3 resultados para Surface active agents
em Digital Commons - Michigan Tech
Resumo:
The proposed work aims to facilitate the development of a microfluidic platform for the production of advanced microcapsules containing active agents which can be the functional constituents of self-healing composites. The creation of such microcapsules is enabled by the unique flow characteristics within microchannels including precise control over shear and interfacial forces for droplet creation and manipulation as well as the ability to form a solid shell either chemically or via the addition of thermal or irradiative energy. Microchannel design and a study of the fluid dynamics and mechanisms for shell creation are undertaken in order to establish a fabrication approach capable of producing healing-agent-containing microcapsules. An in-depth study of the process parameters has been undertaken in order to elucidate the advantages of this production technique including precise control of size (i.e., monodispersity) and surface morphology of the microcapsules. This project also aims to aid the optimization of the mechanical properties as well as healing performance of self-healing composites by studying the effects of the advantageous properties of the as-produced microcapsules. Scale-up of the microfluidic fabrication using parallel devices on a single chip as well as on-chip microcapsule production and shape control will also be investigated. It will be demonstrated that microfluidic fabrication is a versatile approach for the efficient creation of functional microcapsules allowing for superior design of self-healing composites.
Resumo:
Celebrity participation in humanitarianism and politics has received a lot of attention in recent times. Though many researchers have sought to explain the reasons underlying this phenomenon, there appears to be little information as to the efficacy of these celebrity efforts. The present research thus undertakes an analysis of the celebrity's participation through a study on the effectiveness of the celebrity-led campaign. To achieve this, I conduct a discourse and visual analysis of media publications surrounding two celebrity-led campaigns. The research leans heavy on theories underlining the celebrity mechanism and Street et al's framework on celebrity participation in politics. The study confirms Street et al's argument that performance, legitimacy and organization are central to the success of the celebrity-led campaign. For campaigns aimed at initiating policy change, I propose an additional category of stakeholders' response which provides a means of evaluating efficacy. My findings show that organization, legitimization, stakeholders' response and performance are highly dependent on the actions of the lead celebrity, making these celebrities active agents in the production of discourse on the "third world". As celebrities engage in humanitarian work, they take up positions as representatives of the aid recipient. The result is the dispossession and silencing of the aid recipient. Out of my discussion of these practices evolves the concept of the celebrity burden.
Resumo:
Volcán Pacaya is one of three currently active volcanoes in Guatemala. Volcanic activity originates from the local tectonic subduction of the Cocos plate beneath the Caribbean plate along the Pacific Guatemalan coast. Pacaya is characterized by generally strombolian type activity with occasional larger vulcanian type eruptions approximately every ten years. One particularly large eruption occurred on May 27, 2010. Using GPS data collected for approximately 8 years before this eruption and data from an additional three years of collection afterwards, surface movement covering the period of the eruption can be measured and used as a tool to help understand activity at the volcano. Initial positions were obtained from raw data using the Automatic Precise Positioning Service provided by the NASA Jet Propulsion Laboratory. Forward modeling of observed 3-D displacements for three time periods (before, covering and after the May 2010 eruption) revealed that a plausible source for deformation is related to a vertical dike or planar surface trending NNW-SSE through the cone. For three distinct time periods the best fitting models describe deformation of the volcano: 0.45 right lateral movement and 0.55 m tensile opening along the dike mentioned above from October 2001 through January 2009 (pre-eruption); 0.55 m left lateral slip along the dike mentioned above for the period from January 2009 and January 2011 (covering the eruption); -0.025 m dip slip along the dike for the period from January 2011 through March 2013 (post-eruption). In all bestfit models the dike is oriented with a 75° westward dip. These data have respective RMS misfit values of 5.49 cm, 12.38 cm and 6.90 cm for each modeled period. During the time period that includes the eruption the volcano most likely experienced a combination of slip and inflation below the edifice which created a large scar at the surface down the northern flank of the volcano. All models that a dipping dike may be experiencing a combination of inflation and oblique slip below the edifice which augments the possibility of a westward collapse in the future.