Categories: Extrasolar Planets

Will We Find Super Earths?


An extrasolar planet with hypothetical (possible but unproven) water-bearing moons. Image credit: NASA/IPAC/R. Hurt. Click to enlarge
Over the past decade, astronomers using a planet-hunting technique that measures small changes in a star’s speed relative to Earth, have discovered more than 130 extrasolar planets. The first such planets were gas giants, the mass of Jupiter or larger. After several years, the scientists began to detect Saturn-mass planets. And last August, they announced the discovery of a handful of Neptune-mass planets. Could these be super-Earths?

In a recent talk at a symposium on extrasolar planets, Carnegie Institution of Washington astronomer Alan Boss explained the possibilities.

Radial-velocity planet-hunting techniques recently have pushed our discovery capability below the Saturn-mass limit down into what we would call the ice-giant limit.

So we are now able to find planets, close to their host stars, with masses comparable to that of Uranus and Neptune (14 to 17 times the mass of Earth).

In large part this is due to Michel Mayor and his colleagues having a new spectrometer in La Silla, which has unprecedented spectral resolution down to about 1 meter per second or so. And I think Geoff Marcy and Paul Butler’s group are quite close behind that as well.

The interesting question, though, is: What are these things? Are they ice giants that formed several AUs out and migrated in, or are they something else? Unfortunately, we don’t know exactly what their masses are. Even more importantly, we don’t really know what their density is. So they could be 15-Earth-mass rocks, or they could be 15-Earth-mass ice giants.

What we really need to do is to have folks go out and discover another 7 or so. We’ve got 3 so far. If we had 10 altogether, then we’ll have enough that 1 of them, at least, should transit its star and then we’ll be able to get some idea of what its density is.

I think, though, that there’s a good chance that these might actually be a new class of planet altogether: super-Earths. The reason I would argue that is that, at least in 2 of the systems where they’ve been found, these “hot Neptunes” are accompanied by a larger Jupiter-mass planet with a longer-period orbit.

If the lower-mass planets are ice giants that formed far from their stars, unless you have some highly contrived scenario, you wouldn’t imagine them to end up migrating inward, past the larger guys. These systems look more like our own solar system, where you have the low-mass fellows inside of the gas giants.

The planets in a system like our system presumably did not undergo very much migration. So I would claim that perhaps these guys are objects which formed inside the gas giants and only migrated in a little bit, ending up where we can detect them with the short-period spectroscopy surveys.

In support of this idea, there’s some theoretical work from Carnegie’s George Wetherill from almost 10 years ago, now, where he had done some calculations of the accumulation process of rocky planets. He often found there was quite a spread in the masses of what you got out, because accumulation’s a very stochastic process. For the typical parameters he used, at the end of 100 million years or so, he would not only get objects of 1 Earth mass, but also objects ranging up to 3 Earth masses.

Well, at the time, he assumed for his calculations a fairly low surface density at 1 AU, where these planets were forming. Given what we know now, if you want to be able to make a Jupiter at 5 AU using the core-accretion model of planetary formation, you have to crank up the density in the protoplanetary disk by a factor of 7 or so over what Wetherill assumed.

That scales directly with the mass of the planets you’d expect to find as a result. So if you did these calculations over again, assuming this higher initial density, the upper limit on the mass of the inner planets would go from 3 Earth masses, which is what Wetherill got, up to say 21 Earth masses. That is in the range of what we are estimating for these newly discovered hot Neptune-mass objects.

So perhaps what we really are seeing is a new class of objects, super-Earths, rather than ice giants.

Original Source: NASA Astrobiology

Fraser Cain

Fraser Cain is the publisher of Universe Today. He's also the co-host of Astronomy Cast with Dr. Pamela Gay. Here's a link to my Mastodon account.

Recent Posts

Dinkinesh's Moonlet is Only 2-3 Million Years Old

Last November, NASA's Lucy mission conducted a flyby of the asteroid Dinkinish, one of the…

3 hours ago

The Universe Could Be Filled With Ultralight Black Holes That Can't Die

Steven Hawking famously calculated that black holes should evaporate, converting into particles and energy over…

9 hours ago

Starlink on Mars? NASA Is Paying SpaceX to Look Into the Idea

NASA has given the go-ahead for SpaceX to work out a plan to adapt its…

22 hours ago

Did You Hear Webb Found Life on an Exoplanet? Not so Fast…

The JWST is astronomers' best tool for probing exoplanet atmospheres. Its capable instruments can dissect…

1 day ago

Vera Rubin’s Primary Mirror Gets its First Reflective Coating

First light for the Vera Rubin Observatory (VRO) is quickly approaching and the telescope is…

1 day ago

Two Stars in a Binary System are Very Different. It's Because There Used to be Three

A beautiful nebula in the southern hemisphere with a binary star at it's center seems…

2 days ago