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Ground-track resonances around Vesta: potential threats for Dawn?

Delsate, Nicolas

Published in: EPSC-DPS2011-209, 2011 Publication date: 2011 Link to publication

Citation for pulished version (HARVARD):

Delsate, N 2011, Ground-track resonances around Vesta: potential threats for Dawn? in EPSC-DPS2011-209,

2011. vol. 6.

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Ground-track resonances around Vesta:

potential threats for Dawn?

N. Delsate

University of Namur – Dpt of Mathematics & NAXYS, Rempart de la Vierge 8, B-5000 Namur, BELGIUM (nicolas.delsate@math.fundp.ac.be)

Abstract

The aim of Dawn mission is the acquisition of data from orbits around (4)-Vesta and (1)-Ceres, the two most massive asteroids. Due to the low thrust propul-sion, Dawn will slowly transit through ground-track resonances (abbreviated by GTR), where the perturba-tions on Dawn orbit may be significant. In this context, to safety go the Dawn mission from the approach to the lowest orbit, it is essential to know the properties of the crossed resonances. We analytically investigate one of the properties of the 2:3 GTR. This resonance makes the eccentricity of Dawn increase until 0.2. Then the radius of the Dawn orbit changes about 260 km dan-gerously leading Dawn nearer to Vesta. We determine that this increases is due to the C22coefficients

(char-acterizing the equatorial ellipticity of the asteroid).

1. Introduction

Dawn is a mission to explore main belt asteroids in order to yield insights into important questions about the formation and evolution of the solar system [3]. The dynamics of a probe orbiting within ∼ 1 000 km from Vesta is dominated by the gravitational field of Vesta [4]. Due to the low thrust propulsion, Dawn will slowly cross and transit through GTR due to the non uniformity of the gravity field of Vesta. In these res-onances the perturbations on Dawn orbit may be sig-nificant [1, 4]. In particular in the 2:3 resonance the eccentricity increase up to 0.2 [1].

2 Numerical analysis

In Fig. 1, we plot the results of the numerical integra-tions over a time span of 1 year. The fixed initial con-ditions are i = 90◦, Ω = ω = 0and θ = 0for the

sidereal time. These figures allow to locate the GTR. Indeed, when the orbital period of the space probe is close to a commensurability with the rotational period

Figure 1: The amplitude of variation (colorbars) of the semi-major axis, of the eccentricity and of the ra-dial distance computed as functions of the initial mean anomaly and the initial semi-major axis. The equa-tions of motion include the central body attraction, the harmonics until degree and order 4.

of Vesta, the ground-track of the probe will periodi-cally encounter the same configuration of the gravita-tional field. This is a gravitagravita-tional or ground-track res-onance (GTR). Then a part of the effects of the gravi-tational perturbations is amplified leading to a motion with very long period and large perturbations in the semi-major axis of the spacecraft orbit. This is what we observe in the left panel of Fig. 1 where the vari-ation of the semi-major axis is clearly the largest, at 550 km and 720 km. The results obtained here are similar to [4]. We find 5 main GTR. In the right panel of Fig. 1, we notice that the largest resonance is the 1:1 but the strongest perturbations on the radial distance appear in the 2:3 resonance. We can deduce from the central panel that the high value of the amplitude of variation of the radial distance in the 2:3 resonance is due to an increase of the eccentricity.

3 Analytical study

The Hamiltonian describing the motion of a probe around an irregular central body is given by [2] us-ing the eccentricity functions and the inclination func-EPSC Abstracts

Vol. 6, EPSC-DPS2011-209, 2011 EPSC-DPS Joint Meeting 2011

c

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tions. A GTR occurs when there is a commensurability between the orbital period of the probe and the rota-tional period of the asteroid. The properties of GTR around Vesta are already studied in [1]. The Hamilto-nian of the 2:3 resonance, until the first order in eccen-tricity, is given by (σ = 3(Ω + ω + M) − 2θ) [1]: H2:3 = − µ 2 2L2 − 15µ5R3 e 8L8  − S32cos(σ − Ω) C32sin(σ − Ω)  − e21µ4R2e 8L6  C22cos(σ − ω − Ω) + S22sin(σ − ω − Ω)  + ˙θΛ ,

where Re is the equatorial radius of Vesta, ˙θΛ is the

asteroid rotation and Cnm, Snmare the coefficients of

the spherical harmonic gravity field representation [2]. With this Hamiltonian we can qualitatively give the secular equation of the eccentricity ˙e ≈ |∂H

∂ω|. To have

an idea of the variation of the eccentricity during the motion we can look at the ˙e/e value:

˙e/e ≈ e−1∂H/∂ω ∝ 21µ4R2

e/(8L6) C22. (1)

Then the variation of the eccentricity depends on one of the biggest coefficients of the gravity field C22. For

Vesta, this coefficient C22 is 5 times greater than the

coefficient C32responsible for the 2:3 GTR. We

eval-uate (linked to Vesta), near to the 2:3 GTR, the multi-plying coefficient appearing in front of the two major contributions C32and C22: 15µ5R3 e 8L8 C32≈ 6 913 & e 21µ4R2 e 8L6 C22≈ 25 179 e . (2) In the case of Dawn orbiting Vesta, this highlights the importance of this additional term C22in the 2:3

reso-nance.

Now we numerically verify our conclusion. In the left panel of Fig. 2, we only use the J32 (Jnm =

p C2

nm+ Snm2 ) term to modelize the central body. We

see a weak increase of the eccentricity (0.03). In the central panel, we add the J22term and we notice that

the eccentricity reaches higher values(0.15). In the right panel, the gravity field contains also the J2 =

−C20term and the maximum eccentricity reached is

0.2. Then, with the help of Fig. 1 and Fig. 2, we can conclude that the major part of the increase of the ec-centricity in the 2 : 3 GTR is due to the J22

coeffi-cient. Finally, we numerically simulate the slow de-scent, with a continuous −20mN thrust, of Dawn from a radius of 1 000 km to 600 km. We make this test with different gravity field configurations. The first crossed GTR is the 2:3. The eccentricity increases only in the full model and in the models including the coefficient.

Figure 2: Around the 2:3 GTR. The amplitude of vari-ation of the eccentricity (colorbars). The equvari-ations of motion include the harmonic J32(left panel); the

har-monics J22and J32(central panel); and the harmonics

J2, J22and J32(right panel).

Figure 3: Evolution of the semi-major axis and the eccentricity of Dawn going down from 1 000 km to 600 km radius with a thrust of −20mN. The increase of the eccentricity depends on the gravity field model.

4. Summary and Conclusions

The GTR around Vesta has been numerically studied in [4, 1]. The properties (location, aperture, period) of these GTR has been analytically study in [1]. We show in this paper the threat of the 2 : 3 GTR that can increase the eccentricity of Dawn (because of C22)

in-volving a dangerous decrease of the radius of the orbit.

References

[1] Delsate, N., Analytical and numerical study of the ground-track resonances of Dawn orbiting Vesta, Plane-tary and Space Science, DOI 10.1016/j.pss.2011.04.013. [2] Kaula, W.M.:. Theory of satellite geodesy. Waltham,

Mass.: Blaisdell, 1966.

[3] Rayman, M.D., Fraschetti, T.C., Raymond, C.A., Rus-sel, C.T., Dawn: a mission in development for explo-ration of main belt asteroids Vesta and Ceres, Acta As-tronautica, Vol. 58, pp. 605-616, 2006.

[4] Tricarico, P., Sykes, M.V.: The dynamical environment of Dawn at Vesta, Planetary and Space Science, Vol. 58, pp. 1516-1525, 2010.

Figure

Figure 1: The amplitude of variation (colorbars) of the semi-major axis, of the eccentricity and of the  ra-dial distance computed as functions of the initial mean anomaly and the initial semi-major axis
Figure 2: Around the 2:3 GTR. The amplitude of vari- vari-ation of the eccentricity (colorbars)

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