Context. Carbonic acid (H2CO3) is a weak acid relevant to astrobiology which, to date, remains undetected in space. Experimental work has shown that the β-polymorph of H2CO3 forms under space relevant conditions through energetic (UV photon, electron, and cosmic ray) processing of CO2- and H2O-rich ices. Although its α-polymorph ice has been recently reassigned to the monomethyl ester of carbonic acid, a different form of H2CO3 ice may exist and is synthesized without irradiation through surface reactions involving CO molecules and OH radicals, that is to say γ-H2CO3. Aims. We aim to provide a systematic set of vacuum ultraviolet (VUV) photoabsorption spectroscopic data of pure carbonic acid that formed and was destroyed under conditions relevant to space in support of its future identification on the surface of icy objects in the Solar System by the upcoming Jupiter ICy moons Explorer mission and on interstellar dust by the James Webb Space Telescope spacecraft. Methods. We present VUV photoabsorption spectra of pure and mixed CO2 and H2O ices exposed to 1 keV electrons at 20 and 80 K to simulate different interstellar and Solar System environments. Ices were then annealed to obtain a layer of pure H2CO3 which was further exposed to 1 keV electrons at 20 and 80 K to monitor its destruction pathway. Fourier-transform infrared (FT-IR) spectroscopy was used as a secondary probe providing complementary information on the physicochemical changes within an ice. Results. Our laboratory work shows that the formation of solid H2CO3, CO, and O3 upon the energetic processing of CO2:H2O ice mixtures is temperature-dependent in the range between 20 and 80 K. The amorphous to crystalline phase transition of H2CO3 ice is investigated for the first time in the VUV spectral range by annealing the ice at 200 and 225 K. We have detected two photoabsorption bands at 139 and 200 nm, and we assigned them to β-H2CO3 and γ-H2CO3, respectively. We present VUV spectra of the electron irradiation of annealed H2CO3 ice at different temperatures leading to its decomposition into CO2, H2O, and CO ice. Laboratory results are compared to Cassini UltraViolet Imaging Spectrograph observations of the 70−90 K ice surface of Saturn’s satellites Enceladus, Dione, and Rhea.

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<p>Ices are widely present in the cold regions across the Universe, for instance, in the interstellar medium as mantles on interstellar and circumstellar dust and on the surfaces of small bodies of the Solar System - beyond the distance around 3-5 AU known as the “snowline" (i.e. at temperatures below 150-170 K). The continuous energetic processing of icy objects in the Solar System induces physical and chemical changes within the ice. Laboratory experiments that simulate energetic processing (ions, photons, and electrons) of ices are therefore essential for interpreting and directing future astronomical observations.</p> <p> </p> <p>Here we provide vacuum ultraviolet (VUV) and UV-Vis photoabsorption spectroscopic data of pristine and energetically processed (electron irradiated) space-related ices. Experiments were performed using a custom-made Portable Astrochemistry Chamber (PAC), which has a base pressure of 10<sup>-9</sup> mbar. Photoabsorption spectra of ices were measured at the AU-UV beam line of the ASTRID2 synchrotron light source at Aarhus University in Denmark (see Eden et al. 2006; Palmer et al. 2015). We present the results of three series of experiments: one dedicated to the study of nitrogen- and oxygen-rich ices (Ioppolo et al., 2020); the other one to the spectroscopic study of carbonic acid as formed and destroyed under conditions relevant to space (Ioppolo et al., 2021); and the third one to the study of photoabsorption spectra of O<sub>2</sub> ice, both pure and mixed with other species (Migliorini et al, 2021).</p> <p> </p> <p>Results are discussed in light of their relevance to various astrophysical environments, e.g., the icy moons of Saturn and Jupiter. Laboratory VUV-UV-vis spectra of ices can help their future identification on the surface of icy objects in the Solar System by the upcoming Jupiter ICy moons Explorer mission and on interstellar dust by the James Webb Space Telescope spacecraft.</p> <p>This research was partly supported by the Italian Space Agency (Grant ASI-INAF n. 2018-25-HH-0).</p> <p> </p> <p> </p> <p> </p> <p>REFERENCES:</p> <p>Eden, S., Limão-Vieira, P., Hoffmann, S. V., & Mason, N. J. 2006, Chem. Phys., 323, 313</p> <p>Ioppolo, S., Kanuchova Z., James, R.L., Dawes, A., Jones, N.C., Hoffmann, S.V., Mason, N.J., Strazzulla, G. 2020, Astron. Astrophys. 641, A154</p> <p>Ioppolo, S., Kanuchova Z., James, R.L., Dawes, A., Ryabov, A., Dezalay, J., Jones, N.C., Hoffmann, S.V., Mason, N.J., Strazzulla, G. 2021, Astron. Astrophys. 645, A172</p> <p>Migliorini, A., Kanuchova Z., Ioppolo, S., Jones, N.C., Hoffmann, S.V., Tosi, F., Piccioni, G., Barbieri, M. 2021, Icarus, <em>submitted</em></p> <p>Palmer, M. H., Ridley, T., Hoffmann, S. V., et al. 2015, J. Chem. Phys., 142, 134302</p> <p> </p>