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    Central-forces perturbations of conical orbits

    Maurizio M. DEliseo

    Osservatorio S.Elmo - Via A.Caccavello 22, 80129 Napoli Italy

    The relativistic precession of a planetary orbit is treated from the point of view of the analyticgeometry of a conic on the plane.

    I. THE UNPERTURBED ORBIT

    We need the vectorial expression of the conic describedby an unperturbed planet (considered as a test-body)around a star located at the origin. If we let r = r r be the position vector, where r = r r , we have therst-order system

    dr dt

    = v , (1)

    dv dt

    = r 2

    r , (2)

    where = GM is the standard gravitational parameterof the star. Operating on Eq. (2) by r , we get

    r dv dt

    =ddt

    (r v ) =

    r 2r r = 0 , (3)

    and integrating,

    r v = h = const . (4)Since

    (r v ) r = 0 , (5)the motion takes place in the plane h r = 0. We willmatch this plane with the xy-plane. By considering theinnitesimal triangle formed by the vectors r and dr , wesee that |r v | is twice the area swept out by the radiusvector per unit time. In polar coordinates, twice the areaof the triangle swept out in time dt and per unit time arerespectively

    r ( r d), r 2 , (6)

    so we have

    h = h h = r 2 h . (7)

    To get the orbit, we need one more integral of motion:the Laplace integral. We consider the time derivative of the cross product

    ddt

    (v h ) =dv dt h =

    hr 2

    r h = = dr dt

    , (8)

    which may be integrated to give the Laplace integral

    e = v h r , (9)where e is a constant vector. The factor is needed toget a natural geometric interpretation for e , namely that

    being the eccentricity vector, directed toward the perihe-lion, and whose length is the usual scalar eccentricity e.The eccentricity vector is situated, as one can see, in theplane of motion. So, we have constantly a closed vectortriangle formed by the variable vectors v h , r andthe constant vector e . The orbit is obtained dottingEq. (9) with r

    e r = ( v h ) r r , (10)but

    r (v h ) = ( r v ) h = h h = h2 ,

    and so we get

    h h

    = r r + e r . (11)h 2

    = r + er cos( ). (12)

    where we have assumed as reference direction for anglesthe positive x-axis, and denoted with the xed angleformed by e . Equation (12) is the polar expression of themagnitude of the radius vector from which, comparingwith the polar equation of a conic, we deduce that h 2 =a(1

    e2 ), being a the semimajor axis of the orbit. We

    will assume that e < 0, that is the conic is an ellipse.Notice, in particular, that r is comprised between

    a(1 e) r a(1 + e), (13)and that the minimum occurs at the point of orbit when = .

    II. THE PERTURBED ORBIT

    We study now the effects of a perturbing force f whenthe test body is initially moving on a conic described byEq. (11). The method of variation of the arbitrary con-stants assumes that the motion happens always on anorbit of the same type, but whose constants h, e slowlyvary in time in a form depending from the nature of theperturbing force. The problem is thus shifted from thesolution of the unperturbed equation of motion to thesolution of the differential equations related to these un-known functions. The values they assume at each instantt identify the osculating orbit, that is the orbit the planetwould follow if the perturbing force in this same instantwas put equal to zero. From the point of view of the dif-ferential equation of motion, the values of r (t) and r (t)

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    at a particular instant t can be seen as the initial valuesof the unperturbed conic the body would follow, and sor and r are the same at any time for the two paths, thereal and the elliptical. Only the second derivative willreveal the presence of the disturbing force. We introduceso a derivative operator /dt with the property that

    r

    dt = 0

    v

    dt =f

    , (14)and, consequently, we have also

    r dt

    = 0 ,r dt

    = 0 . (15)

    Let rst submit h to the action of this operator. Wehave, by Eq. (11)

    hdt

    =dt

    (r v ) = r v dt

    = r f (16)After we have, by Eq. (9)

    edt

    =1

    v dt h + v

    hdt

    =1

    f h + v hdt

    .

    If the the perturbing force is central, that is of the typef = f ( r ) r , we have

    hdt

    = r f = f (r r ) = 0 , (17)edt

    =fh

    ( r h ) = . (18)

    A consequence of Eq.() is that

    2

    dt= 2

    dt

    = 0 , (19)

    2

    dt=

    dt

    [a(1 e2 )] = (1 e

    2 )adt 2ae

    edt

    = 0 ,(20)

    and by separating the variables

    a

    adt

    =2e

    1 e2edt

    = h (21)

    where h is a constant. Now, a and e are two independentconstants in the unperturbed motion so, for continuityreasons, we can put h = 0.

    We will suppose f ( r ) to be of the form

    f ( r ) = k

    r 5(22)

    III. THE VARIABLE PHASE

    To nd higher order corrections to the relativistic pre-cession formula, we must nd more and more approx-imate solutions to the Eq. ( ?? ), expressing bound pe-riodical motions. Equation ( ?? ) indicates two possiblealternative on the method one can follow to achieve thisresult. We can act by searching the frequency or thephase variations. The study of the phase is more sim-ple, because it leads directly to the perihelion formulawithout the need of any nal transformation.

    Electronic address: [email protected] M. M. DEliseo, The rst-order orbital equation, Am. J.

    Phys. 75 , 352 (2007),2 A. dInverno, Introducing Einsteins Relativity , Oxford Uni-

    verity Press, Oxford, 1992.

    3 A. H. Nayfeh, Perturbation Methods , Interscience, NewYork, 1973.

    4 J.Kevorkian, J. D. Cole, Perturbation Methods in Applied Mathematics Springer-Verlag, New York, 1981.