SCIENCE APPLICATIONS OF THE MARS-OBSERVER GAMMA-RAY SPECTROMETER

被引:38
作者
BOYNTON, WV
TROMBKA, JI
FELDMAN, WC
ARNOLD, JR
ENGLERT, PAJ
METZGER, AE
REEDY, RC
SQUYRES, SW
WANKE, H
BAILEY, SH
BRUCKNER, J
CALLAS, JL
DRAKE, DM
DUKE, P
EVANS, LG
HAINES, EL
MCCLOSKEY, FC
MILLS, H
SHINOHARA, C
STARR, R
机构
[1] UNIV ARIZONA, LUNAR & PLANETARY LAB, TUCSON, AZ 85721 USA
[2] NASA, GODDARD SPACE FLIGHT CTR, GREENBELT, MD 20771 USA
[3] LOS ALAMOS NATL LAB, LOS ALAMOS, NM 87545 USA
[4] UNIV CALIF SAN DIEGO, DEPT CHEM, LA JOLLA, CA 92093 USA
[5] SAN JOSE STATE UNIV, DEPT CHEM, SAN JOSE, CA 95192 USA
[6] JET PROP LAB, PASADENA, CA 91109 USA
[7] CORNELL UNIV, CTR RADIOPHYS & SPACE RES, ITHACA, NY 14853 USA
[8] MAX PLANCK INST CHEM, W-6500 MAINZ, GERMANY
[9] SUNRISE RES INC, EUGENE, OR USA
关键词
D O I
10.1029/92JE00538
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The Mars Observer gamma ray spectrometer will return data related to the elemental composition of Mars. The instrument has both a gamma ray spectrometer and several neutron detectors. The gamma ray spectrometer will return a spectrum nominally every 20 s from Mars permitting a map of the elemental abundances to be made. The gamma rays are emitted from nuclei involved in radioactive decay, from nuclei formed by capture of a thermal neutron, and from nuclei put in an excited state by a fast-neutron interaction. The gamma rays come from an average depth of the order of a few tens of centimeters. The spectrum will show sharp emission lines whose intensity determines the concentration of the element and whose energy identifies the element. The neutron detectors, using the fact that the orbital velocity of the Mars Observer spacecraft is similar to the velocity of thermal neutrons, determine both the thermal and epithermal neutron flux. These parameters are particularly sensitive to the concentration of hydrogen in the upper meter of the surface. By combining the results from both techniques it is possible to map the depth dependence of hydrogen in the upper meter as well. These data permit a variety of Martian geoscience problems to be addressed including the crust and mantle composition, weathering processes, volcanism, and the volatile reservoirs and processes. In addition, the instrument is also sensitive to gamma ray and particle fluxes from non-Martian sources and will be able to address problems of astrophysical interest including gamma ray bursts, the extragalactic background, and solar processes.
引用
收藏
页码:7681 / 7698
页数:18
相关论文
共 50 条
[41]   A CHEMICAL AND PETROLOGICAL MODEL OF THE LUNAR CRUST AND IMPLICATIONS FOR LUNAR CRUSTAL ORIGIN [J].
SPUDIS, PD ;
DAVIS, PA .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1986, 91 (B13) :E84-E90
[42]   NUCLEAR-PHYSICAL METHODS OF ANALYSIS IN LUNAR AND PLANETARY INVESTIGATIONS [J].
SURKOV, YA .
ISOTOPENPRAXIS, 1984, 20 (09) :321-329
[43]   DETERMINATION OF THE ELEMENTAL COMPOSITION OF MARTIAN ROCKS FROM PHOBOS-2 [J].
SURKOV, YA ;
BARSUKOV, VL ;
MOSKALEVA, LP ;
KHARYUKOVA, VP ;
ZAITSEVA, SY ;
SMIRNOV, GG ;
MANVELYAN, OS .
NATURE, 1989, 341 (6243) :595-598
[44]  
SURKOV YA, 1991, IN PRESS REMOTE GEOC
[45]   REANALYSIS OF APOLLO COSMIC GAMMA-RAY SPECTRUM IN 0.3 TO 10 MEV ENERGY REGION [J].
TROMBKA, JI ;
DYER, CS ;
EVANS, LG ;
BIELEFELD, MJ ;
SELTZER, SM ;
METZGER, AE .
ASTROPHYSICAL JOURNAL, 1977, 212 (03) :925-935
[46]  
TROMBKA JI, 1992, IN PRESS 22ND P LUN
[47]  
VANDILLA MA, 1962, IRE T NUCL SCI, V9, P405
[48]   CHEMICAL-COMPOSITION AND ACCRETION HISTORY OF TERRESTRIAL PLANETS [J].
WANKE, H ;
DREIBUS, G .
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES, 1988, 325 (1587) :545-557
[49]   WEAK PEAK PROBLEM IN HIGH-RESOLUTION GAMMA-RAY SPECTROSCOPY [J].
YADAV, JS ;
BRUCKNER, J ;
ARNOLD, JR .
NUCLEAR INSTRUMENTS & METHODS IN PHYSICS RESEARCH SECTION A-ACCELERATORS SPECTROMETERS DETECTORS AND ASSOCIATED EQUIPMENT, 1989, 277 (2-3) :591-598
[50]   DISTRIBUTION AND STATE OF H2O IN THE HIGH-LATITUDE SHALLOW SUBSURFACE OF MARS [J].
ZENT, AP ;
FANALE, FP ;
SALVAIL, JR ;
POSTAWKO, SE .
ICARUS, 1986, 67 (01) :19-36