首页> 外文期刊>Journal of geophysical research. Planets >Wet Chemistry experiments on the 2007 Phoenix Mars Scout Lander mission: Data analysis and results
【24h】

Wet Chemistry experiments on the 2007 Phoenix Mars Scout Lander mission: Data analysis and results

机译:2007年Phoenix Mars Scout Lander任务的湿化学实验:数据分析和结果

获取原文
获取原文并翻译 | 示例
           

摘要

Chemical analyses of three Martian soil samples were performed using the WetChemistry Laboratories on the 2007 Phoenix Mars Scout Lander. One soil sample wasobtained from the top —2 cm (Rosy Red) and two were obtained at N5 cm depth from theice table interface (Sorceress 1 and Sorceress 2). When mixed with water in a 1:25 soilto solution ratio (by volume), a portion of the soil components solvated. Ionconcentrations were measured using an array of ion selective electrodes and solutionconductivity using a conductivity cell. The measured concentrations represent theminimum leachable ions in the soil and do not take into account species remaining in thesoil. Described is the data processing and analysis for determining concentrations of sevenionic species directly measured in the soil/solution mixture. There were no significantdifferences in concentrations, pH, or conductivity, between the three samples. Usinglaboratory experiments, refinement of the surface calibrations, and modeling, we havedetermined a pH for the soil solution of 7.7(±0.3), under prevalent conditions, carbonatebuffering, and P_(CO2_in the cell headspace. Perchlorate was the dominant anion in solutionwith a concentration for Rosy Red of 2.7(±1) mM. Equilibrium modeling indicates thatmeasured [Ca~(2+)at 0.56(±0.5) mM and[Mg +]at 2.9(±1.5) mM, are consistent withcarbonate equilibrium for a saturated solution. The [Nat] and [K+] were 1.4(±0.6), and0.36(±0.3) mM, respectively. Results indicate that the leached portion of soils at thePhoenix landing site are slightly alkaline and dominated by carbonate and perchlorate.However, it should be noted that there is a 5-15 mM discrepancy between measured ionsand conductivity and another species may be present.
机译:使用2007年Phoenix Mars Scout Lander上的WetChemistry实验室对三个火星土壤样品进行了化学分析。从顶部的-2 cm处获得了一个土壤样品(玫瑰红),在距冰台界面N5 cm的深度处获得了两个土壤样品(女巫1和女巫2)。当以1:25的土壤与溶液的比例(按体积计)与水混合时,一部分土壤成分会溶剂化。使用离子选择性电极阵列测量离子浓度,并使用电导率池测量溶液电导率。测得的浓度代表土壤中的最低可浸出离子,未考虑土壤中残留的物质。描述了用于确定直接在土壤/溶液混合物中测量的七离子物种浓度的数据处理和分析。在三个样品之间,浓度,pH或电导率没有显着差异。通过实验室实验,表面校准的完善和建模,我们确定了在普遍条件下,碳酸盐缓冲液和细胞顶空中P_(CO2_)下土壤溶液的pH值为7.7(±0.3)。高氯酸根是溶液中浓度最高的阴离子值为2.7(±1)mM的玫瑰红。平衡模型表明,在饱和溶液的碳酸根平衡下,在0.56(±0.5)mM处测得的[Ca〜(2+)和在2.9(±1.5)mM处测得的[Mg +] 。[Nat]和[K +]分别为1.4(±0.6)和0.36(±0.3)mM,结果表明,菲尼克斯着陆点的土壤浸出部分呈弱碱性,并以碳酸盐和高氯酸盐为主。 ,应注意的是,测得的离子和电导率之间存在5-15 mM的差异,并且可能存在其他物质。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号