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This thesis deals with an axle design for an autonomous minibus. The theoretical part is about axles then the next one goes over the given parameters. Following with a selection of suitable parts for use and designs of parts for production. This chapter is also about geometry and driving characteristics analyzation. The next chapters are devoted to the calculations of the loads on the lower arm, its design and static analysis. The last chapter combines all the parts together into a conceptual design.

京都大学 / 0048 / 新制・課程博士 / 博士(農学) / 甲第21157号 / 農博第2283号 / 新制||農||1059(附属図書館) / 学位論文||H30||N5131(農学部図書室) / 京都大学大学院農学研究科森林科学専攻 / (主査)教授 吉村 剛, 教授 髙野 俊幸, 教授 梅澤 俊明 / 学位規則第4条第1項該当 / Doctor of Agricultural Science / Kyoto University / DFAM

A Research Report submitted to the Faculty of Health Sciences, University of the Witwatersrand Gauteng, 2017 / Background Soccer is a sport that is gaining in popularity in the elite and non-elite populations worldwide. As a result, the number of injuries in soccer is increasing. Hamstring injuries in particular, with a reported incidence rate as high as 63%, are of significant concern. Most hamstring injuries tend to occur during the swing phase of sprinting when hamstring activity is at its highest. As the speed of sprinting increases, greater mobility in the lumbo-pelvic area is required to maximise sprinting efficiency. Any abnormal or dysfunctional lumbo-pelvic movement during this phase could induce pain and hamstring injury. Lumbo-pelvic movement control dysfunction may therefore indirectly link abnormal lumbar spine movement to lumbo-pelvic pain and hamstring injury. The first aim of this study was to compare the performance of the erector spinae, gluteus maximus, hamstrings (biceps femoris) and quadriceps (rectus femoris) muscles in soccer players, with and without recent hamstring injuries, while performing isometric contractions, a functional squat and sprinting. The study’s second aim was to compare lumbo-pelvic movement control in soccer players with and without recent hamstring injuries. Method Thirty soccer players were selected to participate in this study. Fifteen were assigned to the injured group and 15 to an uninjured group. The injured group comprised players who had sustained a hamstring injury six months prior to the research and who had partially returned to training, and the uninjured group comprised players with no recent hamstring injuries and who were actively involved in full training. Players were matched in respect of age, height, weight and playing position. All players gave informed written consent, completed the physical activity, training and injury questionnaire, and the Oslo hamstring injury questionnaire. Physical tests, which included isometric contraction of the erector spinae, gluteus maximus, hamstrings (biceps femoris) and quadriceps (rectus femoris) muscles, a functional squat and a thirty-metre sprint were done. Muscle activity during these tests was recorded via electromyography (EMG). To determine the lumbo-pelvic movement control of the players, the dorsal pelvic tilt, waiter’s bow, one leg stand and prone knee bend tests were used. Cohen's d (parametric) and Spearman’s correlation coefficient (nonparametric) were used to calculate the effect size, and the Chi-square test and Fisher’s exact to analyse the lumbopelvic movement control data. To establish a statistical significance, the p-value of the study was set at p<0.05. Results EMG muscle activity during isometric contractions was lower in the erector spinae muscles (p=0.04) and biceps femoris muscle (p=0.02) of the injured group. Both these findings were statistically significant. There was no statistically significant difference in muscle activity during the functional squat between the study and uninjured groups. The results of the EMG activity in the thirty-metre sprint were determined to be significant as they demonstrated that the hamstring muscle (p=0.01) activation in the injured group was decreased in comparison with the uninjured group. During the performance of the lumbo-pelvic test, no association was found between the two groups in the dorsal pelvic tilt and one leg stand. The performance of the waiter’s bow (p=0.01) and prone knee bend (p=0.004) revealed statistically significant differences between the study and uninjured groups. The majority of the players in the injured group performed both of these functional tests incorrectly (WB n=10; PKB n=14). Conclusion The study found that the hamstring muscle is at great risk of injury during eccentric contraction of the hamstring muscles. This can be associated with poor lumbo-pelvic movement control, as the load on the hamstring muscle is increased to provide intersegmental stability around the neutral zone, the area of high spinal flexibility. / MT2017

The habitat requirements of shovelnose sturgeon populations are unknown for the lower Mississippi River. Active acoustic telemetry was used to measure temporal variation in habitat use of shovelnose sturgeon and preference for depth, surface current velocity, and riverbed rugosity and slope by the population and within sandbar microhabitats. Shovelnose sturgeon occupied habitats differently throughout the year; and, within habitats, areas of moderate depth and surface current velocity and smooth riverbed were preferred. Within sandbars, environmental conditions did not differ from the surrounding environment, yet frequent aggregations of individuals in the lower portion of sandbars often in close proximity suggest habitat preference at a scale greater than the 5 ha measured. Results of this study provide information on seasonal habitat use patterns and methods that can be applied to a long-term dataset to identify the habitat requirements of shovelnose sturgeon.

Interpreting the tectonic significance of high strain zones requires detailed knowledge of the P-T-t-D history of rocks on either side and of tectonized rocks within the shear zone. In-situ monazite geochronology is particularly useful because it generates a time-integrated framework of metamorphism and fabric development. This can be achieved by correlating monazite compositional domains with the growth and consumption of major phases. Furthermore, monazite can be a fabric forming mineral, and can be directly linked to structural fabrics and kinematics. The Cora Lake shear zone (CLsz) represents a major lithotectonic discontinuity within the deep crustal Athabasca Granulite terrain, and preserves intense mylonitic to ultramylonitic fabrics. The 3-5 km wide CLsz strikes ~231°, and dips ~62° to the Northwest, has a moderately plunging stretching lineation (SW trend) with abundant sinistral kinematic indicators. These data indicate oblique extension with NW hanging wall down and to the SW relative to the SE footwall. The NW hangingwall is dominated by the ca. 2.6 Ga charnockitic Mary batholith. The southeastern footwall is primarily underlain by the heterogeneous ca. 3.3-3.0 Ga Chipman tonaite straight gneiss. Although both share common Archean (ca. 2.55 Ga) and Paleoproterozoic (ca. 1.9 Ga) deformation events, the style and P-T conditions of deformation are different. The earliest phase of deformation within the NW hangingwall consists of a penetrative subhorizontal flow fabric at 0.9 GPa and ~725°C (2.56 Ga), but folding in the SE footwall associated with the development of a strong upright axially planar fabric at 1.35 GPa and 850°C. Deformation at ca 1.9 Ga was characterized by upright folding, similar in orientation, in both hangingwall (0.9 GPa; 725°C) and footwall (1.17 GPa; 825°C). Deformation related to the CLsz occurred at 1880 Ma (0.9-1.06 GPa; ~775°C), and is responsible for juxtaposing two levels of lower crust. The Cora Lake shear zone is interpreted to be the culmination of a trend of increased strength, localization, strain partitioning, and vertical coupling. Furthermore, the CLsz overprints fabrics from each wall, marks the development of a major lateral lithotectonic discontinuity, and an introduction of major structural and compositional heterogeneity within the lower continental crust.

<p> The Lower Cretaceous (Upper Albian) Viking Formation of central Alberta contains numerous linear sandbodies and fewer large irregularly-shaped sandbodies. Most studies to date have focused on individual sandbodies, leaving their interrelationships largely unknown. Developing a high-resolution allostratigraphy for the Viking of central Alberta allows mapping of regional bounding discontinuities and the definition of distinct allomembers. Placement of the Viking hydrocarbon fields within this framework permits an understanding of the exact stratigraphic relationships of the various fields. </p> <p> Examination of 120 cores and numerous well log correlations suggests the existence of four regionally mappable bounding discontinuities (BDl-4) which separate five distinct allomembers (I-V). Sandbodies within these allomembers were deposited in a variety of sedimentologically distinct environments. These include 'regional Viking' offshore to shoreface sandstones, prograding highstand shoreface sediments, transgressive incised shoreface sediments, and forced regressive, onlapping shoreface 'tongues'. The series of linear trending hydrocarbon fields from Joffre to Chain are also stratigraphically distinct. The sandbodies exist at five separate stratigraphic horizons and therefore are not all part of the same incised shoreface deposits. </p> <p> The four regional bounding discontinuities are interpreted as transgressive surfaces of erosion formed by four separate drops and subsequent rises of relative sea level. These fluctuations were greater than 30m and each complete cycle occurred over roughly 375,000 years. </p> / Thesis / Master of Science (MSc)

Lower back pain (LBP) is a medical condition that will affect most of us at some point in our lives. Several medical causes have been identified for LBP, yet the large majority of LBP patients do not receive a specific diagnosis. These patients use up a large majority of health care resources, and accumulate billions of dollars in medical costs in countries throughout the globe. In recent years, an increasing focus has been placed on the idea that aquatic therapy may be an effective therapy for LBP patients. Exercise therapy has already proven itself as an effective means for treating LBP. Thus, combined with the unique properties of water, experts believe that aquatic therapy is the future of LBP treatment. This thesis aims to explore the efficacy of aquatic therapy as a treatment for LBP. Through the analysis of controlled peer-reviewed studies, scholarly information databases, and historical data on LBP treatment, this thesis evaluates the relationship between aquatic therapy and LBP in its entirety. Scientific properties of water have shown its many uses in rehabilitative therapy treatments. Water, in theory, is able to manipulate the exercise environment to allow for more substantial progress to be made. In studies where aquatic therapy was tested versus no treatment, aquatic therapy proved to be a more efficient and effective option. Still, when placed against other therapies, aquatic therapy did not always prove more effective. While the analyzed studies support the idea that aquatic therapy is an effective treatment for LBP, further research is needed to determine how aquatic therapy holds up against other forms of treatment.

No description available.