The objective of this master's thesis is to design and implement a system which would be able to transfer a picture (either a bitmap or a vector image) on a foundational material. The main part of the apparatus consists of a plotter controlled by two stepping motors. The engraving itself is provided by a marker mounted to a movable part of engraving head. There was a PCB created for controlling the entire system. It contains power supplies, a microcontroller and motor and engraving head controlling circuits. The second part of the thesis shows a microcontroller program and a user interface in a PC. The image is trasfered from the PC into the microcontroller where it is processed and, based on the controlling program, engraved to the material.

This mater's thesis deals with introducing principles of debugging and debuggers. The thesis examines in detail format of debugging information and it describes the design of debugger created within the project Lissom. Furthermore, the thesis also contains implementation of each designed part, which the debugger consists of. Last part of this thesis deals with testing of the implemented solution with two types of processor architectures and it also contains the conclusion of the results.

The biodiversity value of a wetland is linked not only to its position in the landscape relative to other wetlands, but also to its habitat characteristics. I monitored amphibian species richness among 12 small, isolated, and undisturbed wetlands (which occur on lands permitted for phosphate mining) in central Florida during the 2005 and 2006 breeding seasons. I used seven habitat and landscape variables to characterize the environments of the wetlands and generalized linear models to determine which of these variables had the greatest influence on the occurrence of seven amphibian species (Anaxyrus terrestris, Gastrophryne carolinensis, Hyla gratiosa, Lithobates capito, L. catesbeianus, L. grylio, and Pseudacris nigrita verrucosa). Significant models for each species incorporated six of the seven habitat and landscape variables: distance to permanent water (2 spp.), distance to nearest wetland (3 spp.), vegetation heterogeneity (2 spp.), hydroperiod (2 spp.), presence/absence of fish (1 sp.), and distance to canopy cover (1 sp.). I suggest that source/sink metapopulation and patchy population dynamics in a given year are affected in part by environmental variables of ephemeral wetlands as they affect individual amphibian species. I suggest that a diversity of environmental conditions among wetlands produces the greatest amphibian biodiversity in this system, and that conservation and restoration efforts should emphasize environmental heterogeneity.

Flexible beam structures are popular in civil and mechanical engineering. Many of these structures undergo large displacements and finite rotations, but with small deformations. Their dynamic behaviors are usually investigated using finite beam elements. A well known method to derive such beam elements is the corotational approach. This method has been extensively used in nonlinear static analysis. However, its application in nonlinear dynamics is rather limited. The purpose of this thesis is to investigate the nonlinear dynamic behavior of flexible beam structures using the corotational method. For the 2D case, a new dynamic corotational beam formulation is presented. The idea is to adopt the same corotational kinetic description in static and dynamic parts. The main novelty is to use cubic interpolations to derive both inertia terms and internal terms in order to capture correctly all inertia effects. This new formulation is compared with two classic formulations using constant Timoshenko and constant lumped mass matrices. This work is presented in the first appended journal paper. For the 3D case, update procedures of finite rotations, which are central issues in development of nonlinear beam elements in dynamic analysis, are discussed. Three classic and one new formulations of beam elements based on the three different parameterizations of the finite rotations are presented. In these formulations, the corotational method is used to develop expressions of the internal forces and the tangent stiffness matrices, while the dynamic terms are formulated into a total Lagrangian context. Many aspects of the four formulations are investigated. First, theoretical derivations as well as practical implementations are given in details. The similarities and differences between the formulations are pointed out. Second, numerical accuracy and computational efficiency of these four formulations are compared. Regarding efficiency, the choice of the predictor at each time step and the possibility to simplify the tangent inertia matrix are carefully investigated. This work is presented in the second appended journal paper. To make this thesis self-contained, two chapters concerning the parametrization of the finite rotations and the derivation of the 3D corotational beam element in statics are added. / QC 20120521

Phylloid-algal mounds form heterogeneous hydrocarbon reservoirs in the southeastern portion (Blanding sub-basin) of the Paradox Basin. Well-studied Lower Ismay mounds exposed along walls of the San Juan River gorge in the vicinity of Eight Foot Rapids, the west limb of the Raplee Anticline, and at the classic Honaker Trail locality (southwestern Paradox Basin) have often been cited as outcrop analogs of productive subsurface mounds. Until now, however, there has not been a complete description of the distribution, size, and spacing of outcropping algal mounds at the classic Eight Foot Rapids locality. The Lower Ismay sequence was analyzed in the context of a build-and-fill model of deposition. There are three facies associations within the sequence: 1) a basal lowstand to middle highstand pre-mound facies association, 2) a late highstand to middle falling stage phylloid algal-dominated relief-building facies association, and 3) a late falling stage, post-mound relief-filling facies association. Above the basal maximum flooding surface (Gothic Shale), the facies succession displays a distinct shallowing upward trend through the Lower Ismay sequence. Mound dimensions and facies stacking patterns permit evaluation of two depositional models. The first is a traditional, moderate- to low-energy model of vertical and radial mound accumulation of phylloid algal plates. The second is a high-energy, tidally influenced model of accumulation wherein mounds become hydrodynamically elongate. Outcrop data indicate that algal-dominated buildups are domal in shape with no preferred axis of elongation. These patterns do not support a hydrodynamic accumulation of loose algal plate fragments. The absence of in-situ algal thalli in all but the upper few tens of centimeters of the mounds, however, argues against a purely biological/ecological origin of mounds. A down-stepping ramp model is proposed wherein a muddy algal facies was deposited at the base of the mounds in the low energy of the outer ramp, followed by a grain-rich algal core in the mid-ramp environment. Mounds tops accumulated in an algal bafflestone facies in the inner ramp setting. Restriction of energy due to basinward algal buildup may have also contributed to deposition of algal bafflestone. Mounds accumulated radially at differential rates and were influenced by these variations in energy. This differential deposition of microfacies and subsequent diagenetic alteration have produced heterogeneities in algal reservoir rock, producing algal mound reservoirs that have a high potential for compartmentalization.

No description available.

Master of Music / Department of Music / Frank C. Tracz / This document was submitted to the Graduate School of Kansas State University as a partial requirement for the Master’s of Music Education degree. It contains information about music education philosophy, what defines quality literature, theoretical and historical analyses, and rehearsal plans for each of the three pieces that were performed on the Graduate Student Conducting Recital on Wednesday, March 11, 2009. Selections performed on the recital included in the document’s analysis portion include Four Scottish Dances by Malcolm Arnold, arranged by John Paynter, Mosaic, Op. 30 by Mario Gaetano, and Celebration Fanfare from “Stepping Stones” by Joan Tower, arranged by Jack Stamp. The analytical methods employed in this document and the rehearsal techniques listed are based on the Blocker/Miles unit studies and macro-micro-macro concepts from the Teaching Music Through Performance in Band book series.

This study aims to describe the faunal composition and community structure of the world\'s deepest whale fall and the first found in the South Atlantic Ocean. This discovery adds very important data on the poorly known whale-fall biogeography and provides new insights on the ecological role of the \"bone-eating\" worm Osedax (Polychaeta: Siboglinidae) on associated biota. The whale fall was serendipitously found in April 24th, 2013 at the base of São Paulo Ridge at 4204 m depth in the SW Atlantic Ocean using the HOV Shinkai 6500 during the Brazil-Japan joint Iatá-Piúna Oceanographic Expedition on board RV Yokosuka (Japan Agency for Marine-Earth Science and Technology, JAMSTEC). Detailed video surveys of the carcass were made using high-definition video cameras. Vertebrae, surrounding sediments and fauna were also collected using the submersible manipulators and a slurp gun. The partial skeleton belonged to an Antarctic Minke whale, Balaenoptera bonaerensis, and was composed of nine caudal vertebrae, whose degradation state suggests it was on the bottom for at least 5 years. Most of the 41 invertebrate species found are new to science, with ca. 12% of the genera shared with NE Pacific whale falls, vent and seep ecosystems. This similarity strongly supports the hypothesis that whale falls act as \"stepping-stones\" for the dispersion of chemosynthetic fauna and that some whale-fall specialists are widespread worldwide at genus level. Detailed investigation of inner bone assemblages indicates that Osedax degradation deeply affects their diversity and structure. Bones colonized by Osedax support distinct, significantly more diverse and abundant assemblages. This renders Osedax the status of ecosystem engineer, creating new microhabitats and enhancing biodiversity in deep-sea whale-fall communities. / O presente estudo descreve a composição faunística e a estrutura da comunidade de carcaça de baleia mais profunda do mundo e a primeira a ser encontrada no Oceano Atlântico Sul. A descoberta adiciona dados importantes à quase desconhecida biogeografia destas comunidades, assim como aumenta o conhecimento sobre o papel ecológico dos vermes-zumbis do gênero Osedax (Polychaeta: Siboglinidae), especialistas no consumo e degradação de ossos. A carcaça foi fortuitamente descoberta em 24 de Abril de 2013, na base da Dorsal de São Paulo a 4204 m de profundidade (Atlântico Sudoeste), utilizando-se o submersível de pesquisa tripulado Shinkai 6500 (Agência Japonesa para o Estudo das Ciências do Mar e da Terra e Tecnologia, JAMSTEC na sigla em inglês). Os mergulhos fizeram parte da Expedição Oceanográfica Iatá-Piúna, fruto de um acordo bilateral de cooperação científica em Ciências do Mar entre Brasil e Japão. Durante dois mergulhos foram feitos vídeos detalhados da carcaça através de uma câmera de alta definição. Também foram coletadas vértebras, sedimentos e fauna por meio dos braços manipuladores e de um sugador. O esqueleto parcial pertencia a uma baleia Minke Antártica, Balaenoptera bonaerensis, e era composto por nove vértebras, cujo estado de degradação sugere que a baleia estava no assoalho marinho por pelo menos 5 anos. A maioria das 41 espécies de invertebrados encontradas são novas para a ciência e cerca de 12% dos gêneros são compartilhados com ambientes redutores do Pacífico Nordeste, como carcaças, fontes hidrotermais e exsudações frias. Tal semelhança corrobora fortemente a hipótese de que carcaças de baleia atuam como \"pedras de dispersão\" para a fauna de ambientes quimiossintetizantes e que alguns organismos especialistas de carcaças de baleia possuem distribuição mundial em nível genérico. A investigação detalhada da endofauna dos ossos indicou que a degradação promovida por Osedax afeta profundamente sua diversidade e estrutura. Ossos colonizados por Osedax sustentam assembleias de organismos significativamente mais diversas e abundantes. Isso faz com que Osedax seja considerado um engenheiro ecossistêmico, pois cria novos microhábitats promovendo o aumento da biodiversidade em comunidades de carcaças de baleia no mar profundo.

O objetivo do trabalho é investigar como as condições biomecânicas de portadores de Osteoartrite (OA) de joelho afetam a capacidade de realizar atividades de vida diária. Participaram desse estudo 39 indivíduos, sendo 18 indivíduos com OA de joelho bilateral grau 3, na escala Kellgren Lawrence, e 21 indivíduos saudáveis. Foram utilizadas duas plataformas de força (AMTI) para registrar a Força de Reação do Solo, cinco câmeras (Sistema Vicon) para registrar as variações angulares das articulações do quadril, joelho e tornozelo, nos planos sagital e frontal, e cinco sensores de eletromiografia wireless (Sistema Noraxon) para registrar as atividades dos músculos reto femoris (RF), vastus lateralis (VL), biceps femoris (BF), tibialis anterior (TA) e gastrocnemius lateralis (GL) no segmento dominante (segmento D) dos sujeitos do grupo controle e no segmento com maior gravidade de lesão nos indivíduos com OA (segmento OA). Também foram calculados por meio de dinâmica inversa os momentos articulares nos planos sagital e frontal. Três atividades de vida diária foram investigadas, a marcha, o levantar e sentar em uma cadeira e o descer de um degrau de 20cm. Nos resultados, foi observada uma menor variação angular de forma geral nas articulações do quadril e joelho. Não foi observada diferença nas cargas mecânicas aplicadas ao aparelho locomotor. Nas três atividades cotidianas, os indivíduos com OA apresentaram adução no quadril e abdução no joelho, que denota um alinhamento em valgo durante a execução das tarefas. Poucas diferenças foram observadas nos momentos articulares flexores e extensores, nas três atividades de vida diária investigadas. No levantar e sentar menores momentos extensores foram observados no joelho durante as duas fases do movimento. Nos momentos adutores, poucas diferenças foram observadas na marcha. No levantar e sentar, o segmento OA não apresentou momentos adutores de joelho maiores que nos outros segmentos. No descer degrau, o segmento CL apresentou maior momento adutor que o segmento OA e D. De forma geral, as diferenças na ativação muscular indicam maior intensidade de ativação no grupo controle. O músculo VL nas três atividades apresentou intensidade de ativação menor nos indivíduos com OA. Observou-se maior co-ativação na marcha e no descer degrau, mas não no levantar e sentar. Na marcha a maior co-ativação ocorreu nas três articulações. No descer degrau, ocorreu no quadril e no joelho. Nas três atividades, maior co-contração foi observada e principalmente no joelho. Conclui-se que as alterações na técnica de movimento mostram-se tarefa dependente. As alterações na execução do movimento no plano sagital não foram suficientes para afetar o controle das cargas mecânicas, na marcha e no descer degrau. Apenas na tarefa de levantar e sentar surgiu algum indicio de que a eficiência seria pior. O alinhamento no joelho e os momentos adutores não sugerem maior magnitude de força no compartimento medial do joelho. Aparentemente, as características temporais sejam mais sensíveis à presença da OA no joelho do que a intensidade de ativação / The aim of this study is to investigate the biomechanical characteristics of patients with knee osteoarthritis (OA) and hoe it affects the ability to perform daily living activities. Thirty nine subjects participated in this study, 18 subjects with bilateral knee OA grade 3 Kellgren Lawrence scale) and 21 healthy individuals. Two force platforms (AMTI) were used to register the Grourd Reaction Force (GRF). Five cameras (System Vicon) were used to register the angular variations of the hip, knee and ankle in the sagittal and frontal planes. Five electromyographic electrodes (Noraxon System) were used to record the activities of the rectus femoris (RF), vastus lateralis (VL), biceps femoris (BF), tibialis anterior (TA) and gastrocnemius lateralis (GL) in the dominant segment (D segment) on control group and the segment with greater severity of injury in individuals with OA (OA segment). Inverse dynamics was used to calculate joint moments sagittal and frontal planes. Three daily living activities were investigated, the gait, the Sit-to stand and Stand-to-sit and Stepping down from a 20cm height step. In results, there was a smaller angular variation in hip and knee joints. No difference was observed in the mechanical loads applied to the locomotor system. In the three daily activities, people with knee OA showed hip adduction and knee abduction, in the three daily activities, which suggests an alignment valgus in the knee. Few differences were observed in joint moments in the three daily living activities. In sit-to-stand and stand-to-sit lower peak extensor moments were observed in the knee. Few differences were observed in adductor moments in gait. In sit-to-stand and stand-to-sit, no difference was observed in knee adductor moments. In stepping down, the CL segment showed greater adductor moment than OA segment and D. In general, differences in muscle activation indicate greater activation intensity in the control group. The VL muscle showed lower activation intensity in individuals with OA in all three activities. A higher co-activation was observed in gait and in stepping down, but not in sit-to-stand and stand-to-sit. In gait the higher co-activation occurred subjects with knee OA in the three joints. In stepping down, higher co-activation occurred in the hip and knee. In the three activities, greater co-contraction was observed and especially in the knee. It can be concluded that changes in movement technique appears to be task dependent. Changes in movement technique in the sagittal plane were not enough to affect the control of the mechanical loads on gait and stepping down movements. Only in sit-to-stand and stand-to-sit some indication of worse efficiency to perform the task was observed. Knee alignment and knee adductor moments do not suggest greater magnitude of force in the medial compartment of the knee. Apparently, the temporal characteristics of muscle activity are more sensitive to the presence of knee OA than the intensity of activation

This study aims to describe the faunal composition and community structure of the world\'s deepest whale fall and the first found in the South Atlantic Ocean. This discovery adds very important data on the poorly known whale-fall biogeography and provides new insights on the ecological role of the \"bone-eating\" worm Osedax (Polychaeta: Siboglinidae) on associated biota. The whale fall was serendipitously found in April 24th, 2013 at the base of São Paulo Ridge at 4204 m depth in the SW Atlantic Ocean using the HOV Shinkai 6500 during the Brazil-Japan joint Iatá-Piúna Oceanographic Expedition on board RV Yokosuka (Japan Agency for Marine-Earth Science and Technology, JAMSTEC). Detailed video surveys of the carcass were made using high-definition video cameras. Vertebrae, surrounding sediments and fauna were also collected using the submersible manipulators and a slurp gun. The partial skeleton belonged to an Antarctic Minke whale, Balaenoptera bonaerensis, and was composed of nine caudal vertebrae, whose degradation state suggests it was on the bottom for at least 5 years. Most of the 41 invertebrate species found are new to science, with ca. 12% of the genera shared with NE Pacific whale falls, vent and seep ecosystems. This similarity strongly supports the hypothesis that whale falls act as \"stepping-stones\" for the dispersion of chemosynthetic fauna and that some whale-fall specialists are widespread worldwide at genus level. Detailed investigation of inner bone assemblages indicates that Osedax degradation deeply affects their diversity and structure. Bones colonized by Osedax support distinct, significantly more diverse and abundant assemblages. This renders Osedax the status of ecosystem engineer, creating new microhabitats and enhancing biodiversity in deep-sea whale-fall communities. / O presente estudo descreve a composição faunística e a estrutura da comunidade de carcaça de baleia mais profunda do mundo e a primeira a ser encontrada no Oceano Atlântico Sul. A descoberta adiciona dados importantes à quase desconhecida biogeografia destas comunidades, assim como aumenta o conhecimento sobre o papel ecológico dos vermes-zumbis do gênero Osedax (Polychaeta: Siboglinidae), especialistas no consumo e degradação de ossos. A carcaça foi fortuitamente descoberta em 24 de Abril de 2013, na base da Dorsal de São Paulo a 4204 m de profundidade (Atlântico Sudoeste), utilizando-se o submersível de pesquisa tripulado Shinkai 6500 (Agência Japonesa para o Estudo das Ciências do Mar e da Terra e Tecnologia, JAMSTEC na sigla em inglês). Os mergulhos fizeram parte da Expedição Oceanográfica Iatá-Piúna, fruto de um acordo bilateral de cooperação científica em Ciências do Mar entre Brasil e Japão. Durante dois mergulhos foram feitos vídeos detalhados da carcaça através de uma câmera de alta definição. Também foram coletadas vértebras, sedimentos e fauna por meio dos braços manipuladores e de um sugador. O esqueleto parcial pertencia a uma baleia Minke Antártica, Balaenoptera bonaerensis, e era composto por nove vértebras, cujo estado de degradação sugere que a baleia estava no assoalho marinho por pelo menos 5 anos. A maioria das 41 espécies de invertebrados encontradas são novas para a ciência e cerca de 12% dos gêneros são compartilhados com ambientes redutores do Pacífico Nordeste, como carcaças, fontes hidrotermais e exsudações frias. Tal semelhança corrobora fortemente a hipótese de que carcaças de baleia atuam como \"pedras de dispersão\" para a fauna de ambientes quimiossintetizantes e que alguns organismos especialistas de carcaças de baleia possuem distribuição mundial em nível genérico. A investigação detalhada da endofauna dos ossos indicou que a degradação promovida por Osedax afeta profundamente sua diversidade e estrutura. Ossos colonizados por Osedax sustentam assembleias de organismos significativamente mais diversas e abundantes. Isso faz com que Osedax seja considerado um engenheiro ecossistêmico, pois cria novos microhábitats promovendo o aumento da biodiversidade em comunidades de carcaças de baleia no mar profundo.