Selection of the Mars Science Laboratory Landing Site

被引:0
作者
M. Golombek
J. Grant
D. Kipp
A. Vasavada
R. Kirk
R. Fergason
P. Bellutta
F. Calef
K. Larsen
Y. Katayama
A. Huertas
R. Beyer
A. Chen
T. Parker
B. Pollard
S. Lee
Y. Sun
R. Hoover
H. Sladek
J. Grotzinger
R. Welch
E. Noe Dobrea
J. Michalski
M. Watkins
机构
[1] California Institute of Technology,Jet Propulsion Laboratory
[2] Smithsonian Institution,National Air and Space Museum
[3] U.S. Geological Survey,Laboratory Atmospheric and Space Physics
[4] University of Colorado,Lunar and Planetary Exploration Program Group
[5] Japan Aerospace Exploration Agency,undefined
[6] NASA Ames Research Center,undefined
[7] California Institute of Technology,undefined
[8] University of Colorado,undefined
[9] University of Montana Western,undefined
[10] Planetary Science Institute,undefined
来源
Space Science Reviews | 2012年 / 170卷
关键词
Landing sites; Mars; Surface materials; Surface characteristics; Mars Science Laboratory;
D O I
暂无
中图分类号
学科分类号
摘要
The selection of Gale crater as the Mars Science Laboratory landing site took over five years, involved broad participation of the science community via five open workshops, and narrowed an initial >50 sites (25 by 20 km) to four finalists (Eberswalde, Gale, Holden and Mawrth) based on science and safety. Engineering constraints important to the selection included: (1) latitude (±30°) for thermal management of the rover and instruments, (2) elevation (<−1 km) for sufficient atmosphere to slow the spacecraft, (3) relief of <100–130 m at baselines of 1–1000 m for control authority and sufficient fuel during powered descent, (4) slopes of <30° at baselines of 2–5 m for rover stability at touchdown, (5) moderate rock abundance to avoid impacting the belly pan during touchdown, and (6) a radar-reflective, load-bearing, and trafficable surface that is safe for landing and roving and not dominated by fine-grained dust. Science criteria important for the selection include the ability to assess past habitable environments, which include diversity, context, and biosignature (including organics) preservation. Sites were evaluated in detail using targeted data from instruments on all active orbiters, and especially Mars Reconnaissance Orbiter. All of the final four sites have layered sedimentary rocks with spectral evidence for phyllosilicates that clearly address the science objectives of the mission. Sophisticated entry, descent and landing simulations that include detailed information on all of the engineering constraints indicate all of the final four sites are safe for landing. Evaluation of the traversabilty of the landing sites and target “go to” areas outside of the ellipse using slope and material properties information indicates that all are trafficable and “go to” sites can be accessed within the lifetime of the mission. In the final selection, Gale crater was favored over Eberswalde based on its greater diversity and potential habitability.
引用
收藏
页码:641 / 737
页数:96
相关论文
共 525 条
[1]  
Anderson F.S.(2003)Analysis of MOLA data for the Mars Exploration Rover landing sites J. Geophys. Res. 108 8084-128
[2]  
Haldemann A.F.C.(2010)Geologic mapping and characterization of Gale Crater and implications for its potential as a Mars Science Laboratory landing site Mars 5 76-1630
[3]  
Bridges N.T.(2011)Stratigraphy, mineralogy, and origin of layered deposits inside Terby crater, Mars Icarus 111 1626-1581
[4]  
Golombek M.P.(2006)Nature and origin of the hematite-bearing plains of Terra Meridiani based on analyses of orbital and Mars Exploration rover data sets J. Geophys. Res. 113 8085-404
[5]  
Parker T.J.(2008)Mars Exploration Program 2007 Phoenix landing site selection and characteristics J. Geophys. Res. 287 1576-104
[6]  
Neumann G.(2000)A global view of martian surface compositions from MGS-TES Science 109 400-1775
[7]  
Anderson R.B.(2004)Atmospheric correction and surface spectral unit mapping using thermal emission imaging system data J. Geophys. Res. 108 91-833
[8]  
Bell J.F.(2003)Meter-scale slopes of candidate MER landing sites from point photoclinometry J. Geophys. Res. 32 1766-245
[9]  
Ansan V.(2005)Dynamic river channels suggest a long-lived Noachian crater lake on Mars Geophys. Res. Lett. 307 830-23688
[10]  
Loizeau D.(2005)Mars surface diversity as revealed by the OMEGA/Mars Express observations Science 312 235-62