Southwest Research Institute | 2015 Nov 09
[c][attachment=0]earth-moon[1].jpg[/attachment][/c][hr][/hr]Scientists at Southwest Research Institute combined dynamical, thermal, and chemical models of the Moon’s formation to explain the relative lack of volatile elements in lunar rocks. Lunar rocks closely resemble Earth rocks in many respects, but Moon rocks are more depleted in volatile elements like potassium, sodium, and zinc, which tend to have lower boiling points and vaporize readily.
“Explaining the Moon’s volatile depletion has been a long-standing mystery, and yet it is a key piece of evidence about how the Earth-Moon system formed,” said Dr. Robin Canup, associate vice president in SwRI’s Space Science and Engineering Division and lead author of the Nature Geoscience paper detailing the findings.
Scientists think the Moon formed from an Earth-orbiting disk of vapor and molten matter produced by a giant impact between Earth and another Mars-sized body approximately 4.5 billion years ago. Previously, scientists had considered that volatiles vaporized by the impact might have escaped before the Moon formed.
“However, few volatiles may have actually been lost because the velocity needed to escape the Earth’s gravity is quite high,” said Canup. “The new research suggests instead that as the Moon completed its growth, volatile-rich melt was preferentially deposited onto the Earth, rather than onto the growing Moon.”
Canup’s team — which included researchers from SwRI, Dordt College, and Washington University — began with an existing computer simulation of the Moon’s accumulation from the disk. This was combined with models for how the temperature and chemical composition of the disk material evolve with time.
The models show that the Moon acquires about the final half of its mass from melt condensed in the inner portions of the disk, close to the Earth and just inside the Moon’s initial orbit. Over time, the Moon’s orbit expands due to dynamical interactions with inner disk material. When the Moon is distant enough, it can no longer efficiently accumulate inner disk melt, which is instead scattered inward and assimilated by the Earth. ...
Lunar volatile depletion due to incomplete accretion within an impact-generated disk - Robin M. Canup et al
- Nature Geoscience (online 09 Nov 2015) DOI: 10.1038/ngeo2574