NatGeo: Pluto Has Oceans Under Ice?

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bystander
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NatGeo: Pluto Has Oceans Under Ice?

Post by bystander » Fri Dec 17, 2010 4:50 am

Pluto Has Oceans Under Ice?
National Geographic | 16 Dec 2010
Radioactive heat may warm Pluto's core, model suggests.
Frigid Pluto, home to some of our solar system's chilliest real estate, may well harbor an ocean beneath its miles-thick ice shell, new research suggests.

Despite its extreme cold, the dwarf planet still appears to be warm enough to "easily" have a subsurface ocean, according to a new model of the rate at which radioactive heat might still warm Pluto's core.

And that ocean wouldn't be a mere puddle, noted planetary scientist Guillaume Robuchon of the University of California, Santa Cruz.

Rather, the ocean could be 60 to 105 miles (100 to 170 kilometers) thick beneath a 120-mile (200-kilometer) layer of ice, Robuchon said at an annual meeting of the American Geophysical Union in San Francisco earlier this week.

If so, Pluto would join a list of outer solar system bodies—such as Saturn's moons Titan and Enceladus—believed to possibly hold liquid water, a key ingredient for life as we know it.

Pluto's heat would come from the decay of radioactive nuclides, particularly potassium-40, in rocks deep in the dwarf planet's interior.
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Re: NatGeo: Pluto Has Oceans Under Ice?

Post by neufer » Fri Dec 17, 2010 2:22 pm

bystander wrote:Pluto Has Oceans Under Ice?
National Geographic | 16 Dec 2010
Radioactive heat may warm Pluto's core, model suggests.

Pluto's heat would come from the decay of radioactive nuclides, particularly potassium-40, in rocks deep in the dwarf planet's interior.
Image
Potassium-40 is the largest source of
natural radioactivity in both animals & people.
http://en.wikipedia.org/wiki/Potassium-40 wrote:
<<Potassium-40 (40K) is a rare radioactive isotope of potassium which has a very long half life of 1.248×109 yr. It is a rare example of an isotope which undergoes all three types of beta decay (β−, β+ and electron capture). About 89% of the time 40K decays to calcium-40 (40Ca). However, 11% of the time it decays to argon-40 (40Ar).

Potassium-40 is especially important in potassium–argon dating (K–Ar dating). When rocks melt into lava, it releases argon it previously contained, thus will be an argon-free rock when it cools down. If a cooled rock contains any potassium-40, then argon-40 will build up over time as the remaining 40K decays. This created argon cannot escape from the solid rock. The lifetimes of 40K and 40Ar are well known, thus it is then possible to determine the time elapsed since the rock last cooled by measuring the levels of 40K and 40Ar contained in the rock. Despite trapping of 40Ar in many rocks, it can be released by melting, grinding, and diffusion. Almost all of the argon in the Earth's atmosphere is the product of potassium-40 decay, since 99.6% of Earth atmosphere argon is 40Ar, whereas in the Sun and presumably in primordial star-forming clouds, argon consists of < 15% 40Ar and mostly (85%) 36Ar.>>
Art Neuendorffer

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