Martian analog (JSC200)

Categories
MICRON-COSMIC ANALOGS
MARTIAN ANALOGS
Summary: AEROSOLS
Micron- cosmic analogs subcategories
Martian dust
Origin

the JSC Mars-1 sample consists of weathered volcanic ash from the Pu'u Nene cinder cone on the Island of Hawaii (USA). The original sample was sieved (200 µm sieve). Part of the sample was heated up to 200C for 24 hours to get rid of the volatile components. The heated sample is called JSC200, whereas the non-heated is JSC0

Main constituent
palagonite
Practical significance

high similarity of the VIS/NIR spectrum of the JSC Mars-1 simulant with that corresponding to a martian bright region spectrum as measured from the Earth and the ISM Phobos-2 instrument

Particle size Mie: reff (μm)
28.1
Particle size Mie: veff
1.2
Particle size Fraunhofer: reff (μm)
15.5
Particle size Fraunhofer: veff
2.8
Size distribution plot
Size distribution table
Particle shape

irregular

All SEM images (zip file)
Refractive index

1.5 + i0.01 (488nm) 
1.5 + i0.001 (647nm) (Clancy et al. 1995)

Color
dark gray
Scattering matrix (1) wavelength in nm
488
Scattering matrix (1) plot
Scattering matrix (1) table
Scattering matrix (2) wavelength in nm
647
Scattering matrix (2) plot
Scattering matrix (2) table
Synthetic scattering matrix (1) wavelength in nm
488
Synthetic scattering matrix (1) table M
Synthetic scattering matrix (1) table F
Synthetic scattering matrix (2) wavelength in nm
647
Synthetic scattering matrix (2) table M
Synthetic scattering matrix (2) table F
Angle range (deg)
[3,177]
Full reference paper

Dabrowska DD, Muñoz O, Moreno F, Ramos JL, Martínez-Frías J, Gerhard W. . Scattering matrices of Martian dust analogs 488 nm and 647 nm. Icarus, vol. 250, pp. 83-94, 2015