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A model for non-circular orbits derived from a two-step linearisation of the Kepler laws 
JPAR 
A model for non-circular orbits derived from a two- step linearisation of the Kepler laws 
Lena Strömberg 
Previously Department of Solid Mechanics, Royal Institute of Technology (KTH), Stockholm, Sweden 
Email: lena_str@hotmail.com 
In the Solar System most orbits are circular, but there are some exceptions. The paper addresses results from a two-step linearisation of the Kepler laws, to model non-circular orbits, at Newtonian gravity and other interactions with adjacent bodies. The orbit will then be characterised by a generalised eccentricity and a secondary frequency denoted L- frequency, ωL (and considered proportional to the angular velocity). The path will be that of a circle, superimposed by small vibrations with the L-frequency. Hereby, the amplitude corresponds to an eccentricity, such that the radius varies, with time. When the ratio between the L-frequency and angular velocity is a non-integer, ‘perihelion’ moves. Bounds are derived and resulting orbits are generated and visualized. For the integer ratio 2, results are compared with an ellipsoidal, and a tidal wave. For a non- integer ratio, the orbit is related to data for Mercury. Methods for detecting and measuring the secondary frequency are discussed, in terms of transfer orbits in Spaceflight dynamics. 
Keywords: Kepler laws, planetary orbit, linearization, L-frequency, eccentricity, inertia refinement, perihelion, detection, Mercury, Mars 
INTRODUCTION 
Newtonian gravity gives elliptic orbits, but the eccentricity is not specified, when no additional conditions. For the 2-body problem, or multi-body problem, other forces act along the path, and resulting equations are complex. A related result is (Bruns- Poincaré´s Theorem, 1887), on impossibility of solving the 3-body problem. Recent developments in nonlinear dynamics indicate that systems can self-organise into steady motions, by means of frequency coupling. Here, it is assumed that a planet satisfies linearized Kepler laws with an additional refinement of inertia part (in some contexts, denoted as perturbation theory).This results in radial oscillations around a circular path. The frequency for oscillation will be denoted, the L- frequency. Other relative motions with oscillations are e.g. Satellite librations, c.f. Klemperer and Baker (1957), where several dynamical models are given. EXCEPTIONS FROM CIRCULAR ORBITS 
Most of the planets and moons, in Kepler motion have very low eccentricity, such that the orbits are almost circular. Mercury, closest to the sun do not have a circular orbit, and the eccentricity is about 0.2. The planet has a coupling 3:2, for the siderial rotation and orbital rotation. Hereby it is somewhat related to the sun, as a moon to its primary, where coupling is 1:1. Mars, close to the asteroid belt, has eccentricity approximately 0.1. The other exceptions are two dwarf planets in the asteroid belt, and Pluto. Next, a linearisation of Kepler laws, which gives noncircular orbits with generalised eccentricity 0.25, and 0.2 will be given. LINEARISATION OF KEPLER LAWS OF MOTION In well-known notations, (cf. eg. wikipedia) Kepler law in r-direction reads m(r,tt − (θ,t)2 r) − Fr = 0 (1) 
where m is the mass of orbiting body, r and θ are the radius and angle in the orbit, and Fr is the Newtonian gravity force, Fr = -mGM/r2, G is the universal constant of gravity and M is the central mass. Journal of Physics and Astronomy Research Vol. 1(2), pp. 007-012, October, 2014. © www.premierpublishers.org, ISSN: 2123-503X 
Short Communication
A model for non-circular orbits derived from a two-step linearisation of the Kepler laws 
Figure 1. Orbit o, created from radius vector obtained by a two-step linearization with ωL=2ω. 
Figure 2. Path from a 2-step linearization with ωL= (4.2)1/2W, and generalised eccentricity recc=0.2r0. 
Proposition There are solutions, so called small vibrations rε, with a frequency around r = r0, θ = θ0, where subscript 0, is the path of a circle satisfying (1). One choice of linearisation gives the frequency 2ω, where ω2 = GM/r03, is the angular velocity of the orbital rotation, and amplitude r0/4, and that ω is constant, although the orbit is not circular. This orbit compared with an ellipsoidal is shown in Figure 1. Subsequently, such a frequency will be referred to as the L-frequency, ωL of a noncircular orbit. Proof From Kepler law, the angular momentum is constant, which reads (θ,t)2 r4=(θ0,t)2 r04 (2) Using (2), expansion of inertia part and Fr in (1), and including a nonlinear term from inertia gives rε,tt +5ω2rε+ 4ω2(rε)2/r0= 0 (3) In the 2nd step of linearisation, rε in the nonlinear term is chosen as rε=-r0/4. This gives frequency 2ω and, assuming this location as the innermost point in oscillation, also amplitude. Remark In the general case, any frequency and amplitude can be provided by the linearisation, depending on at which point 2nd step of linearisation is done. Orbit could also change, not maintaining a steady motion with one frequency. Such behavior may be exposed by Mercury, as indicated in Correia and Laskar (2011). RESULTS Solution to the differential equation for an harmonic oscillator, obtained by a linearization of (3), gives that the expression for an orbit reads r=r0+recc sin(ωLt) (4) where r0 is the radius in a circular orbit, recc is the generalised eccentricity. In the figures the orbital paths are shown for two linearisations. In Figure 1, the orbit obtained from a linearisation is shown, compared with ellipsoidals with axis 3r0/4 and 5r0/4. 
In Figure 2, the linearisation is such that the L- frequency will be (5−0.8)1/2ω, and amplitude 0.2r0. At
A model for non-circular orbits derived from a two-step linearisation of the Kepler laws 
the beginning, the path is indicated with o, and then small dots. 
Neglecting the out-of plane components, the eccentricity agrees with the path for Mercury. It is seen that the location for maximum and minimum radius, rotates, since the frequency is not an integer multiple of ω. Depending on the point of linearisation, when amplitude is 0.25r0, the L- frequency will be bounded in an interval such that 2ω ≤ ωL ≤ 61/2ω. 
METHODS FOR DETECTING THE L-FREQUENCY 
Measurments and maneuvering of Earth Satellites. 
To change of orbits for satellites, derivations and formulas are given in Wiesel (2010). With additional analysis, and numerical calculations or simplifications, the control variables may be used for detection: 
Low Thrust 
For low thrust transfer, replace velocity and location with results from two-step, such that dependency on ωL, ω and t, are obtained. 
Modification of the Hohmann transfer. 
To enter the transfer ellipsoidal, assume instead that a velocity in radial direction may be applied. The magnitude for this is derived from differentiation of the radius from a two-step linarisation. 
Eccentricity for planetary orbits. 
More detailed observations and analysis of the paths of Mars and Mercury, e.g. from visibility at Earth on latitude 55, (Modern Astronomi 2014,2, p. 28). 
CONCLUSIONS 
A two-step generalized linearisation, with adjustment to a specified amplitude was derived. This admits solution into a non-circular path, where radius varies due to small vibrations, with a so-called L-frequency. In conjunction with assuming that nonlinear systems may self-organise, this may serve as a solution to an in- plane multi-body problem in celestial mechanics. The capture into a harmonic solution with one frequency agrees, to some extent, with the KAM-theorem. 
• Here, small radial vibrations were considered. In another context (e.g. whirls), it may be of interest to investigate how an original path varies, when subjected to other types of modifications, with a rigorous perturbation theory. 
• Methods for detecting the L-frequency, was discussed. 
• It is possible that other frequency ratios are related, e.g. sidereal versus orbital rotation for Mercury, Correia and Laskar (2011), and the distance between adjacent planets in terms of ratios of angular velocities. Other recent suggestions for locations of all the planets are models based on differential equations, eg. 
Schrödinger equation de Oliveira Neto et al., (2004) and modified Laplaces equation, with eigen-values. 
• The tide at Earth, may be a manifest of the theory, such that the L-frequency for the water is related to the sidereal rotation of earth by ωL=2ω. 
• Maintenance of the noncircular motion may require energy supply, which for Mercury, could be related to energy from the Sun, and for other orbits, to additional gravity. This suggests that the capture into circular orbits are preferable when no extra energy is present. 
• The fact that most orbits are circular, was maybe, at that time, not entirely understood by Kepler, and therefore the ellipsoidals remain as models for the planetary paths. In the present paper, the Kepler model was used as the point of departure, to derive a new possible model for a noncircular orbit, resulting in equation (4), i.e. small vibrations with the frequency ωL around a circular orbit with radius r0 . 
REFERENCES 
Correia A, Laskar J (2011). Mercury’s capture into the 3/2 spin-orbit resonance including the effect of core- mantle friction. Icarus, 201, pp 1-11. 
Klemperer WB, Baker RM (1957); Satellite Librations, AstronauticaActa, 3: 16-27, Springer. 
de Oliveira NM, Maia LA, Carneiro S (2004). An alternative theoretical approach to describe planetary systems through a Schrödinger-type diffusion equation. Chaos, Solitons and Fractals, 21(1): 21–28. 
Wiesel WE (2010). Spaceflight Dynamics, 2nd edn, Aphelion Press. 
Accepted 29 September, 2014. Citation: Strömberg L (2014). A model for non-circular orbits derived from a two-step linearisation of the Kepler laws. Journal of Physics and Astronomy Research 1(2): 013-014. Copyright: © 2014 Strömberg L. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are cited.

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A model for non-circular orbits derived from a two-step linearisation of the Kepler laws

  • 1. A model for non-circular orbits derived from a two-step linearisation of the Kepler laws JPAR A model for non-circular orbits derived from a two- step linearisation of the Kepler laws Lena Strömberg Previously Department of Solid Mechanics, Royal Institute of Technology (KTH), Stockholm, Sweden Email: lena_str@hotmail.com In the Solar System most orbits are circular, but there are some exceptions. The paper addresses results from a two-step linearisation of the Kepler laws, to model non-circular orbits, at Newtonian gravity and other interactions with adjacent bodies. The orbit will then be characterised by a generalised eccentricity and a secondary frequency denoted L- frequency, ωL (and considered proportional to the angular velocity). The path will be that of a circle, superimposed by small vibrations with the L-frequency. Hereby, the amplitude corresponds to an eccentricity, such that the radius varies, with time. When the ratio between the L-frequency and angular velocity is a non-integer, ‘perihelion’ moves. Bounds are derived and resulting orbits are generated and visualized. For the integer ratio 2, results are compared with an ellipsoidal, and a tidal wave. For a non- integer ratio, the orbit is related to data for Mercury. Methods for detecting and measuring the secondary frequency are discussed, in terms of transfer orbits in Spaceflight dynamics. Keywords: Kepler laws, planetary orbit, linearization, L-frequency, eccentricity, inertia refinement, perihelion, detection, Mercury, Mars INTRODUCTION Newtonian gravity gives elliptic orbits, but the eccentricity is not specified, when no additional conditions. For the 2-body problem, or multi-body problem, other forces act along the path, and resulting equations are complex. A related result is (Bruns- Poincaré´s Theorem, 1887), on impossibility of solving the 3-body problem. Recent developments in nonlinear dynamics indicate that systems can self-organise into steady motions, by means of frequency coupling. Here, it is assumed that a planet satisfies linearized Kepler laws with an additional refinement of inertia part (in some contexts, denoted as perturbation theory).This results in radial oscillations around a circular path. The frequency for oscillation will be denoted, the L- frequency. Other relative motions with oscillations are e.g. Satellite librations, c.f. Klemperer and Baker (1957), where several dynamical models are given. EXCEPTIONS FROM CIRCULAR ORBITS Most of the planets and moons, in Kepler motion have very low eccentricity, such that the orbits are almost circular. Mercury, closest to the sun do not have a circular orbit, and the eccentricity is about 0.2. The planet has a coupling 3:2, for the siderial rotation and orbital rotation. Hereby it is somewhat related to the sun, as a moon to its primary, where coupling is 1:1. Mars, close to the asteroid belt, has eccentricity approximately 0.1. The other exceptions are two dwarf planets in the asteroid belt, and Pluto. Next, a linearisation of Kepler laws, which gives noncircular orbits with generalised eccentricity 0.25, and 0.2 will be given. LINEARISATION OF KEPLER LAWS OF MOTION In well-known notations, (cf. eg. wikipedia) Kepler law in r-direction reads m(r,tt − (θ,t)2 r) − Fr = 0 (1) where m is the mass of orbiting body, r and θ are the radius and angle in the orbit, and Fr is the Newtonian gravity force, Fr = -mGM/r2, G is the universal constant of gravity and M is the central mass. Journal of Physics and Astronomy Research Vol. 1(2), pp. 007-012, October, 2014. © www.premierpublishers.org, ISSN: 2123-503X Short Communication
  • 2. A model for non-circular orbits derived from a two-step linearisation of the Kepler laws Figure 1. Orbit o, created from radius vector obtained by a two-step linearization with ωL=2ω. Figure 2. Path from a 2-step linearization with ωL= (4.2)1/2W, and generalised eccentricity recc=0.2r0. Proposition There are solutions, so called small vibrations rε, with a frequency around r = r0, θ = θ0, where subscript 0, is the path of a circle satisfying (1). One choice of linearisation gives the frequency 2ω, where ω2 = GM/r03, is the angular velocity of the orbital rotation, and amplitude r0/4, and that ω is constant, although the orbit is not circular. This orbit compared with an ellipsoidal is shown in Figure 1. Subsequently, such a frequency will be referred to as the L-frequency, ωL of a noncircular orbit. Proof From Kepler law, the angular momentum is constant, which reads (θ,t)2 r4=(θ0,t)2 r04 (2) Using (2), expansion of inertia part and Fr in (1), and including a nonlinear term from inertia gives rε,tt +5ω2rε+ 4ω2(rε)2/r0= 0 (3) In the 2nd step of linearisation, rε in the nonlinear term is chosen as rε=-r0/4. This gives frequency 2ω and, assuming this location as the innermost point in oscillation, also amplitude. Remark In the general case, any frequency and amplitude can be provided by the linearisation, depending on at which point 2nd step of linearisation is done. Orbit could also change, not maintaining a steady motion with one frequency. Such behavior may be exposed by Mercury, as indicated in Correia and Laskar (2011). RESULTS Solution to the differential equation for an harmonic oscillator, obtained by a linearization of (3), gives that the expression for an orbit reads r=r0+recc sin(ωLt) (4) where r0 is the radius in a circular orbit, recc is the generalised eccentricity. In the figures the orbital paths are shown for two linearisations. In Figure 1, the orbit obtained from a linearisation is shown, compared with ellipsoidals with axis 3r0/4 and 5r0/4. In Figure 2, the linearisation is such that the L- frequency will be (5−0.8)1/2ω, and amplitude 0.2r0. At
  • 3. A model for non-circular orbits derived from a two-step linearisation of the Kepler laws the beginning, the path is indicated with o, and then small dots. Neglecting the out-of plane components, the eccentricity agrees with the path for Mercury. It is seen that the location for maximum and minimum radius, rotates, since the frequency is not an integer multiple of ω. Depending on the point of linearisation, when amplitude is 0.25r0, the L- frequency will be bounded in an interval such that 2ω ≤ ωL ≤ 61/2ω. METHODS FOR DETECTING THE L-FREQUENCY Measurments and maneuvering of Earth Satellites. To change of orbits for satellites, derivations and formulas are given in Wiesel (2010). With additional analysis, and numerical calculations or simplifications, the control variables may be used for detection: Low Thrust For low thrust transfer, replace velocity and location with results from two-step, such that dependency on ωL, ω and t, are obtained. Modification of the Hohmann transfer. To enter the transfer ellipsoidal, assume instead that a velocity in radial direction may be applied. The magnitude for this is derived from differentiation of the radius from a two-step linarisation. Eccentricity for planetary orbits. More detailed observations and analysis of the paths of Mars and Mercury, e.g. from visibility at Earth on latitude 55, (Modern Astronomi 2014,2, p. 28). CONCLUSIONS A two-step generalized linearisation, with adjustment to a specified amplitude was derived. This admits solution into a non-circular path, where radius varies due to small vibrations, with a so-called L-frequency. In conjunction with assuming that nonlinear systems may self-organise, this may serve as a solution to an in- plane multi-body problem in celestial mechanics. The capture into a harmonic solution with one frequency agrees, to some extent, with the KAM-theorem. • Here, small radial vibrations were considered. In another context (e.g. whirls), it may be of interest to investigate how an original path varies, when subjected to other types of modifications, with a rigorous perturbation theory. • Methods for detecting the L-frequency, was discussed. • It is possible that other frequency ratios are related, e.g. sidereal versus orbital rotation for Mercury, Correia and Laskar (2011), and the distance between adjacent planets in terms of ratios of angular velocities. Other recent suggestions for locations of all the planets are models based on differential equations, eg. Schrödinger equation de Oliveira Neto et al., (2004) and modified Laplaces equation, with eigen-values. • The tide at Earth, may be a manifest of the theory, such that the L-frequency for the water is related to the sidereal rotation of earth by ωL=2ω. • Maintenance of the noncircular motion may require energy supply, which for Mercury, could be related to energy from the Sun, and for other orbits, to additional gravity. This suggests that the capture into circular orbits are preferable when no extra energy is present. • The fact that most orbits are circular, was maybe, at that time, not entirely understood by Kepler, and therefore the ellipsoidals remain as models for the planetary paths. In the present paper, the Kepler model was used as the point of departure, to derive a new possible model for a noncircular orbit, resulting in equation (4), i.e. small vibrations with the frequency ωL around a circular orbit with radius r0 . REFERENCES Correia A, Laskar J (2011). Mercury’s capture into the 3/2 spin-orbit resonance including the effect of core- mantle friction. Icarus, 201, pp 1-11. Klemperer WB, Baker RM (1957); Satellite Librations, AstronauticaActa, 3: 16-27, Springer. de Oliveira NM, Maia LA, Carneiro S (2004). An alternative theoretical approach to describe planetary systems through a Schrödinger-type diffusion equation. Chaos, Solitons and Fractals, 21(1): 21–28. Wiesel WE (2010). Spaceflight Dynamics, 2nd edn, Aphelion Press. Accepted 29 September, 2014. Citation: Strömberg L (2014). A model for non-circular orbits derived from a two-step linearisation of the Kepler laws. Journal of Physics and Astronomy Research 1(2): 013-014. Copyright: © 2014 Strömberg L. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are cited.