Peroxides and the survivability of microorganisms on the surface of Mars.
Results of the Viking mission seem to indicate that there is a ubiquitous layer of highly oxidizing aeolian material covering the Martian surface.  This layer is thought to oxidize organic material that may settle on it, and is therefore responsible for the lack of detection of organic matter on the planet's surface by Viking.  The mechanism that creates the oxidizing condition is not well understood, nor is the extent of the oxidation potential of this material.  It has been suggested that the oxidizing nature of the soil is due to photochemical reactions which create hydrogen peroxide and superoxides in the surface soil.  One question of importance to planetary protection regarding this material is, what is its potential for destroying terrestrial microorganisms, thus making the surface of Mars "self-sterilizing"?  Using data obtained by the gas exchange experiment on Viking, and for simplicity assuming that all of the O2 released came from H2O2, the concentration range for H2O2 on the surface of Mars can be calculated to be 25-250 ppm.  The microbial disinfection rate by H2O2 is concentration dependent, and is highly variable within the microbial community.  Data from our laboratory indicate that certain soil bacteria survive and grow to stationary phase in 30,000 ppm H2O2.  However, the total number of organisms decreases in the presence of H2O2.  These results indicate that it is doubtful that the presence of H2O2 alone on Mars would make the surface "self-sterilizing".
Mancinelli
R L
RL
Solar System Exploration Branch, NASA/Ames Research Center, Moffett Field, CA 94035.
D001419:Bacteria / Q000254:growth & development*; D003470:Culture Media / Q000633:toxicity; D005118:Extraterrestrial Environment; D006861:Hydrogen Peroxide / Q000633:toxicity*; D018535:Mars; D012987:Soil / Q000032:analysis; D012988:Soil Microbiology; D013026:Space Flight
D003470:Culture Media; D012987:Soil; D006861:Hydrogen Peroxide