sp8b00082_si_001.xlsx (1.47 MB)
Measuring Perchlorate and Sulfate in Planetary Brines Using Raman Spectroscopy
dataset
posted on 2018-09-11, 00:00 authored by Lauren
E. McGraw, Nina D. S. McCollom, Charity M. Phillips-Lander, Megan E. Elwood MaddenLiquid water likely
exists on the surface of Mars and below the
icy crusts of Europa, Enceladus, and Titan. Pluto, Ceres, and Ganymede
also show evidence of liquid water at or near the surface. Quantitative
solute analyses would provide critical data needed to understand geochemical
conditions throughout our solar system, including potential habitability
of planetary bodies. We have developed and tested a Raman spectroscopic
method for measuring perchlorate and sulfate in brines and dilute
waters that utilizes simple Raman peak height ratios rather than peak
area ratios. Ratios of the target anion and OH- bending water peaks
yield linear fits with positive slopes and r2 values >0.99.
Calibration fits for each solute–brine combination and ultrapure
water yield similar linear equations, suggesting this method can detect
and quantitatively measure solutes in complex aqueous solutions. No
sample preparation or physical contact with the sample is required.
Therefore, this method can be employed without contaminating the fluid
or the spacecraft.