Browsing by Subject "displacement"
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Item Experimental examination of wire mesh dampers subjected to large amplitude displacements(2009-06-02) Jones, Adam MatthewWire mesh dampers are under investigation because they are seen as replacements for squeeze film dampers as a source of direct stiffness and damping at bearing locations. There are several advantages of wire mesh dampers over squeeze film dampers, including: temperature insensitivity, oil-free operation, and the ability to contain large amplitude vibrations. Furthermore, due to their direct damping and lack of cross-coupled stiffness, the wire mesh reduces the response to imbalance and increases the stability of the system. The objective of this research was to determine the properties of wire mesh dampers under large amplitude vibrations. Impact testing was first conducted on the wire mesh as a means of obtaining the large amplitudes that were of interest. Next, to verify the results, a second methodology was employed using shaker testing. It was found that both the stiffness and hysteretic damping decrease with increasing displacement. However, they both approached asymptotes around 2 mils of displacement, and further increases in displacement had significantly less effect on the properties. Once the results were verified to be consistent, equations were obtained to describe the response of the wire mesh dampers. These equations were then used to create a new design workbook, which would allow an engineer to determine the properties of wire mesh dampers under conditions that they might experience.Item Selected growth and interaction characteristics of seafloor faults in the central Mississippi Canyon Offshore Continental Shelf (OCS) area, northern Gulf of Mexico(Texas A&M University, 2006-08-16) Wegner, Scott AshleyThe characteristics of some shallow faults in the Gulf of Mexico interpreted to be active are poorly understood. A better understanding of these faults will increase our understanding of formerly and presently active geologic processes in the Gulf. Specifically, the characteristics of growth, interaction, and linkage of faults are of interest. Most of the Gulf has seen continuous clastic sediment deposition since the end of continental rifting in the middle Mesozoic. The Gulf is a tectonically quiescent basin, with the only major structural processes being salt diapirism and subsidence. Numerous styles of faulting have been observed in the Gulf, with each style being related to a specific type of deformation. Numerous authors have concluded that fault growth processes generally involve tipline propagation and linkage of faults. Evidence of these processes has been observed in seismic data sets. This investigation uses a HR 3-D seismic data set to characterize growth, interaction, and linkage of a fault set in the northern Gulf of Mexico. This work shows that linked and interacting faults are present in the study area. These conclusions were reached using measurements of throw on horizons offset by several faults and interpreting the throw data using a model of fault growth and interaction based on separate processes of growth by tipline propagation and growth by linkage of smaller faults. The ratio of these parameters for a fault population can be described by a power law relationship. For the fault set considered here, the power law was found to be valid.