Thesis (M. S.)--Mechanical Engineering, Georgia Institute of Technology, 2006. / Edward Hoffman, Committee Member ; Nolan Hertel, Committee Member ; Weston Stacey, Committee Chair.

Thesis (D. Min.)--Southwestern Baptist Theological Seminary, 2001. / Includes bibliographical references (leaves 125-134, 68-72).

Thesis (D. Min.)--Southwestern Baptist Theological Seminary, 1992. / Includes Participant workbook in Indonesian translation and English. Includes bibliographical references (leaves 211-214).

Thesis (D. Min.)--Ashland Theological Seminary, 2006. / Abstract. Includes bibliographical references (leaves 196-202).

Thesis (M.A.)--Lancaster Bible College, 2005. / Abstract. Includes bibliographical references (leaves 171-175).

Thesis (M.A.)--St. Vladimir's Orthodox Theological Seminary, 2005. / Abstract. Includes bibliographical references (leaf 25).

Thesis (D. Min.)--Ashland Theological Seminary, 1986. / Includes bibliographical references (leaves 115-118).

Iron meteorites are Fe-Ni alloys that are thought to represent samples of the cores of differentiated asteroids. A minority of the iron meteorites contain silicate inclusions, the so-called silicate-bearing or non-magmatic iron meteorites. The presence of chemically evolved silicate inclusions in a high-density Fe-Ni metal raises questions about their origin. The IIE group belongs to the non-magmatic iron meteorites and contains primitive as well as evolved silicate inclusions. The object of this thesis is to investigate the formation processes of the silicate-bearing iron meteorites by examination of the primitive IIE irons. The first chapter provides an overview of the state of the art of silicate-bearing iron meteorites and highlights the existing open questions. The second chapter discusses the most important analytical techniques that have been used during this thesis. The third chapter contains all the research conducted on the Mont Dieu meteorite, a new primitive member of the IIE group. This meteorite represents a unique member of the IIE group as it contains chondrules in its silicate inclusions. Together with the Netschaëvo meteorite, they are the only two IIE irons that show such a primitive texture. Based on the mineralogy, the major element composition and the oxygen isotope composition, we conclude that Mont Dieu originated as an H chondrite. The observation of a series of features, including silicate darkening, thick metal veins containing angular clasts, and the need for a heterogeneous heat source, led to an impact-based origin for Mont Dieu. The fourth chapter is dedicated to the investigation of two samples of the primitive Netschaëvo IIE meteorite, that show lithologies that are very different to those described in the literature. The investigated pieces of Netschaëvo can be classified as impact melt rocks (IMR) and we show that the precursor material of these IMR and the primitive clasts both originated from the same parent body. The occurrence of both lithologies in the same meteorite suggests that Netschaëvo itself is a breccia containing metamorphosed and IMR clasts and that the meteorite formed as the result of an impact event. The fifth chapter focuses on the fine-grained matrix material found in the silicate inclusions of Netschaëvo IIE. This study provides insights into core-mantle boundary environments and confirms the impact-origin of Netschaëvo by the presence of minerals and textures pointing to a very rapid cooling. The investigations show that the re-partitioning of phosphorus from the metal into the silicate material during cooling might be a general process during planetary differentiation. In the sixth chapter, the veins present in the silicate inclusions of Mont Dieu are described in detail, and compared to the veining structures found in Techado IIE silicate. The characteristics of the processes causing the formation of these veins are discussed. The seventh chapter summarizes the conclusions of this thesis. The detailed petrographic and geochemical examinations conducted on the investigated samples show that collisions played a major role in the formation of the IIE iron meteorites. The work performed in the framework of this thesis provides a significant contribution towards a more complete and in-depth understanding of the formation mechanisms of silicate-bearing iron meteorites. / Doctorat en Sciences / info:eu-repo/semantics/nonPublished

With the popularity of outdoor activities like hiking, the demands of certain types of employment, or being a student, an individual’s ability to carry a load is an important mobility consideration. By understanding the changes to an individual’s gait when supporting a backpack load, an individual’s ability to carry heavy loads for prolonged periods could be improved. Most biomechanical studies have examined the changes in able-bodied gait when carrying a load. However, research is lacking on the effect of backpack loads on amputee gait patterns. This project examined the effects of a backpack load on the gait patterns of unilateral transtibial amputees. Ten participants performed walking trials on four surfaces (level ground, uneven ground, walking up an incline, and walking down an incline), without a pack and with a pack. A total of 40 trials were collected per subject, with 10 trials collected on each surface. Three-dimensional motion data were collected with an eight-camera Vicon Motion Analysis system to describe limb motion as well as compare kinematic outcomes between tasks and conditions. Force platform data were collected during the level ground trials and used to calculate kinetic measures for both limbs. With the addition of the pack changes were seen on each surface, with different changes occurring to each limb. The ramp up surface created the most changes when comparing the two conditions. The only change seen across all four surfaces was a decrease in ankle dorsiflexion before push-off on the prosthetic limb. The two next most common changes were increases in knee and hip flexion during weight-acceptance.

It is preferable that control and bearing condition monitoring are integrated, as the condition of the system should influence control actions. As wind turbines mainly work in remote areas, it becomes necessary to develop a wireless platform for the control system. A fuzzy system with self-tuning mechanism was developed. The input speed error and speed change were selected to control the shaft speed, while the kurtosis and peak-to-peak values were used as another set of inputs to monitor the bearing conditions. To enhance effectiveness, wait-and-see (WAS) logic was used as the pre-processing step for the raw vibration signal. The system was implemented on the LabVIEW platform. Experiments have shown that the system can effectively adjust motor rotating speed in response to bearing conditions. For future studies, more advanced fault detection methods can be integrated with proper tuning mechanisms to enrich the performance and function of the controller.