[Rockhounds] Terlingua-type calcite
DonH
donhalterman at verizon.net
Fri Jul 11 22:48:13 PDT 2008
Doug Leeper wrote:
> If you have a piece of this calcite that does this that you can part
> with, I can obtain a very accurate response in the visible spectrum,
> possibly that may show the source?
>
> I'm thinking like emission lines you get from various elements...
>
> I have sources with 365nm, 290nm, 390nm, and 460nm dominant wavelengths
> I could stimulate it with.
Hi Doug,
I think the issue here is that we don't know the exact electron
transitions that cause the colors. I encourage your experimentation,
but you might like to know what has gone before.
Some experiments were performed on this calcite by a young student who
was working with George Rossman at CalTech. The results were published
in UV Waves, a publication of the Fluorescent Mineral Society. I don't
have the issue at hand and I don't remember exactly what was, and was
not, determined by those experiments.
Along with Earl Verbeek at the Sterling Hill Mining Museum and the
Thomas S. Warren Museum of Fluorescence, I used a Varian Cary Eclipse
UV-VIS spectrophotometer to run continuous scans on Terlingua-type
calcites. Their emissions are complex, with at least three and possibly
four emission peaks in the LW UV as well as in the visible, along with
the issues of primary and secondary fluorescence and phosphorescence. I
was speaking with an experienced spectroscopist last week about another
matter, and the subject of this calcite came up. The consensus was that
more detailed work needs to be done, possibly using laser ablation
inductively coupled mass spectrometry to ascertain the trace elements,
and I think it would be useful to conduct single-crystal x-ray
diffraction to try to determine the distributions and ordering of those
trace elements. If anyone has done these things, neither of us was
aware of it.
Certain substitutions and their effects are well known; others are not.
For example, divalent europium can substitute nicely for calcium in
many structures (depending on how many oxygen surround the calcite in
the coordination polyhedron), due to its size and charge. Europium is
known to produce a blue fluorescence, though I imagine this is not an
iron-clad rule and may depend upon what mineral it is substituted into
and also what co-activators exist as well, and also structural defects
introduced into the mineral. On the other hand, some activators are not
well documented at all, though there may be educated speculation for
some of them.
The end result is that you may get a well-defined emission spectrum for
Terlingua-type calcite, but the real challenge is defining the cause of
each primary and secondary fluorescence and the phosphorescence seen at
each excitation wavelength, since it all changes as the excitation
wavelength increases.
Unfortunately, all my specimens are packed away in preparation for
moving to wherever my new job (when I get one) will be, or else I would
send you a piece. If no one on the list has some to spare, you can
always buy a small piece from an Internet dealer. I encourage you to
see what you can discover.
best,
Don
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