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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

Capillary Filling of Large Aspect Ratio Channels With Varying Wall Spacing

Murray, Dallin B. 02 July 2013 (has links) (PDF)
Quantification and prediction of capillary fluid flow in planar nanochannels is essential to the development of many emerging nanofluidic technologies. Planar nanochannels are typically produced using the standard nanofabrication processes of thermal bonding or sacrificial etching. Both approaches may yield nanochannels that are bowed and/or exhibit non-uniform (i.e. non-planar) wall spacing. These variations in wall spacing affect the transient dynamics of a liquid plug filling the nanochannel, causing deviations from the classical behavior in a parallel-plate channel as described by the Washburn model. Non uniform wall spacing impacts the overall frictional resistance and influences the meniscus curvature. In this thesis, a new analytical model that predicts the meniscus location over time in micro- and nanochannels as a function of channel height was compared to experimental filling data of well-characterized channels with different heights. The wall-to-wall spacing of the utilized nanochannels exhibited height variations between 60 and 300 nm. The model was also validated with microscale channels that were fabricated with a linear variation in the wall-to-wall spacing from 100 µm to 400 µm. The filling speed and meniscus shape during the filling process were determined by dynamic imaging of the meniscus front for several different liquids. A modified Washburn equation that utilizes an effective channel height to predict the filling speed corresponding to the location of the tallest height within a channel was derived. A model was also developed to predict the meniscus distortion encountered in a non-constant height channel, provided the cross-sectional channel heights and the distance from the channel entrance are known. The models developed herein account for induced transverse pressure gradients created by non-constant channel heights. The models are compared to experimental data derived from both nanoscale and microscale channels with good qualitative agreement. These results demonstrate that the capillary flow in nanochannels with non-parallel-plate, linear tapered, or parabolic cross sections can be predicted.
2

A Fast Model For Computing Infrared Atmospheric Background Effects

Sivasligil, Mustafa 01 January 2006 (has links) (PDF)
The infrared atmospheric background modeling can be considered as one of the important key factor to develop a successful target detection technique. During the infrared atmospheric background modeling, defining the input parameters of the atmospheric profile are very important for the calculations of the absorption, emission and scattering effects of the atmosphere. The main objective of this thesis is to find the answer for the question &ldquo / is it possible to determine the &ldquo / effective&rdquo / height range for the sea level midlatitude clear weather conditions in the three special wavelength bands, 1-3 &amp / #61549 / m, 3-5 &amp / #61549 / m, 8-12 &amp / #61549 / m ?&rdquo / . The answer is important for three cases. These are to overcome the difficulties of finding all the parameters of the new atmospheric profile, to determine the dominant height range for the midlatitude region, and to shorten the time of the calculations of infrared background processes. In this study, it has been shown that it should be possible to determine the effective height range for sea level midlatitude clear weather conditions in the three special wavelength bands. As a result of this study it is shown that a new atmosphere model can be constructed more easily by overcoming the difficulties of finding all the parameters of the new atmospheric profile for the sea level clear weather midlatitude regions in a short time respectively. In this study the infrared radiation flux below 5 % difference between the whole, 100 km, and the effective height ranges is accepted.

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