Title: The Minimum-Mass Extrasolar Nebula: In-Situ Formations of Close-In Super-Earths
Authors: Eugene Chiang and Gregory Laughlin
Authors’ Institutions: UC Berkeley and UC Santa Cruz
Do planets form in place, or migrate?
How planets form is still a remarkably open question. We haven’t even figured out definitively whether planets formed in the places they are now, or formed in different places and then migrated to their present locations.
A prevailing idea to date has been that the inner parts of solar systems—where our own terrestrial, rocky planets are—do not have enough solid material to form planets larger than about an Earth radius. To have enough solid material to form larger planets, the planets must form beyond the “ice line,” the distance from the star at which volatile materials like water condense to become solids. Since water is so abundant, you should have significantly more material available outside this distance, and planets like Jupiter and Neptune can form.
In our own Solar system this theory hangs together very nicely! The little rocky planets are closer to the Sun, and big, gassy planets like Jupiter are all outside of where this “ice line” would have been in the early solar system (around 5 AU, Jupiter’s present location). But as we find more and more planets, the plot is thickening.
The Kepler space telescope has now found thousands of planet candidates, and the most abundant planets look nothing like any of the planets in our own solar system! These planets are called super-Earths, are on relatively short-period orbits (less than 100 days), and are intermediate in size between Earth and Neptune (see Figure 1). These types of planets orbit more than half the Sun-like stars in the galaxy! In the current favored theory of planet formation, nearly all these planets would have formed beyond the ice line and migrated inwards over time to their current warmer locations.
But what if we’re looking at the problem from the narrow perspective of our own Solar system? Our own Solar system may be the odd man out, since it does not have any of these seemingly ubiquitous super-Earths. Chiang and Laughlin’s work aims to shift the planet formation paradigm and explore whether instead of the mass migration process outlined above, super-Earths might have formed in their present locations.
A series of order-of-magnitude calculations show that it is plausible that these planets did form where they are. (The authors invite the dedicated reader to repeat their calculations, which are doable for any graduate students in astrophysics, or intrepid undergraduates with some extra dynamics background!)
The authors find that:
- To form all these planets in place, a more massive starting disk would be necessary—about 5 times more massive than the one we’d need to form the planets in our own solar system. (See Figure 2).
- Super-Earths should form quickly, before the gas in the disk has disappeared, which happens about 1-10 million years after the star first forms.
- Super-Earths accrete some gas from the primordial disk, which most could probably retain over their lifetimes. This would explain their radii, which are larger than purely rocky bodies like Earth.
Overall, this new paradigm for planet formation is quite plausible and warrants further, more detailed study than the order-of-magnitude treatment of the paper. It’s also testable: the authors make some tangible predictions for the future. Among their predictions are that A and B stars should lack close-in super-Earths because they’re too hot for dust to survive to make planets, while brown dwarfs and M dwarfs should have small planets around them. Orbits of super-Earths should be aligned with the stellar spin axis, and these planets should have H/He-rich atmospheres.
* Surface density is just mass divided by area, and is the analog of regular density for items of which we observe 2-d projections.
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