X-Ray Diffraction Reference Intensity Ratios of Amorphous and Poorly Crystalline Phases: Implications for CheMin on the Mars Science LaboratoryThe CheMin instrument on the Mars Science Laboratory (MSL) rover Curiosity is an X-ray diffraction (XRD) and X-ray fluorescence (XRF) instrument capable of providing the mineralogical and chemical compositions of rocks and soils on the surface of Mars. CheMin uses a microfocus X-ray tube with a Co target, transmission geometry, and an energy-discriminating X-ray sensitive CCD to produce simultaneous 2-D XRD patterns and energy-dispersive X-ray histograms from powdered samples. Piezoelectric vibration of the cell is used to randomize the sample to reduce preferred orientation effects. Instrument details are provided in [1, 2, 3]. Analyses of rock and soil samples by the Mars Exploration Rovers (MER) show nanophase ferric oxide (npOx) is a significant component of the Martian global soil [4] and is thought to be one of the major contributing phases that the Curiosity rover will encounter if a soil sample is analyzed in Gale Crater. Because of the nature of this material, npOx will likely contribute to an X-ray amorphous or short-order component of a XRD pattern measured by the CheMin instrument.
Document ID
20130010071
Acquisition Source
Johnson Space Center
Document Type
Conference Paper
Authors
Morris, R. V. (NASA Johnson Space Center Houston, TX, United States)
Achilles, C. N. (Jacobs Technologies Engineering Science Contract Group Houston, TX, United States)
Chipera, S. J. (Chesapeake Energy Corp. Oklahoma City, OK, United States)
Ming, D. W. (NASA Johnson Space Center Houston, TX, United States)
Rampe, E. B. (NASA Johnson Space Center Houston, TX, United States)