作者: Janice S. Lee , Bonnie J. Buratti , Michael Hicks , Joel Mosher
DOI: 10.1016/J.ICARUS.2009.11.008
关键词: Planetary surface 、 Geology 、 Surface roughness 、 Impact crater 、 Radius 、 ICARUS 、 Albedo 、 Scattering 、 Surface finish 、 Astrobiology 、 Astrophysics
摘要: Abstract The roughness of a planetary surface offers clues to its past geologic history. We apply model developed by Buratti and Veverka (Buratti, B.J., Veverka, J. [1985]. Icarus 64, 320–328) Cassini ISS data from the January 1st, 2005 flyby Iapetus. This uses observed scattering behavior provide depth radius factor q quantifying size idealized craters on surface. Our findings indicate that dark side is significantly smoother than surfaces other icy low-albedo saturnian satellites. have found average leading (dark) 0.084, corresponding Hapke mean slope angle 6°. As compared 13–33° satellites 10 colleagues [2008]. 193, 309–322), our results present clearly different picture for Iapetus, suggesting deposit contributes decrease in macroscopic side. Attempts were made obtain an value trailing (bright) side; however scans bright this exhibited large variations albedo, resulting physically unrealistic.