Re: molten cores
- From: Chris L Peterson <clp@xxxxxxxxxxxxxxxxxx>
- Date: Wed, 25 Mar 2009 11:29:19 -0600
On Wed, 25 Mar 2009 10:10:58 -0400, "Seth Waterston"
<sethwaterston@xxxxxxxxx> wrote:
Radioactive decay from what elements and why wouldn't those element half
lives make them non-radioactive over billions of years? Also, wouldn't the
radioactivity show up in magma reaching the surface?
The primary radioisotopes associated with internal heating are U-238
(4.47 billion year half-life), U-235 (704 million year), Th-232 (14.1
billion year), and K-40 (1.28 billion year). Given these long
half-lifes, there is plenty of remaining activity since the formation of
the material.
The estimated Earth-average bulk heating from radioactive decay in the
core, mantle, and crust is about 6e-12 watts/kg. That's a very small
amount of heat, but still plenty to account for the heating of the
Earth's core.
Although magma doesn't consist of core material at all, and only just
barely consists of mantle material, it is- like all the material making
up the Earth- radioactive. Again, the typical activity level is very
low, but that's all that is required in the case of the well insulated
core.
_________________________________________________
Chris L Peterson
Cloudbait Observatory
http://www.cloudbait.com
.
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