
p
ffiffiffiffiffiffiffiffiffiffiffi
e 1
p
tanðq=2Þ
!#
Therefore, for the hyperbola, Eqn (3.1) becomes
m2
h3
t ¼
1
e2 1
esin q
1 þ ecos q
1
ðe2 1Þ
3
2
ln
ffiffiffiffiffiffiffiffiffiffiffi
e þ 1
p
þ
ffiffiffiffiffiffiffiffiffiffiffi
e 1
p
tanðq=2Þ
ffiffiffiffiffiffiffiffiffiffiffi
e þ 1
p
ffiffiffiffiffiffiffiffiffiffiffi
e 1
p
tanðq=2Þ
!
Multiplying both sides by ðe2 1Þ
3
2, we get
Mh ¼
e
ffiffiffiffiffiffiffiffiffiffiffiffiffi
e2 1
p
sin q
1 þ ecos q
ln
ffiffiffiffiffiffiffiffiffiffiffi
e þ 1
p
þ
ffiffiffiffiffiffiffiffiffiffiffi
e 1
p
tanðq=2Þ
ffiffiffiffiffiffiffiffiffiffiffi
e þ 1
p
ffiffiffiffiffiffiffiffiffiffiffi
e 1
p
tanðq=2Þ
!
(3.33)
where
Mh ¼
m2
h3
e2
1
3
2
t (3.34)
Mh is the hyperbolic mean anomaly. Equation (3.33) is plotted in Figure 3.15. Recall that q cannot
exceed qN (Eqn (2.97)).
We can simplify Eqn (3.33) by introducing an auxiliary angle analogous to the eccentric anomaly E
for the ellipse. Consider a point on a hyperbola whose polar coordinates are r and q. Referring to
Figure 3.16, let x be the horizontal distance of the point from the center C of the hyperbola, and let y be
its distance above the apse line. The ratio y/b defines the hyperbolic sine of the dimensionless variable
0.01
1
100
10,000
2
e = 1.1
e = 1.5
e = 2.0
e = 3.0
e = 5.0
Mean
anomaly,
M
h
FIGURE 3.15
Plots of Eqn (3.33) for several different eccentricities.
3.6 Hyperbolic trajectories (e 1) 165
22. F that we will use as the hyperbolic eccentric anomaly. That is, we define F to be such that
sinh F ¼
y
b
(3.35)
In view of the equation of a hyperbola,
x2
a2
y2
b2
¼ 1
it is consistent with the definition of sinh F to define the hyperbolic cosine as
cosh F ¼
x
a
(3.36)
(It should be recalled that sinhx ¼ ðex exÞ=2 and cosh x ¼ ðex þ exÞ=2 and, therefore, that
cosh2
x sinh2
x ¼ 1.)
From Figure 3.16 we see that y ¼ r sin q. Substituting this into Eqn (3.35), along with
r ¼ aðe2 1Þ=ð1 þ ecos qÞ (Eqn (2.104)) and b ¼ a
ffiffiffiffiffiffiffiffiffiffiffiffiffi
e2 1
p
(Eqn (2.106)), we get
sinh F ¼
1
b
rsin q ¼
1
a
ffiffiffiffiffiffiffiffiffiffiffiffiffi
e2 1
p
a
e2 1
1 þ ecos q
sin q
Focus
P
rp a
Apse
line
C
b
M
x
y
A
s
y
m
p
t
o
t
e
FIGURE 3.16
Hyperbolic parameters.
166 CHAPTER 3 Orbital Position as a Function of Time
23. so that
sinh F ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffi
e2 1
p
sin q
1 þ ecos q
(3.37)
This can be used to solve for F in terms of the true anomaly,
F ¼ sinh1
ffiffiffiffiffiffiffiffiffiffiffiffiffi
e2 1
p
sin q
1 þ ecos q
!
(3.38)
Using the formula sinh1
x ¼ lnðx þ
ffiffiffiffiffiffiffiffiffiffiffiffiffi
x2 þ 1
p
Þ, we can, after simplifying the algebra, write
Eqn (3.38) as
F ¼ ln
sin q
ffiffiffiffiffiffiffiffiffiffiffiffiffi
e2 1
p
þ cos q þ e
1 þ ecos q
!
Substituting the trigonometric identities,
sin q ¼
2tan ðq=2Þ
1 þ tan2 ðq=2Þ
cos q ¼
1 tan2ðq=2Þ
1 þ tan2ðq=2Þ
and doing some more algebra yields
F ¼ ln
1 þ e þ ðe 1Þ tan2ðq=2Þ þ 2 tanðq=2Þ
ffiffiffiffiffiffiffiffiffiffiffiffiffi
e2 1
p
1 þ e þ ð1 eÞ tan2ðq=2Þ
#
Fortunately, but not too obviously, the numerator and the denominator in the brackets have a common
factor, so that this expression for the hyperbolic eccentric anomaly reduces to
F ¼ ln
ffiffiffiffiffiffiffiffiffiffiffi
e þ 1
p
þ
ffiffiffiffiffiffiffiffiffiffiffi
e 1
p
tanðq=2Þ
ffiffiffiffiffiffiffiffiffiffiffi
e þ 1
p
ffiffiffiffiffiffiffiffiffiffiffi
e 1
p
tanðq=2Þ
#
(3.39)
Substituting Eqns (3.37) and (3.39) into Eqn (3.33) yields Kepler’s equation for the hyperbola,
Mh ¼ esinh F F (3.40)
This equation is plotted for several different eccentricities in Figure 3.17.
If we substitute the expression for sinh F, Eqn (3.37), into the hyperbolic trig identity
cosh2
F sinh2
F ¼ 1
we get
cosh2
F ¼ 1 þ
ffiffiffiffiffiffiffiffiffiffiffiffiffi
e2 1
p
sin q
1 þ ecos q
!2
3.6 Hyperbolic trajectories (e 1) 167
24. A few steps of algebra lead to
cosh2
F ¼
cos q þ e
1 þ ecos q
2
so that
cosh F ¼
cos q þ e
1 þ ecos q
(3.41a)
Solving this for cos q, we obtain the inverse relation,
cos q ¼
cosh F e
1 ecosh F
(3.41b)
The hyperbolic tangent is found in terms of the hyperbolic sine and cosine by the formula
tanh F ¼
sinh F
cosh F
In mathematical handbooks, we can find the hyperbolic trig identity,
tanh
F
2
¼
sinh F
1 þ cosh F
(3.42)
Substituting Eqns (3.37) and (3.41a) into this formula and simplifying yields
tanh
F
2
¼
ffiffiffiffiffiffiffiffiffiffiffi
e 1
e þ 1
r
sin q
1 þ cos q
(3.43)
Interestingly enough, Eqn (3.42) holds for ordinary trig functions, too; that is,
tan
q
2
¼
sin q
1 þ cos q
0.01
1
100
10,000
2 4
1 3 6
5
Eccentric anomaly, F
e = 1.1
e = 1.5
e = 2.0
e = 3.0
e = 5.0
Mean
anomaly,
M
h
FIGURE 3.17
Plot of Kepler’s equation for the hyperbola.
168 CHAPTER 3 Orbital Position as a Function of Time
25. Therefore, Eqn (3.43) can be written
tanh
F
2
¼
ffiffiffiffiffiffiffiffiffiffiffi
e 1
e þ 1
r
tan
q
2
(3.44a)
This is a somewhat simpler alternative to Eqn (3.39) for computing eccentric anomaly from true
anomaly, and it is a whole lot simpler to invert:
tan
q
2
¼
ffiffiffiffiffiffiffiffiffiffiffi
e þ 1
e 1
r
tanh
F
2
(3.44b)
If time is the given quantity, then Eqn (3.40)da transcendental equationdmust be solved for F by an
iterative procedure, as was the case for the ellipse. To apply Newton’s procedure to the solution of
Kepler’s equation for the hyperbola, we form the function
fðFÞ ¼ esinhF F Mh
and seek the value of F that makes f(F) ¼ 0. Since
f0
ðFÞ ¼ ecosh F 1
Equation (3.16) becomes
Fiþ1 ¼ Fi
esinh Fi Fi Mh
ecosh Fi 1
(3.45)
All quantities in this formula are dimensionless (radians, not degrees).
n
ALGORITHM 3.2
Solve Kepler’s equation for the hyperbola for the hyperbolic eccentric anomaly F given the ec-
centricity e and the hyperbolic mean anomaly Mh. See Appendix D.12 for the implementation of
this algorithm in MATLAB.
1. Choose an initial estimate of the root F.
a. For hand computations, read a rough value of F0 (no more than two significant figures) from
Figure 3.17 in order to keep the number of iterations to a minimum.
b. In computer software, let F0 ¼ Mh, an inelegant choice that may result in many iterations but
will nevertheless rapidly converge on today’s high-speed desktops and laptops.
2. At any given step, having obtained Fi from the previous step, calculate fðFiÞ ¼ esinh Fi Fi
Mh and f0
ðFiÞ ¼ ecosh Fi 1.
3. Calculate ratioi ¼ fðFiÞ=f0
ðFiÞ.
4. If jratioij exceeds the chosen tolerance (e.g., 108
), then calculate an updated value of F,
Fiþ1 ¼ Fi ratioi
Return to Step 2.
5. If jratioij is less than the tolerance, then accept Fi as the solution to within the desired accuracy.
n
3.6 Hyperbolic trajectories (e 1) 169
26. EXAMPLE 3.5
A geocentric trajectory has a perigee velocity of 15 km/s and a perigee altitude of 300 km. (a) Find the radius and
the time when the true anomaly is 100. (b) Find the position and speed 3 h later.
Solution
We first calculate the primary orbital parameters e and h. The angular momentum is calculated from Eqn (2.31)
and the given perigee data:
h ¼ rpvp ¼ ð6378 þ 300Þ$15 ¼ 100;170 km2
=s
The eccentricity is found by evaluating the orbit equation, r ¼ ðh2=mÞ½1=ð1 þ ecos qÞ, at perigee:
6378 þ 300 ¼
100;1702
398;600
1
1 þ e
0e ¼ 2:7696
(a) Since e 1, the trajectory is a hyperbola. Note that the true anomaly of the asymptote of the hyperbola is,
according to Eqn (2.97),
qN ¼ cos1
1
2:7696
¼ 111:17
Solving the orbit equation at q ¼ 100 yields
r ¼
100;1702
398;600
1
1 þ 2:7696 cos 100
¼ 48;497 km
To find the time since perigee passage at q ¼ 100, we first use Eqn (3.44a) to calculate the hyperbolic
eccentric anomaly,
tanh
F
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
2:7696 1
2:7696 þ 1
r
tan
100
2
¼ 0:81653 0 F ¼ 2:2927 rad
Kepler’s equation for the hyperbola then yields the mean anomaly,
Mh ¼ esinh F F ¼ 2:7696 sinh 2:2927 2:2927 ¼ 11:279 rad
The time since perigee passage is found from Eqn (3.34),
t ¼
h3
m2
1
e2 1
3
2
Mh ¼
100;1703
398;6002
1
2:76962 1
3
2
11:279 ¼ 4141 s
(b) After 3 h, the time since perigee passage is
t ¼ 4141:4 þ 3$3600 ¼ 14;941 s ð4:15 hÞ
The corresponding mean anomaly, from Eqn (3.34), is
Mh ¼
398;6002
100;1703
2:76962
1
3
2
14;941 ¼ 40:690 rad
We will use Algorithm 3.2 with an error tolerance of 106
to find the hyperbolic eccentric anomaly F. Referring to
Figure 3.17, we see that for Mh ¼ 40.69 and e ¼ 2.7696, F lies between 3 and 4. Let us arbitrarily choose F0 ¼ 3
as our initial estimate of F. Executing the algorithm yields the following steps:
F0 ¼ 3
170 CHAPTER 3 Orbital Position as a Function of Time
27. Step 1:
fðF0Þ ¼ 15:944494
f0
ðF0Þ ¼ 26:883397
ratio ¼ 0:59309818
F1 ¼ 3 ð0:59309818Þ ¼ 3:5930982
jratioj 106
; so repeat:
Step 2:
fðF1Þ ¼ 6:0114484
f0
ðF1Þ ¼ 49:370747
ratio ¼ 0:12176134
F2 ¼ 3:5930982 ð0:12176134Þ ¼ 3:4713368
jratioj 106
; so repeat:
Step 3:
fðF2Þ ¼ 0:35812370
f0
ðF2Þ ¼ 43:605527
ratio ¼ 8:2128052 103
F3 ¼ 3:4713368
8:2128052 103
¼ 3:4631240
jratioj 106
; so repeat:
Step 4:
fðF3Þ ¼ 1:4973128 103
f0
ðF3Þ ¼ 43:241398
ratio ¼ 3:4626836 105
F4 ¼ 3:4631240
3:4626836 105
¼ 3:4630894
jratioj 106
; so repeat:
Step 5:
fðF4Þ ¼ 2:6470781 103
f0
ðF4Þ ¼ 43:239869
ratio ¼ 6:1218459 1010
F5 ¼ 3:4630894
6:1218459 1010
¼ 3:4630894
jratioj 106
; so accept F ¼ 3:4631 as the solution:
We substitute this value of F into Eqn (3.44b) to find the true anomaly,
tan
q
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffi
e þ 1
e 1
r
tanh
F
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
2:7696 þ 1
2:7696 1
r
tanh
3:4631
2
¼ 1:3708 0 q ¼ 107:78
With the true anomaly, the orbital equation yields the radial coordinate at the final time
r ¼
h2
m
1
1 þ e cos q
¼
100;1702
398;600
1
1 þ 2:7696 cos 107:78
¼ 163;180 km
3.6 Hyperbolic trajectories (e 1) 171
28. The velocity components are obtained from Eqn (2.31),
vt ¼
h
r
¼
100;170
163;180
¼ 0:61386 km=s
and Eqn (2.49),
vr ¼
m
h
esin q ¼
398;600
100;170
2:7696 sin 107:78
¼ 10:494 km=s
Therefore, the speed of the spacecraft is
v ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
v2
r þ v2
t
q
¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
10:4942 þ 0:613862
p
¼ 10:51 km=s
Note that the hyperbolic excess speed for this orbit is
vN ¼
m
h
e sin qN ¼
398;600
100;170
$2:7696$sin 111:7
¼ 10:277 km=s
The results of this analysis are shown in Figure 3.18.
100°
107.78°
Initial
position
Position three hours later
163,180 km
48,497 km
Perigee
Apse
line
FIGURE 3.18
Given and computed data for Example 3.5.
172 CHAPTER 3 Orbital Position as a Function of Time
29. When determining orbital position as a function of time with the aid of Kepler’s equation, it is
convenient to have position r as a function of eccentric anomaly F. This is obtained by substituting Eqn
(3.41b) into Eqn (2.104),
r ¼
a
e2 1
1 þ ecos q
¼
a
e2 1
1 þ e
cos Fe
1ecos F
This reduces to
r ¼ aðecosh F 1Þ (3.46)
3.7 Universal variables
The equations for elliptical and hyperbolic trajectories are very similar, as can be seen from Table 3.1.
Observe, for example, that the hyperbolic mean anomaly is obtained from that of the ellipse as follows:
Mh ¼ m2
h3
e2 1
3
2
t
¼ m2
h3 ð1Þ
1 e2
3
2
t
¼ m2
h3 ð1Þ
3
2
1 e2
3
2
t
¼ m2
h3 ðiÞ
1 e2
3
2
t
¼ i m2
h3
1 e2
3
2
t
¼ iMe
In fact, the formulas for the hyperbola can all be obtained from those of the ellipse by replacing the
variables in the ellipse equations according to the following scheme, wherein “)” means “replace by”:
a) a
b)ib
Me) iMh
E)iF
i ¼
ffiffiffiffiffiffiffi
1
p
Note in this regard that sin (iF) ¼ i sinh F and cos (iF) ¼ cosh F. Relations among the circular and
hyperbolic trig functions are found in mathematics handbooks, such as Beyer (1991).
In the universal variable approach, the semimajor axis of the hyperbola is considered to have a
negative value, so that the energy equation (row 5 of Table 3.1) has the same form for any type of orbit,
including the parabola, for which a ¼ N. In this formulation, the semimajor axis of any orbit is found
using (row 3),
a ¼
h2
m
1
1 e2
(3.47)
3.7 Universal variables 173
30. If the position r and velocity v are known at a given point on the path, then the energy equation (row 5)
is convenient for finding the semimajor axis of any orbit,
a ¼
1
2
r v2
m
(3.48)
Kepler’s equation may also be written in terms of a universal variable, or universal “anomaly” c, that is
valid for all orbits. See, for example, Battin (1999), Bond and Allman (1993), and Prussing and
Conway (1993). If t0 is the time when the universal variable is 0, then the value of c at time t0 þ Dt is
found by iterative solution of the universal Kepler’s equation
ffiffiffi
m
p
Dt ¼
r0vr0
ffiffiffi
m
p c2
C
ac2
þ ð1 ar0Þc3
S
ac2
þ r0c (3.49)
in which r0 and vr0
are the radius and radial velocity, respectively, at t ¼ t0, and a is the reciprocal of the
semimajor axis
a ¼
1
a
(3.50)
a 0, a ¼ 0, and a 0 for hyperbolas, parabolas, and ellipses, respectively. The units of c are km1/2
(so ac2
is dimensionless). The functions C(z) and S(z) belong to the class known as Stumpff functions,
and they are defined by the infinite series,
SðzÞ ¼
X
N
k¼0
ð1Þk zk
ð2k þ 3Þ!
¼
1
6
z
120
þ
z2
5040
z3
362;880
þ / (3.51a)
Table 3.1 Comparison of Some of the Orbital Formulas for the Ellipse and Hyperbola
Equation Ellipse (e 1) Hyperbola (e 1)
1. Orbit Eqn (2.45) r ¼
h2
m
1
1 þ ecos q
Same
2. Conic equation in Cartesian coordinates (2.79)
and (2.109)
x2
a2
þ
y2
b2
¼ 1
x2
a2
y2
b2
¼ 1
3. Semimajor axis Eqns (2.71) and (2.103) a ¼
h2
m
1
1 e2
a ¼
h2
m
1
e2 1
4. Semiminor axis Eqns (2.76) and (2.06) b ¼ a
ffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 e2
p
b ¼ a
ffiffiffiffiffiffiffiffiffiffiffiffiffiffi
e2 1
p
5. Energy Eqns (2.81) and (2.111) v2
2
m
r
¼
m
2a
v2
2
m
r
¼
m
2a
6. Mean anomaly Eqns (3.7) and (3.34) Me ¼
m2
h3
ð1 e2
Þ
3
2t Mh ¼
m2
h3
ðe2
1Þ
3
2t
7. Kepler’s Eqns (3.14) and (3.40) Me ¼ E esin E Mh ¼ esinh F F
8. Orbit equation in terms of eccentric anomaly
(3.25) and (3.46)
r ¼ a(1 ecos E) r ¼ a(ecosh F 1)
174 CHAPTER 3 Orbital Position as a Function of Time
31. CðzÞ ¼
X
N
k¼0
ð1Þk zk
ð2k þ 2Þ!
¼
1
2
z
24
þ
z2
720
z3
40;320
þ / (3.51b)
C(z) and S(z) are related to the circular and hyperbolic trig functions as follows:
SðzÞ ¼
8
:
ffiffi
z
p
sin
ffiffi
z
p
ð
ffiffi
z
p
Þ3
ðz 0Þ
sinh
ffiffiffiffiffiffi
z
p
ffiffiffiffiffiffi
z
p
ffiffiffiffiffiffi
z
p 3
ðz 0Þ
1
6
ðz ¼ 0Þ
z ¼ ac2
(3.52)
CðzÞ ¼
8
:
1 cos
ffiffi
z
p
z
ðz 0Þ
cosh
ffiffiffiffiffiffi
z
p
1
z
ðz 0Þ
1
2
ðz ¼ 0Þ
z ¼ ac2
(3.53)
Clearly, z 0, z ¼ 0, and z 0 for hyperbolas, parabolas, and ellipses, respectively. It should be
pointed out that if C(z) and S(z) are computed by the series expansions, Eqns (3.51a,b), then the forms
of C(z) and S(z), depending on the sign of z, are selected, so to speak, automatically. C(z) and S(z)
behave as shown in Figure 3.19. Both C(z) and S(z) are nonnegative functions of z. They increase
without bound as z approaches N and tend toward zero for large positive values of z. As can be seen
from Eqn (3.53), for z 0, C(z) ¼ 0 when cos
ffiffi
z
p
¼ 1, that is, when z ¼ (2p)2
, (4p)2
, (6p)2
, ..
–30 –20 –10
2
4
6
8
10
10 20
0.1
0.2
0.3
0.4
100 200 300 400
0.01
0.02
0.03
0
12 0.5
–50
0
–40
0
0 30 0 500
0.04
0
z
z
z
S(z)
C(z)
S(z)
C(z)
C(z)
S(z)
FIGURE 3.19
A plot of the Stumpff functions C(z) and S(z).
3.7 Universal variables 175
32. The price we pay for using the universal variable formulation is having to deal with the relatively
unknown Stumpff functions. However, Eqns (3.52) and (3.53) are easy to implement in both computer
programs and programmable calculators. See Appendix D.13 for the implementation of these ex-
pressions in MATLAB.
To gain some insight into how Eqn (3.49) represents the Kepler equations for all the conic sections,
let t0 be the time at periapse passage and let us set t0 ¼ 0, as we have assumed previously. Then Dt ¼ t,
vr0
¼ 0, and r0 equals rp, the periapsis radius. In that case Eqn (3.49) reduces to
ffiffiffi
m
p
t ¼
1 arp
c3
S
ac2
þ rpc ðt ¼ 0 at periapse passageÞ (3.54)
Consider first the parabola. In this case a ¼ 0, and S ¼ S(0) ¼ 1/6, so that Eqn (3.54) becomes a cubic
polynomial in c,
ffiffiffi
m
p
t ¼
1
6
c3
þ rpc
Multiply this equation through by ð
ffiffiffi
m
p
=hÞ3
to obtain
m2
h3
t ¼
1
6
c
ffiffiffi
m
p
h
3
þ rpc
ffiffiffi
m
p
h
3
Since rp ¼ h2=2m for a parabola, we can write this as
m2
h3
t ¼
1
6
ffiffiffi
m
p
h
c
3
þ
1
2
ffiffiffi
m
p
h
c
(3.55)
Upon setting c ¼ h tan ðq=2Þ=
ffiffiffi
m
p
, Eqn (3.55) becomes identical to Eqn (3.30), the time vs true
anomaly relation for the parabola.
Kepler’s equation for the ellipse can be obtained by multiplying Eqn (3.54) throughout by
ð
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
mð1 e2Þ
p
=hÞ3
:
m2
h3
1 e2
3
2
t ¼
c
ffiffiffi
m
p
h
ffiffiffiffiffiffiffiffiffiffiffiffiffi
1 e2
p 3
1 arp
SðzÞ þ rpc
ffiffiffi
m
p
h
ffiffiffiffiffiffiffiffiffiffiffiffiffi
1 e2
p 3
z ¼ ac2
(3.56)
Recall that for the ellipse, rp ¼ h2=½mð1 þ eÞ and a ¼ 1=a ¼ mð1 e2Þ=h2. Using these two
expressions in Eqn (3.56), along with SðzÞ ¼ ½
ffiffiffi
a
p
c sinð
ffiffiffi
a
p
cÞ=a
3
2c3 (from Eqn (3.52)), and working
through the algebra ultimately leads to
Me ¼
c
ffiffiffi
a
p esin
c
ffiffiffi
a
p
Comparing this with Kepler’s equation for an ellipse (Eqn (3.14)) reveals that the relationship between
the universal variable c and the eccentric anomaly E is c ¼
ffiffiffi
a
p
E. Similarly, it can be shown for
hyperbolic orbits that c ¼
ffiffiffiffiffiffiffi
a
p
F. In summary, the universal anomaly c is related to the previously
encountered anomalies as follows:
c ¼
8
:
h
ffiffiffi
m
p tan
q
2
parabola
ffiffiffi
a
p
E ellipse
ffiffiffiffiffiffiffi
a
p
F hyperbola
ðt0 ¼ 0; at periapseÞ (3.57)
176 CHAPTER 3 Orbital Position as a Function of Time
33. When t0 is the time at a point other than periapsis, so that Eqn (3.49) applies, then Eqn (3.57) becomes
c ¼
8
:
h
ffiffiffi
m
p
tan
q
2
tan
q0
2
parabola
ffiffiffi
a
p
ðE E0Þ ellipse
ffiffiffiffiffiffiffi
a
p
ðF F0Þ hyperbola
(3.58)
As before, we can use Newton’s method to solve Eqn (3.49) for the universal anomaly c, given the time
interval Dt. To do so, we form the function
fðcÞ ¼
r0vr0
ffiffiffi
m
p c2
CðzÞ þ ð1 ar0Þc3
SðzÞ þ r0c
ffiffiffi
m
p
Dt (3.59)
and its derivative
dfðcÞ
dc
¼ 2
r0vr0
ffiffiffi
m
p cCðzÞ þ
r0vr0
ffiffiffi
m
p c2dCðzÞ
dz
dz
dc
þ 3ð1 ar0Þc2
SðzÞ þ ð1 r0aÞc3dSðzÞ
dz
dz
dc
þ r0 (3.60)
where it is to be recalled that
z ¼ ac2
(3.61)
which means of course that
dz
dc
¼ 2ac (3.62)
It turns out that
dSðzÞ
dz
¼
1
2z
½CðzÞ 3SðzÞ
dCðzÞ
dz
¼
1
2z
½1 zSðzÞ 2CðzÞ
(3.63)
Substituting Eqns (3.61)–(3.63) into Eqn (3.60) and simplifying the result yields
dfðcÞ
dc
¼
r0vr0
ffiffiffi
m
p c 1 ac2
SðzÞ þ ð1 ar0Þc2
CðzÞ þ r0 (3.64)
With Eqns (3.59) and (3.64), Newton’s algorithm (Eqn (3.16)) for the universal Kepler’s equation
becomes
ciþ1 ¼ ci
r0vr0
ffiffiffi
m
p c2
i CðziÞ þ ð1 ar0Þc3
i SðziÞ þ r0ci
ffiffiffi
m
p
Dt
r0vr0
ffiffiffi
m
p ci 1 ac2
i SðziÞ þ ð1 ar0Þc2
i CðziÞ þ r0
zi ¼ ac2
i
(3.65)
According to Chobotov (2002), a reasonable estimate for the starting value c0 is
c0 ¼
ffiffiffi
m
p
jajDt (3.66)
3.7 Universal variables 177
34. n
ALGORITHM 3.3
Solve the universal Kepler’s equation for the universal anomaly c given Dt, r0, vr0
, and a. See
Appendix D.14 for an implementation of this procedure in MATLAB.
1. Use Eqn (3.66) for an initial estimate of c0.
2. At any given step, having obtained ci from the previous step, calculate
fðciÞ ¼
r0vr0
ffiffiffi
m
p c2
i CðziÞ þ ð1 ar0Þc3
i SðziÞ þ r0ci
ffiffiffi
m
p
Dt
and
f0
ðciÞ ¼
r0vr0
ffiffiffi
m
p ci 1 ac2
i SðziÞ þ ð1 ar0Þc2
i CðziÞ þ r0
where zi ¼ ac2
i .
3. Calculate ratioi ¼ fðciÞ=f 0
ðciÞ.
4. If jratioij exceeds the chosen tolerance (e.g., 108
), then calculate an updated value of c,
ciþ1 ¼ ci ratioi
Return to Step 2.
5. If jratioij is less than the tolerance, then accept ci as the solution to within the desired accuracy.
n
EXAMPLE 3.6
An earth satellite has an initial true anomaly of q0 ¼ 30, a radius of r0 ¼ 10,000 km, and a speed of v0 ¼ 10 km/s.
Use the universal Kepler’s equation to find the change in universal anomaly c after one hour and use that infor-
mation to determine the true anomaly q at that time.
Solution
Using the initial conditions, let us first determine the angular momentum and the eccentricity of the trajectory.
From the orbit formula, Eqn (2.45), we have
h ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
mr0ð1 þ e cos q0Þ
p
¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
398;600$10;000$ð1 þ e cos 30Þ
p
¼ 63;135
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 þ 0:86602e
p
(a)
This, together with the angular momentum formula, Eqn (2.31), yields
vt0 ¼
h
r0
¼
63;135
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1þ 0:86602e
p
10; 000
¼ 6:3135
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 þ 0:86602e
p
Using the radial velocity relation, Eqn (2.49), we find
vr0 ¼
m
h
esin q0 ¼
398;600
63;135
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 þ 0:86602e
p esin 30
¼ 3:1567
e
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 þ 0:86602e
p (b)
Since v2
r0 þ v2
t0 ¼ v2
0, it follows that
3:1567
e
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 þ 0:86602e
p
2
þ
6:3135
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1 þ 0:86602e
p 2
¼ 102
178 CHAPTER 3 Orbital Position as a Function of Time
35. which simplifies to become 39.86e2
17.563e 60.14 ¼ 0. The only positive root of this quadratic equation is
e ¼ 1:4682
Since e is greater than 1, the orbit is a hyperbola. Substituting this value of the eccentricity back into Eqns (a)
and (b) yields the angular momentum
h ¼ 95;154 km2
=s
as well as the initial radial speed
vr0 ¼ 3:0752 km=s
The hyperbolic eccentric anomaly F0 for the initial conditions may now be found from Eqn (3.44a),
tanh
F0
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffi
e 1
e þ 1
r
tan
q0
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1:4682 1
1:4682 þ 1
r
tan
30
2
¼ 0:16670
Solving for F0 yields
F0 ¼ 0:23448 rad (c)
In the universal variable formulation, we calculate the semimajor axis of the orbit by means of Eqn (3.47),
a ¼
h2
m
1
1 e2
¼
95;1542
398;600
1
1 1:46822
¼ 19;655 km (d)
The negative value is consistent with the fact that the orbit is a hyperbola. From Eqn (3.50) we get
a ¼
1
a
¼
1
19;655
¼ 5:0878 105
km1
which appears throughout the universal Kepler’s equation.
We will use Algorithm 3.3 with an error tolerance of 106
to find the universal anomaly. From Eqn (3.66), our
initial estimate is
c0 ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
398;600
p
$ 5:0878 106
$3600 ¼ 115:6
Executing the algorithm yields the following steps:
c0 ¼ 115:6
Step 1:
fðc0Þ ¼ 370;650:01
f0
ðc0Þ ¼ 26;956:300
ratio ¼ 13:750033
c1 ¼ 115:6 ð13:750033Þ ¼ 129:35003
jratioj 106
; so repeat:
Step 2:
fðc1Þ ¼ 25;729:002
f0
ðc1Þ ¼ 30;776:401
ratio ¼ 0:83599669
c2 ¼ 129:35003 0:83599669 ¼ 128:51404
jratioj 106
; so repeat:
3.7 Universal variables 179
36. Step 3:
fðc2Þ ¼ 102:83891
f0
ðc2Þ ¼ 30;530:672
ratio ¼ 3:3683800 103
c3 ¼ 128:51404 3:3683800 103
¼ 128:51067
jratioj 106
; so repeat:
Step 4:
fðc3Þ ¼ 1:6614116 103
f0
ðc3Þ ¼ 30;529:686
ratio ¼ 5:4419545 108
c4 ¼ 128:51067 5:4419545 108
¼ 128:51067
jratioj 106
So we accept
c ¼ 128:51km
1
2
as the solution after four iterations. Substituting this value of c together with the semimajor axis (Eqn (d)) into
Eqn (3.58) yields
F F0 ¼
c
ffiffiffiffiffiffiffi
a
p ¼
128:51
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
ð19;655Þ
p ¼ 0:91664
It follows from Eqn (b) that the hyperbolic eccentric anomaly after 1 h is
F ¼ 0:23448 þ 0:91664 ¼ 1:1511
Finally, we calculate the corresponding true anomaly using Eqn (3.44b),
tan
q
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffi
e þ 1
e 1
r
tanh
F
2
¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
1:4682 þ 1
1:4682 1
r
tanh
1:1511
2
¼ 1:1926
which means that after one hour
q ¼ 100:04
Recall from Section 2.11 that the position r and velocity v on a trajectory at any time t can be found in
terms of the position r0 and velocity v0 at time t0 by means of the Lagrange f and g coefficients and
their first derivatives,
r ¼ fr0 þ gv0 (3.67)
v ¼ _
fr0 þ _
gv0 (3.68)
Eqns (2.158) give f, g, _
f, and _
g explicitly in terms of the change in true anomaly Dq over the time
interval Dt ¼ t t0. The Lagrange coefficients can also be derived in terms of changes in the eccentric
anomaly DE for elliptical orbits, DF for hyperbolas, or Dtan(q/2) for parabolas. However, if we take
180 CHAPTER 3 Orbital Position as a Function of Time
37. advantage of the universal variable formulation, we can cover all these cases with the same set of
Lagrange coefficients. In terms of the universal anomaly c and the Stumpff functions C(z) and S(z), the
Lagrange coefficients are (Bond and Allman, 1996)
f ¼ 1
c2
r0
C
ac2
(3.69a)
g ¼ Dt
1
ffiffiffi
m
p c3
S
ac2
(3.69b)
_
f ¼
ffiffiffi
m
p
rr0
ac3
S
ac2
c (3.69c)
_
g ¼ 1
c2
r
C
ac2
(3.69d)
The implementation of these four functions in MATLAB is found in Appendix D.15.
n
ALGORITHM 3.4
Given r0 and v0, find r and v at a time Dt later. See Appendix D.16 for an implementation of this
procedure in MATLAB.
1. Use the initial conditions to find:
a. The magnitude of r0 and v0,
r0 ¼
ffiffiffiffiffiffiffiffiffiffiffi
r0$r0
p
v0 ¼
ffiffiffiffiffiffiffiffiffiffiffi
ffi
v0$v0
p
b. The radial component velocity of vr0
by projecting v0 onto the direction of r0,
vr0
¼
r0$v0
r0
c. The reciprocal a of the semimajor axis, using Eqn (3.48), is given by
a ¼
2
r0
v2
0
m
The sign of a determines whether the trajectory is an ellipse (a 0), parabola (a ¼ 0), or hyperbola
(a 0).
2. With r0, vr0
, a, and Dt, use Algorithm 3.3 to find the universal anomaly c.
3. Substitute a, r0, Dt, and c into Eqns (3.69a,b) to obtain f and g.
4. Use Eqn (3.67) to compute r and, from that, its magnitude r.
5. Substitute a, r0, r, and c into Eqns (3.69c,d) to obtain _
f and _
g.
6. Use Eqn (3.68) to compute v.
n
EXAMPLE 3.7
An earth satellite moves in the xy plane of an inertial frame with origin at the earth’s center. Relative to that frame,
the position and velocity of the satellite at time t0 are
r0 ¼ 7000:0^
i 12; 124^
jðkmÞ
v0 ¼ 2:6679^
i þ 4:6210^
jðkm=sÞ
(a)
3.7 Universal variables 181
38. Compute the position and velocity vectors of the satellite 60 min later using Algorithm 3.4.
Solution
Step 1:
r0 ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
7000:02 þ ð12;124Þ2
q
¼ 14;000 km
v0 ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
2:66792 þ 4:62102
p
¼ 5:3359 km=s
vr0
¼
7000:0$2:6679 þ ð12;124Þ$4:6210
14;000
¼ 2:6679 km=s
a ¼
2
14;000
5:33592
398;600
¼ 7:1429 105
km1
The trajectory is an ellipse, because a is positive.
Step 2:
Using the results of Step 1, Algorithm 3.3 yields
c ¼ 253:53 km
1
2
which means
z ¼ ac2
¼ 7:1429 105
$253:532
¼ 4:5911
Step 3:
Substituting the above values of c and z into Eqns (3.69a,b), we find
f ¼ 1
c2
r0
C
ac2
¼ 1
253:532
14;000
Cð4:5911Þ
zfflfflfflfflfflfflfflffl}|fflfflfflfflfflfflfflffl{
0:3357
¼ 0:54123
g ¼ Dt
1
ffiffiffi
m
p c3
S
ac2
¼ 3600
253:533
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
398;600
p Sð4:5911Þ
zfflfflfflfflfflfflfflffl}|fflfflfflfflfflfflfflffl{
0:13233
¼ 184:35 s1
Step 4:
r ¼ fr0 þ gv0
¼ ð0:54123Þ
7000:0^
i 12:124^
j
þ 184:35
2:6679^
i þ 4:6210^
j
¼ 3296:8^
i þ 7413:9^
jðkmÞ
Therefore, the magnitude of r is
r ¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
ð3296:8Þ2
þ 7413:92
q
¼ 8113:9 km
Step 5:
_
f ¼
ffiffiffi
m
p
rr0
ac3S
ac2
c
¼
ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
398;600
p
8113:9$14;000
7:1429 105
$253:533$Sð4:5911Þ
zfflfflfflfflfflfflfflffl}|fflfflfflfflfflfflfflffl{
0:13233
253:53
#
¼ 0:00055298 se1
182 CHAPTER 3 Orbital Position as a Function of Time
39. _
g ¼ 1
c2
r
C
ac2
¼ 1
253:532
8113:9
Cð4:5911Þ
zfflfflfflfflfflfflfflffl}|fflfflfflfflfflfflfflffl{
0:3357
¼ 1:6593
Step 6:
v ¼ _
fr0 þ _
gv0
¼ ð0:00055298Þ
7000:0^
i 12:124^
j
þ ð1:6593Þv0
2:6679^
i þ 4:6210^
j
¼ 8:2977^
i 0:96309^
j ðkm=sÞ
The initial and final position and velocity vectors, as well as the trajectory, are accurately illustrated in Figure 3.20.
Perigee
î
x
ĵ
y
r
t = t0 + 3600 s
t = t0
r0
O
v
v0
FIGURE 3.20
Initial and final points on the geocentric trajectory of Example 3.7.
PROBLEMS
Section 3.2
3.1 If f ¼
1
2
tan
x
2
þ
1
6
tan3x
2
, then show that df=dx ¼ 1=ð1 þ cos xÞ2
, thereby verifying the integral in
Eqn (3.4).
Section 3.2 183
40. Section 3.4
3.2 Find the three positive roots of the equation 10esin x
¼ x2
5x þ 4 to eight significant figures. Use
(a) Newton’s method.
(b) Bisection method.
3.3 Find the first four nonnegative roots of the equation tan (x) ¼ tanh (x) to eight significant
figures. Use
(a) Newton’s method.
(b) Bisection method.
3.4 In terms of the eccentricity e, the period T, and the angles a and b (in radians), find the time t
required to fly from point 1 to point 2 on the ellipse. C is the center of the ellipse.
Ans:: t ¼
T
2p
h
b a 2ecos
b þ a
2
sin
b a
2
i
P
A
F
C
a
α
β
2
1
3.5 Calculate the time required to fly from P to B, in terms of the eccentricity e and the period T. B lies
on the minor axis.
Ans::
1
4
e
2p
T
P
A
B
D
F
C
3.6 If the eccentricity of the elliptical orbit is 0.3, calculate, in terms of the period T, the time required
to fly from P to B.
fAns:: 0:157tg
184 CHAPTER 3 Orbital Position as a Function of Time
41. 3.7 If the eccentricity of the elliptical orbit is 0.5, calculate, in terms of the period T, the time required
to fly from P to B.
{Ans.: 0.170T}
P
A
B
rp
2rp
F
3.8 A satellite is in earth orbit for which the perigee altitude is 200 km and the apogee altitude is
600 km. Find the time interval during which the satellite remains above an altitude of 400 km.
{Ans.: 47.15 min}
3.9 An earth-orbiting satellite has a perigee radius of 7000 km and an apogee radius of 10,000 km. (a)
What true anomaly Dq is swept out between t ¼ 0.5 h and t ¼ 1.5 h after perigee passage? (b)
What area is swept out by the position vector during that time interval?
{Ans.: (a) 128.7; (b) 1.03 108
km2
}
3.10 An earth-orbiting satellite has a period of 14 h and a perigee radius of 10,000 km. At time
t ¼ 10 h after perigee passage, determine
(a) The radial position.
(b) The speed.
(c) The radial component of the velocity.
{Ans.: (a) 42,356 km; (b) 2.303 km/s; (c) 1.271 km/s}
3.11 A satellite in earth orbit has perigee and apogee radii of rp ¼ 7500 km and ra ¼ 16,000 km,
respectively. Find its true anomaly 40 min after passing the true anomaly of 80
.
{Ans.: 174.7}
3.12 Show that the solution to a cos q þ b sin q ¼ c, where a, b, and c are given, is
q ¼ f cos1
c
a
cos f
where tanf ¼ b=a.
3.13 Verify the results of part (b) of Example 3.3.
P
A
B
F
90°
Section 3.4 185
42. Section 3.5
3.14 Calculate the time required for a spacecraft launched into a parabolic trajectory at a perigee
altitude of 200 km to leave the earth’s sphere of influence (see Table A.2).
{Ans.: 7.77 days}
3.15 A spacecraft on a parabolic trajectory around the earth has a perigee radius of 6600 km.
(a) How long does it take to coast from q ¼ 90 degrees to q ¼ þ90 degrees?
(b) How far is the spacecraft from the center of the earth 36 h after passing through perigee?
{Ans.: (a) 0.8897 h; (b) 304,700 km}
Section 3.6
3.16 A spacecraft on a hyperbolic trajectory around the earth has a perigee radius of 6600 km and
a perigee speed of 1.2 vesc.
(a) How long does it take to coast from q ¼ 90
to q ¼ þ90
?
(b) How far is the spacecraft from the center of the earth 24 h after passing through perigee?
{Ans.: (a) 0.9992 h; (b) 656,610 km}
3.17 A trajectory has a perigee velocity 1.1 vesc and a perigee altitude of 200 km. If at 10 AM the
satellite is traveling toward the earth with a speed of 8 km/s, how far will it be from the earth’s
surface at 5 PM the same day?
{Ans.: 136,250 km}
3.18 An incoming object is sighted at an altitude of 100,000 km with a speed of 6 km/s and a flight
path angle of 80
. (a) Will it impact the earth or fly by? (b) What is the time either to impact or
closest approach?
{Partial Ans.: (b) 30.4 min}
Section 3.7
3.19 At a given instant, the radial position of an earth-orbiting satellite is 7200 km and its radial speed
is 1 km/s. If the semimajor axis is 10,000 km, use Algorithm 3.3 to find the universal anomaly
60 min later. Check your result using Eqn (3.58).
3.20 At a given instant, a space object has the following position and velocity vectors relative to an
earth-centered inertial frame of reference:
r0 ¼ 20; 000^
i 105; 000^
j 19; 000^
k ðkmÞ
v0 ¼ 0:9000^
i 3:4000^
j 1:5000^
k ðkm=sÞ
Use Algorithm 3.4 to find r and v 2 h later.
{Ans.: r ¼ 26; 338^
i 128; 750^
j 29; 656^
kðkmÞ; v ¼ 0:862; 800^
i 3:2116^
j 1:4613^
kðkm=sÞ}
186 CHAPTER 3 Orbital Position as a Function of Time