Ryan McReynolds wrote:But since there are possibly Mars- and even Earth-sized objects in the Kuiper Belt and Oort Cloud, calling them "planetoids" just seems inappropriate.
Ryan McReynolds wrote:"Planetessimal" has a very specific definition, unlike "planet." A planetessimal is a small planetary "building block," many of which combine to form planets. What you call a planessimal above is generally called a "planetary embryo" in the literature.
No, I meant 'planetesimals' as in accretion, not 'proto-planets'. I see now I went cross-eyed referring to planetesimals after you referred to planetoids - oops, sorry! - but I should clarify that I think both terms 'planetoid' and 'planetesimal' can apply to KBO's, large and small, even Pluto and Charon. The first talks about physical characteristics, and the other talks about behaviour during the history of the solar system.
Ryan McReynolds wrote:A planetoid sounds like something that is basically but not quite a planet, which accurately describes large KBOs . . . if you reject their planethood, which of course I don't!
Well, why a cut off line for appyling 'planetoid' to large KBO's when it fact it's a general term for those objects in the solar system that are planet-like (shine by reflected light) but are not planets (and that definition avoids defining planet).
My understanding is this:
- 'planetoid' came from 'asteroid', by swapping 'aster-' with 'planet'- as a correction to a misnomer, because those starlike objects such as Ceres were much more akin to planets than stars (they shine by reflected light). But the objects in that belt of planetoids (that belt distinctly between Mars and Jupiter) are still called planetoids even if just a few hundred metres across. Asteroids and KBO's are all planetoids, but we distinguish between two separate belts of planetoids with those names: Asteroid Belt and Edgeworth-Kuiper Belt.
- 'planetesimal' is a term for those small bodies which accrete amongst themselves to form planets. It was used by the likes of George Wetherill when his 'planetesimal theory' challenged the former prevalent 'proto-planet' theory of planet formation in the 1970's, demonstrating the importance of stochastic processes in (initially terrestrial) planet formation.
Yes, of course you can scratch your head over the collision of two equal sized planetesimals to form one planet and then ask yourself the silly question: "which planetesimal should I consider the true embryonic planet," but that just turns the planet-planetoid-planetesimal argument into a problem like whether your bicycle is the same bicycle if you at one time change the wheels and a later time change the frame...
Furthemore, one of his early simulations fo the formationof Mercury through Mars had a planetesimal left over within Mercury's orbit. It was 1000km across, because Wetherill started all planetesimals at 1000km across to keep the number of bodies in the simulation down. It also showed that soem planetesiams were bound to remain unaccreted through luck or lack of time, and that this example would have been at first sight called a planet (Vulcan, probably). Had there been several 1000km bodies there, what would have been decided then? This is analogous to what has happened with KBO's - they ain't finished accreting, there are hundreds of them.
Ryan McReynolds wrote:If I couldn't call all of the round KBOs minor planets, I would prefer "planetoids" to "planetessimals" simply because calling things planetessimals falls into the same trap you mentioned for brown dwarfs: the classification being dependent upon theoretical formation history. There's no way to know, for instance, if Pluto is technically a planetessimal or actually the result of (admittedly small-scale) oligarchic growth of "true" planessimals. And the problem is compounded for Earth-mass KBOs, which may have essentially the same formation history as Earth, but played out over a multi-billion year timetable. There's just no way of knowing how objects combined and accumulated and collided over billions of years. I think that certainly the vast majority (even more than 99%) of KBOs are planetessimals, but there's no way to be sure, especially in the case of the largest objects.
Statistically, you can. Most simulations of planetary accretion since the 1980's have had trouble forming Neptune where it is - the dynamic timescale for accretion there is just too long compared to the age of the solar system. Exoplanet discovery has revived the disk instability proto-planet theory for (eccentric) gas giant formation. Now it seems the answer is that Neptune and such form that way, migrate outward into the as yet unaccreted icy planetesimals at 20-30 A.U. then gets its orbit circularised by scattering these planetesimals out to 30+ A.U. which is where the Edgeworth Kuiper belt is. This includes Pluto and Charon, which are just an outside version of what a Hilda asteroid is to Jupiter. I think these accretion / disk instability simulations are making is very clear what happened now, more easily than telling about individual exoplanet / brown dwarf formation.
Again, why divide KBO's into 1% planets and 99% planetesimals, when really they simply haven't finshed accreting into a planet yet?
If people want to collectively call all those things orbiting the Sun or a star 'planets', then if you are going to call Pluto and planet call 2004 MN4 a planet, but don't try and fudge an excuse about why Pluto is a planet and Quaoar is not. But, I'll have to tag that as just my 2 eurocents.
Spiff.