| Literature DB >> 19574385 |
M H Hecht1, S P Kounaves, R C Quinn, S J West, S M M Young, D W Ming, D C Catling, B C Clark, W V Boynton, J Hoffman, L P Deflores, K Gospodinova, J Kapit, P H Smith.
Abstract
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 approximately 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 approximately 5-centimeter-deep ice table showed no significant difference in soluble chemistry.Entities:
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Year: 2009 PMID: 19574385 DOI: 10.1126/science.1172466
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728