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Media Advisory:

Month July 14, 1997

Contact: Donald D. Clayton, Clemson University, (864) 656-5299
G. Jeffrey Taylor, Hawai'i Inst. of Geophysics and PlanetologyProgram Chair, Meteoritical Society, Meeting(808) 956-3899

 

MORE INFORMATION, INCLUDING PICTURES: Planetary Science Research Discoveries, a science magazine on the World Wide Web edited by Jeff Taylor and Linda Martel of the University of Hawai'i: www.soest.hawaii.edu/PSRdiscoveries

Ancient stardust in meteorites helps explain evolution of galaxy, Maui conference will learn:

Meteorites contain microscopic grains of dust from stars that existed long before our Solar System formed. This ancient stardust holds information not only about the processes that operate inside stars, but about the dynamics and evolution of the Milky Way Galaxy as well. That is the conclusion Donald Clayton of Clemson University's Department of Physics and Astronomy will report Monday afternoon, July 21, at the 60th meeting of the Meteoritical Society.

The July 21-25 conference of meteorite researchers takes place at the Maui Prince Hotel in Makena, Maui, Hawai'i, and will be hosted by the Hawai'i Institute of Geophysics and Planetology. Clayton's study is also published in the July 20 issue of Astrophysical Journal Letters, and a version for the general public appears in the popular web science magazine, Planetary Science Research Discoveries, www.soest.hawaii.edu/PSRdiscoveries.

The research that led to these dramatic conclusions builds on a decade of painstaking work by meteoriticists. One of the pioneers in the study of "presolar grains" is Ernst Zinner of Washington University in St. Louis. Zinner will receive the Meteoritical Society's prestigious Leonard Medal on Wednesday evening, July 23.

Scientists isolate the presolar grains in a meteorite by using a mixture of acids to dissolve away 99.9% of the meteorite. One meteoriticist, Edward Anders (formerly of the University of Chicago, now living in Bern, Switzerland), likens this process to 'burning down the haystack to find the needle.' The grains are identified as "presolar" by their highly unusual abundances of isotopes of several elements, including silicon, carbon, nitrogen, and titanium&emdash;compositions that are drastically different from normal material from the Solar System.

One class of presolar grains, silicon carbide (SiC), was the focus of Clayton's work. Meteorite scientists discovered a decade ago that these presolar grains have a higher proportion of silicon-29 and silicon-30 than common Solar System silicon. (Silicon-28, the most abundant isotope of silicon, forms the "comparison standard." That is, for equal numbers of silicon-28 atoms, the presolar silicon has more silicon-29 and silicon-30 atoms than does average Solar System silicon.) This discovery, primarily by researchers at Chicago, Caltech, Washington University (St. Louis) and Bern University in Switzerland, has astonished, delighted and challenged scientists for several years.

How, they wondered, can presolar stars have more silicon-29 and silicon-30 than the sun has when those stars, by definition, formed and lived their lives prior to the birth of the sun? Theoretical considerations led scientists to expect that presolar stars should have less silicon-29 and silicon-30 than the sun, not more.

Clayton's new work presents a solution that couples his earlier ideas to growing astronomical evidence that the galactic orbits of stars change over time. Because the element abundances are higher in more central regions of the galaxy, Clayton suggests that the carbon stars were born there, rather than at the location of the sun's birth. During their approximately 2-billion-year lifetimes, their orbits enlarged, taking them far from the galaxy's center. Many, Clayton suggests, ended their lives near the cloud in which our Solar System formed, and deposited their dust there.

This explanation meets astronomical knowledge and expectations except in one respect: Why would the carbon stars move to larger orbits? Clayton's explanation involves their "scattering" from molecular clouds in the inner galaxy. Because of their great masses (about 100,000 times that of the sun), these molecular clouds provide a strong gravitational force. When the carbon stars approach, the clouds' gravity field causes the stars to accelerate; the stars' higher speeds then place them on orbits that reach further out. This same scattering phenomenon, Clayton notes, is used in current human efforts to visit the outer solar system. For example, the Voyager spacecraft was allowed to approach Jupiter's strong gravity as it flew past the giant planet and its moons. Jupiter's gravity caused Voyager to pick up speed and it was scattered past that planet to a new orbit farther out. NASA has used this type of "gravity assist" on other missions as well. Clayton now suggests that it was also used by our own Milky Way galaxy to fling stars into orbits far from their origins.

Astronomers as well as meteorite scientists are excited by this possibility. There are not many ways to learn about stars that existed before the sun in the more central portion of our galaxy. Clayton's work suggests that their stardust carries the message of their history. This means that carefully measuring the relative frequencies of these particles will allow astronomers to map the dynamic history of our Milky Way.

"What an astronomical story to read within a stone!" Clayton says.

 

-UH-