TY - JOUR
T1 - Observations of molecular oxygen ions in Saturn's inner magnetosphere
AU - Martens, Hilary R.
AU - Reisenfeld, Daniel B.
AU - Williams, John D.
AU - Johnson, Robert E.
AU - Smith, H. Todd
PY - 2008/10/28
Y1 - 2008/10/28
N2 - We present an analysis of molecular oxygen ion (O2+) abundance in Saturn's inner magnetosphere based on observations made with the Cassini Plasma Spectrometer (CAPS). Using data summed over 23 orbits, we resolve and isolate O2+counts from the tail of the water group ion mass distribution (W+ [O+, OH+, H2O+, H3O+]) and from background sources. O2+ was initially estimated at ∼ 1-2% of the total ion population in the inner magnetosphere based on CAPS data from the Saturn orbital insertion pass. Through refined analysis techniques, we have found O2+ to account for just above 0.3% of all W+ ions at L = 4.5, with only minor fluctuations in relative density out to L = 7.5 - 8.0. Beyond L = 7.5, the relative O2+/ W+ abundance exhibits a statistically significant increase through L = 10.5, which may indicate a neutral O2 source in the vicinity of Rhea.
AB - We present an analysis of molecular oxygen ion (O2+) abundance in Saturn's inner magnetosphere based on observations made with the Cassini Plasma Spectrometer (CAPS). Using data summed over 23 orbits, we resolve and isolate O2+counts from the tail of the water group ion mass distribution (W+ [O+, OH+, H2O+, H3O+]) and from background sources. O2+ was initially estimated at ∼ 1-2% of the total ion population in the inner magnetosphere based on CAPS data from the Saturn orbital insertion pass. Through refined analysis techniques, we have found O2+ to account for just above 0.3% of all W+ ions at L = 4.5, with only minor fluctuations in relative density out to L = 7.5 - 8.0. Beyond L = 7.5, the relative O2+/ W+ abundance exhibits a statistically significant increase through L = 10.5, which may indicate a neutral O2 source in the vicinity of Rhea.
UR - http://www.scopus.com/inward/record.url?scp=58249085976&partnerID=8YFLogxK
U2 - 10.1029/2008GL035433
DO - 10.1029/2008GL035433
M3 - Article
AN - SCOPUS:58249085976
SN - 0094-8276
VL - 35
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 20
M1 - L20103
ER -