Planetary Simulant Database: UC Mars1

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Mineralogy

Component Wt.%
Basalt 47
Washed basalt 37
Volcanic glass 7
Washed volcanic glass 9

Bulk Chemistry

Scott et al. (2017) list the bulk chemistry for the individual components, but not the final mixed simulant

Physical Properties

Property Value
Specific gravity 2.7
Internal friction angle 35°
Simulant Name: UC Mars1
Current Status: Continued development
Developed By: University of Canterbury
Available From: Allan Scott (allan.scott@canterbury.ac.nz)
Publications: Scott, A. N. et al. (2017), Development of a Martian regolith simulant for in-situ resource utilization testing. Acta Astronautica 131, 45-49.

UC Mars1 was developed recently at the University of Canterbury to test ISRU technology, and was based on the bulk chemistry of the Gusev Crater regolith near the Columbia Hills. Various rocks were sampled in the Banks Peninsula in the South Island of New Zealand, and the final mixture for the simulant consisted of 46% basalt, 37% washed basalt, 7% volcanic glass, and 9% washed volcanic glass. Washing was done to remove excess dust.

Scott et al. (2017) describe the production and basic properties of the simulant, and claim that the current production methods would allow for 30 kg/hr to be manufactured. Larger scale production and use as a construction material are planned for the future.

Images

SEM images of the UC Mars1 simulant, from Scott et al. (2017):

Other Martian Simulants
ES-X | JMSS-1 | JSC Mars-1/1A | KMS-1 | MGS-1 | MMS | MMS-1/2 | Salten Skov 1 | UC Mars1 | UF Acid-Alkaline-Salt