00:01
Let's look at the relative entropies of various allotropes of carbon.
00:07
So listed here are the standard entropys of diamond and graphite.
00:12
You can see that the entropy of graphite is larger than that of diamond, but both diamond and graphite are carbon.
00:21
And so what is it about each of these that make the entropies of them different? and remember that entropy in a lot of ways is really just based on translational, vibrational, and rotational energies.
00:38
And so when we think about a diamond in its structure, remember that diamond is carbon that is put together in a network covalent fashion in a tetrahedral structure.
00:50
We can keep drawing these seas further out and further out and further out.
00:54
But they're all locked into place in all three dimensions.
00:59
When we deal with graphite, graphite is in a trigonal planar structure.
01:06
And since it's in a plane, you can think of them as like sheets.
01:10
So if we just rotate this a little to look at it on its side, you would really just see these four carbons.
01:19
The other two back here, these two would be hidden.
01:23
And so you have a sheet and you would have a number of sheets of these to form.
01:32
The graphite.
01:34
Now, why is this important? in a tetrahedral structure, all three dimensions are locked, but in graphite, only two dimensions are locked.
01:48
So what that means is that there can be motion from left to right in each of these...