MKruer wrote:Planet: A celestial body large enough to generate a minimum heat of 1000K at is core through its own radiogenic heating, gravitational (primordial) heating or tidal heating, at any point during its historical past with a minimum duration of 100million years.
OK, here you've tightened up precision - good - but the problem is that you've tightened up precision on parameters that are derived not observed. Therefore these are so open to debate and review that even though I agree with chaos syndrome that it would be nice to have time to settle the issue, we'd be criticised for the impracticality of it.
It's like the astronomer who wanted to differentiate between Brown Dwarves and Superjupiters by their different formation mechanisms. Everyone else* asked, "
how can we decide?," and the guy hasn't got an answer.
MKruer wrote:On top of that I never said that the magnetic field was required to classify any body as a planet.
No, but I'm not sure you ever said it wasn't
. Anyway, I understand it that you're holding finding any (residual) magnetic field as evidence of e.g., a molten core (that has been) hotter than 1,000K for 100 million years.
MKruer wrote:Spaceman Spiff wrote:For Mars the evidence of a molten core is tenuous.
<sarcasm>So Mars is no longer a planet?</sarcasm>
Hey! Good use of humous tags there!
No, I wasn't saying Mars is no longer a planet. I was pointing out that there is not an adbundance of evidence for a Martian molten core. For example, this
reference (
http://www.anl.gov/Media_Center/News/20 ... 26mars.htm ) soon after yours states at one point: "The data support previous models of the martian core. ", which as d.m.falk mentions consider mars to have a solid core, but goes on to discuss inference of a molten core. Ironically (or double ironically!), it says sulphur impurities allow molten iron cores at reduced temperatures, so the core temperature issue is complicated by this discovery.
So there are complications. The global magnetic field of Mercury could have been induced; Venus appears geologically asleep (that is, we still haven't detected the kind of core you require), and impurities could upset the required temperature to molten iron.
MKruer wrote:... what about rouge planets, inner planets that were for one reason or another flung out of a system and are now wondering the void or planets that for one reason or another have a highly eccentric orbit, like some of the extrasolar planets that are 5 times more massive then Jupiter, but highly elliptical orbits?
Doh! I forgot about rogue planets (spelling! sir, otherwise I don't care about the planet's colour.
). I think tracing back the orbit to formation might allow us to recover an original orbit. For the collection of eccentric extrasolar orbits, population identitfication in orbit-mass scattergrams takes care of that.
MKruer wrote:Finally the reason why I came up with the idea for classify planets based upon it thermal core properties is because it is mass, size, orbit, and composition independent. A small rocky body would be classified as a planet sooner then a ball of ice, but at what point should a ball of ice be considered a planet? If you can answer that question precisely then there is no reason for my definition, problem is that any other definition would be more arbitrary then
"... mass, size, orbit, and composition independent", but technically requires spacecraft probe data to derive the necessary parameters. but I can avoid the pitfall of your question of limit by the scattergram method. Even so, why should a 13,000km diameter 'rock ball' be sooner considered a planet than a 13,000km diameter 'ice ball'?
Spiff.
* Another convenient exaggeration by me...