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Showing 1 - 3 of 3 matches in All Departments
Observational, experimental and analytical data show that C60,
larger fullerenes, and related structures of elemental carbon exist
in interstellar space, meteorites, and on Earth and are associated
with meteorite in impact events and in carbon-rich environments
such as coals (shungite) and bitumen. The existence of natural
fullerenes is at best contested and incompletely documented;
realistically it is still controversial. Their presence in
astronomical environments can be experimentally constrained but
observationally they remain elusive. Fullerenes formation in
planetary environments is poorly understood. They survived for
giga-years when the environmental conditions were exactly right but
even then only a fraction of their original abundance survived.
Natural fullerenes and related carbon structures are found in
interstellar space, in carbonaceous meteorites associated with
giant meteorite impacts (including at the Cretaceous-Tertiary
boundary) as well as in soot, coal and natural bitumen.
This text should appeal to all researchers who have an interest in Leonid showers. It contains over 40 research papers that present some of the first observational results of the November 1999 Leonid meteor storm, the first storm observed by modern observing techniques. The book is a glimpse of the large amount of information obtained during NASA's Leonid Multi-Instrument Aircraft Campaign and groundbased campaigns throughout the world. It provides an overview on the state of meteor shower research for any professional researcher or amateur meteor observer interested in studies of meteors and meteoroids and their relation to comets, the origin of life on Earth, the satellite impact hazard issue, and upper atmosphere studies of neutral atom chemistry, the formation of meteoric debris, persistent trains, airglow, noctilucent clouds, sprites and elves.
Observational, experimental and analytical data show that C60,
larger fullerenes, and related structures of elemental carbon exist
in interstellar space, meteorites, and on Earth and are associated
with meteorite in impact events and in carbon-rich environments
such as coals (shungite) and bitumen. The existence of natural
fullerenes is at best contested and incompletely documented;
realistically it is still controversial. Their presence in
astronomical environments can be experimentally constrained but
observationally they remain elusive. Fullerenes formation in
planetary environments is poorly understood. They survived for
giga-years when the environmental conditions were exactly right but
even then only a fraction of their original abundance survived.
Natural fullerenes and related carbon structures are found in
interstellar space, in carbonaceous meteorites associated with
giant meteorite impacts (including at the Cretaceous-Tertiary
boundary) as well as in soot, coal and natural bitumen.
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