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Laboratory experiments on the sublimation of methane through ice dust layers and applications to cometary activity

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Laboratory experiments on the sublimation of methane through ice dust layers and applications to cometary activity

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dc.contributor.author Tamai, Carla es_ES
dc.contributor.author Maté, Belén es_ES
dc.contributor.author Cazaux, Stéphanie es_ES
dc.contributor.author Satorre, M. Á. es_ES
dc.date.accessioned 2024-06-26T18:11:55Z
dc.date.available 2024-06-26T18:11:55Z
dc.date.issued 2023-06-30 es_ES
dc.identifier.issn 0004-6361 es_ES
dc.identifier.uri http://hdl.handle.net/10251/205516
dc.description.abstract [EN] Context. Comets are small celestial bodies made of ice, dust, and rock that orbit the Sun. Understanding their behavior as they warm up at perihelion unveils many pieces of information about the interior and general morphology of the ices hidden under the dust.Aims. The goal of this research is to study the sublimation of CH4 through amorphous solid water (ASW), with a focus on the structural changes in water and the influence of a layer of indene (as a proxy of the crust) during a period of thermal processing, which we use in a controlled laboratory setting to simulate cometary environments.Methods. Ices at a CH4/H2O abundance ratio of about 0.01 are deposited and layered, or co-deposited, at 30 K and are heated until 200 K (or 140 K) with a ramp of either 1 or 5 K min(-1). We use mass spectrometry and infrared spectroscopy to analyze the results.Results. Depending on the heating ramp and type of deposition, the sublimation of methane through ASW varies, being lower in intensity and higher in temperature when the co-deposited structure is considered. When two temperature cycles are applied, the second one sees less intense CH4 desorptions. When indene is placed above the ice mixtures, we find that the thicker its layer, the later the methane desorption. However, this later desorption sees a greater quantity of methane released due to water reorganization and higher desorbed material pressure.Conclusions. The structural changes of water ice drive volatile and hyper-volatile desorption because of the transition from high to low intrinsic density and transformation from amorphous to crystalline. This desorption indicates that such material has been deposited at low temperatures in agreement with previous theories on cometary ices formed in the pre-stellar cloud. During the two temperature cycles of our experiments, most of the released material is seen to be pristine and the processed part, if any, is of a negligible quantity, in agreement with dust-rock cometary studies. es_ES
dc.description.sponsorship Funds from the Spanish MINECO PID2020-118974GB-C22 and PID2020-113084GB-I00 projects are acknowledged. es_ES
dc.language Inglés es_ES
dc.publisher EDP Sciences es_ES
dc.relation.ispartof Astronomy and Astrophysics es_ES
dc.rights Reconocimiento (by) es_ES
dc.subject Comets es_ES
dc.subject General es_ES
dc.subject Methods es_ES
dc.subject Laboratory es_ES
dc.subject Solid state es_ES
dc.subject.classification FISICA APLICADA es_ES
dc.title Laboratory experiments on the sublimation of methane through ice dust layers and applications to cometary activity es_ES
dc.type Artículo es_ES
dc.identifier.doi 10.1051/0004-6361/202346358 es_ES
dc.relation.projectID info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PID2020-113084GB-I00/ES/LIGANDO GAS, HIELO Y POLVO: ASTROFISICA DE LABORATORIO/ es_ES
dc.relation.projectID info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/PID2020-118974GB-C22/ES/PROPIEDADES DE HIELOS ASTROFISICOS/ es_ES
dc.rights.accessRights Abierto es_ES
dc.contributor.affiliation Universitat Politècnica de València. Escuela Politécnica Superior de Alcoy - Escola Politècnica Superior d'Alcoi es_ES
dc.description.bibliographicCitation Tamai, C.; Maté, B.; Cazaux, S.; Satorre, MÁ. (2023). Laboratory experiments on the sublimation of methane through ice dust layers and applications to cometary activity. Astronomy and Astrophysics. 675. https://doi.org/10.1051/0004-6361/202346358 es_ES
dc.description.accrualMethod S es_ES
dc.relation.publisherversion https://doi.org/10.1051/0004-6361/202346358 es_ES
dc.type.version info:eu-repo/semantics/publishedVersion es_ES
dc.description.volume 675 es_ES
dc.relation.pasarela S\497670 es_ES
dc.contributor.funder Agencia Estatal de Investigación es_ES


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