Thermal and Electrical Conductivity Probe (TECP) for Phoenix

Received 29 November 2007; revised 1 August 2008; accepted 30 November 2008; published 25 March 2009. [1] The Thermal and Electrical Conductivity Probe (TECP) is a component of the Microscopy, Electrochemistry and Conductivity Analyzer (MECA) payload on the Phoenix Lander. TECP will measure the temperature, thermal conductivity, and volumetric heat capacity of the regolith. It will also detect and quantify the population of mobile H2O molecules in the regolith, if any, throughout the polar summer, by measuring the electrical conductivity of the regolith as well as the dielectric permittivity. In the vapor phase, TECP is capable of measuring the atmospheric H2O vapor abundance as well as augmenting the wind velocity measurements from the meteorology instrumentation. TECP is mounted near the end of the 2.3 m Robotic Arm and can be placed either in the regolith material or held aloft in the atmosphere. This paper describes the development and calibration of the TECP. In addition, substantial characterization of the instrument has been conducted to identify behavioral characteristics that might affect landed surface operations. The greatest potential issue identified in characterization tests is the extraordinary sensitivity of the TECP to placement. Small gaps alter the contact between the TECP and regolith, complicating data interpretation. Testing with the Phoenix Robotic Arm identified mitigation techniques that will be implemented during flight. A flight model of the instrument was also field tested in the Antarctic Dry Valleys during the 2007–2008 International Polar Year.

[1]  Z. Voros,et al.  Intermittent turbulence, noisy fluctuations, and wavy structures in the Venusian magnetosheath and wake , 2008, Journal of Geophysical Research.

[2]  A. Zent A historical search for habitable ice at the Phoenix landing site , 2008 .

[3]  E. Lellouch,et al.  Investigation of water vapor on Mars with PFS/SW of Mars Express , 2008 .

[4]  Paul S. Smith,et al.  Mars Exploration Program 2007 Phoenix landing site selection and characteristics , 2008 .

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

[6]  A. McEwen,et al.  A Closer Look at Water-Related Geologic Activity on Mars , 2007, Science.

[7]  J. Roberts,et al.  Study of dielectric properties of dry and saturated Green River oil shale , 2007 .

[8]  Hugh M. French,et al.  The Periglacial Environment: French/The Periglacial Environment , 2007 .

[9]  D. Fisher A process to make massive ice in the martian regolith using long-term diffusion and thermal cracking , 2005 .

[10]  O. Aharonson,et al.  Stability and exchange of subsurface ice on Mars , 2005 .

[11]  R.C. Anderson,et al.  Prospecting for in situ resources on the Moon and Mars using wheel-based sensors , 2005, 2005 IEEE Aerospace Conference.

[12]  T. Quinn,et al.  A 1 Gyr climate model for Mars: new orbital statistics and the importance of seasonally resolved polar processes , 2004 .

[13]  D. Robinson,et al.  The Dielectric Permittivity of Calcite and Arid Zone Soils with Carbonate Minerals , 2004 .

[14]  Jacques Laskar,et al.  Long term evolution and chaotic diffusion of the insolation quantities of Mars , 2004 .

[15]  P. Price,et al.  Temperature dependence of metabolic rates for microbial growth, maintenance, and survival. , 2004, Proceedings of the National Academy of Sciences of the United States of America.

[16]  John F. Mustard,et al.  Recent ice ages on Mars , 2003, Nature.

[17]  Scott B. Jones,et al.  Modeled Effects on Permittivity Measurements of Water Content in High Surface Area Porous Media , 2003 .

[18]  Mark I. Richardson,et al.  On the orbital forcing of Martian water and CO2 cycles: A general circulation model study with simplified volatile schemes , 2003 .

[19]  M. Mellon,et al.  Subfreezing activity of microorganisms and the potential habitability of Mars' polar regions. , 2003, Astrobiology.

[20]  Robert M. Haberle,et al.  Orbital change experiments with a Mars general circulation model , 2003 .

[21]  J. Bada,et al.  Radiation-Dependent Limit for the Viability of Bacterial Spores in Halite Fluid Inclusions and on Mars , 2003, Radiation research.

[22]  Robert L. Tokar,et al.  Global Distribution of Neutrons from Mars: Results from Mars Odyssey , 2002, Science.

[23]  P. A. J. Englert,et al.  Distribution of Hydrogen in the Near Surface of Mars: Evidence for Subsurface Ice Deposits , 2002, Science.

[24]  F. Forget,et al.  Formation of Recent Martian Debris Flows by Melting of Near-Surface Ground Ice at High Obliquity , 2001, Science.

[25]  Hugh H. Kieffer,et al.  TES mapping of Mars' north seasonal cap , 2001 .

[26]  L. Hinzman,et al.  Non-conductive heat transfer associated with frozen soils , 2001 .

[27]  Kenneth M. Hinkel,et al.  Patterns of soil temperature and moisture in the active layer and upper permafrost at Barrow, Alaska: 1993 1999 , 2001 .

[28]  C. McKay,et al.  Metabolic Activity of Permafrost Bacteria below the Freezing Point , 2000, Applied and Environmental Microbiology.

[29]  M. Mellon,et al.  High-Resolution Thermal Inertia Mapping from the Mars Global Surveyor Thermal Emission Spectrometer , 2000 .

[30]  J. Dojčilović,et al.  TEMPERATURE DEPENDENCE OF ELECTRIC PERMITTIVITY OF LINEAR DIELECTRICS WITH IONIC AND POLAR COVALENT BONDS , 1998 .

[31]  M. Mellon Small‐scale polygonal features on Mars: Seasonal thermal contraction cracks in permafrost , 1997 .

[32]  L. Finegold Molecular and biophysical aspects of adaptation of life to temperatures below the freezing point , 1996 .

[33]  Philip S. Anderson,et al.  MECHANISM FOR THE BEHAVIOR OF HYDROACTIVE MATERIALS USED IN HUMIDITY SENSORS , 1995 .

[34]  Hugh H. Kieffer,et al.  Quasi-periodic climate change on Mars. , 1992 .

[35]  Tyler Gregory Hicks,et al.  The McGraw-Hill Handbook of Essential Engineering Information and Data , 1991 .

[36]  S. Squyres,et al.  Geomorphic Evidence for the Distribution of Ground Ice on Mars , 1986, Science.

[37]  W. Conley Linear systems revisited , 1985 .

[38]  M. Carr,et al.  Possible precipitation of ice at low latitudes of Mars during periods of high obliquity , 1985, Nature.

[39]  B. Jakosky The role of seasonal reservoirs in the Mars water cycle: II. Coupled models of the regolith, the polar caps, and atmospheric transport , 1983 .

[40]  J. Pollack,et al.  Quasi-periodic climate changes on Mars: A review , 1982 .

[41]  W. Banerdt,et al.  Mars: The regolith-atmosphere-cap system and climate change , 1982 .

[42]  S. Judson,et al.  Ground ice on Mars: Inventory, distribution, and resulting landforms , 1981 .

[43]  J. Burns,et al.  The astronomical theory of climatic change on Mars , 1980 .

[44]  A. P. Annan,et al.  Electromagnetic determination of soil water content: Measurements in coaxial transmission lines , 1980 .

[45]  R. F. Black,et al.  The Periglacial Environment , 1971 .

[46]  E. I. Parkhomenko Electrical properties of rocks , 1967 .

[47]  B. Murray,et al.  Behavior of Carbon Dioxide and Other Volatiles on Mars , 1966, Science.

[48]  Irene A. Stegun,et al.  Handbook of Mathematical Functions. , 1966 .

[49]  A. Lachenbruch Mechanics of Thermal Contraction Cracks and Ice-Wedge Polygons in Permafrost , 1962 .

[50]  D. D. Vries A NONSTATIONARY METHOD FOR DETERMINING THERMAL CONDUCTIVITY OF SOIL IN SITU , 1952 .

[51]  L. Rosenhead Conduction of Heat in Solids , 1947, Nature.