The Disturbing Function in Solar System Dynamics

Size: px
Start display at page:

Download "The Disturbing Function in Solar System Dynamics"

Transcription

1 Icarus 4, 9 44 (000) doi:0.006/icar , available online at on The Disturbing Function in Solar System Dynamics Keren M. Ellis and Carl D. Murray Astronomy Unit, Queen Mary and Westfield College, University of London, Mile End Road, London E 4NS, UK c.d.murray@qmw.ac.uk Received June, 995; revised February 8, 000 The planetary disturbing function is the basis of much analytical work in Solar System dynamics and series expansions of it that were derived in the last century are still in common use today. However, most previous expansions have the disadvantage of being in terms of the mutual inclination of the two masses. Also, several of the classical, high-order expansions contain a number of errors. A new algorithm for the derivation of the disturbing function in terms of the individual orbital elements of the two masses is presented. It allows the calculation, to any order, of the terms associated with any individual argument without the need for expanding the entire disturbing function. The algorithm is used to generate a new expansion which is complete to fourth-order in the eccentricities and inclinations, and incorporates a consistent numbering system for each argument. The properties of the expansion for a selected argument are discussed, and the use of the expansion is illustrated using the examples of the Titan Hyperion :4 resonance and the possible Jupiter Pallas 8: resonance. c 000 Academic Press Key Words: celestial mechanics; orbits; resonances.. INTRODUCTION The Solar System is not just a collection of objects moving in arbitrary orbits. It has an intricate dynamical structure that has evolved over time. To understand the structure and evolution of the Solar System we must understand the consequences of Newton s universal law of gravitation. To do this we must understand the properties of the perturbing potential experienced by one object due to another; this is also known as the planetary disturbing function. Despite its importance for planetary science, guidance on the properties and practical use of the disturbing function can only be found in the specialist literature on celestial mechanics. Our own experience is that when the disturbing function is encountered, many authors give resonant arguments and simply state that the terms in the semimajor axis are of order unity. Typically a reference is given to a textbook on celestial mechanics without any way of knowing which particular arguments are being considered. Invariably these texts fail to provide a clear presentation, even allowing for inconsistencies in their approach and their use of a mutual inclination. In an era when, for example, the locations of resonant structures in planetary rings can be determined to within km, it seems unusual that there is no consistent approach to the use of the disturbing function given that, effectively, it determines the location of the resonant feature. Our discovery of a new algorithm to facilitate the derivation of the terms associated with an explicit argument and its subsequent application to the generation of a fourth-order expansion makes it appropriate to combine the two by writing a paper incorporating these results in a form suitable for a nonspecialist readership. Therefore the aims of this paper are (i) to present an efficient algorithm to calculate the terms associated with a given argument and (ii) to present a completely new expansion of the disturbing function in a systematic form together with examples of its use. In this section we provide some basic definitions and an outline of previous work on the disturbing function. Consider a mass m orbiting a primary of mass M c in an elliptical path. Let the orbiting mass have position vector r relative to M c and assume that the gravitational effect of the primary arises from a point mass (see Fig. ). This problem is integrable and the orbital elements a, e, I, ϖ, and, which denote semimajor axis, eccentricity, inclination, longitude of pericenter, and longitude of ascending node, respectively, of the mass m are constant. Consider now a third mass, m, with position vector r relative to M c and orbital elements a, e, I, ϖ, and. Assume r < r always. The mutual gravitational force between the two orbiting masses m and m results in accelerations in addition to the standard two-body accelerations due to M c (see Fig. ). These additional accelerations of the secondary masses with respect to the primary can be obtained from the gradient of the disturbing function. The equations of motion of the two orbiting masses can be written as where r = (U+R) and r = (U +R ), () U = G (M c + m) r and U = G (M c + m ) r () are the central, or two-body parts of the total potential and it is understood that the and operators denote that the gradient is with respect to the coordinates of the mass m and m, /00 $5.00 Copyright c 000 by Academic Press All rights of reproduction in any form reserved.

2 0 ELLIS AND MURRAY The j i are all integers, and λ and λ denote the mean longitudes of each mass. We define the order of the argument as N = j +j. (8) FIG.. The position vectors, r and r of the two masses m and m with respect to the central mass M c. The angle between the position vectors is ψ. respectively. The R and R terms in Eq. () are the disturbing functions which represent the potentials arising from the gravitational effects of the external and internal masses respectively. These are given by R = R = Gm r r r Gm () r r Gm r r Gm r r r. (4) The first term in each of these expressions is called the direct term while the second term, which arises from the choice of the origin of the coordinate system, is called the indirect term. If the origin of the coordinate system is at the center of mass, then there are no indirect terms. At this stage we should point out one peculiarity of the disturbing function as used throughout this paper. The equation for the perturbing force is written as F = Rrather than the more usual F = R, because R is actually the negative of the true potential. This is an historical quirk and has no effect on the inherent dynamics of the system. It is clear that it is a trivial task to write R and R in terms of the standard cartesian coordinates of each orbiting mass. The cartesian equations of motion of the inner perturbed body can be written in terms of the gradient of U and R as in Eq. () and numerical techniques can be used to study the orbit. However, in many problems it is often more useful to consider the variation of the orbital elements of the perturbed body with time. Hence we must express the relevant disturbing function in terms of the orbital elements of each body. Such an expansion is achieved by expanding R or R as infinite series of the form and R = µ S(a, a, e, e, I, I ) cos φ (5) R = µ S (a, a, e, e, I, I ) cos φ, (6) where µ = Gm, µ = Gm, and φ = j λ + j λ + j ϖ + j 4 ϖ + j 5 + j 6. () As we shall see in Sect. below, the value of N is the same as the lowest power of e, e, I, and I that occurs in S or S. Thus, when we refer to an Nth-order expansion we mean an expansion that includes all possible arguments up to and including order N, together with the corresponding terms in powers of the eccentricities or inclinations up to and including the N th power. The literature on the disturbing function has a distinguished history. The first paper to be published in the Astronomical Journal contained the start of a sixth-order expansion by Peirce (849). Le Verrier (855) produced a seventh-order expansion which was subsequently extended to eighth-order by Boquet (889). Newcomb (895) carried out work on a seventh-order expansion, while Norén and Wallberg (899) produced a secondorder expansion in canonical elements. Brown and Shook (9) gave a clear derivation of the expansion to second-order in the keplerian orbital elements. In more recent times the expansion contained in Brouwer and Clemence (96) has become widely adopted as a standard, low-order expansion; it is complete to third-order in all terms but contains some fourth-order terms associated with particular arguments. In the expressions for S and S in Eqs. (5) and (6) in each of these expansions the dependence on a and a is given by means of Laplace coefficients (functions of α = a/a ) and their derivatives (see, for example, Brouwer and Clemence 96 and Sect. below). The compact notation afforded by the use of Laplace coefficients means that they can be handled easily in calculations involving the disturbing function. Another common but undesirable characteristic of all of these expansions is the use of angles referred to the mutual node of the orbiting masses, and the mutual inclination, J, of the orbits given by cos J = cos I cos I + sin I sin I cos( ). (9) This has the advantage of making the resulting size of the expansions more manageable, but it has the disadvantage of making studies of the effect of perturbations on individual inclinations or nodes more difficult. As well as their consistent use of a mutual inclination there is a more serious drawback to some of these expansions they contain errors. Most are typographical mistakes that are easy to identify and correct. For example, following the publication of the expansion by Le Verrier (855), several editions of the Annales de l Observatoire de Paris contained corrections to Le Verrier s original text. Murray (985) pointed out a single sign error in Le Verrier s work that had not been corrected. The early printings of Brouwer and Clemence (96) contained errors in the expansion that were corrected only with the third printing in 9.

3 DISTURBING FUNCTION Using mathematical techniques from geophysics and artificial satellite theory, Kaula (96) developed a form of the expansions using Legendre polynomials. This form of the expansion had the advantage that one could specify an argument of interest, φ say, and then isolate only those terms associated with that particular argument, avoiding the need to carry out a complete expansion. Another advantage was that because the dependence on e, e, I, and I was given in the form of explicit functions, expansions to any order could be generated for the terms associated with any particular argument. This made Kaula s expansion ideal for use in a number of fields (see, for example, Allan 969, 90, Murray 98, Dermott and Murray 98). However, one disadvantage of Kaula s work was the absence of Laplace coefficients the dependence on a and a appeared as a summation in powers of α and reduced the compactness and ease of use of the expansion. It is important to recognize that the classical expansions of the last century are still in use today. For example, Goldreich and Nicholson (9) used the expansion by Peirce (849), while Wisdom (98), Murray (986), and Šidlichovský and Melendo (986) all used the expansion by Le Verrier (855) in their work on algebraic mappings for asteroid motion at resonance. In one of the first applications of computer algebra to celestial mechanics Deprit et al. (9) discovered mistakes in Delaunay s lunar theory. Since then a number of authors have developed their own software packages for the development of series (see the review by Henrard 989). For example, Broucke and Smith (9) (and the references therein) describe a technique for computing the expansion of the disturbing function. Brumberg (995) made use of a generic Poisson series processor to show how the disturbing function can be expanded; similar methods were employed by Laskar (99) using Poincaré variables. The need for correct, higher-order expansions and the ability to perform complicated, error-free series manipulation by computer, led Murray and Harper (99) to generate an eighth-order expansion of the disturbing function in the individual orbital elements. The expansion was first produced using Mathematica (Wolfram 99) and written as a file of integers that was then compared with a similar file produced independently using Maple. As a final check the expansion was compared with Kaula s form of the expansion for a large number of explicit cases. Details of the derivation are given in Harper and Murray (994). Our own experience suggests that many members of the Solar System dynamics community find the existing forms of the expansion difficult to derive and use. Therefore one of the goals of this paper is to present a new algorithm for the determination of the terms associated with a given argument in the expansion of the planetary disturbing function. This obviates the need for a complete series expansion involving all arguments up to and including a specified order. The expressions for each term involve e, e, I, and I (instead of the mutual inclination, J )as well as explicit Laplace coefficients (instead of infinite series in the ratio of the semimajor axes) and can be calculated up to any desired power of the eccentricities and inclinations. We present the algorithm in the next section and in Section we provide detailed information on the properties of the expansion. In Section 4 we illustrate the use of the expansion by giving examples of how the appropriate terms are calculated for two specific cases in Solar System dynamics. A complete fourthorder expansion of the direct and indirect parts of the disturbing function is given in the Appendix; each argument in this expansion has been given a unique identification number for ease of reference. Some of the concepts and results developed in this paper, including the fourth-order expansion are made use of by Murray and Dermott (999) where the disturbing function and its properties are examined in some detail. Murray and Dermott also derive an expansion (from first principles) of the disturbing function complete to second-order in the individual elements, and provide several analytical and numerical comparisons.. EXPANSION OF THE DISTURBING FUNCTION It is unlikely that anyone making use of the planetary disturbing function requires all the arguments in the expansion; in practice the terms associated with only a few arguments are required. Therefore, although we give a complete fourth-order expansion in the Appendix for reference purposes, our primary objective is to produce a new form of the expansion which retains the advantages of Kaula s (96) approach but expressed in terms of Laplace coefficients and their derivatives. Full details of the procedure for accomplishing this new derivation will be published elsewhere (K. Ellis, in preparation). Here we confine ourselves to giving the explicit form of the series. From Eqs. () and (4) it is clear that we can write the disturbing function due to an external perturber as R = µ a (R D + αr E ) (0) and that due to an internal perturber as R = µ ( αr D + ) a α R I, () where α = a/a is the ratio of the semimajor axes of the two orbits, and µ = Gm, µ = Gm. The direct part in both cases is given by R D = a, () with = r + r rr cos ψ. Since r r = rr cos ψ, () where ψ is the angle between the two position vectors (see Fig. ), we have R E = r a a cos ψ (4) r

4 ELLIS AND MURRAY for the indirect part in the case of an external perturber and R I = r a cos ψ (5) a r for the indirect part in the case of an internal perturber. We find that the series for the direct part, R D is given by (i)! ( ) i R D = αi i! i+ i=0 { + ( ) l l ( } l )( ) k α l dl j) b( (α) l! k dαl i+ j= i i s s=0 l=0 s n m=0 + q,q = l=0 k=0 ( ) s s [s/] (s 4n + )(s n)! (i s l)! l! n=0 n n!(s n + )! κ m (s n m)! (s n + m)! X s n p,p =0 i+k, i+ j l n p i+ j l n p+q F s n,m,p (I ) F s n,m,p (I ) (e) X (i+k+), i+ j l n p i+ j l n p +q (e ) cos[(i + j l n p + q )λ (i + j l n p + q)λ q ϖ + qϖ + (m s + n + p ) (m s + n + p) ], (6) where κ m = ifm=0 and κ m = ifm>0. The series for the indirect parts, R E and R I are given by R E = and R I = m=0 κ m ( m)! ( + m)! + q,q = p,p =0 F,m,p (I ) F,m,p (I ) X, p, p p+q (e) X p +q (e ) cos[( p + q )λ ( p + q)λ q ϖ + qϖ ( p m) + ( p m) ] () m=0 κ m ( m)! ( + m)! + q,q = p,p =0 F,m,p (I ) F,m,p (I ) X, p, p p+q (e) X p +q (e ) cos[( p + q )λ ( p + q)λ q ϖ + qϖ ( p m) + ( p m) ]. (8) In the expression for R D the coefficients b ( j) (α) are Laplace i+ coefficients (see, for example, Brouwer and Clemence 96) given by j) b( s (α) = π π 0 cos jϕ dϕ ( α cos ϕ + α ) s, (9) where s is a half integer. They can also be written in series form as j) b( s (α) = [ s(s + ) (s+ j ) α j s(s+ j) + j ( j + ) α ] + s(s + )(s + j)(s + j + ) α 4 + ( j + )( j + ) (0) or, equivalently in terms of elliptical integrals or hypergeometric functions. In the special case where j = 0 the factor outside the brackets in Eq. (0) is equal to unity. It can be shown that the series forms of the Laplace coefficient and its derivatives are always convergent for α<. Note that there are no Laplace coefficients in R E and R I. The functions of inclination in all three expressions are defined by F s n,m,p (I ) = s n (s n)! min(p,[(s n m)/]) t=0 sin s n m t I ( ) (s 4n t)! s n (s n m t)! t m ( ) m cos g I g s n t g=0 min(p t,s n m t+g) c=max(0,p t m+g) ( ) s n m t + g c ( ) m g ( ) c [(s n m)/], () p t c where s n = inr E and R I and the square brackets denote the integer part of the enclosed expression. The functions of eccentricity, Xc a,b (e), in all three expressions are Hansen coefficients (see, for example, Plummer 98, Jarnigan 965, and Hughes 98) which are defined by X a,b c (e) = e c b σ =0 X a,b σ +α,σ +β eσ, () where, in this context, α = max(0, c b), β = max(0, b c), and the X a,b c,d are Newcomb operators which can be defined recursively by X a,b 0,0 = () X a,b,0 = b a/. (4)

5 DISTURBING FUNCTION If d = 0, then If d 0, then 4cX a,b a,b+ a,b+ c,0 = (b a)xc,0 + (b a)xc,0. (5) 4dX a,b a,b a,b c,d = (b + a)xc,d (b + a)xc,d (c 5d b + a)x a,b c,d + (c d + b) ( / ( ) j j j ) X a,b c j,d j. (6) If c < 0ord<0, then X a,b a,b c,d = 0. If d > c then Xc,d = X a, b d,c. A fourth-order expansion of the direct and indirect parts of the disturbing function was generated by implementing the above algorithm in Mathematica (Wolfram 99). A list of possible arguments was generated for each order (0,,,, 4) and then the terms associated with each argument were calculated. The resulting file of integers was compared with a similar expansion obtained by carrying out a full expansion using the technique employed by Murray and Harper (99); the expansions agreed in all respects. Generating a full expansion using the new algorithm was found to be an order of magnitude faster than using the older method. The full expansions of R D, R E, and R I are given in the Appendix.. USE OF THE DISTURBING FUNCTION The expansion of the direct and indirect parts of the disturbing function given in Eqs. (6) (8) appears to be compact but at first glance its structure and the number of summations is intimidating. However, it is important to bear in mind that in a given application we are only interested in generating the terms associated with particular arguments. Before showing how the number of summations can be reduced, we demonstrate the relationship between the integer coefficients in the cosine argument and the powers of the eccentricity and inclination in the corresponding term. Comparing Eq. () with the cosine argument in Eq. (6) gives the following relationships between the integers: j = (s n p + q ) + (i + j l s) () j = (s n p+q) (i+j l s) (8) j = q (9) j 4 = q (0) j 5 = m (s n p ) () j 6 = m+(s n p), () where we have added and subtracted a term in s in the expressions for j and j. Because all the angles in the cosine argument are longitudes, the argument satisfies the d Alembert rule, whereby 6 j i = 0. () i= Hamilton (994) has investigated the d Alembert rule and similar properties in his comparison of Lorentz resonances with planetary gravitational resonances and satellite gravitational resonances. From Eq. () we see that the lowest power of e arising from the Hansen coefficient Xc a,b (e) is c b. Therefore, by inspection of the Hansen coefficients in e and e in Eq. (6) we see that and i+k,i+ j l n p Xi+ j l n p+q (e) = O( e q ) (4) (i+k+),i+ j l n p Xi+ j l n p +q (e ) = O ( e q ). (5) Therefore one property of the disturbing function is that the lowest powers of e and e are the absolute values of the coefficients of ϖ and ϖ, respectively, in the cosine argument. Similarly, an inspection of the inclination function defined in Eq. () shows that and F s n,m,p (I ) = O ( sin m s+n+p I ) (6) F s n,m,p (I ) = O ( sin m s+n+p I ). () Therefore the lowest powers of sin I and sin I that occur in Eq. (6) are the absolute values of the coefficients of and, respectively, in the cosine argument. Now consider the various summations inherent in Eq. (6). By adding Eq. () and Eq. () we have j 5 + j 6 = p p (8) and so j 5 + j 6 is always even. This places another constraint on the permissible arguments in the expansion, in addition to the constraint imposed by the d Alembert relation. It also implies that the sum of the powers of the inclinations is always an even number and hence that the expansion can never contain an isolated, single power of an inclination. This property has also been investigated by Hamilton (994). An inspection of the various integers involved in the summations in Eq. (6) allows us to reduce the range of several of the summations. Let N max be the maximum order of the expansion; this is the maximum sum of the powers of e, e, I, and I that is desired in any one term associated with a given argument. Note that we must have N max N, where N is the order of the argument as defined in Eq. (8). The following relationships hold throughout the calculation, q = j 4 (9) q = j (40)

6 4 ELLIS AND MURRAY l max = N max j 5 j 6 (4) p min = (j 5 +j 6 )/, p min = 0 if j 5+ j 6 <0 (4) p min = 0, p min = ( j 5 + j 6 )/ if j 5 + j 6 0 (4) s min = max(p min, p min, j 6 + p min, j 5 + p min ) (44) i max = [(N max j j 4 )/], (45) where, as before, the square brackets in Eq. (45) denote the integer part of the expression. As well as these global relationships, there are a number of intermediate definitions required for the summation. These are n max = [(s s min )/] (46) m min = 0 if s, j 5 are both even or both odd (4) m min = if s, j 5 are neither both even nor both odd (48) p = ( j 6 m + s n)/ with p s n and p p min (49) p = ( j 5 m + s n)/ with p s n and p p min (50) j = j +i l n p+q. (5) Again the square brackets denote the integer part of the expression. Note that q and q are determined directly from the coefficients of ϖ and ϖ in the argument of interest, and remain fixed over all the summations. This removes the infinite summation over all values of q and q in Eq. (6). On the other hand, p and p change with s, n, and m but the relationships given in Eqs. (49) and (50) always hold. We can now rewrite Eq. (6) as R D = i max i=0 (i)! i! i s=s min n=0 ( ) i αi i+ n max (s 4n + )(s n)! n n!(s n + )! l=0 s n m=0 i s F s n,m,p (I ) F s n,m,p (I ( ) s s ) (i s l)!l! l max ( ) l l! l=0 l k=0 ( l )( ) k α l dl j) b( (α) k dαl i+ κ m (s n m)! (s n + m)! X i+k, j j 4 j (e) X (i+k+), j + j j (e ) cos[ j λ + j λ + j ϖ + j 4 ϖ + j 5 + j 6 ], (5) where, as before, κ m = ifm=0 and κ m = ifm>0. In the form of the expansion for R D given in Eq. (5) above, it is understood that the summations involved in the definitions of the functions of eccentricity and inclination need only be evaluated to a finite order which is at most equal to N max. The Hansen coefficient in e need only include terms up to order N max j j 5 j 6 in e; similarly the Hansen coefficient in e need only include terms up to order N max j 4 j 5 j 6 in e. The F inclination function in I need only include terms up to order N max j j 4 j 5 in I ; similarly the F function in I need only include terms up to order N max j j 4 j 6 in I. In producing the truncated form of the full expression for R D we have also replaced the upper limit on the summation in l from l = to l = l max, where l max is defined in Eq. (4). This is not part of the general truncation process; it arises from the fact that for values of l>l max all additional contributions to the summation are zero. This is because l k=0 ( ) l ( ) k f (k) = 0, (5) k where f (x) is any polynomial of degree less than l. Most previous expansions did not involve any sin I or cos I terms in the inclination parts. Instead the expansions were carried out in terms of sin I, or, to be more precise, sin J.We can follow this example by noting that sin I = s s and cos I = s where s = sin I and make the appropriate substitutions in the definition of the F inclination function given in Eq. (). This requires an additional series expansion in s (and s ) and permits a direct comparison with the expansion of Murray and Harper (99). Now consider the indirect part for an external perturber (see Eq. ()). A comparison of Eqs. () and () gives the following relationships between the integers: j = p + q (54) j = ( p + q) (55) j = q (56) j 4 = q (5) j 5 = ( p m) (58) j 6 = p m. (59) An analysis of the integers involved in the expansion of this indirect part gives the following relationships: q = j 4 (60) q = j (6) p = ( j + j 4 + )/ (6) p = (j +j )/ (6) m = j 5 p + (64)

7 DISTURBING FUNCTION 5 and the expansion itself can now be written R E = κ m ( m)! ( + m)! F,m,p (I )F,m,p (I )X, j j 4 j (e)x, j + j j (e ) cos[ j λ + j λ + j ϖ + j 4 ϖ + j 5 + j 6 ], (65) where each of the quantities p, p, and m must be integers and equal to 0 or. If these conditions are not satisfied then the given argument does not appear in the expansion of the indirect part. As with the direct part we can reduce the extent of the series expansions in powers of the eccentricity and inclination, and the same modifications apply. The equivalent expression for the indirect part due to an internal perturber is R I = κ m ( m)! ( + m)! F,m,p (I )F,m,p (I )X, j j 4 j (e) X, j + j j (e ) cos[ j λ + j λ + j ϖ + j 4 ϖ + j 5 + j 6 ]. (66) The same restrictions on p, p, and m apply. In reality, the expansions of R D, R E, and R I are infinite series. However, in practice we are only interested in terms that are appropriate for a particular problem. Thus we need to isolate the relevant terms from the expansion, ignoring all other nonrelevant terms; effectively this assumes that the remaining terms produce only short-period effects which average out to zero. This is known as the averaging principle and it is the basis of much analytical work in Solar System dynamics. What constitutes a relevant term is not always obvious, but some general principles apply. A study of the dynamics of an object moving close to a p + q : p resonance with a perturber would require the isolation of those arguments with j =±(p+q) and j = p. For example, if we were interested in studying motion close to the 5:4 resonance we would isolate those terms associated with arguments that contained 5λ 4λ and 5λ + 4λ (i.e., p + q =±5, q=±). We now consider the procedure for determining the appropriate averaged term, R or R in the disturbing function, based on the fourth-order expansion given in the Appendix, or the eighth order expansion given by Murray and Harper (99). This procedure is also given in Murray and Dermott (999).. Decide which particular combination of angles, φ = j λ + j λ + j ϖ + j 4 ϖ + j 5 + j 6, is applicable to the problem at hand; this requires knowledge of the physical problem under investigation.. Determine the order, N = j + j, of the argument. This is just the absolute value of the sum of the coefficients of λ and λ in φ.. By looking at the appropriate order terms in the expansion of R D, determine the value of the integer j which gives agreement with the desired argument, φ. 4. Calculate the combination of Laplace coefficients for that value of j to give the explicit form of the term of interest, R D say. 5. Decide whether an external or an internal perturbation is being considered. This is determined by the nature of the problem. 6. If the perturbation is external, then look at the appropriate order terms in the expansion of the indirect part, R E, and isolate a matching argument, if it exists, and read off the corresponding indirect term R E.. If the perturbation is internal, then look at the appropriate order terms in the expansion of the indirect part, R I, and isolate a matching argument, if it exists, and read off the corresponding indirect term R I. 8. If the perturbation is external then R = µ a ( R D +α R E ). (6) 9. If the perturbation is internal then R = µ a ( α R D + ) α R I. (68) It is important to note that other terms may also have to be considered. For example, if the : resonance is being studied with a fourth-order expansion, then the contributions from arguments containing 4λ λ,6λ λ, and 8λ 4λ (and their negatives) should also be included since they are associated with resonances at almost the same location and can make significant contributions if the eccentricity is large enough. Furthermore, any expansion above the first-order should also include the secular terms which contain second- and higher-order terms in the eccentricities and inclinations. These arise from arguments of order 0 which do not contain the mean longitudes. For example, inspection of the Appendix shows that the arguments 4D0., 4D0., and 4D0. in Table I with j = 0 will give rise to arguments without the mean longitudes where the associated terms contain terms of order in e, e, s, and s ; all remaining secular terms are of order 4 or higher and there are no contributions from the indirect terms. Derivation of the disturbing function should not be considered an end in itself. The actual value of R is unimportant because we are interested only in the terms in its series expansion which will make significant contributions to the force acting on the perturbed body. To calculate the resulting changes in orbital elements due to particular terms we need to make use of Lagrange s planetary equations (see, for example, Brouwer and Clemence 96).

8 6 ELLIS AND MURRAY 4. EXAMPLES In order to demonstrate the use of the fourth order expansion given in the Appendix as well as the algorithm given in Section, we now consider two examples. In each case we show how the averaged resonant terms can be obtained using each method. Again we stress that if the derived expressions are to be used in a study of the motion of the objects then it may be necessary to include the secular as well as the resonant terms. 4.. The Titan Hyperion :4 Resonance The saturnian satellites Titan and Hyperion are involved in a :4 resonance where the librating resonant argument is φ = 4λ λ ϖ, (69) where the primed quantities refer to Hyperion and the unprimed ones refer to Titan. Because the mass of Titan is so large, it is customary to neglect the perturbations of Hyperion on Titan. Note that this is a first-order resonance with an internal perturber. The eccentricity of Hyperion s orbit is e = 0.04 and this value is forced on the orbit as a result of the perturbations from Titan. Thus an expansion to order is unlikely to be sufficient to model the system; consequently we will derive a fourth-order expansion for this particular resonant argument. The appropriate resonant argument from the Appendix is 4D. in Table IV with j = 4. This gives { R D = e [ + αd]b () (α) + 8 e e [ 5 0αD + α D + α D ]b () (α) + 6 e [ 58 6αD + α D + α D ]b () (α) ( ) } 4 e (s + s )[8α + α D] b () (α) + b (4) (α) cos[4λ λ ϖ ], (0) where the operator D denotes d/dα and where s = sin I, s = sin I. There are no indirect terms for this argument to this order and so R =(Gm/a ) R D. Now consider the derivation using the algorithm discussed in Sections and. From the definition of φ =+(4λ λ ϖ ) and the relationships given in Eqs. (9) (5), we have q =, q = 0, l max = 4, p min = 0, p min = 0, s min = 0, i max = ; we can also deduce that the only permissible values of n, p, and p are n = 0, p = 0, and p = 0. Hence, R D + = i=0 (i)! i! ( ) i αi i+ i s=0 s! (s)! s m=0 κ m (s m)! (s + m)! i s F s,m,0 (I ) F s,m,0 (I ( ) s s ) (i s l)!l! 4 ( ) l l=0 l! l k=0 l=0 ( ) l ( ) k α l D l b ( j) (α)x i+k, k i+ (e) X (i+k+), 4 (e ) cos[4λ λ ϖ ], () where D d/dα. If we consider the terms arising from taking φ = (4λ λ ϖ )wehaveq =, q = 0, l max = 4, p min = 0, p min = 0, s min = 0, i max = ; we can also deduce that the only permissible values of n, p, and p are n = 0, p = 0, and p = 0. Hence, R D = i=0 (i)! i! ( ) i αi i+ i s=0 s! (s)! l=0 s m=0 κ m (s m)! (s + m)! i s F s,m,0 (I ) F s,m,0 (I ( ) s s ) (i s l)!l! 4 ( ) l l=0 l! l k=0 ( l k ) ( ) k α l D l b ( j) i+ (α)x i+k, (e) X (i+k+), 4 (e ) cos[4λ λ ϖ ]. () The required inclination functions are given without approximation by F 0,0,0 (I ) = F 0,0,0 (I ) =, F,,0 (I ) = s and F,,0 (I ) = s. The required Hansen coefficients to O(e ) and O(e ) are given by X 0, 0, (e) = X () X, 4 (e ) = X, 4 (e ) = e 9 8 e (4) X,, (e) = X (e) = e (5) X, 4 (e ) = X, 4 (e ) = 4e 4e (6) X,, 5 (e) = X (e) = e () X, 4 (e ) = X, 4 (e ) = 9 e 4e (8) X,, (e) = X (9) X 4, 4 (e ) = X 4, 4 (e ) = 5e e (80) X 4, 4, (e) = X (8) X 5, 4 (e ) = X 5, 4 (e ) = e 4 8 e (8) X 5, 5, (e) = X (e) = e (8) X 6, 4 (e ) = X 6, 4 (e ) = 6e e. (84)

9 DISTURBING FUNCTION There are no indirect terms in the expansion associated with this argument and so R =(Gm/a )( R D + + R D ). The resulting expansion agrees with that obtained above using the Appendix. A good orbital theory of Hyperion is notoriously difficult to achieve (see, for example, the study by Message 99). It is beyond the scope of this paper to investigate this further and we content ourselves with the derivation of some of the higher-order terms which would be appropriate to include in any analytical investigation of the perturbations on Hyperion s orbit. 4.. The Jupiter Pallas 8: Resonance As an example of a higher order resonance argument for which there is no existing, general literal expansion, we consider one of the terms relevant to a description of the motion of minor planet Pallas. If n and n denote the mean motions of Jupiter and Pallas, respectively, then from observation, 8n n = 0.45 year. (85) This implies that Jupiter and Pallas are close to an 8: resonance. To th order there are 8 arguments associated with this resonance. In order to illustrate the use of our algorithm we derive the terms associated with just one of these arguments, namely φ = 8λ λ 5ϖ 6. (86) Applying the definitions given in Eqs. (9) (45) gives q = 5, q = 0, l max = 5, p min =, p min = 0, s min =, i max =. Since s min = i max the only contribution will come from i = s = and hence l = 0. Similarly, since n max = [(s )/] = 0 we must have n = 0. Hence, from Eq. (49) the only valid value of p is p = ; hence m = and so from Eq. (50) p = 0; we also have j = 5. We can now write the simplified form of Eq. (5) as R D + = α 0 5 ( ) l l=0 l! l k=0 ( ) l ( ) k α l D l b (5) / k (α)f,,(i ) F,,0 (I )X +k, (e) X (4+k),8 8 (e ) cos[8λ λ 5ϖ 6 ]. (8) In order to complete the calculation we need to investigate the possibility that there are terms associated with the negative of our original argument, namely φ = (8λ λ 5ϖ 6 ). In this case inspection of Eqs. (9) (5) shows that there are no contributions and R D = 0. We require only two evaluations of the inclination function and evaluations of Hansen coefficients. Although our expansion is to th order, according to the approximations given in Eqs. (4) () the function F,, (I ) will produce terms of O(I 6 ) and X +k, (e) will produce terms of O(e 5 ). Thus we are concerned only with the lowest order terms in all function evaluations. This means that we can ignore the higher order terms in F,,0 (I ) = 5 + O(I (4 + k),8 ) and X8 (e ) = + O(e ) for k = 0,,...5. We have F,, (I ) = 5s 6 (88) X, (e) = e5 (89) X 4, (e) = 40 e (90) X 5, (e) = e5 (9) X 6, (e) = 486 e (9) X, (e) = 0848 e (9) X 8, (e) = e5, (94) and the resulting expression for R D is R D = e5 s 6 88 [444α + 665α 4 D α 5 D + 50α 6 D + 5α D 4 + α 8 D 5 ]b (5) / (α) cos[8λ λ 5ϖ 6 ]. (95) Application of the algorithm given in Sections and for the indirect parts shows that none exist in this case; furthermore, there are no indirect terms associated with any of the 8 possible arguments to th order at this resonance. Therefore the averaged part of the disturbing function for this argument is given by R =(Gm /a ) R D. Note that this example was chosen to illustrate the calculation of a high-order term; we do not imply that this particular argument is likely to be the dominant one at the 8: resonance. 5. DISCUSSION Our overriding aim in this work is to present a new, workable algorithm for producing expansions of the planetary disturbing function to any order in the eccentricities and inclinations of both objects. This obviates the need for the major expansions of the last century which, although they are still in use, have a number of drawbacks and contain errors. In particular we have now developed the capability to produce a high-order expansion for only those arguments of interest in a particular problem

10 8 ELLIS AND MURRAY in Solar System dynamics. It is our hope that this work, and the fourth-order expansion given in the Appendix, will provide Solar System dynamicists with a clearer understanding of the disturbing function, its use, and its applications. We do not pretend that the algebraic effort involved in generating and manipulating such expansions is trivial. However, an underlying assumption of this work is that software packages for algebraic manipulation will become even more widespread, powerful, and affordable than they already are. For our own purposes we have developed a package in Mathematica (Wolfram 99), which implements the algorithm given here and contains a number of useful routines for generating and manipulating the series involved. The package is available free of charge to interested researchers and further information can be obtained from the second author. APPENDIX In Section we outlined an algorithm for obtaining an expansion of the disturbing function, R. Here we give a literal expansion of the direct part, R D, and the indirect part for an external perturber, R E, and an internal perturber, R I, complete to fourth-order in the eccentricities and inclinations of the two bodies. The notation is the same as that used in Sections and where the expansion is given in terms of Laplace coefficients and their derivatives. The use of the disturbing function is described in the main text of this paper. In our expansion each cosine argument has been labeled for the order of the expansion (4 in this case) followed by a letter denoting that the term is associated with the direct (prefix D) or indirect (prefix E or I) part of the disturbing function. The next character denotes the order of the argument, i.e., the absolute value of the sum of the coefficients of λ and λ, and hence the order of the resonance associated with that argument. The final number identifies the argument. These are ordered with priority being given to those involving only ϖ, ϖ,, and in that order. This means that terms involving e occur before those involving e, etc. This follows the procedure adopted by Murray and Harper (99). For example, 4D.4 denotes the fourth possible argument of the third-order direct part of the fourth order expansion. The entry for this argument should be interpreted as R D =e 48 [ j 0 j + 8 j + 6αD jαd + j αd α D + 6 jα D + α D ]b ( j ) (α) cos[ jλ + ( j)λ ϖ ], (96) where D denotes the differential operator d/dα. If we consider the same argument for a particular value of j, then we must also look at the expansion of the indirect part for any matching arguments. For example, if j = 4 and we are dealing with an external perturber then we must also include the argument 4E.. The total contribution of this argument to the averaged part of the disturbing function is then [ R = Gm a e 6 α + 4 b() (α) α d dα b() (α) + d α 6 dα b() (α) + d α 48 dα b() ] (α) cos[4λ λ ϖ ]. (9) Tables I XIX below give all arguments and associated terms in an expansion of the disturbing function complete to fourth-order. The expansion is arranged TABLE I Zeroth-Order Arguments: Direct Part 4D0. jλ jλ f + (e + e ) f + (s + s ) f + e 4 f 4 +e e f 5 +e 4 f 6 +(e s + e s + e s + e s ) f + (s 4 + s 4 ) f 8 + s s f 9 4D0. jλ jλ + ϖ ϖ ee f 0 + e e f + ee f +ee (s + s ) f 4D0. jλ jλ + ss f 4 + ss (e + e ) f 5 + ss (s + s ) f 6 4D0.4 jλ jλ + ϖ ϖ e e f 4D0.5 jλ jλ + ϖ e s f 8 4D0.6 jλ jλ + ϖ + ϖ ee s f 9 4D0. jλ jλ + ϖ e s f 0 4D0.8 jλ jλ + ϖ e ss f 4D0.9 jλ jλ + ϖ ϖ + ee ss f 4D0.0 jλ jλ + ϖ ϖ + ee ss f 4D0. jλ jλ + ϖ + ϖ ee ss f 4 4D0. jλ jλ + ϖ e ss f 5 4D0. jλ jλ + ϖ e s f 8 4D0.4 jλ jλ + ϖ + ϖ ee s f 9 4D0.5 jλ jλ + ϖ e s f 0 4D0.6 jλ jλ + s s f 6 TABLE II Zeroth-Order Arguments: Indirect Part (External and Internal Perturbers) 4E0., 4I0. λ λ + (e +e )+ 64 (e4 +e 4 ) 4 e e + s (e + e ) (s + s ) + s s s 4E0., 4I0. λ λ ϖ + ϖ ee + 4 e e + 4 ee + ee s + ee s 4E0., 4I0. λ λ + ss + e ss + e ss + s s +ss 4E0.4, 4I0.4 λ λ ϖ + ϖ 64 e e 4E0.5, 4I0.5 λ λ ϖ + ϖ 8 64 e e 4E0.6, 4I0.6 λ λ + ϖ 8 e s 4E0., 4I0. λ λ ϖ + 8 e s 4E0.8, 4I0.8 λ λ + ϖ 4 e ss 4E0.9, 4I0.9 λ λ ϖ + ϖ + ee ss 4E0.0, 4I0.0 λ λ ϖ e ss 4E0., 4I0. λ λ + ϖ 8 e s 4E0., 4I0. λ λ ϖ + 8 e s 4E0., 4I0. λ λ + s s

11 DISTURBING FUNCTION 9 i TABLE III Zeroth-Order Arguments: Functions of Semimajor Axis A j 8 [ 4j +αd +α D ]A j 4 [ α]b j + 4 [ α]b j+ 8 [ 9 j + 6 j 4 8 j αd 8 j α D + 4α D + α 4 D 4 ]A j [6 j 4 + 4αD 6 j αd + 4α D 8 j α D + 8α D + α 4 D 4 ]A j 8 [ j + 6 j 4 + 4αD 4 j αd + 6α D 8 j α D + α D + α 4 D 4 ]A j 6 [ α + 4 j α 4α D α D ](B j + B j+ ) 6 [α ]C j + 4 [α ]C j + 6 [α ]C j+ 4 [α](b j + B j+ ) + 8 [α ]C j [α ]C j + 8 [α ]C j+ 4 [ + 6 j + 4 j αd α D ]A j+ [ 6 j 6 j 6 j 6 j jαd + j αd 4α D + jα D + 8 j α D 6α D α 4 D 4 ]A j+ [4 + j j 6 j 6 j 4 4αD + jαd + 0 j αd α D + jα D + 8 j α D 0α D α 4 D 4 ]A j+ 8 [ 6 jα 4 j α + 4α D + α D ](B j + B j+ ) 4 [α]b j+ 5 4 [α 4 j α + 4α D + α D ]B j+ 6 [ α]b j+ + [ α ]C j + [ α ]C j+ 64 [ + 64 j + 09 j + j + 6 j 4 αd 8 jαd 6 j αd + 6α D 4 jα D 8 j α D + 8α D + α 4 D 4 ]A j [α 5 jα + 4 j α + 8α D 4 jα D + α D ]B j 8 [6 jα 4 j α 4α D + 4 jα D α D ]B j 6 [ jα + 4 j α 4 jα D + α D ]B j+ 8 [ α + 5 jα 4 j α 8α D + 4 jα D α D ]B j 4 [6 jα + 4 j α 4α D α D ]B j 4 [6 jα + 4 j α 4α D α D ]B j+ 4 [ 6 jα + 4 j α + 4α D 4 jα D + α D ]B j 8 [ jα 4 j α + 4 jα D α D ]B j+ [α]b j+ + 4 [α ]C j + [α ]C j+ TABLE IV First-Order Arguments: Direct Part 4D. jλ + ( j)λ ϖ ef + e f 8 + ee f 9 + e(s + s ) f 0 4D. jλ + ( j)λ ϖ e f + e e f + e f + e (s + s ) f 4 4D. jλ + ( j)λ + ϖ ϖ e e f 5 4D.4 jλ + ( j)λ ϖ + ϖ ee f 6 4D.5 jλ + ( j)λ + ϖ es f 4D.6 jλ + ( j)λ + ϖ e s f 8 f i TABLE IV Continued 4D. jλ + ( j)λ ϖ + ess f 9 4D.8 jλ + ( j)λ ϖ + ess f 40 4D.9 jλ + ( j)λ + ϖ ess f 4 4D.0 jλ + ( j)λ ϖ + e ss f 4 4D. jλ + ( j)λ ϖ + e ss f 4 4D. jλ + ( j)λ + ϖ e ss f 44 4D. jλ + ( j)λ + ϖ es f 4D.4 jλ + ( j)λ + ϖ e s f 8 TABLE V First-Order Arguments: Indirect Part (External Perturber) 4E. λ λ + ϖ e + 8 e + 4 ee + es + es 4E. λ ϖ e 4 ee es es 4E. λ λ ϖ e + e e + e + e s + e s 4E.4 λ λ ϖ + ϖ 4 e e 4E.5 λ ϖ + ϖ 6 ee 4E.6 λ λ ϖ + ϖ 6 ee 4E. λ + ϖ es 4E.8 λ λ + ϖ + ess 4E.9 λ ϖ + ess 4E.0 λ + ϖ ess 4E. λ λ ϖ + 4e ss 4E. λ + ϖ es TABLE VI First-Order Arguments: Indirect Part (Internal Perturber) 4I. λ λ + ϖ e + e + ee + es + es 4I. λ ϖ e 4 e e e s e s 4I. λ λ ϖ e + 4 e e + 8 e + e s + e s 4I.4 λ + ϖ ϖ 6 e e 4I.5 λ λ ϖ + ϖ 6 e e 4I.6 λ λ ϖ + ϖ 4 ee 4I. λ + ϖ e s 4I.8 λ λ + ϖ + 4ess 4I.9 λ ϖ + e ss 4I.0 λ + ϖ e ss 4I. λ λ ϖ + e ss 4I. λ + ϖ e s

12 40 ELLIS AND MURRAY i TABLE VII First-Order Arguments: Functions of Semimajor Axis [ j αd]a j 6 [ j 0 j + 8 j + αd jαd + 4 j αd α D jα D α D ]A j f i 8 [8 j αd 4 jαd + 4 j αd 4α D jα D α D ]A j 4 [α + jα + α D](B j + B j+ ) [ + j + αd]a j 8 [4 6 j + 0 j 8 j 4αD + jαd 4 j αd + α D + jα D + α D ]A j 6 [ j + 0 j 8 j + αd + 9 jαd 4 j αd + 5α D + jα D + α D ]A j 4 [ jα α D](B j + B j ) 6 [ j 0 j 8 j αd jαd 4 j αd + α D + jα D α D ]A j+ 6 [ 8 + j 0 j + 8 j + 8αD jαd + 4 j αd 4α D jα D α D ]A j 4 [ 5α + jα α D]B j 4 [ jα + α D]B j [ α jα α D]B j [ α jα α D]B j+ [5α jα + α D]B j [ jα + α D]B j [ jα + α D]B j [ jα α D]B j TABLE VIII Second-Order Arguments: Direct Part 4D. jλ + ( j)λ ϖ e f 45 + e 4 f 46 + e e f 4 + e (s + s ) f 48 4D. jλ + ( j)λ ϖ ϖ ee f 49 + e e f 50 + ee f 5 + ee (s + s ) f 5 4D. jλ + ( j)λ ϖ e f 5 + e e f 54 + e 4 f 55 + e (s + s ) f 56 4D.4 jλ + ( j)λ s f 5 + e s f 58 + e s f 59 + s 4 f 60 + s s f 6 4D.5 jλ + ( j)λ ss f 6 +e ss f 6 +e ss f 64 + s s f 65 + ss f 66 4D.6 jλ + ( j)λ s f 5 +e s f 58 +e s f 59 + s s f 6 + s 4 f 60 TABLE VIII Continued 4D. jλ + ( j)λ + ϖ ϖ e e f 68 4D.8 jλ + ( j)λ ϖ + ϖ ee f 69 4D.9 jλ + ( j)λ ϖ + ϖ ee s f 0 4D.0 jλ + ( j)λ + ϖ ϖ ee s f 4D. jλ + ( j)λ ϖ + e ss f 4D. jλ + ( j)λ ϖ + e ss f 4D. jλ + ( j)λ ϖ ϖ + ee ss f 4 4D.4 jλ + ( j)λ ϖ ϖ + ee ss f 5 4D.5 jλ + ( j)λ ϖ + ϖ ee ss f 6 4D.6 jλ + ( j)λ + ϖ ϖ ee ss f 4D. jλ + ( j)λ ϖ + e ss f 8 4D.8 jλ + ( j)λ ϖ + e ss f 9 4D.9 jλ + ( j)λ + s s f 80 4D.0 jλ + ( j)λ ϖ + ϖ ee s f 0 4D. jλ + ( j)λ + ϖ ϖ ee s f 4D. jλ + ( j)λ + ss f 8 TABLE IX Second-Order Arguments: Indirect Part (External Perturber) 4E. λ λ + ϖ 8 e + 8 e4 + 6 e e + 8 e s + 8 e s 4E. λ + λ ϖ 8 e 4 e4 + 6 e e + 8 e s + 8 e s 4E. λ ϖ ϖ ee 9 4 ee ee s ee s 4E.4 λ + λ ϖ 8 e + 6 e e 4 e e s + 8 e s 4E.5 λ λ ϖ 8 e + 6 e e + 8 e e s + 8 e s 4E.6 λ + λ s + e s + e s + s s 4E. λ + λ ss e ss e ss s s ss 4E.8 λ + λ s + e s + e s + s s 4E.9 λ 4λ ϖ + ϖ e e 4E.0 λ ϖ + ϖ 4 ee 4E. 4λ λ ϖ + ϖ 8 ee 4E. λ ϖ + ϖ ee s 4E. λ λ + ϖ + 4 e ss 4E.4 λ + λ ϖ + 4 e ss 4E.5 λ ϖ ϖ + 6ee ss 4E.6 λ ϖ + ϖ 6ee ss 4E. λ + λ ϖ + 4 e ss 4E.8 λ λ ϖ + 4 e ss 4E.9 λ ϖ + ϖ ee s

13 DISTURBING FUNCTION 4 TABLE X Second-Order Arguments: Indirect Part (Internal Perturber) 4I. λ λ + ϖ 8 e + 8 e4 + 6 e e + 8 e s + 8 e s 4I. λ + λ ϖ 8 e 4 e4 + 6 e e + 8 e s + 8 e s 4I. λ ϖ ϖ ee 9 4 e e ee s ee s 4I.4 λ + λ ϖ 8 e + 6 e e 4 e e s + 8 e s 4I.5 λ λ ϖ 8 e + 6 e e + 8 e e s + 8 e s 4I.6 λ + λ s + e s + e s + s s 4I. λ + λ ss e ss e ss s s ss 4I.8 λ + λ s + e s + e s + s s 4I.9 λ + ϖ ϖ 4 e e 4I.0 λ 4λ ϖ + ϖ 8 e e 4I. 4λ λ ϖ + ϖ ee 4I. λ + ϖ ϖ ee s 4I. λ λ + ϖ + 4 e ss 4I.4 λ + λ ϖ + 4 e ss 4I.5 λ ϖ ϖ + 6ee ss 4I.6 λ + ϖ ϖ 6ee ss 4I. λ + λ ϖ + 4 e ss 4I.8 λ λ ϖ + 4 e ss 4I.9 λ + ϖ ϖ ee s i TABLE XI Second-Order Arguments: Functions of Semimajor Axis 8 [ 5 j + 4 j αd + 4 jαd + α D ]A j 96 [ j 64 j + 60 j 6 j 4 + 6αD 46 jαd + 48 j αd 6 j αd α D + 9 jα D + 4 jα D + α 4 D 4 ]A j [0 j 6 j 4 4αD jαd + 6 j αd 6 j αd α D + jα D + 4α D + 4 jα D + α 4 D 4 ]A j f i 6 [α + jα 4 j α 4 jα D α D ](B j + B j+ ) 4 [ + 6 j 4 j + αd 4 jαd α D ]A j [0 86 j + 6 j 6 j + 6 j 4 0αD + 4 jαd 64 j αd + 6 j αd + 4α D jα D α D 4 jα D α 4 D 4 ]A j i TABLE XI Continued [ 4 + j + j 6 j + 6 j 4 + 4αD + 6 jαd j αd + 6 j αd α D 9 jα D 6α D 4 jα D α 4 D 4 ]A j 8 [ jα + 4 j α + 4 jα D + α D ](B j + B j ) 8 [ j + 4 j αd + 4 jαd + α D ]A j [ + 44 j 84 j + 9 j 6 j 4 + αd 0 jαd + 80 j αd 6 j αd 6α D + 5 jα D + 4α D + 4 jα D + α 4 D 4 ]A j 96 [ 4 j 40 j + 5 j 6 j 4 αd 0 jαd + 48 j αd 6 j αd + 6α D + jα D + 8α D + 4 jα D + α 4 D 4 ]A j 56 6 [ jα 4 j α 4 jα D α D ](B j + B j ) 5 [α]b j 58 8 [ 4α + 6 jα 4 j α + 4α D + α D ]B j 59 8 [α 4 j α + 4α D + α D ]B j 60 4 [ α ]C j + 4 [ α ]C j 6 [ α]b j + 4 [ α ]C j [ α ]C j 6 [ α]b j 6 4 [4α 6 jα + 4 j α 4α D α D ]B j 64 4 [ α + 4 j α 4α D α D ]B j 65 [α]b j + [α ]C j + [α ]C j 66 [α]b j + [α ]C j + [α ]C j 6 [ α]b j [ α ]C j + 4 [ α ]C j [4 j 6 j 4 j + 6 j 4 4αD jαd + 6 j αd + 6α D jα D α D 4 jα D α 4 D 4 ]A j [6 86 j + 8 j 08 j + 6 j 4 6αD + 0 jαd 96 j αd + 6 j αd + 8α D jα D 6α D jα D α 4 D 4 ]A j 8 [ 4 jα + 4 j α 8α D α D ]B j 8 [ jα + 4 j α α D ]B j 8 [ α jα + 4 j α + 4 jα D + α D ]B j 8 [ α jα + 4 j α + 4 jα D + α D ]B j+ 4 [ jα 4 j α 4 jα D α D ]B j 4 [ jα 4 j α 4 jα D α D ]B j 4 [4 jα 4 j α + 8α D + α D ]B j 4 [ jα 4 j α + α D ]B j 8 [ jα + 4 j α + 4 jα D + α D ]B j 8 [ jα + 4 j α + 4 jα D + α D ]B j [α ]C j [α ]C j f i

14 4 ELLIS AND MURRAY TABLE XII Third-Order Arguments: Direct Part 4D. jλ + ( j)λ ϖ e f 8 4D. jλ + ( j)λ ϖ ϖ e e f 8 4D. jλ + ( j)λ ϖ ϖ ee f 84 4D.4 jλ + ( j)λ ϖ e f 85 4D.5 jλ + ( j)λ ϖ es f 86 4D.6 jλ + ( j)λ ϖ e s f 8 4D. jλ + ( j)λ ϖ ess f 88 4D.8 jλ + ( j)λ ϖ e ss f 89 4D.9 jλ + ( j)λ ϖ es f 86 4D.0 jλ + ( j)λ ϖ e s f 8 TABLE XIII Third-Order Arguments: Indirect Part (External Perturber) i TABLE XV Third-Order Arguments: Functions of Semimajor Axis 48 [ 6 j + 0 j 8 j 9αD + jαd j αd + 6α D 6 jα D α D ]A j f i 6 [ 9 + j 0 j + 8 j + 9αD 5 jαd + j αd 5α D + 6 jα D + α D ]A j 6 [8 j + 0 j 8 j 8αD + jαd j αd + 4α D 6 jα D α D ]A j 48 [ j 0 j + 8 j + 6αD jαd + j αd α D + 6 jα D + α D ]A j 4 [α jα α D]B j 4 [ jα + α D]B j [ α + jα + α D]B j [ jα α D]B j 4E. λ 4λ + ϖ e 4E. λ + λ ϖ 4 e 4E. λ + λ ϖ ϖ 4 e e 4E.4 λ + λ ϖ ϖ 6 ee 4E.5 λ ϖ 8 ϖ 6 ee 4E.6 λ + λ ϖ 6 e 4E. 4λ λ ϖ 6 e 4E.8 λ + λ ϖ es 4E.9 λ + λ ϖ e s 4E.0 λ + λ ϖ ess 4E. λ + λ ϖ 4e ss 4E. λ + λ ϖ es 4E. λ + λ ϖ e s by the order of the argument, i.e., the absolute value of the sum of the coefficients of the mean longitudes in each argument. Tables I III, Tables IV VII, Tables VIII XI, Tables XII XV, and Tables XVI XIX contain the arguments and terms for the zeroth-, first-, second-, third-, and fourth-order arguments, respectively. The full, fourth-order expansion of R (or R ) should be considered as the sum of the direct and indirect terms for an external (or internal) perturber over all values of the integer j. TABLE XVI Fourth-Order Arguments: Direct Part 4D4. jλ + (4 j)λ 4ϖ e 4 f 90 TABLE XIV Third-Order Arguments: Indirect Part (Internal Perturber) 4I. λ 4λ + ϖ 6 e 4I. λ + λ ϖ 6 e 4I. λ ϖ 8 ϖ 6 e e 4I.4 λ + λ ϖ ϖ 6 e e 4I.5 λ + λ ϖ ϖ 4 ee 4I.6 λ + λ ϖ 4 e 4I. 4λ λ ϖ e 4I.8 λ + λ ϖ es 4I.9 λ + λ ϖ e s 4I.0 λ + λ ϖ 4ess 4I. λ + λ ϖ e ss 4I. λ + λ ϖ es 4I. λ + λ ϖ e s 4D4. jλ + (4 j)λ ϖ ϖ e e f 9 4D4. jλ + (4 j)λ ϖ ϖ e e f 9 4D4.4 jλ + (4 j)λ ϖ ϖ ee f 9 4D4.5 jλ + (4 j)λ 4ϖ e 4 f 94 4D4.6 jλ + (4 j)λ ϖ e s f 95 4D4. jλ + (4 j)λ ϖ ϖ ee s f 96 4D4.8 jλ + (4 j)λ ϖ e s f 9 4D4.9 jλ + (4 j)λ 4 s 4 f 98 4D4.0 jλ + (4 j)λ ϖ e ss f 99 4D4. jλ + (4 j)λ ϖ ϖ ee ss f 00 4D4. jλ + (4 j)λ ϖ e ss f 0 4D4. jλ + (4 j)λ s s f 0 4D4.4 jλ + (4 j)λ ϖ e s f 95 4D4.5 jλ + (4 j)λ ϖ ϖ ee s f 96 4D4.6 jλ + (4 j)λ ϖ e s f 9 4D4. jλ + (4 j)λ s s f 0 4D4.8 jλ + (4 j)λ ss f 0 4D4.9 jλ + (4 j)λ 4 s 4 f 98

Orbital and Celestial Mechanics

Orbital and Celestial Mechanics Orbital and Celestial Mechanics John P. Vinti Edited by Gim J. Der TRW Los Angeles, California Nino L. Bonavito NASA Goddard Space Flight Center Greenbelt, Maryland Volume 177 PROGRESS IN ASTRONAUTICS

More information

An Introduction to Celestial Mechanics

An Introduction to Celestial Mechanics An Introduction to Celestial Mechanics This accessible text on classical celestial mechanics the principles governing the motions of bodies in the solar system provides a clear and concise treatment of

More information

Resonance and chaos ASTRONOMY AND ASTROPHYSICS. II. Exterior resonances and asymmetric libration

Resonance and chaos ASTRONOMY AND ASTROPHYSICS. II. Exterior resonances and asymmetric libration Astron. Astrophys. 328, 399 48 (1997) ASTRONOMY AND ASTROPHYSICS Resonance and chaos II. Exterior resonances and asymmetric libration O.C. Winter 1,2 and C.D. Murray 2 1 Grupo de Dinâmica Orbital e Planetologia,

More information

The precession of the perihelion of Mercury explained by Celestial Mechanics of Laplace Valdir Monteiro dos Santos Godoi

The precession of the perihelion of Mercury explained by Celestial Mechanics of Laplace Valdir Monteiro dos Santos Godoi The precession of the perihelion of Mercury explained by Celestial Mechanics of Laplace Valdir Monteiro dos Santos Godoi valdir.msgodoi@gmail.com ABSTRACT We calculate in this article an exact theoretical

More information

Symplectic Correctors for Canonical Heliocentric N-Body Maps

Symplectic Correctors for Canonical Heliocentric N-Body Maps Symplectic Correctors for Canonical Heliocentric N-Body Maps J. Wisdom Massachusetts Institute of Technology, Cambridge, MA 02139 wisdom@poincare.mit.edu Received ; accepted 2 ABSTRACT Symplectic correctors

More information

A STUDY OF CLOSE ENCOUNTERS BETWEEN MARS AND ASTEROIDS FROM THE 3:1 RESONANCE. Érica C. Nogueira, Othon C. Winter

A STUDY OF CLOSE ENCOUNTERS BETWEEN MARS AND ASTEROIDS FROM THE 3:1 RESONANCE. Érica C. Nogueira, Othon C. Winter A STUDY OF CLOSE ENCOUNTERS BETWEEN MARS AND ASTEROIDS FROM THE 3: RESONANCE Érica C. Nogueira, Othon C. Winter Grupo de Dinâmica Orbital e Planetologia UNESP -- Guaratinguetá -- Brazil Antonio F.B. de

More information

Third Body Perturbation

Third Body Perturbation Third Body Perturbation p. 1/30 Third Body Perturbation Modeling the Space Environment Manuel Ruiz Delgado European Masters in Aeronautics and Space E.T.S.I. Aeronáuticos Universidad Politécnica de Madrid

More information

Theory of mean motion resonances.

Theory of mean motion resonances. Theory of mean motion resonances. Mean motion resonances are ubiquitous in space. They can be found between planets and asteroids, planets and rings in gaseous disks or satellites and planetary rings.

More information

Research Article Variation of the Equator due to a Highly Inclined and Eccentric Disturber

Research Article Variation of the Equator due to a Highly Inclined and Eccentric Disturber Hindawi Publishing Corporation Mathematical Problems in Engineering Volume 009, Article ID 467865, 10 pages doi:10.1155/009/467865 Research Article Variation of the Equator due to a Highly Inclined and

More information

THIRD-BODY PERTURBATION USING A SINGLE AVERAGED MODEL

THIRD-BODY PERTURBATION USING A SINGLE AVERAGED MODEL INPE-1183-PRE/67 THIRD-BODY PERTURBATION USING A SINGLE AVERAGED MODEL Carlos Renato Huaura Solórzano Antonio Fernando Bertachini de Almeida Prado ADVANCES IN SPACE DYNAMICS : CELESTIAL MECHANICS AND ASTRONAUTICS,

More information

Planetenbewegung in Sternsystemen. The Effect of Resonances. Part 2

Planetenbewegung in Sternsystemen. The Effect of Resonances. Part 2 Planetenbewegung in Sternsystemen The Effect of Resonances Part 2 Topics overview 1. Definition and examples of resonances 2. Disturbing function 3. Mean-motion resonance (MMR) 4. Secular resonance (SR)

More information

Research Article Dynamics of Artificial Satellites around Europa

Research Article Dynamics of Artificial Satellites around Europa Mathematical Problems in Engineering Volume 2013, Article ID 182079, 7 pages http://dx.doi.org/10.1155/2013/182079 Research Article Dynamics of Artificial Satellites around Europa Jean Paulo dos Santos

More information

Dynamical properties of the Solar System. Second Kepler s Law. Dynamics of planetary orbits. ν: true anomaly

Dynamical properties of the Solar System. Second Kepler s Law. Dynamics of planetary orbits. ν: true anomaly First Kepler s Law The secondary body moves in an elliptical orbit, with the primary body at the focus Valid for bound orbits with E < 0 The conservation of the total energy E yields a constant semi-major

More information

Resonance Capture. Alice Quillen. University of Rochester. Isaac Newton Institute Dec 2009

Resonance Capture. Alice Quillen. University of Rochester. Isaac Newton Institute Dec 2009 Resonance Capture Alice Quillen University of Rochester Isaac Newton Institute Dec 2009 This Talk Resonance Capture extension to nonadiabatic regime Astrophysical settings: Dust spiraling inward via radiation

More information

arxiv: v2 [astro-ph.ep] 28 Sep 2017

arxiv: v2 [astro-ph.ep] 28 Sep 2017 Noname manuscript No. (will be inserted by the editor) Tilting Styx and Nix but not Uranus with a Spin-Precession-Mean-motion resonance Alice C. Quillen 1, Yuan-Yuan Chen 1,2, Benoît Noyelles 3, & Santiago

More information

EFFICIENT INTEGRATION OF HIGHLY ECCENTRIC ORBITS BY QUADRUPLE SCALING FOR KUSTAANHEIMO-STIEFEL REGULARIZATION

EFFICIENT INTEGRATION OF HIGHLY ECCENTRIC ORBITS BY QUADRUPLE SCALING FOR KUSTAANHEIMO-STIEFEL REGULARIZATION The Astronomical Journal, 128:3108 3113, 2004 December # 2004. The American Astronomical Society. All rights reserved. Printed in U.S.A. EFFICIENT INTEGRATION OF HIGHLY ECCENTRIC ORBITS BY QUADRUPLE SCALING

More information

ORBITAL CHARACTERISTICS DUE TO THE THREE DIMENSIONAL SWING-BY IN THE SUN-JUPITER SYSTEM

ORBITAL CHARACTERISTICS DUE TO THE THREE DIMENSIONAL SWING-BY IN THE SUN-JUPITER SYSTEM ORBITAL CHARACTERISTICS DUE TO THE THREE DIMENSIONAL SWING-BY IN THE SUN-JUPITER SYSTEM JORGE K. S. FORMIGA 1,2 and ANTONIO F B A PRADO 2 National Institute for Space Research -INPE 1 Technology Faculty-FATEC-SJC

More information

Analysis of frozen orbits for solar sails

Analysis of frozen orbits for solar sails Trabalho apresentado no XXXV CNMAC, Natal-RN, 2014. Analysis of frozen orbits for solar sails J. P. S. Carvalho, R. Vilhena de Moraes, Instituto de Ciência e Tecnologia, UNIFESP, São José dos Campos -

More information

THE PLANE OF THE KUIPER BELT

THE PLANE OF THE KUIPER BELT The Astronomical Journal, 127:2418 2423, 2004 April # 2004. The American Astronomical Society. All rights reserved. Printed in U.S.A. THE PLANE OF THE KUIPER BELT Michael E. Brown Division of Geological

More information

ISIMA lectures on celestial mechanics. 3

ISIMA lectures on celestial mechanics. 3 ISIMA lectures on celestial mechanics. 3 Scott Tremaine, Institute for Advanced Study July 2014 1. The stability of planetary systems To understand the formation and evolution of exoplanet systems, we

More information

Tutorial on obtaining Taylor Series Approximations without differentiation

Tutorial on obtaining Taylor Series Approximations without differentiation Tutorial on obtaining Taylor Series Approximations without differentiation Professor Henry Greenside February 2, 2018 1 Overview An important mathematical technique that is used many times in physics,

More information

The behavior of the AZ and QZ solutions in Figure 3 shows only dierences of

The behavior of the AZ and QZ solutions in Figure 3 shows only dierences of years; the latter is magnied by about a factor of 50 for better visualization. The reduced solution has a high and a low eccentricity state with regular and fast transitions between them. Its phase is

More information

Some Notes on Linear Algebra

Some Notes on Linear Algebra Some Notes on Linear Algebra prepared for a first course in differential equations Thomas L Scofield Department of Mathematics and Statistics Calvin College 1998 1 The purpose of these notes is to present

More information

Physics 342 Lecture 23. Radial Separation. Lecture 23. Physics 342 Quantum Mechanics I

Physics 342 Lecture 23. Radial Separation. Lecture 23. Physics 342 Quantum Mechanics I Physics 342 Lecture 23 Radial Separation Lecture 23 Physics 342 Quantum Mechanics I Friday, March 26th, 2010 We begin our spherical solutions with the simplest possible case zero potential. Aside from

More information

HM NAUTICAL ALMANAC OFFICE NAO TECHNICAL N OTE

HM NAUTICAL ALMANAC OFFICE NAO TECHNICAL N OTE Council for the Central Laboratory of the Research Councils HM NAUTICAL ALMANAC OFFICE NAO TECHNICAL N OTE No. 73 2003 June Approximate ephemerides and phenomena of natural satellites by D.B. Taylor and

More information

arxiv: v1 [astro-ph.ep] 3 Apr 2018

arxiv: v1 [astro-ph.ep] 3 Apr 2018 Astronomy& Astrophysics manuscript no. zanardi_ c ESO 28 September 2, 28 The role of the general relativity on icy body reservoirs under the effects of an inner eccentric Jupiter M. Zanardi, 2, G. C. de

More information

The dynamics of Plutinos

The dynamics of Plutinos The dynamics of Plutinos Qingjuan Yu and Scott Tremaine Princeton University Observatory, Peyton Hall, Princeton, NJ 08544-1001, USA ABSTRACT Plutinos are Kuiper-belt objects that share the 3:2 Neptune

More information

SOME CONGRUENCES ASSOCIATED WITH THE EQUATION X α = X β IN CERTAIN FINITE SEMIGROUPS

SOME CONGRUENCES ASSOCIATED WITH THE EQUATION X α = X β IN CERTAIN FINITE SEMIGROUPS SOME CONGRUENCES ASSOCIATED WITH THE EQUATION X α = X β IN CERTAIN FINITE SEMIGROUPS THOMAS W. MÜLLER Abstract. Let H be a finite group, T n the symmetric semigroup of degree n, and let α, β be integers

More information

PRECALCULUS BISHOP KELLY HIGH SCHOOL BOISE, IDAHO. Prepared by Kristina L. Gazdik. March 2005

PRECALCULUS BISHOP KELLY HIGH SCHOOL BOISE, IDAHO. Prepared by Kristina L. Gazdik. March 2005 PRECALCULUS BISHOP KELLY HIGH SCHOOL BOISE, IDAHO Prepared by Kristina L. Gazdik March 2005 1 TABLE OF CONTENTS Course Description.3 Scope and Sequence 4 Content Outlines UNIT I: FUNCTIONS AND THEIR GRAPHS

More information

A REGION VOID OF IRREGULAR SATELLITES AROUND JUPITER

A REGION VOID OF IRREGULAR SATELLITES AROUND JUPITER The Astronomical Journal, 136:909 918, 2008 September c 2008. The American Astronomical Society. All rights reserved. Printed in the U.S.A. doi:10.1088/0004-6256/136/3/909 A REGION VOID OF IRREGULAR SATELLITES

More information

Satellite Communications

Satellite Communications Satellite Communications Lecture (3) Chapter 2.1 1 Gravitational Force Newton s 2nd Law: r r F = m a Newton s Law Of Universal Gravitation (assuming point masses or spheres): Putting these together: r

More information

Analysis of Lunisolar Resonances. in an Artificial Satellite Orbits

Analysis of Lunisolar Resonances. in an Artificial Satellite Orbits Applied Mathematical Sciences, Vol., 008, no., 0 0 Analysis of Lunisolar Resonances in an Artificial Satellite Orbits F. A. Abd El-Salam, Yehia A. Abdel-Aziz,*, M. El-Saftawy, and M. Radwan Cairo university,

More information

Secular dynamics of extrasolar-systems

Secular dynamics of extrasolar-systems Secular dynamics of extrasolar-systems Marco Sansottera [1] [1] Università degli Studi di Milano [2] Namur Center for Complex Systems (naxys) Based on a research project in collaboration with A.-S. Libert

More information

Lecture 13. Gravity in the Solar System

Lecture 13. Gravity in the Solar System Lecture 13 Gravity in the Solar System Guiding Questions 1. How was the heliocentric model established? What are monumental steps in the history of the heliocentric model? 2. How do Kepler s three laws

More information

Stability of the Lagrange Points, L 4 and L 5

Stability of the Lagrange Points, L 4 and L 5 Stability of the Lagrange Points, L 4 and L 5 Thomas Greenspan January 7, 014 Abstract A proof of the stability of the non collinear Lagrange Points, L 4 and L 5. We will start by covering the basics of

More information

HAMILTONIAN STABILITY OF SPIN ORBIT RESONANCES IN CELESTIAL MECHANICS. 1. Introduction

HAMILTONIAN STABILITY OF SPIN ORBIT RESONANCES IN CELESTIAL MECHANICS. 1. Introduction HAMILTONIAN STABILITY OF SPIN ORBIT RESONANCES IN CELESTIAL MECHANICS ALESSANDRA CELLETTI 1 and LUIGI CHIERCHIA 2 1 Dipartimento di Matematica, Università di Roma Tor Vergata, Via della Ricerca Scientifica,

More information

INVESTIGATION OF ORBITAL EVOLUTION OF INTERPLANETARY DUST PARTICLES ORIGINATING FROM KUIPER BELT AND ASTEROID BELT OBJECTS

INVESTIGATION OF ORBITAL EVOLUTION OF INTERPLANETARY DUST PARTICLES ORIGINATING FROM KUIPER BELT AND ASTEROID BELT OBJECTS INVESTIGATION OF ORBITAL EVOLUTION OF INTERPLANETARY DUST PARTICLES ORIGINATING FROM KUIPER BELT AND ASTEROID BELT OBJECTS 1 PALAK DHARSANDIA, 2 DR. JAYESH PABARI, 3 DR. CHARMY PATEL 1 Research Scholar,

More information

Towards stability results for planetary problems with more than three bodies

Towards stability results for planetary problems with more than three bodies Towards stability results for planetary problems with more than three bodies Ugo Locatelli [a] and Marco Sansottera [b] [a] Math. Dep. of Università degli Studi di Roma Tor Vergata [b] Math. Dep. of Università

More information

Searching for less perturbed elliptical orbits around Europa

Searching for less perturbed elliptical orbits around Europa Journal of Physics: Conference Series PAPER OPEN ACCESS Searching for less perturbed elliptical orbits around Europa To cite this article: J Cardoso dos Santos et al 2015 J. Phys.: Conf. Ser. 641 012011

More information

A SYMPLECTIC MAPPING MODEL FOR THE STUDY OF 2:3 RESONANT TRANS-NEPTUNIAN MOTION

A SYMPLECTIC MAPPING MODEL FOR THE STUDY OF 2:3 RESONANT TRANS-NEPTUNIAN MOTION 3 A SYMPLECTIC MAPPING MODEL FOR THE STUDY OF 2:3 RESONANT TRANS-NEPTUNIAN MOTION K.G. HADJIFOTINOU and JOHN D. HADJIDEMETRIOU Department of Physics, University of Thessaloniki, 540 06 Thessaloniki, Greece

More information

orbits Moon, Planets Spacecrafts Calculating the and by Dr. Shiu-Sing TONG

orbits Moon, Planets Spacecrafts Calculating the and by Dr. Shiu-Sing TONG A Science Enrichment Programme for Secondary 3-4 Students : Teaching and Learning Resources the and Spacecrafts orbits Moon, Planets Calculating the 171 of by Dr. Shiu-Sing TONG 172 Calculating the orbits

More information

Introduction to tensors and dyadics

Introduction to tensors and dyadics 1 Introduction to tensors and dyadics 1.1 Introduction Tensors play a fundamental role in theoretical physics. The reason for this is that physical laws written in tensor form are independent of the coordinate

More information

A connection between number theory and linear algebra

A connection between number theory and linear algebra A connection between number theory and linear algebra Mark Steinberger Contents 1. Some basics 1 2. Rational canonical form 2 3. Prime factorization in F[x] 4 4. Units and order 5 5. Finite fields 7 6.

More information

5.4 Bessel s Equation. Bessel Functions

5.4 Bessel s Equation. Bessel Functions SEC 54 Bessel s Equation Bessel Functions J (x) 87 # with y dy>dt, etc, constant A, B, C, D, K, and t 5 HYPERGEOMETRIC ODE At B (t t )(t t ), t t, can be reduced to the hypergeometric equation with independent

More information

Linear Algebra. The analysis of many models in the social sciences reduces to the study of systems of equations.

Linear Algebra. The analysis of many models in the social sciences reduces to the study of systems of equations. POLI 7 - Mathematical and Statistical Foundations Prof S Saiegh Fall Lecture Notes - Class 4 October 4, Linear Algebra The analysis of many models in the social sciences reduces to the study of systems

More information

The Three Body Problem

The Three Body Problem The Three Body Problem Joakim Hirvonen Grützelius Karlstad University December 26, 2004 Department of Engineeringsciences, Physics and Mathematics 5p Examinator: Prof Jürgen Füchs Abstract The main topic

More information

THE exploration of planetary satellites is currently an active area

THE exploration of planetary satellites is currently an active area JOURNAL OF GUIDANCE, CONTROL, AND DYNAMICS Vol. 9, No. 5, September October 6 Design of Science Orbits About Planetary Satellites: Application to Europa Marci E. Paskowitz and Daniel J. Scheeres University

More information

In this work is used the version of the Mathematica software for Windows environment. The examples which are treated are "generic" and should ex

In this work is used the version of the Mathematica software for Windows environment. The examples which are treated are generic and should ex How to Use Mathematica to Solve Typical Problems in Celestial Mechanics D.C. Lob~ao y Λ y Instituto de Pesquisa e Desenvolvimento IPD Universidade do Vale do Para ba UNIVAP S~ao José dos Campos, SP Brasil

More information

0.1 Rational Canonical Forms

0.1 Rational Canonical Forms We have already seen that it is useful and simpler to study linear systems using matrices. But matrices are themselves cumbersome, as they are stuffed with many entries, and it turns out that it s best

More information

ELEMENTARY LINEAR ALGEBRA

ELEMENTARY LINEAR ALGEBRA ELEMENTARY LINEAR ALGEBRA K. R. MATTHEWS DEPARTMENT OF MATHEMATICS UNIVERSITY OF QUEENSLAND Second Online Version, December 1998 Comments to the author at krm@maths.uq.edu.au Contents 1 LINEAR EQUATIONS

More information

Orbital Evolution in Extra-solar systems

Orbital Evolution in Extra-solar systems Orbital Evolution in Extra-solar systems George Voyatzis Section of Astronomy, Astrophysics and Mechanics, Department of Physics, Aristotle University of Thessaloniki, Greece. Abstract Nowadays, extra-solar

More information

Two special equations: Bessel s and Legendre s equations. p Fourier-Bessel and Fourier-Legendre series. p

Two special equations: Bessel s and Legendre s equations. p Fourier-Bessel and Fourier-Legendre series. p LECTURE 1 Table of Contents Two special equations: Bessel s and Legendre s equations. p. 259-268. Fourier-Bessel and Fourier-Legendre series. p. 453-460. Boundary value problems in other coordinate system.

More information

ISIMA lectures on celestial mechanics. 1

ISIMA lectures on celestial mechanics. 1 ISIMA lectures on celestial mechanics. 1 Scott Tremaine, Institute for Advanced Study July 2014 The roots of solar system dynamics can be traced to two fundamental discoveries by Isaac Newton: first, that

More information

PURE Math Residents Program Gröbner Bases and Applications Week 3 Lectures

PURE Math Residents Program Gröbner Bases and Applications Week 3 Lectures PURE Math Residents Program Gröbner Bases and Applications Week 3 Lectures John B. Little Department of Mathematics and Computer Science College of the Holy Cross June 2012 Overview of this week The research

More information

d 1 µ 2 Θ = 0. (4.1) consider first the case of m = 0 where there is no azimuthal dependence on the angle φ.

d 1 µ 2 Θ = 0. (4.1) consider first the case of m = 0 where there is no azimuthal dependence on the angle φ. 4 Legendre Functions In order to investigate the solutions of Legendre s differential equation d ( µ ) dθ ] ] + l(l + ) m dµ dµ µ Θ = 0. (4.) consider first the case of m = 0 where there is no azimuthal

More information

Planetary system dynamics. Planetary migration Kozai resonance Apsidal resonance and secular theories Mean motion resonances Gravitational scattering

Planetary system dynamics. Planetary migration Kozai resonance Apsidal resonance and secular theories Mean motion resonances Gravitational scattering Planetary system dynamics Planetary migration Kozai resonance Apsidal resonance and secular theories Mean motion resonances Gravitational scattering How should the planets of a typical planetary system

More information

GATE Engineering Mathematics SAMPLE STUDY MATERIAL. Postal Correspondence Course GATE. Engineering. Mathematics GATE ENGINEERING MATHEMATICS

GATE Engineering Mathematics SAMPLE STUDY MATERIAL. Postal Correspondence Course GATE. Engineering. Mathematics GATE ENGINEERING MATHEMATICS SAMPLE STUDY MATERIAL Postal Correspondence Course GATE Engineering Mathematics GATE ENGINEERING MATHEMATICS ENGINEERING MATHEMATICS GATE Syllabus CIVIL ENGINEERING CE CHEMICAL ENGINEERING CH MECHANICAL

More information

arxiv: v3 [astro-ph.im] 23 Nov 2016

arxiv: v3 [astro-ph.im] 23 Nov 2016 Celestial Mechanics and Dynamical Astronomy manuscript No. (will be inserted by the editor) Andoyer construction for Hill and Delaunay variables Jacques Laskar arxiv:1409.5880v3 [astro-ph.im] 23 Nov 2016

More information

CALCULATION OF POSITION AND VELOCITY OF GLONASS SATELLITE BASED ON ANALYTICAL THEORY OF MOTION

CALCULATION OF POSITION AND VELOCITY OF GLONASS SATELLITE BASED ON ANALYTICAL THEORY OF MOTION ARTIFICIAL SATELLITES, Vol. 50, No. 3 2015 DOI: 10.1515/arsa-2015-0008 CALCULATION OF POSITION AND VELOCITY OF GLONASS SATELLITE BASED ON ANALYTICAL THEORY OF MOTION W. Góral, B. Skorupa AGH University

More information

Analytical Mechanics. of Space Systems. tfa AA. Hanspeter Schaub. College Station, Texas. University of Colorado Boulder, Colorado.

Analytical Mechanics. of Space Systems. tfa AA. Hanspeter Schaub. College Station, Texas. University of Colorado Boulder, Colorado. Analytical Mechanics of Space Systems Third Edition Hanspeter Schaub University of Colorado Boulder, Colorado John L. Junkins Texas A&M University College Station, Texas AIM EDUCATION SERIES Joseph A.

More information

Chapter One Hilbert s 7th Problem: It s statement and origins

Chapter One Hilbert s 7th Problem: It s statement and origins Chapter One Hilbert s 7th Problem: It s statement and origins At the second International Congress of athematicians in Paris, 900, the mathematician David Hilbert was invited to deliver a keynote address,

More information

A practical method for enumerating cosets of a finite abstract group

A practical method for enumerating cosets of a finite abstract group A practical method for enumerating cosets of a finite abstract group By J. A. ODD (University of Manchester), and H.. M. COXBEB (University of Cambridge). (Received nd January,. Mead th February,.) Introduction.

More information

Computational Astrophysics

Computational Astrophysics Computational Astrophysics Lecture 1: Introduction to numerical methods Lecture 2: The SPH formulation Lecture 3: Construction of SPH smoothing functions Lecture 4: SPH for general dynamic flow Lecture

More information

Planetary Perturbations on the 2 : 3 Mean Motion Resonance with Neptune

Planetary Perturbations on the 2 : 3 Mean Motion Resonance with Neptune PASJ: Publ. Astron. Soc. Japan 54, 493 499, 2002 June 25 c 2002. Astronomical Society of Japan. Planetary Perturbations on the 2 : 3 Mean Motion Resonance with Neptune Tetsuharu FUSE Subaru Telescope,

More information

EART162: PLANETARY INTERIORS

EART162: PLANETARY INTERIORS EART162: PLANETARY INTERIORS Francis Nimmo Last Week Applications of fluid dynamics to geophysical problems Navier-Stokes equation describes fluid flow: Convection requires solving the coupled equations

More information

On the Estimated Precession of Mercury s Orbit

On the Estimated Precession of Mercury s Orbit 1 On the Estimated Precession of Mercury s Orbit R. Wayte. 9 Audley Way, Ascot, Berkshire, SL5 8EE, England, UK e-mail: rwayte@googlemail.com Research Article, Submitted to PMC Physics A 4 Nov 009 Abstract.

More information

EFFECTS OF DIRECT AND INDIRECT SOLAR RADIATION PRESSURE IN ORBITAL PARAMETERS OF GPS SATELITTES

EFFECTS OF DIRECT AND INDIRECT SOLAR RADIATION PRESSURE IN ORBITAL PARAMETERS OF GPS SATELITTES DOI: 10.2478/auom-2014-0039 An. Şt. Univ. Ovidius Constanţa Vol. 22(2),2014, 141 150 EFFECTS OF DIRECT AND INDIRECT SOLAR RADIATION PRESSURE IN ORBITAL PARAMETERS OF GPS SATELITTES Sergiu Lupu and Eugen

More information

Mathematics Syllabus UNIT I ALGEBRA : 1. SETS, RELATIONS AND FUNCTIONS

Mathematics Syllabus UNIT I ALGEBRA : 1. SETS, RELATIONS AND FUNCTIONS Mathematics Syllabus UNIT I ALGEBRA : 1. SETS, RELATIONS AND FUNCTIONS (i) Sets and their Representations: Finite and Infinite sets; Empty set; Equal sets; Subsets; Power set; Universal set; Venn Diagrams;

More information

Today in Astronomy 111: rings, gaps and orbits

Today in Astronomy 111: rings, gaps and orbits Today in Astronomy 111: rings, gaps and orbits Gap sizes: the Hill radius Perturbations and resonances The variety of structures in planetary rings Spiral density waves Titan Bending waves Horseshoe and

More information

Fundamentals of Astrodynamics and Applications

Fundamentals of Astrodynamics and Applications Fundamentals of Astrodynamics and Applications Third Edition David A. Vallado with technical contributions by Wayne D. McClain Space Technology Library Published Jointly by Microcosm Press Hawthorne, CA

More information

A first order divided difference

A first order divided difference A first order divided difference For a given function f (x) and two distinct points x 0 and x 1, define f [x 0, x 1 ] = f (x 1) f (x 0 ) x 1 x 0 This is called the first order divided difference of f (x).

More information

THE CURIOUSLY WARPED MEAN PLANE OF THE KUIPER BELT

THE CURIOUSLY WARPED MEAN PLANE OF THE KUIPER BELT Draft version September 17, 217 Typeset using LATEX default style in AASTeX61 THE CURIOUSLY WARPED MEAN PLANE OF THE KUIPER BELT Kathryn Volk 1 and Renu Malhotra 1 1 Lunar and Planetary Laboratory, The

More information

ELEMENTARY LINEAR ALGEBRA

ELEMENTARY LINEAR ALGEBRA ELEMENTARY LINEAR ALGEBRA K R MATTHEWS DEPARTMENT OF MATHEMATICS UNIVERSITY OF QUEENSLAND First Printing, 99 Chapter LINEAR EQUATIONS Introduction to linear equations A linear equation in n unknowns x,

More information

The Mars 1:2 Resonant Population. Tabaré Gallardo.

The Mars 1:2 Resonant Population. Tabaré Gallardo. 1 The Mars 1:2 Resonant Population Tabaré Gallardo Departamento de Astronomía, Facultad de Ciencias, Iguá 4225, 11400 Montevideo, Uruguay gallardo@fisica.edu.uy Icarus, in press May 2007 2 Abstract An

More information

Observational Astronomy - Lecture 4 Orbits, Motions, Kepler s and Newton s Laws

Observational Astronomy - Lecture 4 Orbits, Motions, Kepler s and Newton s Laws Observational Astronomy - Lecture 4 Orbits, Motions, Kepler s and Newton s Laws Craig Lage New York University - Department of Physics craig.lage@nyu.edu February 24, 2014 1 / 21 Tycho Brahe s Equatorial

More information

FUNCTIONS OVER THE RESIDUE FIELD MODULO A PRIME. Introduction

FUNCTIONS OVER THE RESIDUE FIELD MODULO A PRIME. Introduction FUNCTIONS OVER THE RESIDUE FIELD MODULO A PRIME DAVID LONDON and ZVI ZIEGLER (Received 7 March 966) Introduction Let F p be the residue field modulo a prime number p. The mappings of F p into itself are

More information

Previous Lecture. The Von Zeipel Method. Application 1: The Brouwer model. Application 2: The Cid-Lahulla model. Simplified Brouwer transformation.

Previous Lecture. The Von Zeipel Method. Application 1: The Brouwer model. Application 2: The Cid-Lahulla model. Simplified Brouwer transformation. 2 / 36 Previous Lecture The Von Zeipel Method. Application 1: The Brouwer model. Application 2: The Cid-Lahulla model. Simplified Brouwer transformation. Review of Analytic Models 3 / 36 4 / 36 Review:

More information

Shijun Liao. Homotopy Analysis Method in Nonlinear Differential Equations

Shijun Liao. Homotopy Analysis Method in Nonlinear Differential Equations Shijun Liao Homotopy Analysis Method in Nonlinear Differential Equations Shijun Liao Homotopy Analysis Method in Nonlinear Differential Equations With 127 figures Author Shijun Liao Shanghai Jiao Tong

More information

Research Article Geodesic Effect Near an Elliptical Orbit

Research Article Geodesic Effect Near an Elliptical Orbit Applied Mathematics Volume 2012, Article ID 240459, 8 pages doi:10.1155/2012/240459 Research Article Geodesic Effect Near an Elliptical Orbit Alina-Daniela Vîlcu Department of Information Technology, Mathematics

More information

Long-Term Evolution of High Earth Orbits: Effects of Direct Solar Radiation Pressure and Comparison of Trajectory Propagators

Long-Term Evolution of High Earth Orbits: Effects of Direct Solar Radiation Pressure and Comparison of Trajectory Propagators Long-Term Evolution of High Earth Orbits: Effects of Direct Solar Radiation Pressure and Comparison of Trajectory Propagators by L. Anselmo and C. Pardini (Luciano.Anselmo@isti.cnr.it & Carmen.Pardini@isti.cnr.it)

More information

a 11 x 1 + a 12 x a 1n x n = b 1 a 21 x 1 + a 22 x a 2n x n = b 2.

a 11 x 1 + a 12 x a 1n x n = b 1 a 21 x 1 + a 22 x a 2n x n = b 2. Chapter 1 LINEAR EQUATIONS 11 Introduction to linear equations A linear equation in n unknowns x 1, x,, x n is an equation of the form a 1 x 1 + a x + + a n x n = b, where a 1, a,, a n, b are given real

More information

The 3 dimensional Schrödinger Equation

The 3 dimensional Schrödinger Equation Chapter 6 The 3 dimensional Schrödinger Equation 6.1 Angular Momentum To study how angular momentum is represented in quantum mechanics we start by reviewing the classical vector of orbital angular momentum

More information

Unit VIII Matrices, Eigenvalues and Eigenvectors

Unit VIII Matrices, Eigenvalues and Eigenvectors Unit VIII Matrices, Eigenvalues and Eigenvectors These materials were developed for use at Grinnell College and neither Grinnell College nor the author, Mark Schneider, assume any responsibility for their

More information

Review of Vector Analysis in Cartesian Coordinates

Review of Vector Analysis in Cartesian Coordinates Review of Vector Analysis in Cartesian Coordinates 1 Scalar: A quantity that has magnitude, but no direction. Examples are mass, temperature, pressure, time, distance, and real numbers. Scalars are usually

More information

exceptional value turns out to be, "RAC" CURVATURE calling attention especially to the fundamental Theorem III, and to emphasize

exceptional value turns out to be, RAC CURVATURE calling attention especially to the fundamental Theorem III, and to emphasize VOL. 18, 1932 V,MA THEMA TICS: E. KASNER 267 COMPLEX GEOMETRY AND RELATIVITY: "RAC" CURVATURE BY EDWARD KASNER DEPARTMENT OF MATHEMATICS, COLUMBIA UNIVERSITY Communicated February 3, 1932 THEORY OF THE

More information

EXTENDING NACOZY S APPROACH TO CORRECT ALL ORBITAL ELEMENTS FOR EACH OF MULTIPLE BODIES

EXTENDING NACOZY S APPROACH TO CORRECT ALL ORBITAL ELEMENTS FOR EACH OF MULTIPLE BODIES The Astrophysical Journal, 687:1294Y1302, 2008 November 10 # 2008. The American Astronomical Society. All rights reserved. Printed in U.S.A. EXTENDING NACOZY S APPROACH TO CORRECT ALL ORBITAL ELEMENTS

More information

CHAPTER XVI The search for consistency for intricate exponential algebras.

CHAPTER XVI The search for consistency for intricate exponential algebras. 16.1. Introduction. CHAPTER XVI The Dw hyperintricate exponential algebras We use the hyperintricate representation of matrices and explore exponentiation for these objects. Proofs by contradiction are

More information

Extrasolar Planets in Mean-Motion Resonance: Apses Alignment and Asymmetric Stationary Solutions

Extrasolar Planets in Mean-Motion Resonance: Apses Alignment and Asymmetric Stationary Solutions Submitted to Astrophysical Journal Extrasolar Planets in Mean-Motion Resonance: Apses Alignment and Asymmetric Stationary Solutions C. Beaugé 1 Observatorio Astronómico, Universidad Nacional de Córdoba,

More information

This pre-publication material is for review purposes only. Any typographical or technical errors will be corrected prior to publication.

This pre-publication material is for review purposes only. Any typographical or technical errors will be corrected prior to publication. This pre-publication material is for review purposes only. Any typographical or technical errors will be corrected prior to publication. Copyright Pearson Canada Inc. All rights reserved. Copyright Pearson

More information

Long term orbital inclination and eccentricity oscillations of the. planets in our solar system

Long term orbital inclination and eccentricity oscillations of the. planets in our solar system Long term orbital inclination and eccentricity oscillations of the Abstract planets in our solar system The orbits of the planets in our solar system are not in the same plane, therefore natural torques

More information

Earth-Centered, Earth-Fixed Coordinate System

Earth-Centered, Earth-Fixed Coordinate System Fundamentals of Global Positioning System Receivers: A Software Approach James Bao-Yen Tsui Copyright 2000 John Wiley & Sons, Inc. Print ISBN 0-471-38154-3 Electronic ISBN 0-471-20054-9 CHAPTER FOUR Earth-Centered,

More information

The Theory of the Lunar Motion

The Theory of the Lunar Motion The Theory of the Lunar Motion (Lunar cycles) V. D. Krasnov E-mail: apeyron7@yandex.ru Abstract Continuous attempts to create theories of the Moon's motion have been made since the time of Isaac Newton.

More information

WILLIAM I. NEWMAN, UCLA PHILIP W. SHARP, U. OF AUCKLAND BRUCE G. BILLS, JPL

WILLIAM I. NEWMAN, UCLA PHILIP W. SHARP, U. OF AUCKLAND BRUCE G. BILLS, JPL CATASTROPHIC METEORITE 1 IMPACTS ON EARTH WILLIAM I. NEWMAN, UCLA PHILIP W. SHARP, U. OF AUCKLAND BRUCE G. BILLS, JPL Solar system with different scales for distance and for size: presents role of giant

More information

A Kozai-resonating Earth quasi-satellite

A Kozai-resonating Earth quasi-satellite MNRASL 437, L85 L89 (2014) Advance Access publication 2013 November 13 doi:10.1093/mnrasl/slt147 A Kozai-resonating Earth quasi-satellite M. Connors Athabasca University Observatories, Athabasca AB T9S

More information

DIFFUSION OF ASTEROIDS IN MEAN MOTION RESONANCES

DIFFUSION OF ASTEROIDS IN MEAN MOTION RESONANCES DIFFUSION OF ASTEROIDS IN MEAN MOTION RESONANCES KLEOMENIS TSIGANIS and HARRY VARVOGLIS Section of Astrophysics, Astronomy and Mechanics, Department of Physics, University of Thessaloniki, 540 06 Thessaloniki,

More information

Perihelion Precession in the Solar System

Perihelion Precession in the Solar System International Journal of Multidisciplinary Current Research ISSN: 2321-3124 Research Article Available at: http://ijmcr.com Sara Kanzi * Hamed Ghasemian! * Currently pursuing Ph.D. degree program in Physics

More information

DYNAMICS OF THE LUNAR SPIN AXIS

DYNAMICS OF THE LUNAR SPIN AXIS The Astronomical Journal, 131:1864 1871, 2006 March # 2006. The American Astronomical Society. All rights reserved. Printed in U.S.A. DYNAMICS OF THE LUNAR SPIN AXIS Jack Wisdom Massachusetts Institute

More information

Secular Evolution of Extrasolar Planetary Systems:

Secular Evolution of Extrasolar Planetary Systems: Secular Evolution of Extrasolar Planetary Systems: an Extension of the Laplace-Lagrange Secular Theory Marco Sansottera [a] [a] Namur Center for Complex Systems (naxys) Based on a research work in collaboration

More information

Symbolic Solution of Kepler s Generalized Equation

Symbolic Solution of Kepler s Generalized Equation Symbolic Solution of Kepler s Generalized Equation Juan Félix San-Juan 1 and Alberto Abad 1 Universidad de La Rioja, 6004 Logroño, Spain juanfelix.sanjuan@dmc.unirioja.es, Grupo de Mecánica Espacial, Universidad

More information

A TREATISE ON DIFFERENTIAL EQUATIONS

A TREATISE ON DIFFERENTIAL EQUATIONS A TREATISE ON DIFFERENTIAL EQUATIONS A. R. Forsyth Sixth Edition Dover Publications, Inc. Mineola, New York CONTENTS CHAPTER I. INTBODUCTION. ABT. 1 4. Formation of Differential Equations and character

More information