An electrochemically based total organic carbon analyzer for planetary and terrestrial on-site applications.

The search for organics on Mars began over 30 years ago. Neither the Viking GC/MS nor the more recent thermal and evolved gas analyzer (TEGA) aboard Phoenix were successful in detecting organics in the Martian soil. The most recent hypothesis for the "missing" Martian organics is thermal decomposition of organic material to CO(2) during the pyrolysis step of these analyses caused by the recently discovered ~1 wt % perchlorate in the Martian soil. To avoid this problem, an entirely different approach for the analysis of organics on Mars has been developed using an electrochemically based total organic carbon (TOC) analyzer, designated the Mars Organic Carbon Analyzer (MOCA). MOCA is designed as a small, lightweight, low-power instrument that electrochemically oxidizes organics to CO(2). The CO(2) is subsequently detected and quantified to determine the amount of TOC in the soil. MOCA can use the perchlorate present in the Martian soil to its advantage as an electrolyte, thus requiring only a buffered solution. Through a series of proof-of-concept tests, MOCA is shown to oxidize a variety of low-molecular-weight 1-5-carbon-containing molecules, including those containing carbon-13 using platinum and boron-doped diamond (BDD) electrodes at concentrations as low as 10 mg/kg. MOCA can also be used in terrestrial settings for on-site analysis of dissolved TOC.

Discovery of natural perchlorate in the Antarctic Dry Valleys and its global implications.

In the past few years, it has become increasingly apparent that perchlorate (ClO(4)(-)) is present on all continents, except the polar regions where it had not yet been assessed, and that it may have a significant natural source. Here, we report on the discovery of perchlorate in soil and ice from several Antarctic Dry Valleys (ADVs) where concentrations reach up to 1100 microg/kg. In the driest ADV, perchlorate correlates with atmospherically deposited nitrate. Far from anthropogenic activity, ADV perchlorate provides unambiguous evidence that natural perchlorate is ubiquitous on Earth. The discovery has significant implications for the origin of perchlorate, its global biogeochemical interactions, and possible interactions with the polar ice sheets. The results support the hypotheses that perchlorate is produced globally and continuously in the Earth's atmosphere, that it typically accumulates in hyperarid areas, and that it does not build up in oceans or other wet environments most likely because of microbial reduction on a global scale.