Issue 
A&A
Volume 587, March 2016



Article Number  L8  
Number of page(s)  4  
Section  Letters  
DOI  https://doi.org/10.1051/00046361/201628227  
Published online  08 March 2016 
Constraints on the location of a possible 9th planet derived from the Cassini data
^{1}
GéoAzur, CNRSUMR 7329, Observatoire de la Côte d’Azur, Université
Nice Sophia Antipolis, 250 Av. A.
Einstein, 06560
Valbonne,
France
email:
fienga@oca.eu
^{2}
ASD/IMCCE, CNRSUMR 8028, Observatoire de Paris, PSL, UPMC, 77 avenue
DenfertRochereau, 75014
Paris,
France
email:
laskar@imcce.fr
Received: 31 January 2016
Accepted: 16 February 2016
To explain the unusual distribution of Kuiper belt objects, several authors have advocated the existence of a superEarth planet in the outer solar system. It has recently been proposed that a 10 M_{⊕} object with an orbit of 700 AU semi major axis and 0.6 eccentricity can explain the observed distribution of Kuiper belt objects around Sedna. Here we use the INPOP planetary ephemerides model as a sensor for testing for an additional body in the solar system. We test the possibility of adding the proposed planet without increasing the residuals of the planetary ephemerides, fitted over the whole INPOP planetary data sample. We demonstrate that the presence of such an object is not compatible with the most sensitive data set, the Cassini radio ranging data, if its true anomaly is in the intervals [−130°: −100° ] or [−65°:85° ]. Moreover, we find that the addition of this object can reduce the Cassini residuals, with a most probable position given by a true anomaly v = 117.8°^{+11°}_{10°} .
Key words: Kuiper belt: general / planets and satellites: detection
© ESO, 2016
1. Introduction
The discovery in 2014 of the Kuiper belt object (KBO) 2012 VP_{113} (Trujillo & Sheppard 2014) in the inner Oort cloud revived the question of a planet X. With a relatively large radius (R ≈ 200–1000 km), this object has orbital parameters similar to those of Sedna, another large planetlike KBO, with a high eccentric orbit (e> 0.7), a perihelia distance greater than 30 AU, and arguments of perihelia ω around 0°. As stressed in Trujillo & Sheppard (2014), de la Fuente Marcos & de la Fuente Marcos (2014), the recent observed distribution of ω for the inner Oort cloud objects is concentrated around 0°. One proposed explanation for such an unlikely spatial distribution is the existence of a superEarth mass planet with mass between 2 to 15 M_{⊕} and a semimajor axis of 200 to 300 AU (Trujillo & Sheppard 2014).
The existence of such object can have an important impact not only on the mass distribution of the material beyond the limit of 50 AU but also on the spatial distribution of objects between 40 to 50 AU (Lykawka & Mukai 2008; Kenyon & Bromley 2015). The present mass distribution in the outer edge of our solar system can be seen as a footprint of the mechanism of formation of our solar system. Characterization of the orbit parameters of a superEarth beyond 200 AU can give some estimations of the mass and the outer radius of the solar nebula (Bromley & Kenyon 2014) as well as some clues to the scenario of formation. Low eccentric orbits is compatible with migrating scenario (Ward 1997; Crida et al. 2009), higher eccentricity for low mass planet being more compatible with a gas drag formation model (Kenyon & Bromley 2015). Such an object has also been invoked to explain some periodicities in mass extinction events (Raup & Sepkoski 1984; Whitmire 2016).
The question of the existence of a massive object in the outer solar system thus becomes important for studying the present solar system’s architecture and understanding its formation. Very recently, this quest has reached a new level with the publication by Batygin & Brown (2016) of a proposal of a ninth planet to explain the clustering of the distant KBO in the vicinity of 2012 VP_{113}. The gravitional interaction with this object (which we will call P9 from now on) should have scattered the bodies that are not confined in the vicinity of the central island of a pseudo resonance^{1} with P9. To be able to remove the bodies that were originally evenly distributed in a disk, P9 needs to be massive enough and not too far, with high eccentricity. Batygin & Brown (2016) propose a 10 M_{⊕} planet with 0.6 eccentricity and a 700 AU semi major axis. In the present work, we examine the contraints given by the analysis of the dynamics of the solar system on the possibility of such a new planet.
2. Searching for planet X
The hunt for a planet X started in 1915 Lowell (1915), and some important limitations were provided by different approaches. The direct imaging survey of the far solar system by infrared space telescopes IRAS and WISE did not detect any massive objects of Jupiter size inside 25 000 AU and of Saturn size inside 10 000 UA Luhman (2014). In 1993, Standish (1993) demonstrated that no anomalous residuals can be seen in the residual of the outer planet orbits. However since this work, no direct confrontation has been performed between the perturbations induced by a planet X on the orbits of the main planets of our solar system and the best fitted planetary ephemerides. The only estimates were made indirectly, based on the results of the ephemerides, but without refitting the whole parameters of these ephemerides (Iorio 2012, 2016).
Since 1993, very accurate observations of Saturn orbit were obtained thanks to the tracking of the Cassini spacecraft during its exploration of the Saturnian system. As described in Folkner et al. (2014), Hees et al. (2014) and Fienga et al. (2016), the ten year positions of Saturn allow significant improvement in our knowledge of Saturn’s orbit, as well as of Jupiter, Uranus, and Neptune orbits. These Cassini data have already been used very successfully to put some strict limits on the possibility of an anomalous Pioneer acceleration (Anderson et al. 2002; Fienga et al. 2010). Furthermore, thanks to the Cassini flyby of Jupiter, a supplementary accurate position of Jupiter is also used to build the ephemerides. Finally, the flyby of the New Horizons spacecraft of the PlutoCharon system should bring some supplementary information and constraints for the existence of a superEarth.
We use here the dynamical model of the INPOP planetary ephemerides (Fienga et al. 2008, 2009, 2010, 2011, 2016) for testing the possibility of an additional planet, focussing on the proposed nominal planet P9 of Batygin & Brown (2016). In the dynamical model of INPOP planetary ephemerides, we add a superEarth object of 10 M_{⊕} with different orbital characteristics, in agreement with the proposed orbit of P9. We then build new ephemerides including these objects and perform a global fit of the perturbed planet orbits to the whole data set that is used to construct the INPOP and DE430 JPL ephemerides (Folkner et al. 2014).
3. Method
3.1. INPOP planetary ephemerides
Since Fienga et al. (2008), the INPOP planetary ephemerides are regularly produced and used for testing alternative theories of gravity, studying variations in the solar plasma density, and estimating asteroid masses (Fienga et al. 2009, 2010, 2011, 2016). The INPOP ephemerides of the eight planets of our solar system, of Pluto, and of the Moon, are obtained by numerically integrating the barycentric EinsteinInfeldHoffmann equations of motion (Moyer 1971) in a suitable relativistic timescale, and taking up to 298 asteroids of the main belt into account.
In 2015, we released the latest INPOP ephemerides, built over the whole sample of modern and ancient planetary observations, from ten years of Cassini roundtrip around Saturn and its system, up to the first photographic plates of Pluto. Besides the differences in the dynamical modeling and in fitting choices explained in Fienga et al. (2016), this latest version of INPOP is very close to the JPL DE430 planetary ephemerides (Folkner et al. 2014).
3.2. INPOP: a tool to test the presence of P9
To test the possible presence of P9, we add it to the dynamical model of the solar system in INPOP. We then proceed to a complete fit of all the initial conditions and parameters for the planetary orbits of INPOP, totalling 150 variable quantities. The fit is performed over the full set of about 150 000 planetary and satellite observations that are currently used to determine the INPOP ephemerides, although the INPOP ephemerides also comprise the adjustment of the parameters of the Moon which will not be considered here. The presence of P9 is only possible if the postfit residuals are not increased after the introduction of P9 in the INPOP model. The increase of the residual will be a clue that P9 cannot exist at the given location. In the same way, a significant decrease in the residuals could be the signature of P9.
Orbital elements of P9, as given in Batygin & Brown (2016), in ecliptic (IERS) orbital elements (a,e,i,ω,Ω), respectively semimajor axis, eccentricity, inclination, argument of perihelion, and longitude of the node.
For P9, we use the ecliptic orbital parameters of Batygin & Brown (2016, Table 1). In Batygin & Brown (2016), only the long term evolution is considered as a constraint for the distribution of the KBO, so the true anomaly is left as an unknown. With a large eccentricity of e = 0.6, the radius vector from the Sun, r, can vary from 280 to 1120 AU, depending on the true anomaly v of P9. We thus sample the possible values of v over a full orbit (v ∈ [ −180°:180° ]).
4. Results
In Fig. 1 we represented the post fit residuals of the INPOP ephemerides after the addition of P9 for various values of the true anomaly v = 60°,80°,85°,90°,95°. For comparison, the INPOP residuals are also plotted. We have not plotted the residuals for values of v less than 60°, as for v = 60°, it is already obvious that P9 cannot exist. For v = 95° the difference in the residuals is too small to be significant, while these residuals already increase for v = 85°. In Fig. 2, we have gathered the results computed for all values of v by plotting, for the prefit (, in blue) and postfit (Δσ, in red) residuals, the relative change in root mean square residuals (Δσ = (σ − σ_{0}) /σ_{0}), where σ_{0} = 74.9 m is the standard deviation for the INPOP nominal ephemerides over the Cassini data.
The prefit residuals are differences between the observations (here, radio ranging) and the computed values of observed quantities, for INPOP ephemerides, with the addition of P9 to the INPOP model, without fitting the parameters. The variation in these residuals with the true anomaly reflects how much the perturbation of P9 on Saturn changes with the geometry of the problem, and not only with the distance of P9 from the Sun. The postfit σ are the residuals after the fit of 56 planetary parameters in the INPOP ephemerides after the addition of P9 in the model. This fit is performed over the whole set of more than 150 000 planetary observations.
Fig. 1
Post fit residuals (in m) for the Cassini observations over [ 2004.4:2014.4 ]. In blue are the nominal residuals of INPOP. In red are the post fit residuals after the introduction of P9 in the INPOP model. 
The shaded region corresponds to a relative increase in the postfit residuals of more than 10% after the addition of P9. This is about the level of precision of the INPOP σ_{0}, estimated by comparison with DE430. We thus consider that an increase of Δσ above 10% is significant and denotes the impossibility of fitting a P9 planet for this value of the true anomaly v. The shaded regions ([−130°:−100° ] ∪ [ −65°:85° ]) are thus the forbidden regions for P9. The Δσ curve presents two minima. We do not believe that the minimum at v = −80° is really significant, since it also corresponds to a minimum of the prefit residuals and amounts to only Δσ = −2.5%.
The other minimum at v = 117.8° is more interesting. It corresponds both to the observed minimum of the residuals curve (Fig. 3), with Δσ = −7.09%, and to the result of a direct fit of the mean anomaly over the Saturn Cassini range data sample that provided an uncertainty at 2σ of ±1.8° on v. Owing to the relatively flat behaviour around the minimum in Fig. 3, we prefer a conservative approach here, and we defined an empirical uncertainty by the zone (in green in Fig. 3) for which Δσ< −6%, which gives^{2}.
5. Extrapolation of Cassini data
Although the INPOP ephemerides were fitted to all 150 000 planetary observations, we have shown here only the residuals with the Cassini data because they are most sensitive to the presence of an additional perturber P9. We have only used the data available up to 2014.4, but new data will be available until the end of the mission, which is programmed for 2017, unless the mission is extended. To evaluate the impact of an increase in the time span of the Cassini mission, we have simulated additional data, by adding to the INPOP prediction (without P9) a Gaussian noise of 200 m sigma, which is slightly pessimistic with respect to the already analysed data set. As previously, P9 is then added, and the ephemerides are fitted to all observations, including the extrapolated Cassini data, through several iterations (Figs. 4, 5). Extending Cassini mission until 2020 would thus allow to state for the non existence of P9 on the interval v ∈ [ −132°:106.5° ] (Fig. 5). The respective area of exclusion of a possible P9 from the present data and from the extrapolated Cassini data up to 2020 are displayed in Fig. 6, together with the most probable zone for finding P9.
Fig. 2
Relative change in the root mean square residuals of a fitted INPOP solution including P9, with respect to those of the nominal INPOP, with respect to the true anomaly of P9 (v in x axis). Prefit residuals are in blue with the right yscale (in %). Postfit residuals are in red with the left yscale (in %). 
Fig. 3
Enlargement of Fig. 2 around the minimum (green bar, at v = 117.8°). In the green zone, Δσ< −6%. 
Fig. 4
Same as Fig. 1 with the addition of simulated Cassini data over [ 2014.4:2020 ], for v = 60° and v = 120°. 
6. Conclusions
Fig. 6
Allowed zone for P9. The red zone (C14) is excluded by the analysis of the Cassini data up to 2014 (Sect. 4). The pink zone (C20) is how much this zone can be enlarged by extending the Cassini data to 2020 (Sect. 4). The green zone is the most probable zone for P9 (v ∈ [ 108°:129° ]), with maximum reduction of the residuals at v = 117.8° (blue dot P9). The white zone is the uncertainty zone where the P9 perturbation is too faint to be detected. 
The Cassini data provides an exceptional set of measures that acts as a very sensitive device for testing the possibility of an additional massive body in the solar system. With the data accumulated until 2014.4, we can exclude the possibility that P9 is in the section of the orbit depicted in red in Fig. 6, with a true anomaly v in [−130°: −100° ] ∪ [ −65°:85° ]. We thus contradict the affirmation of Iorio (2016), who states that a body of 10 M_{⊕} is excluded if it resides closer to 1000 AU of the Sun. Iorio (2016)
does not properly consider how much the presence of an additional body can be absorbed by the fit of all the other parameters in the solar system ephemerides. The global fit that we present here avoids this drawback. Moreover, we found that the presence of P9 could significantly decrease the Cassini residuals if v is in the interval [ 108°:129° ], with a most probable position at .
Since the Cassini data is at present the most precise sensor for testing the possibility of an additional body in the solar system, it is essential that Cassini continues to provide ranging data, since there will not be very soon an additional spacecraft around one of the planets beyond Saturn. Extending the Cassini data up to 2020 will already allow to state for the existence of P9 for v ∈ [−132°:106.5°]. Juno will soon arrive around Jupiter and will thus allow us to improve the orbit of Jupiter. This may not directly improve the constraints on P9, because Jupiter is less sensitive than Saturn to the perturbations of P9. Nevertheless, constraining Jupiter more tightly will allow us to improve the determination of P9, because less flexibility will exist for absorbing the perturbations due to P9.
We denote this kind of resonance a pseudo resonance, because it does not involve the existence of separatrices in the phase space (Batygin & Brown 2016).
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All Tables
Orbital elements of P9, as given in Batygin & Brown (2016), in ecliptic (IERS) orbital elements (a,e,i,ω,Ω), respectively semimajor axis, eccentricity, inclination, argument of perihelion, and longitude of the node.
All Figures
Fig. 1
Post fit residuals (in m) for the Cassini observations over [ 2004.4:2014.4 ]. In blue are the nominal residuals of INPOP. In red are the post fit residuals after the introduction of P9 in the INPOP model. 

In the text 
Fig. 2
Relative change in the root mean square residuals of a fitted INPOP solution including P9, with respect to those of the nominal INPOP, with respect to the true anomaly of P9 (v in x axis). Prefit residuals are in blue with the right yscale (in %). Postfit residuals are in red with the left yscale (in %). 

In the text 
Fig. 3
Enlargement of Fig. 2 around the minimum (green bar, at v = 117.8°). In the green zone, Δσ< −6%. 

In the text 
Fig. 4
Same as Fig. 1 with the addition of simulated Cassini data over [ 2014.4:2020 ], for v = 60° and v = 120°. 

In the text 
Fig. 5
Same as Fig. 2 with extrapolated Cassini data (wihout P9) up to 2020. 

In the text 
Fig. 6
Allowed zone for P9. The red zone (C14) is excluded by the analysis of the Cassini data up to 2014 (Sect. 4). The pink zone (C20) is how much this zone can be enlarged by extending the Cassini data to 2020 (Sect. 4). The green zone is the most probable zone for P9 (v ∈ [ 108°:129° ]), with maximum reduction of the residuals at v = 117.8° (blue dot P9). The white zone is the uncertainty zone where the P9 perturbation is too faint to be detected. 

In the text 
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