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dc.contributor.advisorSasselov, Dimitaren_US
dc.contributor.advisorOberg, Karinen_US
dc.contributor.authorPiso, Ana-Maria Adrianaen_US
dc.date.accessioned2017-07-25T14:41:46Z
dc.date.created2016-05en_US
dc.date.issued2016-05-04en_US
dc.date.submitted2016en_US
dc.identifier.citationPiso, Ana-Maria Adriana. 2016. Origins of Gas Giant Compositions: The Role of Disk Location and Dynamics. Doctoral dissertation, Harvard University, Graduate School of Arts & Sciences.en_US
dc.identifier.urihttp://nrs.harvard.edu/urn-3:HUL.InstRepos:33493454
dc.description.abstractThe composition of planets is determined by and tightly linked to the composition of the protoplanetary disk in which they form. In the first part of my thesis, I study giant planet formation through core accretion. I show how the minimum core mass required to form a giant planet during the lifetime of the protoplanetary disk depends on the location in the disk, the equation of state of the nebular gas and dust opacity. This minimum applies when planetesimal accretion does not substantially heat the core's atmosphere. The minimum core mass decreases with semimajor axis, and may be significantly lower than the typically quoted value of 10 Earth masses, thus challenging previous studies that core accretion cannot operate in the outer disk. In the second part, I explore how the composition and evolution of protoplanetary disks may affect the formation and chemical composition of giant planets. Volatile snowlines are highly important in the planet formation process. I thus show how the snowline locations of the main carbon, oxygen and nitrogen carriers, as well as the C/N/O ratios, are affected by disk dynamics and ice morphology. Compared to a static disk, disk dynamics and ice morphology combined may change the CO and N_2 snowline locations by a factor of 7. Moreover, the gas-phase N/O ratio is highly enhanced throughout most of the disk, meaning that wide-separation giants should have an excess of nitrogen in their atmospheres which may be used to trace their origins. The large range of possible CO and N_2 snowline locations, and hence of regions with highly enhanced N/O ratios, implies that snowline observations at various stages of planet formation are crucial in order to use C/N/O ratios as beacons for planet formation zones.en_US
dc.description.sponsorshipAstronomyen_US
dc.format.mimetypeapplication/pdfen_US
dc.language.isoenen_US
dash.licenseLAAen_US
dc.subjectPhysics, Astronomy and Astrophysicsen_US
dc.titleOrigins of Gas Giant Compositions: The Role of Disk Location and Dynamicsen_US
dc.typeThesis or Dissertationen_US
dash.depositing.authorPiso, Ana-Maria Adrianaen_US
dc.date.available2017-07-25T14:41:46Z
thesis.degree.date2016en_US
thesis.degree.grantorGraduate School of Arts & Sciencesen_US
thesis.degree.levelDoctoralen_US
thesis.degree.nameDoctor of Philosophyen_US
dc.contributor.committeeMemberAndrews, Seanen_US
dc.contributor.committeeMemberCiesla, Fredericken_US
dc.contributor.committeeMemberHolman, Mathewen_US
dc.type.materialtexten_US
thesis.degree.departmentAstronomyen_US
dash.identifier.vireohttp://etds.lib.harvard.edu/gsas/admin/view/837en_US
dc.description.keywordsplanet formation; disk and planet compositionsen_US
dash.author.emailanamaria.piso@gmail.comen_US
dash.contributor.affiliatedPiso, Ana-Maria Adriana


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