Detection of Perchlorate and the Soluble Chemistry of Martian Soil at the Phoenix Lander Site

被引:843
作者
Hecht, M. H. [1 ]
Kounaves, S. P. [2 ]
Quinn, R. C. [3 ]
West, S. J. [4 ]
Young, S. M. M. [2 ]
Ming, D. W. [5 ]
Catling, D. C. [6 ,7 ]
Clark, B. C. [8 ]
Boynton, W. V. [9 ]
Hoffman, J. [10 ]
DeFlores, L. P. [1 ]
Gospodinova, K. [2 ]
Kapit, J. [2 ]
Smith, P. H. [9 ]
机构
[1] CALTECH, Jet Prop Lab, Pasadena, CA 91109 USA
[2] Tufts Univ, Dept Chem, Medford, MA 02155 USA
[3] NASA, Ames Res Ctr, SETI Inst, Moffett Field, CA 94035 USA
[4] Invensys Proc Syst, Foxboro, MA 02035 USA
[5] NASA, Lyndon B Johnson Space Ctr, Astromat Res & Explorat Sci Directorate, Houston, TX 77058 USA
[6] Univ Bristol, Dept Earth Sci, Bristol BS8 1RJ, Avon, England
[7] Univ Washington, Dept Earth & Space Sci, Seattle, WA 98195 USA
[8] Space Sci Inst, Boulder, CO 80301 USA
[9] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA
[10] Univ Texas Dallas, Dept Phys, Richardson, TX 75080 USA
关键词
CHEMICAL-COMPOSITION; MARS; SURFACE; SPECTROMETER; ORIGIN; ROCKS;
D O I
10.1126/science.1172466
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The Wet Chemistry Laboratory on the Phoenix Mars Lander performed aqueous chemical analyses of martian soil from the polygon-patterned northern plains of the Vastitas Borealis. The solutions contained similar to 10 mM of dissolved salts with 0.4 to 0.6% perchlorate (ClO4) by mass leached from each sample. The remaining anions included small concentrations of chloride, bicarbonate, and possibly sulfate. Cations were dominated by Mg2+ and Na+, with small contributions from K+ and Ca2+. A moderately alkaline pH of 7.7 +/- 0.5 was measured, consistent with a carbonate-buffered solution. Samples analyzed from the surface and the excavated boundary of the similar to 5-centimeter-deep ice table showed no significant difference in soluble chemistry.
引用
收藏
页码:64 / 67
页数:4
相关论文
共 44 条
[1]   Microbial perchlorate reduction: A precise laboratory determination of the chlorine isotope fractionation and its possible biochemical basis [J].
Ader, Magali ;
Chaudhuri, Swades ;
Coates, John D. ;
Coleman, Max .
EARTH AND PLANETARY SCIENCE LETTERS, 2008, 269 (3-4) :604-612
[2]  
[Anonymous], 1992, Mars
[3]  
[Anonymous], 2004, Journal ofGeophysicalResearch, DOI [10.1029/2003JE002160, DOI 10.1029/2003JE002160]
[4]   Natural perchlorate has a unique oxygen isotope signature [J].
Bao, HM ;
Gu, BH .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2004, 38 (19) :5073-5077
[5]   MARINER 9 ULTRAVIOLET SPECTROMETER EXPERIMENT - SEASONAL-VARIATION OF OZONE ON MARS [J].
BARTH, CA ;
HORD, CW ;
STEWART, AI ;
LANE, AL ;
DICK, ML ;
ANDERSON, GP .
SCIENCE, 1973, 179 (4075) :795-796
[6]  
Besley L.M., 1969, The Journal of Chemical Thermodynamics, V1, P13, DOI DOI 10.1016/0021-9614(69)90032-9
[7]   Mars surface diversity as revealed by the OMEGA/Mars Express observations [J].
Bibring, JP ;
Langevin, Y ;
Gendrin, A ;
Gondet, B ;
Poulet, F ;
Berthé, M ;
Soufflot, A ;
Arvidson, R ;
Mangold, N ;
Mustard, J ;
Drossart, P .
SCIENCE, 2005, 307 (5715) :1576-1581
[8]   On the ability of the Viking gas chromatograph-mass spectrometer to detect organic matter [J].
Biemann, Klaus .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2007, 104 (25) :10310-10313
[9]   Perchlorate isotope forensics [J].
Böhlke, JK ;
Sturchio, NC ;
Gu, BH ;
Horita, J ;
Brown, GM ;
Jackson, WA ;
Batista, J ;
Hatzinger, PB .
ANALYTICAL CHEMISTRY, 2005, 77 (23) :7838-7842
[10]   Evidence for Calcium Carbonate at the Mars Phoenix Landing Site [J].
Boynton, W. V. ;
Ming, D. W. ;
Kounaves, S. P. ;
Young, S. M. M. ;
Arvidson, R. E. ;
Hecht, M. H. ;
Hoffman, J. ;
Niles, P. B. ;
Hamara, D. K. ;
Quinn, R. C. ;
Smith, P. H. ;
Sutter, B. ;
Catling, D. C. ;
Morris, R. V. .
SCIENCE, 2009, 325 (5936) :61-64