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XI. Workshop of Physical Chemists and Electrochemists´11 Brno<br />

4. WET CHEMISTRY LAB<br />

The wet chemistry lab (WCL) sensor assembly and leaching solution were designed<br />

and built by Thermo Fisher Scientific. The WCL actuator assembly was designed and built<br />

by Starsys Research in Boulder, Colorado. Tufts University developed the reagent pellets,<br />

barium ISE, ASV electrodes, and performed the preflight characterization of the sensor<br />

array [9-13].<br />

The robotic arm scooped up some soil, put it in one of four wet chemistry lab cells,<br />

where water was added, and while stirring, an array of electrochemical sensors measured<br />

a dozen dissolved ions such as sodium, magnesium, calcium, and sulfate that have leached<br />

out from the soil into the water. This provided information on the biological compatibility<br />

of the soil, both for possible indigenous microbes and for possible future Earth visitors<br />

[14]. Every wet chemistry cell has 26 chemical sensors and a temperature sensor. The<br />

polymer Ion Selective Electrodes were able to determine the concentration of ions by<br />

measuring the change of electric potential within the sensor, which is separated from the<br />

wet chemistry cell by an ion selective membrane. The two gas sensing electrodes for<br />

oxygen and carbon dioxide work on the same principle and are separated from the wet<br />

chemistry cell by a gas permeable membrane. A gold micro-electrode array is used for the<br />

Cyclic voltammetry and Anodic Stripping Voltammetry. Cyclic voltammetry is a method<br />

to study ions by applying a waveform of varying potential and measuring the currentvoltage<br />

curve. Anodic Stripping Voltammetry first deposits the metals onto the gold<br />

electrode with an applied potential. After the potential is reversed, the current is<br />

measured while the metals are stripped off the electrode. The first measurement indicated<br />

that the surface layer contained water soluble salts and had a pH between 8 and 9.<br />

Additional tests on soil composition revealed the presence of perchlorate [14].<br />

Later publication of results in the journals Science and JGR reported that chloride, bicarbonate,<br />

magnesium, sodium potassium, calcium, and possibly sulfate were detected in the samples. The pH<br />

was narrowed down to 7.7 + or – 0.5 [9-11]. Further data analysis has indicated that the soil contains<br />

soluble sulfate at a minimum of 1.1% wt % SO3 and provided a refined formulation of the soil [9].<br />

5. ACKNOWLEDGEMENT<br />

The work was by NanoBioTECell GA ČR P102/11/1068.<br />

6. REFERENCES<br />

[1] R.A. Kerr, Science 329 (2010) 1267.<br />

[2] R.G. Bonitz, L. Shiraishi, M. Robinson, R.E. Arvidson, P.C. Chu, J.J. Wilson, K.R. Davis, G. Paulsen,<br />

A.G. Kusack, D. Archer, P. Smith, Journal of Geophysical Research-Planets 113 (2008) 10.<br />

[3] J.R. Guinn, M.D. Garcia, K. Talley, Journal of Geophysical Research-Planets 113 (2008) 16.<br />

[4] J.H. Hoffman, R.C. Chaney, H. Hammack, Journal of the American Society for Mass Spectrometry 19<br />

(2008) 1377.<br />

[5] H.U. Keller, W. Goetz, H. Hartwig, S.F. Hviid, R. Kramm, W.J. Markiewicz, R. Reynolds, C.<br />

Shinohara, P. Smith, R. Tanner, P. Woida, R. Woida, B.J. Bos, M.T. Lemmon, Journal of Geophysical<br />

Research-Planets 113 (2008) 15.<br />

[6] P.A. Taylor, D.C. Catling, M. Daly, C.S. Dickinson, H.P. Gunnlaugsson, A.M. Harri, C.F. Lange,<br />

Journal of Geophysical Research-Planets 113 (2008) 8.<br />

[7] R.E. Arvidson, R.G. Bonitz, M.L. Robinson, J.L. Carsten, R.A. Volpe, A. Trebi-Ollennu, M.T. Mellon,<br />

P.C. Chu, K.R. Davis, J.J. Wilson, A.S. Shaw, R.N. Greenberger, K.L. Siebach, T.C. Stein, S.C. Cull, W.<br />

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