MarsMag
Financiado
Magnetic Sounding of Mars
Magnetic sounding is a powerful tool to explore the interior structure of a planetary body because electrical conductivity carries information on mineralogy, temperature and volatile content. We propose to apply this to Mars and t...
Magnetic sounding is a powerful tool to explore the interior structure of a planetary body because electrical conductivity carries information on mineralogy, temperature and volatile content. We propose to apply this to Mars and thus shed light on important questions such as crustal water and therefore habitability of extraterrestrial bodies.
Magnetic sounding relies on the principle that external fields induce currents in the subsurface. These induced responses provide information on subsurface electrical conductivity structure and can be measured from orbit and on the ground. While a range of techniques have mainly been developed for terrestrial investigations, this field of study has mostly been unexplored for other planets. Here, the magnetic field environment dictates the nature and geometry of the inducing external fields, and often times limited data sets pose new challenges. We plan to fully exploit martian data sets from orbit and on the ground to (1) characterize the magnetic field environment of Mars and (2) explore the electrical conductivity structure within the planet. This project will also pave the way for applying magnetic sounding methodologies to other terrestrial bodies, including Merurcy or the Moon.
The deep interior of a planet or moon carries information on its formation and evolution and contributes to the goals of ongoing planetary missions such as the InSight mission to Mars. InSight, the first surface mission equipped with a magnetometer landed on Mars last fall and the host professor and the candidate are involved as Co-PI on the seismometer team and as science investigator on the magnetometer team, respectively. This Fellowship will therefore contribute and further consolidate ETH involvement with InSight. Finally, Martian seismic activity thus far seems to originate mainly in the crust and complementary investigations using magnetic sounding will improve our understanding of crust and mantle structure and its relations to marsquakes.
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Duración del proyecto: 40 meses
Fecha Inicio: 2020-04-09
Fecha Fin: 2023-08-31
Fecha Fin: 2023-08-31
Línea de financiación: concedida
El organismo H2020 notifico la concesión del proyecto el día 2023-08-31
Línea de financiación objetivo
El proyecto se financió a través de la siguiente ayuda:
MSCA-IF-2019:
Individual Fellowships
Cerrada
hace 5 años
Presupuesto
El presupuesto total del proyecto asciende a
191K€
Líder del proyecto
EIDGENOESSISCHE TECHNISCHE HOCHSCHULE ZUERICH
No se ha especificado una descripción o un objeto social para esta compañía.
401.37K€ |
Participante