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origin of deuterium astrochemistry

dc.contributor.authorHugo, Edouard
dc.date.accessioned2010-10-12T19:28:09Z
dc.date.available2010-10-12T19:28:09Z
dc.date.issued2008
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-3191-9
dc.description.abstractDense cold molecular clouds reckoned to be stellar nurseries are the scene of an extreme molecular deuteration. Despite the cosmic D/H ratio of 10^{-5}, molecular species in prestellar cores are observed to contain nearly as much deuterium as hydrogen. This astonishing deuterium enrichment promoted by low temperatures is the work of H3+. It is the key species which unlocks the deuterium from its HD reservoir via reactions like H3+ + HD -> H2D+ + H_2 and drags it further to other species in successive reactions. For this reason, the H3+ + H2 isotopic system is outstandingly critical for the astrochemistry of cold environments. However, its understanding is yet incomplete and insufficient. This thesis thus focuses on the H3+ + H2 isotopic system from a theoretical, experimental and astronomical point of view giving a particular look into the role of nuclear spins...
dc.format.extent202 S.
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.publisherUniv. Köln
dc.rights.urihttp://e-docs.geo-leo.de/rights
dc.subject.ddc523
dc.subject.gokTJM 000
dc.titleThe H_1n+3 + H2 isotopic system
dc.title.alternativeorigin of deuterium astrochemistry
dc.typemonograph
dc.subject.gokverbalKosmochemie {Weltraumforschung}
dc.identifier.doi10.23689/fidgeo-263
dc.identifier.ppn59607624X
dc.identifier.urnurn:nbn:de:hbz:38-26469
dc.type.versionpublishedVersion
dc.relation.collectionAstronomie, Astrophysik, Weltraumforschung
dc.description.typethesis


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