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Kepler problem

From Wikipedia, the free encyclopedia
(Redirected fromKeplerian problem)
Special case of the two-body problem
This article is about a special case of thetwo-body problem inclassical mechanics. For the problem offinding the densest packing of spheres in three-dimensional Euclidean space, seeKepler conjecture.

Inclassical mechanics, theKepler problem is a special case of thetwo-body problem, in which the two bodies interact by acentral force that varies in strength as theinverse square of the distance between them. The force may be either attractive or repulsive. The problem is to find the position or speed of the two bodies over time given theirmasses,positions, andvelocities. Using classical mechanics, the solution can be expressed as aKepler orbit using sixorbital elements.

The Kepler problem is named afterJohannes Kepler, who proposedKepler's laws of planetary motion (which are part ofclassical mechanics and solved the problem for the orbits of the planets) and investigated the types of forces that would result in orbits obeying those laws (calledKepler's inverse problem).[1]

For a discussion of the Kepler problem specific to radial orbits, seeRadial trajectory.General relativity provides more accurate solutions to the two-body problem, especially in stronggravitational fields.

Applications

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The inverse square law behind the Kepler problem is the most important central force law.[1]: 92 The Kepler problem is important incelestial mechanics, sinceNewtonian gravity obeys aninverse square law. Examples include a satellite moving about a planet, a planet about its sun, or two binary stars about each other. The Kepler problem is also important in the motion of two charged particles, sinceCoulomb’s law ofelectrostatics also obeys aninverse square law.

The Kepler problem and thesimple harmonic oscillator problem are the two most fundamental problems inclassical mechanics. They are theonly two problems that have closed orbits for every possible set of initial conditions, i.e., return to their starting point with the same velocity (Bertrand's theorem).[1]: 92 

The Kepler problem also conserves theLaplace–Runge–Lenz vector, which has since been generalized to include other interactions. The solution of the Kepler problem allowed scientists to show that planetary motion could be explained entirely by classical mechanics andNewton’s law of gravity; the scientific explanation of planetary motion played an important role in ushering in theEnlightenment.

History

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The Kepler problem begins with the empirical results ofJohannes Kepler arduously derived by analysis of the astronomical observations ofTycho Brahe. After some 70 attempts to match the data to circular orbits, Kepler hit upon the idea of theelliptic orbit. He eventually summarized his results in the form ofthree laws of planetary motion.[2]

What is now called the Kepler problem was first discussed byIsaac Newton as a major part of his Principia. His "Theorema I" begins with the first two of his three axioms orlaws of motion and results in Kepler's second law of planetary motion. Next Newton proves his "Theorema II" which shows that if Kepler's second law results, then the force involved must be along the line between the two bodies. In other words, Newton proves what today might be called the "inverse Kepler problem": the orbit characteristics require the force to depend on the inverse square of the distance.[3]: 107 

Mathematical definition

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Thecentral forceF between two objects varies in strength as theinverse square of the distancer between them:

F=kr2r^{\displaystyle \mathbf {F} ={\frac {k}{r^{2}}}\mathbf {\hat {r}} }

wherek is a constant andr^{\displaystyle \mathbf {\hat {r}} } represents theunit vector along the line between them.[4] The force may be either attractive (k < 0) or repulsive (k > 0). The correspondingscalar potential is:

V(r)=kr{\displaystyle V(r)={\frac {k}{r}}}

Solution of the Kepler problem

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The equation of motion for the radiusr{\displaystyle r} of a particle of massm{\displaystyle m} moving in acentral potentialV(r){\displaystyle V(r)} is given byLagrange's equations

md2rdt2mrω2=md2rdt2L2mr3=dVdr{\displaystyle m{\frac {d^{2}r}{dt^{2}}}-mr\omega ^{2}=m{\frac {d^{2}r}{dt^{2}}}-{\frac {L^{2}}{mr^{3}}}=-{\frac {dV}{dr}}}

ωdθdt{\displaystyle \omega \equiv {\frac {d\theta }{dt}}} and theangular momentumL=mr2ω{\displaystyle L=mr^{2}\omega } is conserved. For illustration, the first term on the left-hand side is zero for circular orbits, and the applied inwards forcedVdr{\displaystyle {\frac {dV}{dr}}} equals thecentripetal force requirementmrω2{\displaystyle mr\omega ^{2}}, as expected.

IfL is not zero the definition ofangular momentum allows a change of independent variable fromt{\displaystyle t} toθ{\displaystyle \theta }

ddt=Lmr2ddθ{\displaystyle {\frac {d}{dt}}={\frac {L}{mr^{2}}}{\frac {d}{d\theta }}}

giving the new equation of motion that is independent of time

Lr2ddθ(Lmr2drdθ)L2mr3=dVdr{\displaystyle {\frac {L}{r^{2}}}{\frac {d}{d\theta }}\left({\frac {L}{mr^{2}}}{\frac {dr}{d\theta }}\right)-{\frac {L^{2}}{mr^{3}}}=-{\frac {dV}{dr}}}

The expansion of the first term is

Lr2ddθ(Lmr2drdθ)=2L2mr5(drdθ)2+L2mr4d2rdθ2{\displaystyle {\frac {L}{r^{2}}}{\frac {d}{d\theta }}\left({\frac {L}{mr^{2}}}{\frac {dr}{d\theta }}\right)=-{\frac {2L^{2}}{mr^{5}}}\left({\frac {dr}{d\theta }}\right)^{2}+{\frac {L^{2}}{mr^{4}}}{\frac {d^{2}r}{d\theta ^{2}}}}

This equation becomes quasilinear on making the change of variablesu1r{\displaystyle u\equiv {\frac {1}{r}}} and multiplying both sides bymr2L2{\displaystyle {\frac {mr^{2}}{L^{2}}}}

dudθ=1r2drdθ{\displaystyle {\frac {du}{d\theta }}={\frac {-1}{r^{2}}}{\frac {dr}{d\theta }}}
d2udθ2=2r3(drdθ)21r2d2rdθ2{\displaystyle {\frac {d^{2}u}{d\theta ^{2}}}={\frac {2}{r^{3}}}\left({\frac {dr}{d\theta }}\right)^{2}-{\frac {1}{r^{2}}}{\frac {d^{2}r}{d\theta ^{2}}}}

After substitution and rearrangement:

d2udθ2+u=mL2dduV(1u){\displaystyle {\frac {d^{2}u}{d\theta ^{2}}}+u=-{\frac {m}{L^{2}}}{\frac {d}{du}}V\left({\frac {1}{u}}\right)}

For an inverse-square force law such as thegravitational orelectrostatic potential, thescalar potential can be written

V(r)=kr=ku{\displaystyle V(\mathbf {r} )={\frac {k}{r}}=ku}

The orbitu(θ){\displaystyle u(\theta )} can be derived from the general equation

d2udθ2+u=mL2dduV(1u)=kmL2{\displaystyle {\frac {d^{2}u}{d\theta ^{2}}}+u=-{\frac {m}{L^{2}}}{\frac {d}{du}}V\left({\frac {1}{u}}\right)=-{\frac {km}{L^{2}}}}

whose solution is the constantkmL2{\displaystyle -{\frac {km}{L^{2}}}} plus a simple sinusoid

u1r=kmL2[1+ecos(θθ0)]{\displaystyle u\equiv {\frac {1}{r}}=-{\frac {km}{L^{2}}}\left[1+e\cos(\theta -\theta _{0})\right]}

wheree{\displaystyle e} (theeccentricity) andθ0{\displaystyle \theta _{0}} (thephase offset) are constants of integration.

This is the general formula for aconic section that has one focus at the origin;e=0{\displaystyle e=0} corresponds to acircle,e<1{\displaystyle e<1} corresponds to an ellipse,e=1{\displaystyle e=1} corresponds to aparabola, ande>1{\displaystyle e>1} corresponds to ahyperbola. The eccentricitye{\displaystyle e} is related to the totalenergyE{\displaystyle E} (cf. theLaplace–Runge–Lenz vector)

e=1+2EL2k2m{\displaystyle e={\sqrt {1+{\frac {2EL^{2}}{k^{2}m}}}}}

Comparing these formulae shows thatE<0{\displaystyle E<0} corresponds to an ellipse (all solutions which areclosed orbits are ellipses),E=0{\displaystyle E=0} corresponds to aparabola, andE>0{\displaystyle E>0} corresponds to ahyperbola. In particular,E=k2m2L2{\displaystyle E=-{\frac {k^{2}m}{2L^{2}}}} for perfectlycircular orbits (the central force exactly equals thecentripetal force requirement, which determines the required angular velocity for a given circular radius).

For a repulsive force (k > 0) onlye > 1 applies.

See also

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References

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  1. ^abcGoldstein, Herbert (1980).Classical mechanics. Addison-Wesley series in physics (2. ed.). Reading, Mass.:Addison-Wesley.ISBN 978-0-201-02969-7.
  2. ^Cooper, Leon N. (1981).An introduction to the meaning and structure of physics. Peleus Press.OCLC 15205048.
  3. ^Speiser, David (August 1996). "The Kepler Problem from Newton to Johann Bernoulli".Archive for History of Exact Sciences.50 (2):103–116.doi:10.1007/BF02327155.ISSN 0003-9519.
  4. ^Arnolʹd, V. I. (2009).Mathematical methods of classical mechanics. Graduate texts in mathematics (2. ed.). New York, NY:Springer. p. 38.ISBN 978-0-387-96890-2.
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