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2005 FY 9<br />

is the third brightest known TNO, after 2003<br />

UB 313<br />

and Pluto. The size <strong>of</strong> 2005 FY 9<br />

is approximately 0.7<br />

times that <strong>of</strong> Pluto. The semi-major axis <strong>of</strong> its orbit is 46<br />

AU, the perihelion distance is 39 AU and the inclination <strong>of</strong><br />

the orbit is 29°. These values are typical <strong>of</strong> the classical<br />

TNO family.<br />

Visible spectroscopy <strong>of</strong> 2005FY 9<br />

was obtained using the<br />

ISIS spectrograph on the WHT, and near-infrared<br />

spectroscopy was obtained using the NICS spectrograph<br />

on the TNG. The complete visible and near-infrared spectra<br />

were compared with the spectrum <strong>of</strong> Pluto and that <strong>of</strong> pure<br />

methane ice and it was found that the spectra <strong>of</strong> both TNOs<br />

are very similar. They are dominated by strong absorption<br />

bands produced by methane ice. In fact, the absorption<br />

bands in the spectrum <strong>of</strong> 2005 FY 9<br />

are <strong>de</strong>eper than in the<br />

spectrum <strong>of</strong> Pluto, as a result <strong>of</strong> the larger abundance <strong>of</strong><br />

methane ice in 2005 FY 9<br />

. Also the colour <strong>of</strong> the surface <strong>of</strong><br />

the TNO (indicated by the slope <strong>of</strong> the spectrum) is red,<br />

similar to that <strong>of</strong> Pluto. This shows the presence <strong>of</strong> complex<br />

organic compounds in the surface.<br />

Until now only one known TNO, Pluto, showed the<br />

presence <strong>of</strong> strong methane ice absorption bands in its<br />

spectrum. However, apart from 2005 FY 9<br />

, these bands<br />

were also recently observed in the spectrum <strong>of</strong> the largest<br />

yet known TNO, 2003UB 313<br />

, as shown in the Figure 5. The<br />

near infrared spectrum <strong>of</strong> 2003 UB 313<br />

is very similar to that<br />

<strong>of</strong> 2005 FY 9<br />

.<br />

The visible spectrum <strong>of</strong> 2003UB 313<br />

shows very prominent<br />

absorption bands from solid CH 4<br />

. The icy-CH 4<br />

bands are<br />

significantly stronger than those <strong>of</strong> Pluto and slightly<br />

weaker than those observed in the spectrum <strong>of</strong> 2005 FY 9<br />

.<br />

A shift relative to the position <strong>of</strong> the bands in the spectrum<br />

<strong>of</strong> laboratory CH 4<br />

ice is observed in the bands at larger<br />

wavelengths, but not at shorter wavelengths, which can be<br />

explained by a vertical compositional gradient. Purer<br />

methane could have con<strong>de</strong>nsed first, while 2003 UB 313<br />

moved towards aphelion during the last 200 years: as the<br />

atmosphere gradually collapsed, the composition became<br />

more nitrogen-rich due to the fact that most volatile<br />

components con<strong>de</strong>nsed and CH 4<br />

diluted in N 2<br />

, present in<br />

the outer surface layers.<br />

THE YORP EFFECT DETECTED ON NEAR-<br />

EARTH ASTEROID 2000 PH5<br />

The Yarkovsky-O’Keefe-Radzievskii-Paddack (YORP)<br />

effect is believed to alter the way small bodies in the solar<br />

system rotate. YORP is a torque due to sunlight hitting the<br />

surfaces <strong>of</strong> asteroids and meteoroids and warming their<br />

Figure 4. Top: The spectrum <strong>of</strong> 2005 FY 9 compared with the<br />

spectrum <strong>of</strong> Pluto and that <strong>of</strong> pure methane ice. Notice the strong<br />

methane ice absorption bands present in the spectrum <strong>of</strong> both<br />

TNOs. Bottom: Near infrared spectrum <strong>of</strong> 2005 FY 9 compared<br />

with that <strong>of</strong> TNO 2003 UB313. The similarity <strong>of</strong> both spectra shows<br />

that the surface composition <strong>of</strong> the two objects must be similar<br />

(figure from Licandro et al., 2006, A&A, 445, L35).<br />

surfaces, leading to a gentle recoil effect as the heat is<br />

emitted. By analogy, if one were to shine light on a propeller<br />

over a long enough period, it would start spinning.<br />

Although this is an almost immeasurably weak force,<br />

astronomers believe it may be responsible for spinning<br />

some asteroids up so fast that they break apart, perhaps<br />

leading to the formation <strong>of</strong> binary asteroids. Others may be<br />

slowed down so that they take many days to rotate once.<br />

The YORP effect also plays an important role in changing<br />

the orbits <strong>of</strong> asteroids between Mars and Jupiter, including<br />

their <strong>de</strong>livery to planet-crossing orbits. Despite its<br />

importance, the effect has never been seen acting on a<br />

solar system body, until now.<br />

Using extensive optical and radar imaging from powerful<br />

Earth-based observatories, astronomers have directly<br />

14 • ING BIENNIAL R EPORT 2006–2007

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