Planetary science: Sodium at Io
نویسندگان
چکیده
منابع مشابه
Sodium Emission from Io: Implications
The surface of lo may be covered with a layer of ammonia ice containing trace amounts of sodium potassium, and calcium; and atmospheric nitrogen could be formed as a photochemical product of ammonia photolysis. Intense sporadic sodium emission from Io can be excited by collisions involving vib~ationally excited n.itrogen molecules. These metastable molecules may be formed by electron impact, wi...
متن کاملGalactic planetary science
Planetary science beyond the boundaries of our Solar System is today in its infancy. Until a couple of decades ago, the detailed investigation of the planetary properties was restricted to objects orbiting inside the Kuiper Belt. Today, we cannot ignore that the number of known planets has increased by two orders of magnitude nor that these planets resemble anything but the objects present in o...
متن کاملPLANETARY SCIENCE Dust observations at orbital altitudes surrounding Mars
Dust is common close to the martian surface, but no known process can lift appreciable concentrations of particles to altitudes above ~150 kilometers.We present observations of dust at altitudes ranging from 150 to above 1000 kilometers by the Langmuir Probe and Wave instrument on the Mars Atmosphere and Volatile Evolution spacecraft. Based on its distribution, we interpret this dust to be inte...
متن کاملLAPLAS: Laboratory Planetary Science at Future FAIR Facility
Study of the structures of giant planets, Jupiter, Saturn, Uranus and Neptune is a very interesting subject as this knowledge could lead to clues about formation of the solar system and can also shed light on the early stages of evolution of life on earth. The first two planets are believed to be made mainly of hydrogen that exists under extreme conditions, while the latter two are expected to ...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: Nature
سال: 2003
ISSN: 0028-0836
DOI: 10.1038/421030a