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Circular orbit

From Wikipedia, the free encyclopedia
Orbit with a fixed distance from the barycenter
For other uses of "orbit", seeOrbit (disambiguation).
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(April 2020)
Isaac Newton's Cannonball. Path C depicts a circular orbit.
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Acircular orbit is anorbit with a fixed distance around thebarycenter; that is, in the shape of acircle.In this case, not only the distance, but also the speed,angular speed,potential andkinetic energy are constant. There is noperiapsis or apoapsis. This orbit has noradial version.

Listed below is a circular orbit inastrodynamics orcelestial mechanics under standard assumptions. Here thecentripetal force is thegravitational force, and the axis mentioned above is the line through thecenter of the central massperpendicular to theorbital plane.

Circular acceleration

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Transverse acceleration (perpendicular to velocity) causes a change in direction. If it is constant in magnitude and changing in direction with the velocity,circular motion ensues. Taking two derivatives of the particle's coordinates concerning time gives thecentripetal acceleration

a=v2r=ω2r{\displaystyle a\,={\frac {v^{2}}{r}}\,={\omega ^{2}}{r}}

where:

The formula isdimensionless, describing a ratio true for all units of measure applied uniformly across the formula. If the numerical valuea{\displaystyle \mathbf {a} } is measured in meters per second squared, then the numerical valuesv{\displaystyle v\,} will be in meters per second,r{\displaystyle r\,} in meters, andω {\displaystyle \omega \ } in radians per second.

Velocity

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The speed (or the magnitude of velocity) relative to the centre of mass is constant:[1]: 30 

v=GMr=μr{\displaystyle v={\sqrt {GM\! \over {r}}}={\sqrt {\mu \over {r}}}}

where:

Equation of motion

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Theorbit equation in polar coordinates, which in general givesr in terms ofθ, reduces to:[clarification needed][citation needed]

r=h2μ{\displaystyle r={{h^{2}} \over {\mu }}}

where:

This is becauseμ=rv2{\displaystyle \mu =rv^{2}}

Angular speed and orbital period

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ω2r3=μ{\displaystyle \omega ^{2}r^{3}=\mu }

Hence theorbital period (T{\displaystyle T\,\!}) can be computed as:[1]: 28 

T=2πr3μ{\displaystyle T=2\pi {\sqrt {r^{3} \over {\mu }}}}

Compare two proportional quantities, thefree-fall time (time to fall to a point mass from rest)

Tff=π22r3μ{\displaystyle T_{\text{ff}}={\frac {\pi }{2{\sqrt {2}}}}{\sqrt {r^{3} \over {\mu }}}} (17.7% of the orbital period in a circular orbit)

and the time to fall to a point mass in aradial parabolic orbit

Tpar=23r3μ{\displaystyle T_{\text{par}}={\frac {\sqrt {2}}{3}}{\sqrt {r^{3} \over {\mu }}}} (7.5% of the orbital period in a circular orbit)

The fact that the formulas only differ by a constant factor is a priori clear fromdimensional analysis.[citation needed]

Energy

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A circular orbit is depicted in the top-left quadrant of this diagram, where thegravitational potential well of the central mass shows potential energy, and the kinetic energy of the orbital speed is shown in red. The height of the kinetic energy remains constant throughout the constant speed circular orbit.

Thespecific orbital energy (ϵ{\displaystyle \epsilon \,}) is negative, and

ϵ=v22{\displaystyle \epsilon =-{v^{2} \over {2}}}
ϵ=μ2r{\displaystyle \epsilon =-{\mu \over {2r}}}

Thus thevirial theorem[1]: 72  applies even without taking a time-average:[citation needed]

  • the kinetic energy of the system is equal to the absolute value of the total energy
  • the potential energy of the system is equal to twice the total energy

Theescape velocity from any distance is2 times the speed in a circular orbit at that distance: the kinetic energy is twice as much, hence the total energy is zero.[citation needed]

Delta-v to reach a circular orbit

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Maneuvering into a large circular orbit, e.g. ageostationary orbit, requires a largerdelta-v than anescape orbit, although the latter implies getting arbitrarily far away and having more energy than needed for theorbital speed of the circular orbit. It is also a matter of maneuvering into the orbit. See alsoHohmann transfer orbit.

Orbital velocity in general relativity

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InSchwarzschild metric, the orbital velocity for a circular orbit with radiusr{\displaystyle r} is given by the following formula:

v=GMrrS{\displaystyle v={\sqrt {\frac {GM}{r-r_{S}}}}}

whererS=2GMc2{\displaystyle \scriptstyle r_{S}={\frac {2GM}{c^{2}}}} is the Schwarzschild radius of the central body.

Derivation

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For the sake of convenience, the derivation will be written in units in whichc=G=1{\displaystyle \scriptstyle c=G=1}.

Thefour-velocity of a body on a circular orbit is given by:

uμ=(t˙,0,0,ϕ˙){\displaystyle u^{\mu }=({\dot {t}},0,0,{\dot {\phi }})}

(r{\displaystyle \scriptstyle r} is constant on a circular orbit, and the coordinates can be chosen so thatθ=π2{\displaystyle \scriptstyle \theta ={\frac {\pi }{2}}}). The dot above a variable denotes derivation with respect to proper timeτ{\displaystyle \scriptstyle \tau }.

For a massive particle, the components of thefour-velocity satisfy the following equation:

(12Mr)t˙2r2ϕ˙2=1{\displaystyle \left(1-{\frac {2M}{r}}\right){\dot {t}}^{2}-r^{2}{\dot {\phi }}^{2}=1}

We use the geodesic equation:

x¨μ+Γνσμx˙νx˙σ=0{\displaystyle {\ddot {x}}^{\mu }+\Gamma _{\nu \sigma }^{\mu }{\dot {x}}^{\nu }{\dot {x}}^{\sigma }=0}

The only nontrivial equation is the one forμ=r{\displaystyle \scriptstyle \mu =r}. It gives:

Mr2(12Mr)t˙2r(12Mr)ϕ˙2=0{\displaystyle {\frac {M}{r^{2}}}\left(1-{\frac {2M}{r}}\right){\dot {t}}^{2}-r\left(1-{\frac {2M}{r}}\right){\dot {\phi }}^{2}=0}

From this, we get:

ϕ˙2=Mr3t˙2{\displaystyle {\dot {\phi }}^{2}={\frac {M}{r^{3}}}{\dot {t}}^{2}}

Substituting this into the equation for a massive particle gives:

(12Mr)t˙2Mrt˙2=1{\displaystyle \left(1-{\frac {2M}{r}}\right){\dot {t}}^{2}-{\frac {M}{r}}{\dot {t}}^{2}=1}

Hence:

t˙2=rr3M{\displaystyle {\dot {t}}^{2}={\frac {r}{r-3M}}}

Assume we have an observer at radiusr{\displaystyle \scriptstyle r}, who is not moving with respect to the central body, that is, theirfour-velocity is proportional to the vectort{\displaystyle \scriptstyle \partial _{t}}. The normalization condition implies that it is equal to:

vμ=(rr2M,0,0,0){\displaystyle v^{\mu }=\left({\sqrt {\frac {r}{r-2M}}},0,0,0\right)}

Thedot product of thefour-velocities of the observer and the orbiting body equals the gamma factor for the orbiting body relative to the observer, hence:

γ=gμνuμvν=(12Mr)rr3Mrr2M=r2Mr3M{\displaystyle \gamma =g_{\mu \nu }u^{\mu }v^{\nu }=\left(1-{\frac {2M}{r}}\right){\sqrt {\frac {r}{r-3M}}}{\sqrt {\frac {r}{r-2M}}}={\sqrt {\frac {r-2M}{r-3M}}}}

This gives thevelocity:

v=Mr2M{\displaystyle v={\sqrt {\frac {M}{r-2M}}}}

Or, in SI units:

v=GMrrS{\displaystyle v={\sqrt {\frac {GM}{r-r_{S}}}}}
At the top of the diagram, a satellite in a clockwise circular orbit (yellow spot) launches objects of negligible mass:
(1 - blue) towards Earth,
(2 - red) away from Earth,
(3 - grey) in the direction of travel, and
(4 - black) backwards in the direction of travel.

Dashed ellipses are orbits relative to Earth. Solid curves are perturbations relative to the satellite: in one orbit, (1) and (2) return to the satellite having made a clockwise loop on either side of the satellite. Unintuitively, (3) spirals farther and farther behind whereas (4) spirals ahead.

See also

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References

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  1. ^abcLissauer, Jack J.; de Pater, Imke (2019).Fundamental Planetary Sciences : physics, chemistry, and habitability. New York, NY, USA: Cambridge University Press. p. 604.ISBN 9781108411981.
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