The MECA Wet Chemistry Laboratory on the 2007 Phoenix Mars Scout Lander

[1] To analyze and interpret the chemical record, the 2007 Phoenix Mars Lander includes four wet chemistry cells. These Wet Chemistry Laboratories (WCLs), part of the Microscopy, Electrochemistry, and Conductivity Analyzer (MECA) package, each consist of a lower “beaker” containing sensors designed to analyze the chemical properties of the regolith and an upper “actuator assembly” for adding soil, water, reagents, and stirring. The beaker contains an array of sensors and electrodes that include six membrane-based ion selective electrodes (ISE) to measure Ca2+, Mg2+, K+, Na+, NO3−/ClO4−, and NH4+; two ISEs for H+ (pH); a Ba2+ ISE for titrimetric determination of SO42−; two Li+ ISEs as reference electrodes; three solid crystal pellet ISEs for Cl−, Br−, and I−; an iridium oxide electrode for pH; a carbon ring electrode for conductivity; a Pt electrode for oxidation reduction potential (Eh); a Pt and two Ag electrodes for determination of Cl−, Br−, and I− using chronopotentiometry (CP); a Au electrode for identifying redox couples using cyclic voltammetry (CV); and a Au microelectrode array that could be used for either CV or to indicate the presence of several heavy metals, including Cu2+, Cd2+, Pb2+, Fe2/3+, and Hg2+ using anodic stripping voltammetry (ASV). The WCL sensors and analytical procedures have been calibrated and characterized using standard solutions, geological Earth samples, Mars simulants, and cuttings from a Martian meteorite. Sensor characteristics such as limits of detection, interferences, and implications of the Martian environment are also being studied. A sensor response library is being developed to aid in the interpretation of the data.

[1]  H Y McSween,et al.  The chemical composition of Martian soil and rocks returned by the mobile alpha proton X-ray spectrometer: preliminary results from the X-ray mode. , 1997, Science.

[2]  Sheng Yao,et al.  A long-term stable iridium oxide pH electrode , 2002 .

[3]  Michael H. Carr,et al.  Water on Mars , 1987, Nature.

[4]  K. Herkenhoff,et al.  Sulfate deposition in subsurface regolith in Gusev crater, Mars , 2006 .

[5]  T. Encrenaz,et al.  Mars Surface Diversity as Revealed by the OMEGA/Mars Express Observations , 2005, Science.

[6]  William H. Farrand,et al.  Geochemical and mineralogical indicators for aqueous processes in the Columbia Hills of Gusev crater, Mars , 2006 .

[7]  Martin S. Frant Where Did Ion Selective Electrodes Come From? The Story of Their Development and Commercialization , 1997 .

[8]  David C. Catling,et al.  A chemical model for evaporites on early Mars: Possible sedimentary tracers of the early climate and implications for exploration , 1999 .

[9]  A. Bard Correction for the Inconstancy of the Chronopotentiometric Constant at Short Transition Times , 1963 .

[10]  M. Hecht,et al.  Mars Surveyor Program '01 Mars Environmental Compatibility Assessment wet chemistry lab: a sensor array for chemical analysis of the Martian soil. , 2003, Journal of geophysical research.

[11]  Carol R. Stoker,et al.  Introduction to special section on the Phoenix Mission: Landing Site Characterization Experiments, Mission Overviews, and Expected Science , 2008 .

[12]  B. Clark,et al.  The salts of Mars , 1981 .

[13]  R. Rieder,et al.  Chemistry of Rocks and Soils in Gusev Crater from the Alpha Particle X-ray Spectrometer , 2004, Science.

[14]  H. Wänke,et al.  Phosphorus in Martian rocks and soils and the global surface chemistry of Mars as derived from APXS on Pathfinder , 2000 .

[15]  Lorraine Schnabel,et al.  Chemical composition of Martian fines , 1982 .

[16]  D. Ming,et al.  Evidence for Montmorillonite or its Compositional Equivalent in Columbia Hills, Mars , 2007 .

[17]  William H. Farrand,et al.  Rocks of the Columbia Hills , 2006 .

[18]  Gregory T. A. Kovacs,et al.  Field Evaluation of an Electrochemical Probe for in Situ Screening of Heavy Metals in Groundwater , 1998 .

[19]  Christopher H. Fry,et al.  Ion-Selective Electrodes for Biological Systems , 2001 .

[20]  Raymond E. Arvidson,et al.  Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) on Mars Reconnaissance Orbiter (MRO) , 2007 .

[21]  Jeffrey R. Johnson,et al.  Provenance and diagenesis of the evaporite-bearing Burns formation, Meridiani Planum, Mars , 2005 .

[22]  A. Knoll,et al.  Stratigraphy and sedimentology of a dry to wet eolian depositional system, Burns formation, Meridiani Planum, Mars , 2005 .

[23]  Feeney,et al.  On-site analysis of arsenic in groundwater using a microfabricated gold ultramicroelectrode array , 2000, Analytical chemistry.

[24]  S. Kounaves,et al.  Analysis of Simulated Martian Regolith Using an Array of Ion Selective Electrodes , 2005 .

[25]  R. Rieder,et al.  Chemistry of Rocks and Soils at Meridiani Planum from the Alpha Particle X-ray Spectrometer , 2004, Science.

[26]  G. C. Carle,et al.  Preliminary findings of the Viking gas exchange experiment and a model for Martian surface chemistry , 1977, Nature.

[27]  William H. Farrand,et al.  Chemistry and mineralogy of outcrops at Meridiani Planum , 2005 .

[28]  Jeffrey R. Johnson,et al.  Hydrothermal processes at Gusev Crater: An evaluation of Paso Robles class soils , 2008 .

[29]  A. Zent,et al.  Decomposition of aqueous organic compounds in the Atacama Desert and in Martian soils , 2007 .