Dans la première partie de cette thèse, nous étudions le renversement de l'aimantation de nanofils d'alliage FePt à forte anisotropie magnétocristalline. Lorsque la largeur du fil devient inférieure à la taille des dendrites, nous avons montré qu'il existe une transition du processus de renversement de l'aimantation, de la croissance de dendrites vers la propagation d'une paroi magnétique unique qui renverse tout le fil. Au-delà, la diminution de la largeur du fil jusqu'à la taille caractéristique du désordre et/ou de la rugosité moyenne conduit au renforcement de la coercivité. Ceci conduit finalement dans les fils ultra-fins à un renversement consistant en un mélange de nucléation de domaines et de propagation de parois magnétiques. Dans la deuxième partie, nous rapportons l'utilisation de la magnétorésistance de Magnon (MMR), qui provient de la contribution des magnons à la résistivité, pour mesurer le renversement d'aimantation, dans des nanostructures avec aimantation perpendiculaire (FePt) ou planaire (NiFe). Nous avons montré que la MMR peut être utilisée pour détecter le retournement de l'aimantation dans les nanofils et nano-aimants, et en particulier pour détecter la position d'une paroi magnétique le long d'un nanofil fabriqués à partir d'une couche unique. Enfin, nous étudions dans une dernière partie la dynamique de dépiégeage de paroi magnétique sous champ et sous courant, dans les deux systèmes FePt et NiFe. Nous observons trois types de dépiégeage de paroi, qui dépendent de la nature des défauts ou de la géométrie de la constriction. L'analyse statistique du temps de piégeage montre que le processus de dépiégeage peut être décrit comme procédant d'un chemin simple, de chemins en série, ou de chemins alternatifs. En outre, l'effet du courant sur tous ces mécanismes de dépiégeage s'est révélé équivalent à l'effet du champ appliqué, ce qui permet de mesurer l'efficacité du transfer de spin dans ces systèmes. Keywords: Magnetization reversal, magnon magnetoresistance, domain wall, spins transfer torque.

Imaging techniques provide a method for non-invasive longitudinal monitoring of cancer therapies, but common metrics such as tumour size are late markers and do not indicate heterogeneity of response. Apoptotic cell death is an earlier marker of tumour response and produces molecular and cellular-level changes (macromolecular breakdown, membrane changes and cell shrinkage) that may be detectable by magnetic resonance imaging (MRI). Previous studies using conventional MRI methods have shown little sensitivity to apoptosis. In this thesis it is hypothesized that, using an extracellular contrast agent to affect the MRI property of relaxation for extracellular water preferentially, parameters related to water in the intracellular and extracellular environments and the exchange between them can be obtained and will be sensitive to apoptosis. It is also hypothesized that membrane changes and macromolecular breakdown are detectable by the technique of magnetization transfer. Measurements of relaxation in the presence of contrast agent in vitro demonstrated a decrease in extracellular water fraction and an increase in the rate of water exchange across the plasma membrane during apoptosis. In vivo, this method was complicated by the difficulty of delivering contrast agent to the tumour, but regions with good delivery showed correlation between high water exchange rates from MRI and apoptosis in histology. Magnetization transfer studies indicated only small changes in vitro during apoptosis and these were largely related to changes in the free water, so this method was not investigated further. Further work is required to determine the tumour lines where the water exchange methods may be applied reliably. Nevertheless, the method of measuring water exchange presented in this thesis can be performed in a clinically-feasible amount of time (~20 minutes). It therefore has potential in detecting apoptosis and predicting therapy response. It also emphasizes the role of water exchange in conventional MRI relaxation experiments.

This thesis consists of three distinct components: (1) a test of Slocnzewski's theory of spin-transfer torque using the Boltzmann equation, (2) a comparison of macrospin models of spin-transfer dynamics in spin valves with experimental data, and (3) a study of spin-transfer torque in continuously variable magnetization. Slonczewski developed a simple circuit theory for spin-transfer torque in spin valves with thin spacer layer. We developed a numerical method to calculate the spin-transfer torque in a spin valve using Boltzmann equation. In almost all realistic cases, the circuit theory predictions agree well with the Boltzmann equation results. To gain a better understanding of experimental results for spin valve systems, current-induced magnetization dynamics for a spin valve are studied using a single-domain approximation and a generalized Landau-Lifshitz-Gilbert equation. Many features of the experiment were reproduced by the simulations. However, there are two significant discrepancies: the current dependence of the magnetization precession frequency, and the presence and/or absence of a microwave quiet magnetic phase with a distinct magnetoresistance signature. Spin-transfer effects in systems with continuously varying magnetization also have attracted much attention. One key question is under what condition is the spin current adiabatic, i.e., aligned to the local magnetization. Both quantum and semi-classical calculations of the spin current and spin-transfer torque are done in a free-electron Stoner model. The calculation shows that, in the adiabatic limit, the spin current aligns to the local magnetization while the spin density does not. The reason is found in an effective field produced by the gradient of the magnetization in the wall. Non-adiabatic effects arise for short domain walls, but their magnitude decreases exponentially as the wall width increases.

Knowledge of energy dissipation and relaxation in electron, spin, and lattice degrees of freedom is of fundamental importance from both a technological and scientific point of view. In this dissertation, the electronic and magnetization dynamics of photoexcited colloidal cobalt substituted iron oxide nanocrystals, CoxFe3-xO4, were investigated through transient absorption and pump-probe Faraday rotation measurements. In this dissertation, linearly polarized femtosecond optical pulses at 780 nm were used to excite the weak absorption originating from the intervalence charge transfer transition (IVCT) between Fe2+ and Fe3+ ions of Fe3O4 nanocrystals. The timescale and corresponding relaxation processes of electronic relaxation dynamics of the excited IVCT state were first discussed. Size effect on electronic relaxation dynamics in Fe3O4 nanocrystals is not distinct on the basis of result from this study. One interesting feature of electronic dynamics data of photoexcited Fe3O4 nanocrystals is the creation of coherent acoustic phonons. Information on lattice temperature was obtained by measuring the period of coherent acoustic phonon as a function of excitation fluence and fit into a simple model based on Lamb’s theory. Since optical control of the magnetization can be either through optical or heating mechanisms, quantitative estimation of degree of demagnetization caused by lattice temperature is made by using Langevin function. The result from such estimation indicates the effect of lattice temperature rise on magnetization is too small to significantly affect the magnetization of Fe3O4 nanocrystals. Magnetization dynamics were studied via pump-probe Faraday rotation measurements. Optical excitation with near-infrared pulse resulted in an ultrafast demagnetization in 100fs. The energy of the excited state then relaxed through spin-lattice relaxation (SLR). Effects of surface spin and chemical tuning on the SLR were investigated by comparing the magnetization recovery timescales of nanocrystal with different particle sizes and cobalt concentration respectively. The experimental result is explained by a simple model where interior and surface spins contributed to the spin-lattice relaxation process differently. The observations suggest that spin-orbit coupling of the surface is stronger and less sensitive to stoichiometric variation than the interior spins of the nanocrystals.

No description available.

Thesis (M.S.)--Florida State University, 2004. / Advisor: Dr. Justin Schwartz, Florida State University, College of Engineering, Dept. of Mechanical Engineering. Title and description from dissertation home page (viewed June 17, 2004). Includes bibliographical references.

The ability of sub 100 nm nanoparticles to target and modulate the biology of cells will enable major advancements in cellular imaging and therapy in cancer and atherosclerosis. A key challenge is to load an extremely high degree of targeting, imaging, and therapeutic functionality into small, yet stable particles. A general mechanism is presented for thin autocatalytic growth on nanoparticle substrates (TAGS), as demonstrated for a homologous series of < 5 nm textured Au coatings on < 42 nm iron oxide cluster cores. Very low Au supersaturation levels are utilized to prevent commonly encountered excessive autocatalytic growth that otherwise produce thick shells. The degree of separation of nucleation to form the seeds from growth is utilized to control the morphology and uniformity of the thin Au coatings. The thin and asymmetric Au shells produce strong near infrared (NIR) absorbance with a cross section of ~10⁻¹⁴ m², whereas the high magnetic content per particles provides strong r2 spin-spin magnetic relaxivity of 200 mM⁻¹s⁻¹. TAGS may be generalized to a wide variety of substrates and high energy coatings to form core-shell nanoparticles of interest in a variety of applications as diverse as catalysis and bionanotechnology. High uptake of the nanoclusters by macrophages is facilitated by the dextran coating, producing intense NIR contrast both in cell culture and an in vivo rabbit model of atherosclerosis. A novel conjugation technique further allows covalent binding of anti-epidermal growth factor receptor (EGFR) monoclonal antibody (Ab) to the nanoclusters for highly selective targeting to EGFR over expressing cancer cells. AlexaFluor 488 tagged Ab nanocluster conjugates were prepared to correlate the number of conjugated Abs with the hydrodynamic diameter. The high targeting efficacy was evaluated by dark field reflectance imaging and atomic absorbance spectrometry (AAS). Colocalization of the nanoparticles by dual mode in-vitro imaging with dark field and fluorescence microscopy demonstrates the Abs remained attached to the Au surfaces. The extremely high curvature of the Au shells with features below 5 nm influence the spacing and orientations of the Abs on the surface, which has the potential to have a marked effect on biological pathways within cells. These targeted small multifunctional nanoclusters may solve some key molecular imaging challenges for cancer and atherosclerosis. / text

This is a new method of determining magnetization strength, direction, and paleopole location from magnetic anomalies across edges of the equatorial band of magnetic sources on Mars. Different assumed locations of paleopoles result in different inducing field directions in the vicinity of an edge. Thus, with different paleopoles, the resulting magnetic fields from the edges of magnetic sources are different, and correlate differently with the observed fields. Best correlating observed and computed magnetic edge effect fields yield the potential paleopoles. The total gradient (TG) of the z-component magnetic field was used to identify the edges of magnetization boundaries. Three edge segments yielded meaningful paleopoles. They are: (15°S, 285°E)/(0°, 292.5°E) across the northeast trending edge east of Tharsis; (15°N, 195°E) across the southern boundary located in the Terra Cimmeria and Terra Sirenum area; and (15°S, 165°E)/(45°S, 180°E) across the northeast edge of Hellas Planitia. The effective magnetization in these regions (assuming 40km magnetic layer thickness) is 7.02, 42.13-94.79, and 2.63-3.51 A/m, respectively. Evidence from the overlap of regions of TG and chronostratigraphy suggests that the dynamo was active during the Noachian and may have been active in the early Hesperian.

The area of ultrafast (sub-nanosecond) magnetization dynamics of ferromagnetic elements and thin films, usually driven by a strong femtosecond laser pulse, has experienced intense research interest. In this dissertation, laser-induced demagnetization is theoretically studied by taking into account interactions among electrons, spins, and lattice. We propose a microscopic approach under the three temperature framework and derive the equations that govern the demagnetization at arbitrary temperatures.To address the question of magnetization reversal at high temperatures, the conventional Landau-Lifshitz equation is obviously unsatisfactory, since it fails to describe the longitudinal relaxation. So by using the equation of motion for the quantum density matrix within the instantaneous local relaxation time approximation, we propose an effective equation that is capable of addressing magnetization dynamics for a wide range of temperatures. The longitudinal and transverse relaxations are analyzed, magnetization reversal processes near Curie temperatures is also studied. Furthermore, we compared our derived Self-consistent Bloch equation and Landau-Lifshitz-Bloch equation in detail. Finally, the demagnetzation dynamics for ferromagnetic and ferrimagnetic alloys is studied by solving the Self-consistent Bloch equation.

The use of geophysical techniques to image the interiors of active volcanoes can provide a better understanding of their structure and plumbing. The need for such information is especially critical for undersea volcanoes, whose environment makes them difficult to investigate. Because undersea volcanoes are made up of highly magnetic basaltic rock, it is possible to use variations in the magnetic field to explore the internal structure of such edifices. This study combines magnetic survey data from 12 research cruises to make a magnetic anomaly map of volcanically active Loihi, located in the Hawaiian Island chain. NRM intensities and susceptibility measurements were measured from recovered rock samples and suggest that magnetic properties of Loihi are widely varied (NRM intensities range from 1-157 A/m and susceptibilities from 1.26 x 10-3 to 3.62 x 10-2 S.I.). The average NRM intensity is 26 A/m. The size and strength of magnetic source bodies were determined by using various modeling techniques. A strongly magnetized shield can explain most of the anomaly with a large nonmagnetic zone inside, beneath the summit. Prominent magnetic highs are located along Loihi's north and south rift zone dikes and modeling solutions suggest strongly magnetized source bodies in these areas as well as a thin, magnetic layer atop the nonmagnetic zone. The strong magnetic anomalies found along the volcano's rift zones cannot be readily attributed to recent lava flows at the surface. Instead, the source bodies must continue several kilometers in depth to give reasonable magnetization values and are interpreted as dike intrusions. Nonmagnetic anomalies at the summit and south of the summit suggest the presence of a magma system. The model solution suggests Loihi is an inhomogeneously magnetized seamount with highly magnetic dike intrusions along the rift zones with a nonmagnetic body at its center overlain with a magnetic layer.