The Mars Odyssey Gamma-Ray Spectrometer instrument suite

被引:227
作者
Boynton, WV [1 ]
Feldman, WC
Mitrofanov, IG
Evans, LG
Reedy, RC
Squyres, SW
Starr, R
Trombka, JI
D'Uston, C
Arnold, JR
Englert, PAJ
Metzger, AE
Wänke, H
Brückner, J
Drake, DM
Shinohara, C
Fellows, C
Hamara, DK
Harshman, K
Kerry, K
Turner, C
Ward, M
Barthe, H
Fuller, KR
Storms, SA
Thornton, GW
Longmire, JL
Litvak, ML
Ton'chev, AK
机构
[1] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA
[2] Los Alamos Natl Lab, Los Alamos, NM 87545 USA
[3] Space Res Inst, Moscow, Russia
[4] Comp Sci Corp, Sci Programs, Lanham, MD 20706 USA
[5] Univ New Mexico, Inst Meteorit, Albuquerque, NM 87131 USA
[6] Cornell Univ, Ctr Radiophys & Space Res, Ithaca, NY 14853 USA
[7] Catholic Univ Amer, Dept Phys, Washington, DC 20064 USA
[8] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[9] Ctr Etud Spatiale Rayonnements, Toulouse, France
[10] Univ Calif San Diego, Dept Chem, La Jolla, CA 92093 USA
[11] Univ Hawaii Manoa, Honolulu, HI 96822 USA
[12] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[13] Max Planck Inst Chem, D-55128 Mainz, Germany
[14] Techsource, Santa Fe, NM 87505 USA
关键词
D O I
10.1023/B:SPAC.0000021007.76126.15
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The Mars Odyssey Gamma-Ray Spectrometer is a suite of three different instruments, a gamma subsystem (GS), a neutron spectrometer, and a high-energy neutron detector, working together to collect data that will permit the mapping of elemental concentrations on the surface of Mars. The instruments are complimentary in that the neutron instruments have greater sensitivity to low amounts of hydrogen, but their signals saturate as the hydrogen content gets high. The hydrogen signal in the GS, on the other hand, does not saturate at high hydrogen contents and is sensitive to small differences in hydrogen content even when hydrogen is very abundant. The hydrogen signal in the neutron instruments and the GS have a different dependence on depth, and thus by combining both data sets we can infer not only the amount of hydrogen, but constrain its distribution with depth. In addition to hydrogen, the GS determines the abundances of several other elements. The instruments, the basis of the technique, and the data processing requirements are described as are some expected applications of the data to scientific problems.
引用
收藏
页码:37 / 83
页数:47
相关论文
共 77 条
[51]   GAMMA-RAY SPECTROSCOPIC MEASUREMENTS OF MARS [J].
METZGER, AE ;
ARNOLD, JR .
APPLIED OPTICS, 1970, 9 (06) :1289-&
[52]   HIGH-ENERGY IRRADIATIONS SIMULATING COSMIC-RAY-INDUCED PLANETARY GAMMA-RAY PRODUCTION .1. FE TARGET [J].
METZGER, AE ;
PARKER, RH ;
YELLIN, J .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1986, 91 (B4) :D495-D504
[53]   IDENTIFICATION OF LUNAR ROCK TYPES AND SEARCH FOR POLAR ICE BY GAMMA-RAY SPECTROSCOPY [J].
METZGER, AE ;
DRAKE, DM .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1990, 95 (B1) :449-460
[54]   DETECTION OF INTERSTELLAR FLUX OF GAMMA-RAYS [J].
METZGER, AE ;
ANDERSON, EC ;
VANDILLA, MA ;
ARNOLD, JR .
NATURE, 1964, 204 (496) :766-+
[55]  
METZGER AE, 1986, LUNAR PLANET SCI, V17, P549
[56]  
METZGER AE, 1984, B AM ASTRON SOC, V16, P678
[57]  
METZGER AE, 1975, P LUNAR PLANET SCI C, P2769
[58]   Maps of subsurface hydrogen from the high energy neutron detector, Mars Odyssey [J].
Mitrofanov, I ;
Anfimov, D ;
Kozyrev, A ;
Litvak, M ;
Sanin, A ;
Tret'yakov, V ;
Krylov, A ;
Shvetsov, V ;
Boynton, W ;
Shinohara, C ;
Hamara, D ;
Saunders, RS .
SCIENCE, 2002, 297 (5578) :78-81
[59]   HIGH-ENERGY PROTON RADIATION-DAMAGE OF HIGH-PURITY GERMANIUM DETECTORS [J].
PEHL, RH ;
VARNELL, LS ;
METZGER, AE .
IEEE TRANSACTIONS ON NUCLEAR SCIENCE, 1978, 25 (01) :409-417
[60]  
PRETTYMAN TH, 2002, 33 LUN PLAN SCI C