Livermore research tops NASA's science highlights
Allende meteorite. Image courtesy of NASA GSFC.
Research
conducted by Livermore scientists that determined some of the oldest objects in
the solar system formed far away from our sun and then later fell back into the
mid-plane of the solar system has landed a top spot in this year's NASA Science
Highlights.
The research may lead to a greater understanding of how our solar system and
possibly other solar systems formed and evolved.
Calcium,
aluminum-rich inclusions (CAIs), roughly millimeter- to centimeter in size, are
believed to have formed very early in the evolution of the solar system and had
contact with nebular gas, either as solid condensates or as molten droplets.
Relative to planetary materials, CAIs are enriched with the lightest oxygen
isotope and are believed to record the oxygen composition of solar nebular gas
where they grew. CAIs, at 4.57 billion years old, are millions of years older
than more modern objects in the solar system, such as planets, which formed
about 10-50 million years after CAIs.
Using Lawrence Livermore's NanoSIMS (nanometer-scale secondary-ion mass
spectrometer) -- an instrument that can analyze samples with nanometer-scale
spatial resolution -- LLNL scientists in conjunction with NASA Johnson Space
Center, University of California, Berkeley and the University of Chicago
measured the concentrations of oxygen isotopes found in the CAIs.
In the recent research, the team studied a specific CAI found in a piece of the
Allende meteorite. Allende is the largest carbonaceous chondrite meteorite ever
found on Earth. It fell to the ground in 1969 over the Mexican state of
Chihuahua and is notable for possessing abundant CAIs.
For more information on the research, see the first item on the NASA Science
Highlights Website.
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