Subcritical water extraction of amino acids from Atacama Desert soils

Details Subcritical water extraction of amino acids from Atacama Desert soils Subcritical water extraction of amino acids from Atacama Desert soils

Sep 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007jgrg..11204s16a&link_type=abstract

Journal of Geophysical Research, Volume 112, Issue G4, CiteID G04S16

Biology

3

Planetary Sciences: Astrobiology: Origin Of Life, Biogeosciences: Instruments And Techniques, Biogeosciences: Life In Extreme Environments

Scientific paper

Amino acids are considered organic molecular indicators in the search for extant and extinct life in the Solar System. Extraction of these molecules from a particulate solid matrix, such as Martian regolith, will be critical to their in situ detection and analysis. The goals of this study were to optimize a laboratory amino acid extraction protocol by quantitatively measuring the yields of extracted amino acids as a function of liquid water temperature and sample extraction time and to compare the results to the standard HCl vapor-phase hydrolysis yields for the same soil samples. Soil samples from the Yungay region of the Atacama Desert (Martian regolith analog) were collected during a field study in the summer of 2005. The amino acids (alanine, aspartic acid, glutamic acid, glycine, serine, and valine) chosen for analysis were present in the samples at concentrations of 1-70 parts-per-billion. Subcritical water extraction efficiency was examined over the temperature range of 30-325 °C, at pressures of 17.2 or 20.0 MPa, and for water-sample contact equilibration times of 0-30 min. None of the amino acids were extracted in detectable amounts at 30 °C (at 17.2 MPa), suggesting that amino acids are too strongly bound by the soil matrix to be extracted at such a low temperature. Between 150 °C and 250 °C (at 17.2 MPa), the extraction efficiencies of glycine, alanine, and valine were observed to increase with increasing water temperature, consistent with higher solubility at higher temperatures, perhaps due to the decreasing dielectric constant of water. Amino acids were not detected in extracts collected at 325 °C (at 20.0 MPa), probably due to amino acid decomposition at this temperature. The optimal subcritical water extraction conditions for these amino acids from Atacama Desert soils were achieved at 200 °C, 17.2 MPa, and a water-sample contact equilibration time of 10 min.

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