The mid-sized Kuiper belt object (KBO) measures 650 kilometers (400 miles) across, and yet it has a density less than water (less than 1 gram per cubic centimeter). Yes, if you put it in a huge bathtub, 2002 UX25 would float.
As we probably all know by now, the Kuiper belt — a populated region of the solar system found just beyond the orbit of Neptune — is a strange place. Once thought to have a population of just one, astronomers have identified thousands of other minor planetary bodies. In fact, it was the accelerated discoveries in the Kuiper belt that ultimately led to the reclassification (or demotion, depending on which way you look at it) of Pluto from “planet” to lowly “dwarf planet.”
Now, in a paper accepted for publication in the The Astrophysical Journal Letters, planetary scientist Mike Brown, of the California Institute of Technology (Caltech) in Pasadena, has taken a measure of 2002 UX25′s density and discovered that it is “the largest solid known object in the solar system with a measured density below that of pure water ice.” Measuring the density of these distant objects are very difficult and require a small moonlet in orbit around the KBO so its orbital characteristics can be accurately measured and KBO density probed. The KBOs satellite was discovered by Hubble in 2005 and follow-up observations by the Keck Observatory in Hawaii refined its orbit.
This finding adds an extra twist to a strange dichotomy of KBOs. Objects with diameters less than 350 kilometers (218 miles) generally have densities less than that of water; objects over 800 kilometers (500 miles) have densities greater than water. One point in the gray area — between the diameter range of 350-800 kilometers — has just been added by 2002 UX25. But it is very large to have a density 18 percent less than water ice, a fact that surprised the veteran KBO hunter.
It is thought that KBOs formed in a similar way to asteroids and planets. Over the evolution of our solar system, small bits of rocky and icy debris coalesced, eventually forming planetesimals that then gathered more and more debris as their gravitational oomph grew. In this scenario, one would expect the density of minor planetary bodies to increase with increasing mass; the gravitational pressure of progressively larger bodies would cause more compression, thus increasing the density.
However, the very low densities of smaller KBOs are hard to explain without assuming that the bodies have a high degree of porosity. Porosity is a known factor in the formation of asteroids throughout the solar system — gaps throughout the structure of rocky bodies less than 350 kilometers in diameter are thought to lower the overall density. Asteroids over 350 kilometers become so massive that porosity decreases; the gravitational compression pulls the material closer together, reducing porosity and increasing density.
According to Brown, this porosity transition should occur in KBOs larger than 350 kilometers wide. But as 2002 UX25 shows, this transition hasn’t happened up to a size of 650 kilometers. This factor creates a problem. If larger KBOs over 1,000 kilometers (620 miles) formed through the coalescence of smaller KBOs (like 2002 UX25), it isn’t possible that large rock-rich KBOs could have such high densities.
In the case of an object the size of Eris, for example, with a measured density of 2.5 g/cm3, even with the gravitational compression exerted by the 2,326 kilometer-wide dwarf planet, the low density, high porosity material from an objects like 2002 UX25 cannot be compressed to such a high degree. Such an object “would still have a density close to 1 g/cm3 rather than the 2.5 g/cm3 density of Eris,” writes Brown. On this evidence alone, large KBOs cannot form through agglomeration of many small KBOs like 2002 UX25.
So what’s going on in the Kuiper belt? Brown offers a few explanations.
Perhaps there is some observational bias in the measurements of KBO density, or perhaps 2002 UX25′s density is not representative of mid-sized KBOs — it could be the ‘black sheep’ of the Kuiper flock. Could it be that the highest density, large KBOs formed through conventional agglomeration processes, only to have their densities beefed-up by energetic collisions early in the solar system’s history? Dwarf planet Haumea shows evidence for a massive collision in its past, which smashed the majority of its icy mantle away, leaving a rocky core behind — this had the effect of increasing the overall density of the object.
“None of these alternatives appears likely,” concludes Brown. “We are left in the uncomfortable state of having no satisfying mechanism to explain the formation of the icy dwarf planets. While objects up to the size of 2002 UX25 can easily be formed through standard coagulation scenarios, the rock rich larger bodies may require a formation mechanism separate from the rest of the Kuiper belt.”
Read more at Discovery News
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