Surface Properties of Kuiper Belt Objects and Centaurs

The outer solar system is inhabited by a population of small solar system bodies called Kuiper belt Objects (KBOs) and Centaurs. I present a survey of visible and near infrared (NIR) spectra of the brightest KBOs and Centaurs. The visible spectra of 19 KBOs were obtained at Palomar Observatory. At the W.M. Keck Observatory, NIR spectra were obtained for 33 KBOs and 12 Centaurs. This data marks a significant leap in the available spectra, allowing for the population to be studied as whole. The spectra reveal that most KBOs are covered with a material with characteristics similar to irradiate ices rich in complex organic compounds. Water ice is also observed on some KBOs and Centaurs, though its abundance is variable across the samples. A two end member mixing model is found to describe the NIR spectral properties well, but poorly fits the visible-NIR data. This suggests that the non-water ice component is heterogeneous across the KBO and Centuar populations. To characterize the non-ice component better, the visible spectra are analyzed for signatures of both organic and mineralogical features. No evidence is found for the presence of minerals, but the spectra suggest complex organics are a dominant spectral component. The abundance of water is shown to directly correlate with diameter for KBOs, but not Centaurs, suggesting it is controlled by geophysical processes on KBOs. The analysis of these spectra has revealed an unusual population of KBOs that are now identified as mantle fragments from the large KBO 2003 EL61. The collision that spun-up 2003 EL61, formed its satellite system, and ejected the mantle fragments into the Kuiper belt is discussed. The unusual spectral properties of 2003 EL61, its brightest satellite, and the fragments are examined. Analysis suggests that the surfaces of all these objects can be composed of nearly pure water ice, suggesting that their volatile organic inventory has been lost. The discovery of crystalline water ice on these small KBOs suggests that crystallization is not an indication of recent surface activity as was previously suggested.</p

The Surface of 2003 EL_(61) in the Near-Infrared

We report the detection of crystalline water ice on the surface of 2003 EL_(61). Reflectance spectra were collected from the Gemini North telescope in the 1.0 to 2.4 μm wavelength range and from the Keck telescope across the 1.4-2.4 μm wavelength range. The signature of crystalline water ice is obvious in all data collected. Like the surfaces of many outer solar system bodies, the surface of 2003 EL_(61) is rich in crystalline water ice, which is energetically less favored than amorphous water ice at low temperatures, suggesting that resurfacing processes may be taking place. The near-infrared color of the object is much bluer than a pure water ice model. Adding a near-infrared blue component such as hydrogen cyanide or phyllosilicate clays improves the fit considerably, with hydrogen cyanide providing the greatest improvement. The addition of hydrated tholins and bitumens also improves the fit, but is inconsistent with the neutral V - J reflectance of 2003 EL_(61). A small decrease in reflectance beyond 2.3 μm may be attributable to cyanide salts. Overall, the reflected light from 2003 EL_(61) is best fit by a model of 2/3-4/5 pure crystalline water ice and 1/3-1/5 near-infrared blue component such as hydrogen cyanide or kaolinite. The surface of 2003 EL_(61) is unlikely to be covered by significant amounts of dark material such as carbon black, as our pure ice models reproduce published albedo estimates derived from the spin state of 2003 EL_(61)

A collisional family of icy objects in the Kuiper belt

The small bodies in the Solar System are thought to have been highly affected by collisions and erosion. In the asteroid belt, direct evidence of the effects of large collisions can be seen in the existence of separate families of asteroids—a family consists of many asteroids with similar orbits and, frequently, similar surface properties, with each family being the remnant of a single catastrophic impact. In the region beyond Neptune, in contrast, no collisionally created families have hitherto been found. The third largest known Kuiper belt object, 2003 EL_(61), however, is thought to have experienced a giant impact that created its multiple satellite system, stripped away much of an overlying ice mantle, and left it with a rapid rotation. Here we report the discovery of a family of Kuiper belt objects with surface properties and orbits that are nearly identical to those of 2003 EL_(61). This family appears to be fragments of the ejected ice mantle of 2003 EL_(61)

Photometric Observations Constraining the Size, Shape, and Albedo of 2003 El61, a Rapidly Rotating, Pluto-Sized Object in the Kuiper Belt

We present measurements at optical wavelengths of the spectral reflectance, rotational light curve, and solar phase curve of 2003 EL61. With apparent visual magnitude 17.5 at 51 AU from the sun, this newly discovered member of the classical Kuiper Belt is now the third brightest KBO after Pluto and 2005 FY9. Our observations reveal an unambiguous, double-peaked rotational light curve with period 3.9154 +/- 0.0002 hours and peak to peak amplitude 0.28 +/- 0.04 mag. This is the fastest rotation period reliably determined for any body in the solar system larger than 100 km. Assuming the body has relaxed over time to the shape taken by a homogenous fluid body, our observations tightly constrain the shape and density. Given the mass we recently determined for 2003 EL61 from the orbit of a small satellite, we also constrain the size and albedo. We find a total length of 1960 to 2500 km, a mean density of 2600 to 3340 kg m-3, and a visual albedo greater than 0.6. We also measure a neutral reflectance at visible wavelengths and a linear phase curve with slope varying from 0.09 mag deg-1 in the B band to 0.13 mag deg-1 in the I band. The absolute V-band magnitude is 0.444+/-0.021.Comment: 27 pages, six figure