Rock and soil samples from the planet Mars are due to be returned to Earth
within a decade. Martian samples initially will be tested for evidence of l
ife and biological hazard under strict biological containment. Wider distri
bution of samples for organic and inorganic analysis may occur only if neit
her evidence of life nor hazard is detected, or if the samples ate first st
erilized. We subjected a range of Mars analog rocks and minerals to high do
ses of gamma radiation in order to determine the effects of gamma steriliza
tion on the samples' isotopic, chemical, and physical properties. Gamma pho
tons from Co-60 (1.17 and 1.33 MeV) in doses as high as 3 x 10(7) rads did
not induce radioactivity in the samples and produced no measurable changes
in their isotopic and chemical compositions. This level of irradiation also
produced no measurable changes in the crystallographic structure of any sa
mple, the surface areas of soil analogs, or the fluid inclusion homogenizat
ion temperature of quartz. The only detectable effects of irradiation were
dose-dependent changes in the visible and near-infrared spectral region (e.
g., discoloration and darkening of quartz and halite and an increase in alb
edo of carbonates) and increases in the thermoluminescence of quartz and pl
agioclase. If samples returned from Mars require biological sterilization,
gamma irradiation provides a feasible option.