Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/160038
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dc.contributor.authorMichaud, F.-
dc.contributor.authorVentolà, L.-
dc.contributor.authorCalvet Pallàs, Maria Teresa-
dc.contributor.authorCuevas Diarte, Miguel Ángel-
dc.contributor.authorSolans, Xavier, 1949-2007-
dc.contributor.authorFont Bardia, Ma. Mercedes-
dc.date.accessioned2020-05-13T13:53:43Z-
dc.date.available2020-05-13T13:53:43Z-
dc.date.issued2000-
dc.identifier.issn0108-2701-
dc.identifier.urihttp://hdl.handle.net/2445/160038-
dc.description.abstractIn the crystal of the title compound, C20H42O, the mol­ecules are packed in layers parallel to the (100) plane. The alkyl chains are parallel to the [30inline image] direction and these molecular chains are hydrogen‐bonded into chains parallel to the c axis. All C¿C bonds of the alkyl chain show an antiperiplanar (trans) conformation, with a slight deviation from the ideal value (180°) in the C¿C bonds close to the hydrogen bonds. The length of the alkyl chain is 27.92 (2) Å and the tilt angle is 59.7 (2)°.-
dc.format.extent3 p.-
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherInternational Union of Crystallography-
dc.relation.isformatofReproducció del document publicat a: https://doi.org/10.1107/S010827019901392X-
dc.relation.ispartofActa Crystallographica Section C: Crystal Structure Communications, 2000, num. 56, p. 219-221-
dc.relation.urihttps://doi.org/10.1107/S010827019901392X-
dc.rights(c) International Union of Crystallography, 2000-
dc.sourceArticles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)-
dc.subject.classificationCristal·lografia-
dc.subject.otherCrystallography-
dc.titleThe γ-form of n-eicosanol-
dc.typeinfo:eu-repo/semantics/article-
dc.typeinfo:eu-repo/semantics/publishedVersion-
dc.identifier.idgrec563116-
dc.date.updated2020-05-13T13:53:44Z-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess-
Appears in Collections:Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)

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