Thermal conductivity measurements of macroscopic frozen salt ice analogues of Jovian icy moons in support of the planned JUICE mission

Author:

González Díaz C1ORCID,Aparicio Secanellas S2,Muñoz Caro G M1,Anaya Velayos J J2,Carrascosa H1,Hernández M G2,Muñoz-Iglesias V1,Marcos-Fernández Á3,Prieto-Ballesteros O1,Witasse O4,Lorente R5,Altobelli N5

Affiliation:

1. Centro de Astrobiología (CSIC-INTA), Ctra. de Ajalvir, km 4, Torrejón de Ardoz, E-28850 Madrid, Spain

2. Instituto de Tecnologías Físicas y de la Información, Leonardo Torres Quevedo, (ITEFI-CSIC), c/ Serrano 144, E-28006 Madrid, Spain

3. Instituto de Ciencia y Tecnologías de Polímeros (ICTP-CSIC), Juan de la Cierva, 3, E-28006 Madrid, Spain

4. European Space Agency (ESA), European Space Research and Technology Centre (ESTEC), Keplerlaan 1, 2201 AZ, Noordwijk, the Netherlands

5. European Space Agency (ESA) - European Space Astronomy Centre (ESAC), Camino Bajo del Castillo, s/n Villafranca del Castillo, E-28692 Villanueva de la Cañada (Madrid), Spain

Abstract

ABSTRACT The study of thermal properties of frozen salt solutions representative of ice layers in Jovian moons is crucial to support the JUpiter ICy moons Explorer (JUICE) (ESA) and Europa Clipper (NASA) missions, which will be launched in the upcoming years to make detailed observations of the giant gaseous planet Jupiter and three of its largest moons (Ganymede, Europa, and Callisto), due to the scarcity of experimental measurements. Therefore, we have conducted a set of experiments to measure and study the thermal conductivity of macroscopic frozen salt solutions of particular interest in these regions, including sodium chloride (NaCl), magnesium sulphate (MgSO4), sodium sulphate (Na2SO4), and magnesium chloride (MgCl2). Measurements were performed at atmospheric pressure and temperatures from 0 to −70 °C in a climatic chamber. Temperature and calorimetry were measured during the course of the experiments. An interesting side effect of these measurements is that they served to spot phase changes in the frozen salt solutions, even for very low salt concentrations. A small sample of the liquid salt-water solution was set aside for the calorimetry measurements. These experiments and the measurements of thermal conductivity and calorimetry will be valuable to constrain the chemical composition, physical state, and temperature of the icy crusts of Ganymede, Europa, and Callisto.

Funder

European Space Agency

Publisher

Oxford University Press (OUP)

Subject

Space and Planetary Science,Astronomy and Astrophysics

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