[ RadSafe ] Radioactivity from volcanic eruptions?

Brennan, Mike (DOH) Mike.Brennan at DOH.WA.GOV
Mon Apr 19 15:44:33 CDT 2010


The last time Mt. St. Helen burped I researched the subject some.  In
the VERY short term, as in when the ash is falling.  Some of the people
at PNNL went outside and caught some ash, then ran it in and counted it.
The activity was fairly high (I don't remember numbers) from radon
daughter products.  This would indicate that it is a bad idea to breath
volcanic ash if you can avoid it, but I suspect there are more pressing
reasons to avoid doing that.

-----Original Message-----
From: radsafe-bounces at health.phys.iit.edu
[mailto:radsafe-bounces at health.phys.iit.edu] On Behalf Of Dan W McCarn
Sent: Friday, April 16, 2010 2:23 PM
To: 'Bjorn Cedervall'
Cc: radsafe at health.phys.iit.edu
Subject: Re: [ RadSafe ] Radioactivity from volcanic eruptions?

A good question, but I don't know the exact answer. "It depends."

What I can suggest is that as far as basaltic-type eruptions, basalt
normally contains only a small amount of uranium and is higher in
ferromagnesium content with relatively little free quartz and water, so
I
imagine that the answer would be a relatively small amount of radiation
in
gas (radon / thoron) associated with basaltic-type lavas.

Andesite, a quartz-rich volcanic rock, on the other hand, may contain
significant amounts of uranium, and I suppose, radon. It also contains a
larger quantity of free quartz & water and is generally far more
explosive
than basalts.  Uranium is frequently derived from these acidic
(quartz-rich)
volcanic tuffs or ash which is reconcentrated in sandstone deposits.  So
the
genesis of quite a few sandstone deposits is associated spatially with
uraniferous tuffs and ash falls.

The Hawaiian volcanoes are basaltic, deriving their magma from the upper
mantle / lower crust.  The andesitic volcanoes, such as those in the
Andes,
is generally remelted, subducted crust in which uranium has probably
been
concentrated.

I would imagine that in zones of elevated crustal abundance of uranium,
such
as the Western USA, the effusive vulcanism would reflect the elevated
concentration. Enrichment mechanisms, if present, could further increase
the
concentration.  Generally, the late-stage differentiation of a magma
will
retain water, quartz and uranium thus allowing for a processes of
reconcentration.  Volcanic rocks derived from such a magma would show
significant uranium enrichment.

http://tinyurl.com/BowenReactionSeries


The very large, 1 million year-old caldera near Los Alamos, the Valles
Caldera, has associated hot springs with about 10X background radiation,
probably from radium / radon and progeny.  Hot water bubbles-up through
fractures carrying minerals forming the travertine.  The water loses
both
H2S and CO2 as it arrives at the surface and immediately precipitates
CaCO3.
The travertine at the "Soda Dam", on the Jemez Spring side is a good
place
to observe elevated levels of radiation. The incredibly thick and
extensive,
welded tuff of the Bandelier Tuff was derived from successive, massive
explosions from the center of the caldera, emptying the magma chamber
and
allowing the caldera to collapse.  The heat source for this feature is
probably the Rio Grande Rift, a zone of crustal rifting, thin crust and
high
heat flow.

http://tinyurl.com/VallesCaldera

The Solar System abundance of elements ranks uranium as #92 of 92.  The
crustal abundance is about #34, so the processes of forming the earth's
crust have enriched uranium to about the same level as arsenic whose
crustal
and solar system abundance is about the same (#35, as I recall).

So, in summary, the process of crustal enrichment and magma
differentiation
would increase the amount of uranium in late-stage volcanic rocks.

Dan ii

--
Dan W McCarn, Geologist
2867 A Fuego Sagrado
Santa Fe, NM 87505
+1-505-310-3922 (Mobile - New Mexico)
HotGreenChile at gmail.com (Private email)
-----Original Message-----
From: radsafe-bounces at health.phys.iit.edu
[mailto:radsafe-bounces at health.phys.iit.edu] On Behalf Of Bjorn
Cedervall
Sent: Friday, April 16, 2010 08:28
To: radsafe at health.phys.iit.edu
Subject: [ RadSafe ] Radioactivity from volcanic eruptions?


Any comments regarding amounts and whether they can effect the
background
levels in any sense?

 

Perhaps some Radsafers good point at good sources of information for
those
of us who aren't too familiar with the topic?

 

Bjorn Cedervall   bcradsafers at hotmail.com

 
 		 	   		  
_________________________________________________________________
The New Busy is not the old busy. Search, chat and e-mail from your
inbox.
http://www.windowslive.com/campaign/thenewbusy?ocid=PID28326::T:WLMTAGL:
ON:W
L:en-US:WM_HMP:042010_3
_______________________________________________
You are currently subscribed to the RadSafe mailing list

Before posting a message to RadSafe be sure to have read and understood
the
RadSafe rules. These can be found at:
http://health.phys.iit.edu/radsaferules.html

For information on how to subscribe or unsubscribe and other settings
visit:
http://health.phys.iit.edu

_______________________________________________
You are currently subscribed to the RadSafe mailing list

Before posting a message to RadSafe be sure to have read and understood
the RadSafe rules. These can be found at:
http://health.phys.iit.edu/radsaferules.html

For information on how to subscribe or unsubscribe and other settings
visit: http://health.phys.iit.edu



More information about the RadSafe mailing list