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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
1

Programmable voltage reference generator for a SAR-ADC

Mylonas, Georgios January 2013 (has links)
SAR-ADCs are very popular and suitable for conversions up to few tens of MHz with 8 to 12 bits of resolution. A very popular type is the Charge Redistribution SAR-ADC which is based on a capacitive array. Higher speeds can be achieved by using the interleaving technique where a number of SAR-ADCs are working in parallel. These speeds, however, can only be achieved if the reference voltage can cope with the switching of the capacitive array. In this thesis the design of a programmable voltage reference generator for a Charge Redistribution SAR-ADC was studied. A number of architectures were studied and one based on a Current Steering DAC was chosen because of the settling time that could offer to the Charge Redistribution SAR-ADC switching operation. This architecture was further investigated in order to spot the weak points of the design and try to minimize the settling time. In the end, the final design was evaluated and possible trimming techniques were proposed that could further speed up the design.
2

The Structure of the Agulhas Current System during the Agulhas Undercurrent Experiment

Casal, Tania Gil Duarte 08 April 2008 (has links)
The Agulhas Undercurrent Experiment took place in February-March 2003 off the east coast of South Africa and included 112 CTD and LADCP casts along four cross-slope sections and three offshore sections. Direct absolute velocities in the Agulhas Current show a narrow and swift current, 180 km wide and up to 2 m s-1 in speed, that deepens as it flows south, eventually detaching from the continental slope at 36ºS. Results also show the northward Agulhas Undercurrent against the continental slope, beneath the Agulhas Current with peak velocities of 10 cm s-1. Several mesoscale cyclonic eddies extending down to the intermediate layer were sampled during the survey, in particular a shear-edge eddy inshore of the Agulhas Current at 36ºS. A deep water anticyclonic eddy was found for the first time in this region centered at 2800 m in the northward flowing North Atlantic Deep Water (NADW) layer. Anomalous water properties reveal that it was formed in the Agulhas Retroflection region and may have been generated by the coupling of a deep Agulhas Ring with the NADW slope current in the SE Atlantic and later entrained into the deep flow of the Agulhas Return Current, until ejected in the Agulhas Current region by localized recirculations in the deep layers of the Agulhas Current system. An inverse model was applied to the hydrographic and LADCP data; results show that the Agulhas Current had a considerably higher transport of 103 Sv at the historical 32ºS section than earlier estimates, consistent with altimetry time series for the region. The growth of the Agulhas Current transport is given primarily by the Sverdrup transport from the supergyre connecting the southern Pacific and Indian Oceans, and the Indonesian Throughflow and Indian Ocean overturning need to be included to account for the total transport. The bulk of the Agulhas Current transport is concentrated in the thermocline layer in the cross-sections and in the intermediate layer in the offshore sections. Inshore of the Agulhas Current core, mixing is inhibited from the surface to the thermocline layers, with no transport growth downstream. Cross-stream mixing does appear to occur in the intermediate layer. The Mozambique Channel and East Madagascar Current appear to have similar contributions as sources to the Agulhas Current at the northern most section of 16 Sv each, with the Indian Ocean wind-driven sub-gyre contribution increasing as the current flows southward. In the intermediate layer, Red Sea Water is actively mixing with Antarctic Intermediate Water when eddies are present. Red Sea Water appears to advect in the form of parcels and not as a continuous flow. Results also suggest the occurrence of small localized recirculations in the deep layers. In the deepest layer of lower NADW the flow is upwelling into the overlaying layer due to the shallowing topography at the northern most section.
3

Posouzení možností regulace napětí v distribučních sítích nn / Evaluation of possibilities for voltage control in a LV distribution network

Bolgár, Robert January 2013 (has links)
This paper deals with possible ways of voltage regulation. Theoretical part includes a search of published methods and the available voltage regulators. Acquired theoretical knowledge has been applied in the development of mathematical models of two selected controllers applied to the testing network. The result of this work is a summary of the outcomes of dynamic simulations with two selected regulators at various locations in testing network. Comparing the results of dynamic simulation for two selected states was chosen the most appropriate regulator and its optimal location in testing network.

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