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Chemistry / Re: Why do we add elements to the periodic table that decay instantly?
« on: 21/10/2016 22:54:40 »Thanks to evan, janus and chiral for all your valuable comments.
The point that "heavy" elements are always getting created in supernovae, is one that I realised with a head-smack after posting. But I didn't to bother to edit, as it was obviously bound to get picked up.
However, going back to the original question, about whether very transient, swiftly-decaying elements should be added to the Periodic Table. I would say not, because it would make the list of "elements" too long.
If I might cite a comparable example from Astronomy. The list of "planets" in the Solar System was eight, until the year 1930. In that year, a new "planet", Pluto, was discovered. Right from the time of its discovery, there were doubts whether "Pluto", should properly be added as a planet, as it's very small. However it got accepted until 2006, when the IAU threw it out.
This was because a lot of new objects were being discovered, like Eris, which is bigger than Pluto. So if you accept Pluto as a planet, you'd have to accept Eris too. And there were more objects of comparable size. You could eventually end up with a list of 40 or 50 "planets". Which is far too long.
So the IAU demoted Pluto to dwarf status. Now astronomers (well, most of them), only acknowledge eight planets on the list. Pluto and the rest are regarded as interesting, but not genuine.
Couldn't this approach be adopted with the Periodic list of elements? That's to say, physicists and chemists, should only recognise 92 genuine elements, the rest being merely interesting?
Because half-life doesn't make a good parameter by which to judge whether something is an element or not. With Pluto, we didn't have a clear cut definition for what a planet was until the IAU decided on the most recent definition.
We do have a good definition for element.
Besides, using half-life would not be consistent with a cut off at element 92. Neptunium, Plutonium, and Americium all have Isotopes with half-lives that are longer than the longest lived isotopes of a number of elements with atomic numbers less than 92, the shortest being Americium at 7270 yrs. Compare this to Actinium, Radium, Francium, Radon, astatine and Polonium, The longest lived isotope in this group belongs to Radium at 1600 yrs, and the longest lived isotope of Francium (atomic number 87) is a mere 22 min.
Why include it as a "real" element while rejecting higher numbered elements with more stable isotopes?
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