Hecht M H, Kounaves S P, Quinn R C, West S J, Young S M M, Ming D W, Catling D C, Clark B C, Boynton W V, Hoffman J, Deflores L P, Gospodinova K, Kapit J, Smith P H
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA.
Science. 2009 Jul 3;325(5936):64-7. doi: 10.1126/science.1172466.
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.
凤凰号火星着陆器上的湿化学实验室对来自北极广阔平原多边形图案北部的火星土壤进行了水相化学分析。溶液中含有约10 mM的溶解盐,每个样品浸出的高氯酸盐(ClO4)质量分数为0.4%至0.6%。其余阴离子包括少量的氯离子、碳酸氢根离子,可能还有硫酸根离子。阳离子以Mg2+和Na+为主,K+和Ca2+的含量较少。测得的pH值为7.7±0.5,呈中等碱性,与碳酸盐缓冲溶液一致。对约5厘米深冰表的表面和挖掘边界处分析的样品,其可溶性化学性质没有显著差异。