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dc.contributor.advisorMackenzie, Andrew
dc.contributor.advisorGrigera, Santiago A.
dc.contributor.authorSlobinsky, Demian G.
dc.coverage.spatial158en_US
dc.date.accessioned2012-09-20T20:37:04Z
dc.date.available2012-09-20T20:37:04Z
dc.date.issued2012-06
dc.identifier.urihttp://hdl.handle.net/10023/3102
dc.description.abstractA way to obtain materials that show novel phenomena is to explore the interplay between geometry and interactions. When it is not geometrically possible to satisfy all the interactions by a given configuration, then to find the ground state becomes very complicated. This interplay between geometry and interactions defines geometrical frustration. One of the most popular examples of geometrical frustration in magnetism is spin ice. In this system, nearest neighbour ferromagnetic interactions between Ising spins in a pyrochlore structure emulate water ice by showing the same degree of frustration. This is manifested by the same ground state residual entropy. Although the clearest example of spin ice among magnets is shown by Dy₂Ti₂O₇, the behaviour of this material is richer than that of pure spin ice. The large magnetic moments of the rare earth Dy form a spin ice that also interacts via dipolar interactions. These long range interactions give rise to monopolar excitations which dramatically affect the dynamics of the system with respect to the pure spin ice case. In this thesis magnetisation experiments and numerical methods are used to explore the properties of the magnetic insulator Dy₂Ti₂O₇. We study its excitations at low temperature and describe the out-of-equilibrium characteristics of the magnetisation processes, below a temperature where the system freezes out. For temperatures above the freezing temperature, we describe and measure a 3D Kasteleyn transition and the concomitant Dirac strings associated to it, for the field in the [100] crystallographic direction. For temperatures below the freezing temperature, we find new out-of-equilibrium phenomena. Magnetic jumps are measured and their sweep rate dependence analysed. A deflagration theory is proposed and supported by simultaneous magnetisation and sample temperature measurements obtained by a new design of a Faraday magnetometer.en_US
dc.language.isoenen_US
dc.publisherUniversity of St Andrews
dc.subjectSpin iceen_US
dc.subjectMonopolesen_US
dc.subjectFrustrationen_US
dc.subjectGeometrical frustrationen_US
dc.subjectPyrochloreen_US
dc.subjectTetrahedronen_US
dc.subjectOut-of-equilibriumen_US
dc.subjectMagnetismen_US
dc.subjectLow temperatureen_US
dc.subjectCryogenicsen_US
dc.subjectMagnetometeren_US
dc.subjectMagnetisationen_US
dc.subject.lccQC754.2M34S6
dc.subject.lcshMagnetizationen_US
dc.subject.lcshDysprosium--Magnetic propertiesen_US
dc.subject.lcshTitanates--Magnetic propertiesen_US
dc.subject.lcshLow temperaturesen_US
dc.titleLow temperature magnetisation properties of the spin ice material Dy₂Ti₂O₇en_US
dc.typeThesisen_US
dc.contributor.sponsorEngineering and Physical Sciences Research Council (EPSRC)en_US
dc.type.qualificationlevelDoctoralen_US
dc.type.qualificationnamePhD Doctor of Philosophyen_US
dc.publisher.institutionThe University of St Andrewsen_US


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