[Geysers] Re: Radioactive rodents on the Pitchstone
TSBryan at aol.com
TSBryan at aol.com
Sun Apr 10 10:14:05 PDT 2011
I clearly recall having had a paper, published somewhere sometime like
maybe 30 years ago, that cited PLANTS from down around Polecat Creek (and so,
southeast Pitchstone area) radioactive enough to leave images on film.
Seems to me one of the plants was a locoweed. I've looked several places around
this mess and cannot find the article -- sorry. Not my field so I could be
wrong, but would plants be more likely to absorb this amount of
radioactive stuff?
Scott Bryan
In a message dated 4/10/2011 5:53:00 A.M. US Mountain Standard Time,
canbelto at gmail.com writes:
This has apparently been studied at least slightly, and another paper is
by R. Howald (or Howlad, sources differ), "'N22 HOWALD, Reed Montana state
University Radioactivity from Pitchstone Plateau area of YNP.' 1982", cited
in the YNP archives, as reached by
_http://www.nps.gov/yell/historyculture/upload/natural.pdf_
(http://www.nps.gov/yell/historyculture/upload/natural.pdf) -- Lee W may have easier and more complete access to this than the
rest of us.
This gets pretty close to what I do for a living (or did before I became a
useless paper pusher...), and I'd like to learn more of what actually
happened in this study and any others like it. The notion of radioactive
critters fogging photographic film seems far-fetched, to put it mildly.
However, naturally-occurring potassium contains about 1% K-40, a long-lived
radioactive isotope easily detected with modern sensors (and the bane of us folks
who do low-level detection because it's in natural background and you
can't get rid of it). K-40 is therefore present in living things in tiny
quantities, whether on the Pitchstone Plateau or elsewhere. Really long
exposures would be necessary to see it on photographic film, though. Radon in
rodents is not a credible source of photographic film fogging for various
reasons.
One of the pages that cites that Howald (Howlad? Howard) study says
something to the effect that the basalts of the Pitchstone Plateau contain "two
to three times" as much radioactivity as rocks elsewhere at YNP. To this,
all that I can say is "big deal." There are any number of places in the
world where you can get in a car and drive for five minutes, and produce
order-of-magnitude variations in natural background; I live in one of them
(Jemez Mountains of New Mexico) which just happens to have geology very similar
to YNP.
This whole thing strikes me as much ado about nothing, but the scientist
in me is interested in learning more about it, just out of curiosity. Other
links appreciated.
-- Bill, speaking only for himself.
On Thu, Apr 7, 2011 at 8:46 PM, Ruth & Leslie Quinn
<_ruthleslie.ynp at gmail.com_ (mailto:ruthleslie.ynp at gmail.com) > wrote:
I found the source where I think the original paper on this subject is
located. It's:
Linn, Robert M., editor, Proceedings of the 1st Conference on Scientific
Research in the National Parks (U. S. Department of the Interior, U. S.
Government Printing Office, Washington, DC, 1976, 2 volumes, 1325 pages). I
don't recall exactly where in there the paper is, but I'm pretty sure I saw it
in there once upon a time.
Leslie Quinn
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