P43D-2149
Pathway Study of Cl-cycle on Mars, Step-I & II: Oxychlorine Salts and Electrostatic Discharge Phenomenon in a Mars Chamber

Thursday, 17 December 2015
Poster Hall (Moscone South)
Zhongchen WU1, Alian Wang2, Zongcheng Ling1, Bo Li1, Jiang Zhang1 and Weijie Xu1, (1)Shandong University at Weihai, Weihai, China, (2)Washington University in St. Louis, Dept. Earth and Planetary Sciences and McDonnell Center for Space Sciences, St. Louis, MO, United States
Abstract:
The directly measured high ClO4-/Cl- ratio (4.3-8.75) at Phoenix site and the implied ClO4- existences at Curiosity and Viking sites reminded Mars science community on the importance of (1) the global distribution of ClO4-/Cl- ratio; (2) the mechanisms that are responsible for Cl- to ClOy- (y=1,2,3,4) transformation; and (3) the current and historical Cl- cycle on Mars.

Our goal is to study electrostatic discharge (ESD) in a Mars Chamber, as one of the four proposed mechanisms for the formation of Martian perchlorate. ESD was anticipated during dust storm/devil on Mars. A model estimated that ESD generated oxidants can be 200 times of those produced by photochemistry.

Our study is conducted in three steps. Firstly, oxychlorine salts, NaClOy, Mg(ClO4)2.xH2O (x=0,6), and Ca(ClO4)2.xH2O (x=0,4), were analyzed at ambient conditions using MIR, NIR (1.4-2.6 µm), Raman spectroscopy, and in a Mars Chamber using in-situ NIR and Raman spectroscopy. Our purpose is to understand their phase transition and spectral change at Mars pressure (P) and temperature (T) conditions. We have found: (1) Under current surface/subsurface P-T conditions in mid-latitudes/equatorial regions on Mars, Mg(ClO4)2.6H2O and Ca(ClO4)2.4H2O are stable, while the hydration degree of NaClO4.H2O would increase at T<-30 and decrease in 5<T<21with dehydration rate increases at higher T; (2) Within the P-T range anticipated in above environments, Raman ν1 peak positions of hydrous and anhydrous oxychlorine species have no obvious change, but H2O peak would down-shift when T decreases; (3) In Mars 2020 and ExoMars, the Raman ν1 peak can be used to characterize oxychlorine salts, e.g., the oxidation degree changes from Cl+ to Cl7+ in NaClOy- that causes over 243 cm-1 shift, the cation changes from Na+ to Mg2+ to Ca2+ that cause over 33 cm-1 shift; (4) The dehydration of NaClO4.H2O was quantified by in situ NIR spectroscopy, based on which the dehydration rate as function of T was derived.

We are currently conducting ESD in a Mars Chamber, to detect the oxidant species in ESD generated plasma, first in pure CO2 atmosphere then in simulated Mars gas mixture. Results will be reported at conference. Our step-3 will study the production/yield from chlorides mixed with Mars-relevant materials to oxychlorine salts through ESD process.