We present a detailed experimental investigation into Bose-Einstein condensates loaded into a one-dimensional optical standing wave at the Bragg condition. The main emphasis of this thesis is the experimental and theoretical investigation into Bragg spectroscopy performed on circularly accelerating Bose-Einstein condensates. The condensate undergoes circular micromotion in a magnetic time-averaged orbiting potential trap and the effect of this motion on the Bragg spectrum is analysed. A simple frequency modulation model is used to interpret the observed complex structure, and broadening effects are considered using numerical solutions to the Gross-Pitaevskii equation. The second part of this thesis is an experimental investigation into the effect of nonlinearity on the non-adiabatic loading of a condensate into a optical lattice at the Brillouin zone boundary. Results of using a phase shifting technique to load a single Bloch band in the presence of strong interactions are presented. We observe a depletion of the condensed component, and we propose possible mechanisms for this result.

The Double-TOP trap is a new type of magnetic trap for neutral atoms, and is suitable for Bose-Einstein condensates (BECs) and evaporatively cooled atoms. It combines features from two other magnetic traps, the Time-averaged Orbiting Potential (TOP) and Ioffe-Pritchard traps, so that a potential barrier can be raised in an otherwise parabolic potential. The cigar-like cloud of atoms (in the single-well configuration) is divided halfway along its length when the barrier is lifted. A theoretical model of the trap is presented. The double-well is characterised by the barrier height and well separation, which are weakly coupled. The accessible parameter space is found by considering experimental limits such as noise, yielding well separations from 230 [mu]m up to several millimetres, and barrier heights from 65 pK to 28 [mu]K (where the energies are scaled by Boltzmann�s constant). Potential experiments for Bose-Einstein condensates in this trap are considered. A Double-TOP trap has been constructed using the 3-coil style of Ioffe-Pritchard trap. Details of the design, construction and current control for these coils are given. Experiments on splitting thermal clouds were carried out, which revealed a tilt in the potential. Two independent BECs were simultaneously created by applying evaporative cooling to a divided thermal cloud. The Double-TOP trap is used to form a linear collider, allowing direct imaging of the interference between the s and d partial waves. By jumping from a double to single-well trap configuration, two ultra-cold clouds are launched towards a collision at the trap bottom. The available collision energies are centred on a d-wave shape resonance so that interference between the s and d partial waves is pronounced. Absorption imaging allows complete scattering information to be collected, and the images show a striking change in the angular distribution of atoms post-collision. The results are compared to a theoretical model, verifying that the technique is a useful new way to study cold collisions.

Thesis (Ph. D.)--University of Missouri-Columbia, 2007. / The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file (viewed Dec. 12, 2007). Vita. Includes bibliographical references.

Les sources renouvelables (solaire, éolien, vapeur d'eau atmosphérique) représentent des solutions alternatives intéressantes pour répondre aux besoins de certaines populations isolées sans électricité et en stress hydrique (moins de 15 L d'eau par jour). Des condenseurs radiatifs de production d'eau douce potable ont été élaborés par l'utilisation d'un phénomène naturel (refroidissement radiatif) ne nécessitant pas d'apport d'énergie. Depuis 2000, l'Université de Corse, le CEA et le CNRS se sont conventionnés pour développer des outils et des technologies performantes pour effectuer la transition entre des prototypes de laboratoire et des systèmes réels. Afin de s'approcher du rendement théorique maximum (0,8 L m-2), des protocoles de mesure, puis des prototypes " plan "de 30 m² ont été construits. Un code numérique (CFD) a été développé pour estimer les performances de systèmes complexes à grande échelle (plusieurs centaines de m²) avant leur installation. De nouveaux matériaux de condensation faisant l'objet d'un brevet déposé, sélectifs en longueur d'onde, ont été formulés pour répondre à la fois à des contraintes de climatisation passive des bâtiments en cycle diurne et de production d'eau en cycle nocturne. En partenariat avec l'association OPUR (www.opur.u-bordeaux.fr), une toiture de démonstration de 15,1 m² à Biševo en Croatie (0,181 mm en moyenne), ainsi qu'une usine de production de 850 m² (15000 m² à terme) confirment le potentiel de la technologie puisque les rendements attendus pourront atteindre 5 m3 d'eau par jour. Parallèlement, le solaire et l'éolien, dans un système hybride de production d'énergie décentralisée (couplés avec une source auxiliaire type fossile ou hydrogène) peuvent pallier l'absence d'électrification de certaines régions du Globe. Dans ce mémoire, des codes de calcul de dimensionnement de ces systèmes ont été élaborés pour une optimisation physique et économique de ces techniques répondant soit à l'électrification de sites isolés soit à la production massive d'électricité par connexion à un réseau de distribution pour différentes applications (relevage de chutes de tension ou production en continu). Les résultats obtenus permettent d'envisager l'utilisation du couplage EnR-H2. A ce titre, notre équipe de recherches a obtenu le financement d'une centrale PV-H2 sur le site du laboratoire : 3,6 MW couplé à un électrolyseur et une pile à combustible de puissance de plus de 100 kW.

Systems of linear equations are central to many science and engineering application domains. Given the abundance of low-cost parallel processing fabrics, the study of fast and accurate parallel algorithms for solving such systems is receiving attention. Fast linear solvers generally use a form of LU factorization. These methods face challenges with workload distribution and communication overhead that hinder their application in a true broadcast communication environment. Presented is an efficient framework for solving large-scale linear systems by means of a novel utilization of Cramer's rule. While the latter is often perceived to be impractical when considered for large systems, it is shown that the algorithm proposed has an order N^3 complexity with pragmatic forward and backward stability. To the best of our knowledge, this is the first time that Cramer's rule has been demonstrated to be an order N^3 process. Empirical results are provided to substantiate the stated accuracy and computational complexity, clearly demonstrating the efficacy of the approach taken. The unique utilization of Cramer's rule and matrix condensation techniques yield an elegant process that can be applied to parallel computing architectures that support a broadcast communication infrastructure. The regularity of the communication patterns, and send-ahead ability, yields a viable framework for solving linear equations using conventional computing platforms. In addition, this dissertation demonstrates the algorithm's potential for solving large-scale sparse linear systems.

Atomic force microscopy (AFM) is a particularly useful tool, for obtaining structural information about drug-nucleic acid interactions. The mode of drug binding intercalation versus groove binding can be determined from images acquired on individual DNA molecules as the length of a DNA molecule increases in direct proportion to the number of intercalators bound to it. The efforts of this research were directed toward elucidating the mode of binding of a series of drugs based on polymers of naphthalenetetracarboxyl diimide (NDI) interacting with a linearized DNA plasmid. During the course of the investigation of these drugs, DNA intercalation was confirmed as the mode of binding and the binding affinity estimated. Unexpectedly, concentration-dependent formation of secondary DNA structures including condensates was observed. DNA toroids, spheres, and rods were imaged and measured. Conformations that are believed to be intermediate condensate forms were also identified at lower poly-NDI concentrations. Models for the DNA condensation process have been proposed. Ultimately, this research furthers the understanding of DNA condensation which can be applied to gene delivery systems and anti-viral agents. It may also help direct the development of better drugs based on the insight of poly-intercalators interactions with DNA.

No description available.

A Differential Mobility Analyzer/Tandem Differential Mobility Analyzer (DMA/TDMA) system was used to measure simultaneously the size distribution and hygroscopicity of the ambient aerosol population. The system was operated aboard the National Center for Atmospheric Research/National Science Foundation (NCAR/NSF) C-130 during the 2006 Megacity Initiative: Local and Global Research Observations (MILAGRO) field campaign followed by the 2006 Intercontinental Chemical Transport Experiment – Phase B (INTEX-B) field campaign. The research flights for the MILAGRO campaign were conducted within the Mexico City basin and the region to the northeast within the pollution plume. The aerosol within the basin is dominated by organics with an average measured kappa value of 0.21 /- 0.18, 0.13 /- 0.09, 0.09 /- 0.06, 0.14 /- 0.07, and 0.17 /- 0.04 for dry particle diameters of 0.025, 0.050, 0.100, 0.200, and 0.300 mu m, respectively. As the aerosols are transported away from the Mexico City Basin, secondary organic aerosol formation through oxidation and condensation of sulfate on the aerosols surface rapidly increases the solubility of the aerosol. The most pronounced change occurs for a 0.100 mu m diameter aerosol where, after 6 hours of transport, the average kappa value increased by a factor of 3 to a kappaof 0.29 /- 0.13. The rapid increase in solubility increases the fraction of the aerosol size distribution that could be activated within a cloud. The research flights for the INTEX-B field campaign investigated the evolution of the physicochemical properties of the Asian aerosol plume after 3 to 7 days of transport. The Asian aerosol within the free troposphere exhibited a bimodal growth distribution roughly 50 percent of the time. The more soluble mode of the growth distribution contributed between 67-80 percent of the overall growth distribution and had an average kappabetween 0.40 and 0.53 for dry particle diameters of 0.025, 0.050, 0.100, and 0.300 mu m. The secondary mode was insoluble with an average kappabetween 0.01 and 0.05 for all dry particle diameters. Cloud condensation nuclei closure was attained at a supersaturation of 0.2 percent for all particles within the free troposphere by either assuming a pure ammonium bisulfate composition or a binary composition of ammonium bisulfate and an insoluble organic.

Submarine channels are important conduits for sediment in deep marine environments, and understanding their formation is critical to modeling basin fill processes. Most models describing channel evolution focus on turbidity currents as the erosive and constructive force in channel initiation. However, slope failure and slumping can be significant drivers of channelization, particularly in upper slope and ramp environments. Determining the relative roles of slumping and erosion by turbidity currents can provide important insight into the timing of channelization and the geometries of subsequent deposits. Samples were collected from Guadalupe Mountains National Park from two primary localities at Salt Flat Bench (Figure 2). Three vertical sections were measured at both locations. A total of 16 samples were collected for petrographic analysis and X-ray fluorescence (XRF) imaging. Spectacular outcrop quality makes the Middle Permian Brushy Canyon Formation in Guadalupe Mountains National Park an ideal location for the study of early channel evolution. A detailed facies analysis of fine-grained channel deposits was conducted in the Upper Brushy Canyon Formation in the Salt Flat Bench outcrops. After channelization, an interval of relative condensation dominated by hemipelagic settling of organic matter and silt was followed by an interval of incomplete sediment bypass by turbidity currents. This sequence of events suggests that sea level was at a relative highstand at the time of channel inception, whereas channel inception by turbidity currents is expected during a lowstand. Slumping rather than erosion by turbidity currents is the most likely mechanism to have initiated a channel at the study area. There is no evidence for the existence for high energy currents until after the interval of condensation. However, the action of weak contour currents during early channel evolution is observed in outcrop and microtextural features. Early carbonate cementation of channel-lining silts may have stabilized the slump surface with respect to erosion by later turbidity currents.

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