Chlorine-containing salts as water ice nucleating particles on Mars

• Published in: Icarus (New York, N.Y. 1962) N.Y. 1962), 2018-03, Vol.303, p.280-287
• Main Authors: Santiago-Materese, D.L., Iraci, L.T., Clapham, M.E., Chuang, P.Y.
• Format: Article
• Language: English
• Subjects: Atmosphere; Atmospheres; Composition; Mars
• ISSN: 0019-1035; 1090-2643
• DOI: 10.1016/j.icarus.2017.11.001

•Sodium chloride and sodium perchlorate are examined as ice nucleating particles under Martian atmospheric conditions.•Sodium perchlorate supports depositional nucleation at lower saturation levels than other substrates tested and is comparable to smectite-rich clay in its ability to support cloud initiation.•Air masses on Mars containing uplifted salts such as perchlorates could form water ice clouds at lower atmospheric supersaturation than in areas absent similar particles. Water ice cloud formation on Mars largely is expected to occur on the most efficient ice nucleating particle available. Salts have been observed on the Martian surface and have been known to facilitate water cloud formation on Earth. We examined heterogeneous ice nucleation onto sodium chloride and sodium perchlorate substrates under Martian atmospheric conditions, in the range of 150 to 180 K and 10−7 to 10−5 Torr water partial pressure. Sub-155 K data for the critical saturation ratio (Scrit) suggests an exponential model best describes the temperature-dependence of nucleation onset of water ice for all substrates tested. While sodium chloride does not facilitate water ice nucleation more easily than bare silicon, sodium perchlorate does support depositional nucleation at lower saturation levels than other substrates shown and is comparable to smectite-rich clay in its ability to support cloud initiation. Perchlorates could nucleate water ice at partial pressures up to 40% lower than other substrates examined to date under Martian atmospheric conditions. These findings suggest air masses on Mars containing uplifted salts such as perchlorates could form water ice clouds at lower saturation ratios than in air masses absent similar particles.