Problem: Pluto + Charon orbiting the sun This three body system is interesting because the orbital plane of PlutoCharon is nearly perpendicular to the orbital plane of the P-C center of mass (COM) with the sun. Here to make the calculations simpler, we will assume that the two orbital planes are exactly orthogonal. Kinetic Energy First, we will easily take care of the kinetic energy for this three body system. We start by writing the kinetic energy as the sum of the kinetic energies of the sun, Pluto, and Charon in some inertial frame external to the three bodies. Then, following the same procedure used in Ch. 3, the kinetic energy of Pluto + Charon can be rewritten as the sum of the P-C COM kinetic energy and the P-C kinetic energy relative to its local COM: = + + (1) We then note that the sun and the P-C COM form a separate two-body system whose kinetic energy can similarly be decomposed into a COM piece and a relative piece. The contribution for the three-body COM can be neglected because it is simply an additive constant (no net force acts on this COM), and the physically relevant kinetic energy is, thus, just the sum of the two relative kinetic energies, which we can write using plane polar coordinates for the two separate two body systems. We use and Θ for the sun-PC COM coordinate system and and for the PC system. Here, as shown in the figure, is the radial separation of the sun and the PC COM and is the radial distance between P and C, = |r02 − r01 |. Also in the figure, is the mass of the sun, 1 is Pluto’s mass, and 2 is Charon’s mass. . m1 r1/ R1 . M R r2/ . R2 m2 Fig. 1. Position vectors and masses for the Pluto-Charon-sun system. The kinetic energy is thus given as the sum, ·2 ·2 M ·2 ·2 ( + 2 Θ ) + ( + 2 ) 2 2 where M is the reduced mass of the sun-PC COM system, = M= + 1 (2) (3) with = 1 + 2 , and is the reduced mass of the PC system, = 1 2 1 + 2 (4) Potential energy The potential energy requires more work to put it into a useable form. We start by writing the exact gravitational potential as =− 1 2 1 2 − − 1 2 (5) where 1 and 2 are defined in the figure. Now, we note from the figure, the following vector identity R = R + r0 (6) from which it follows that = q 2 + 02 (7) after noting that R · r0 = 0 because of the assumed orthogonality of the two orbital planes. Next, we take advantage of the huge disparity in size between and 0 to expand −1 to first order, thereby obtaining the excellent approximation, −1 = −1 (1 − 02 (22 )) (8) After substituting Eq.(8) into Eq.(5), the first two terms of that equation, which we will temporarily refer to as , reduce to = − (1 102 + 2 202 ) + 23 (9) Next, we know from our analysis of the two body problem that 0 = (10) 2 + 23 (11) which allows us to simplify as = − and the total potential then becomes =− 1 2 2 − + 23 (12) It is interesting to note that the central term in this approximate form is repulsive for the motion, but is attractive (Hooke’s law potential, ∼ 2 ) for the relative PC motion. This will have important consequences for the orbital motion of the PC system. 2 (I) EOM for the sun-PC COM system Let us first analyze the relative motion of the sun-PC COM system. Skipping the details, the equation of motion for the one-dimensional radial problem is easy to find as ·· 2 M = () = − (13) + M3 M · where M is the constant angular momentum, M = M2 Θ. The perturbative simplification of is seen to give rise to a 1-3 potential is defined as () = − 1 2 2 + 23 (14) where 1 and 2 are positive constants, 1 = (15) 2 = (16) and With 2 = 0, we recover the unperturbed Kepler problem. Given how small is, the repulsive −3 term is a very small perturbation to the pure Kepler potential. Because is so small, any variations in for typical PC orbits will also be small compared to , and we may safely regard as a constant in this part of the problem. The radial equation of motion can be written explicitly as ·· M = () = − 1 2 0 + 4 + M3 = − 2 M (17) where is just another constant, = 32 2 2 (18) 0 and is the effective potential for this problem, 0 = () + 2 M 2M2 (19) (Ia) Circular Orbits: The circular orbit condition is that the effective 0 ( ) ] = 0, where is force must vanish when = , ( ) = −[ the radius of the circular orbit, ( ) = − 2 1 M + + = 0 2 4 M3 (20) This equation can be simplified and solved as follows. First, introduce a scaled radial coordinate = 0 (21) 3 where 0 is the radius of the circular orbit when = 0, 2 M1 0 = M (22) −3 − −2 + −4 = 0 (23) Then Eq.(20) reduces to where is the positive, dimensionless constant = (1 02 ) (24) Then, after multiplying Eq.(23) by 4 , we obtain a quadratic equation for the variable , 2 − − = 0 (25) with a solution given by the quadratic formula √ 2 = 1 + 1 + 4 (26) Because ≥ 0, a positive root is possible only for by choosing the positve sign for the square root. (Ib) Period of Circular Motion: From conservation of angular momentum for the circular orbit, we have M = M2 (27) where is the frequency of circular motion. The definition of is = 2 , from which, with the help of Eqs.(20) and (27), we find 1 1 = 2M2 M = 2M2 (M1 − M ) 2 = 0 [5 (2 − )] 2 (28) where 0 is the period of the circular orbit with = 0 1 0 = 2(M1 ) 2 (0 )32 (29) Two other forms for the answer are found by using Eq.(25)) to replace 2 − with to get = 0 2 = 0 ( + ) (30) The latter form follows from the use of Eq. (25) to replace 2 with + . (Ic) Period of Small Oscillations: The oscillation frequency of the slightly perturbed orbit is defined as 2 = −(1M)( ())|= (31) ¸ ¸ ∙ 2 ∙ 3M 1 21 4 1 1 − 3 + 5 = + = M M4 M 3 5 (32) It follows that 2 4 2 after substituting for M from the circular orbit condition, Eq.(20). For , we have ∙ ¸ 12 5 2 (33) = = 0 2 + using Eqs.(32), (21), (24), and (29) . For stable circular orbits, 2 0, and this is manifestly true here. Taking the ratio of Eqs.(33) and (28) yields ∙ 2 ¸1 − 2 = 2 + (34) and using Eq.(25) to replace 2 we also have ∙ ¸ 12 = + 2 (35) (Id) Precession of the stable perturbed orbits: The form of Eq.(35) implies that for all stable circular orbits. Because of this, the precession is in the opposite direction as the orbital motion. (Ie)Plot of the effective radial potential for V(R) = V 0 As defined by Eqs.(14), (18), and (19), is the effective potential for this problem, 1 2 0 () = − + + M 2 (36) 3 3 2M To discuss the qualitative nature of the motion, we need to make a plot of 0 M versus . It will be convenient to introduce a scaled radial coordinate = 0 , where 0 is the radius of the circular orbit when = 0, 2 0 = M M1 This allows us to write 0 1 1 M = − e () = + 2 1 0 2 3 3 (37) where is the positive constant = 1 02 We saw earlier that all positive values of were allowed. To illustrate these possibilities, the dimensionless potential of Eq.(37) is shown for = 1800. Note that even this tiny value is probably unrealistically large for the PC-sun system. The -axis corresponds to e (). 5 y 2 1 0 1 2 3 x -1 Fig. 2. Effective potential for the sun-PC COM system with =1/800. p There is an attractive well with a minimum at = (1 + 210200)2 ≈ 10012, where a stable circular orbit is possible. When 0 , only unbound scattering orbits are possible. When 0, bound, but generally unclosed orbits are possible in the shallow potential well. (II) EOM for the perturbed PC system Now we analyze the relative motion for the PC system. Notice that the relevant part of the potential for this problem consists of the second and third terms of Eq.(12), so we are treating a Keplerian potential with a Hooke’s law perturbation. (IIa) Again skipping the details, the equation of motion for the one-dimensional radial problem is 2 ·· = () = − (38) + 3 with the potential defined as () = − 3 + 2 2 (39) where 3 is the gravitational force constant, is the Hooke’s law force constant, · is the constant angular momentum, 2 , and is the reduced mass of the two particle system. For the PC-sun system, 3 and are defined as 3 = 1 2 (40) and (41) 3 Although varies inversely with 3 , we may regard as a constant for this part of problem because on the timescale of motion for the PC pair, will be changing very slowly. The radial equation can be written explicitly as = ·· = () = − 3 2 0 − + = − 2 3 6 (42) where 0 is the effective potential for this problem, 0 = () + 2 22 (43) To make a sketch of 0 versus it will be convenient to introduce a scaled radial coordinate = 0 , where 0 is the radius of the circular orbit when =0 2 0 = (44) This allows us to write 2 0 0 1 1 e () = = 2 + − 2 2 where is the small positive constant = (45) 03 3 (46) To illustrate these possibilities, the dimensionless potential of Eq.(45) is shown below for three values of , 0, 0.1, and 0.01. The -axis corresponds to e (). All curves are nearly the same at small values of , but differences emerge at larger values of . The bottom curve is for the pure Kepler problem with = 0. The curve that crosses the axis at ≈ 77 corresponds to = 0002. The curve will rise monotonically as increases, so the effect of the perturbative term is to make all orbits bound. The curve that crosses the axis at ≈ 25 corresponds to = 01. This is probably too big a value of to be considered a small perturbation, but you can see how much the potential well is narrowed compared to the original effective Kepler potential. Even the value = 0002 is probably far too large for the PC system. y 0.4 0.2 0.0 1 2 3 4 5 6 7 8 9 10 x -0.2 -0.4 Fig. 3. Effective potential for the PC system with = 0, 0.002, and 0.1 (b)To find the period for a circular orbit with nonzero values of , we first consider the condition that the effective force should vanish, ( ) = − 2 − + =0 2 3 7 (47) where is the radius of the circular orbit. It follows that 2 = + 4 (48) The period follows from the conservation of angular momentum for the circular orbit · (49) = = 2 so that with Eq(48) we have 2 = 1 ( + 3 ) 3 (50) s (51) The period is 2 = 2 = 3 + 3 (c) To find the period of a slightly noncircular orbit, we substitute = + (52) into the EOM, Eq.(38) or (42), and expand the effective force in a Taylor series in the small parameter . The result is ∙ ¸ () ·· = ( ) + + ··· (53) = where, of course, ( ) = 0 and ∙ ¸ () 2 32 = 3 − − 4 = −( 3 + 4) = (54) after substituting for 2 using Eq.(48). To first order terms in we can write Eq.(53) as ·· = − 2 (55) where the orbital frequency can be put in the form 2 = ¢ 1 ¡ 3 + 43 = 2 + 3 after using Eq.(50). Since = , we have s s 3 + 43 = = 1+ 2 + 3 (56) (57) The square root definitely exceeds 1, so that 8 (58) This implies that the perturbed orbit will generally precess. · (d) To find the direction of precession, we integrate = 2 . For a slightly · noncircular orbit, because is very small, can be well approximated as , · = = 2 (1 − 2 + · · · ) ' 2 (59) We may, thus, integrate Eq.(59) over the difference in the periods of the circular and noncircular orbit to obtain the angular displacement of the noncircular orbit per revolution as µ ¶ ∆ = ( − ) = 2 −1 (60) Because ∆ is negative, the precession will be opposite (or clockwise) to the direction of the orbital motion. 9
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