ok, I think I got it.
Hmm, perhaps not.
I notice in
Message 159, you wrote:
But one thing I am certain of is that that has to be the assumption--that the rock was originally 100% Potassium. Otherwise, it would be imposssible to determine its age.
No, it doesn't have to be 100% potassium. If it were, the potassium would likely oxidize pretty quickly, and that "rock" wouldn't last long. Other elements in the rock would not affect the ratio of potassium 40 to argon 40.
What you need is a stable rock, containing some measurable amount of a chemically stable potassium compound. You need the rock to be such that argon cannot escape from the rock. What you measure, is the amount of potassium 40 still present in the rock, and the amount of argon 40. It is the ratio of potassium 40 to argon 40 that indicates how much of the potassium has decayed.
For example, if there are about equal amounts of potassium 40 and argon 40, then half of the original potassium 40 has decayed. Hence the age of the rock is about the half-life of potassium 40 (1.3 billion years).
The assumption being made is that the argon 40 all comes from potassium 40 decay. Since argon 40 is a gas, it is unlikely that any significant amount would be trapped in the rock at the time the rock solidified. The method is applied to igneous rock (rock that solidified from a lava flow, for example), and gives the age of the rock since the time it solidified.
It doesn't matter what else is in the rock, provided that there are no other sources of argon 40, and no ways that some of the argon 40 could have escaped.