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Mechanistic study of menisci motion within homogeneously and heterogeneously wet porous mediaMotealleh, Siyavash 19 October 2009 (has links)
Oil reservoirs and soil can be homogeneously wet (water-wet, oil-wet, neutralwet)
or heterogeneously wet (mixed wet or fractionally wet). The goal of this research is
to model the detailed configuration of wetting and non-wetting phases within
homogeneously and heterogeneously wet porous media. We use a dense random pack of
equal spheres as a model porous medium. The geometry of the sphere pack is complex
but it is known.
In homogeneously wet porous media we quantify the effect of low saturations of
the wetting phase on the non-wetting phase relative permeability by solving analytically
the geometry of the wetting phase. At low saturations (at or near the drainage endpoint)
the wetting phase exists largely in the form of pendular rings held at grain contacts. Pore
throats correspond to the constriction between groups of three grains, each pair of which
can be in contact. Thus the existence of these pendular rings decreases the void area available for the flowing non-wetting phase. Consequently, the existence of the pendular
rings decreases the permeability of non-wetting phase. Our model explains the significant
permeability reduction of the non-wetting phase with a small change in the wetting phase
in a low permeability porous medium.
To model heterogeneously wet porous medium, we assume that the porous
medium is fractionally wet where each grain is either oil-wet or water-wet. These waterwet
or oil-wet grains are distributed randomly within the porous medium. We calculate
analytically the stable fluid configuration in individual pores and throats of a fractionally
wet medium. The calculation is made tractable by idealizing the configurations as locally
spherical (menisci) or toroidal (pendular rings.) Because the calculation of the interface
position is entirely local and grain-based, it provides a single, generalized, geometric
basis for computing pore-filling events during drainage as well as imbibition. This
generality is essential for modeling displacements in fractionally wet media. Pore filling
occurs when an interface becomes unstable in a pore throat (analogous to the Haines
condition for drainage in a uniformly wet throat), when two or more interfaces come into
contact and merge to form a single interface (analogous to the Melrose condition for
imbibition in uniformly wet medium), or when a meniscus in a throat touches a nearby
grain (a new stability criterion). The concept of tracking the fluid/fluid interfaces on each grain means that a
traditional pore network is not used in the model. The calculation of phase saturation or
other quantities that are conveniently computed in a network can be done with any
approach for defining pore bodies and throats. The fluid/fluid interfaces are mapped from
the grain-based model to the network as needed. Consequently, the model is robust as
there is no difference in the model between drainage and imbibition, as all criteria are
accounted for both increasing and decreasing capillary pressure. / text
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Low temperature wet oxidation and catalytic wet oxidation of specific organic compounds in highly alkaline solution (synthetic Bayer liquor)Tardio, James Andrew, james.tardio@rmit.edu.au January 2002 (has links)
Low temperature (165°C) Wet Oxidation (WO) and Catalytic Wet Oxidation (CWO) of 12 organic compounds has been studied in highly alkaline, high ionic strength solution (simulating that encountered in the Bayer process used to refine alumina) for the first time. Most (11 out of 12) of the 12 organic compounds studied (formic, acetic, propionic, butyric, oxalic, malonic, succinic, glutaric, citric, lactic, malic and tartaric acids) have been identified in various worldwide Bayer liquors. The various aspects of WO and CWO studied for each of the above-mentioned compounds were as follows; -Extent of complete oxidation to carbonate (i.e. extent of removal of organic compound) -Extent of overall oxidation (i.e. extent of complete oxidation and partial oxidation to stable products) -The product(s) formed from partial (incomplete) oxidation -The reaction mechanism occurring -Why certain compounds undergo low temperature WO and/or CWO in highly alkaline, high ionic strength solution -The ability of various transition metal oxides to catalyse the WO of the selected organic compounds Of the 12 organic compounds studied only six (formic, malonic, citric, lactic, malic and tartaric acids) underwent appreciable (>2% overall oxidation) WO in isolation under the reaction conditions used (4.4 -7.0 M NaOH, 165°C, 500 kPa Po₂, 2 hours). Each of these six compounds underwent some complete oxidation and therefore can be partly removed from highly alkaline, high ionic strength solution using low temperature WO. The order of extent of complete oxidation determined was as follows tartaric> citric> malonic> formic> lactic> malic. All of these compounds also underwent some partial oxidation under the reaction conditions used, excluding formic acid, which only underwent complete oxidation. Oxalic acid was a major product of partial oxidation of all of the above-mentioned compounds (excluding formic acid), while acetic acid was a major product of partial oxidation of citric, lactic, malic and tartaric acids. The WO of formic, malonic, citric, lactic, malic and tartaric acids varied considerably with NaOH concentration over the NaOH concentration range studied (4.4 - 7.0 M). The extent of overall oxidation undergone by each of these compounds increased significantly with increasing NaOH concentration. All of the compounds that underwent appreciable WO under the reaction conditions studied contained hydrogen(s) significantly more acidic then the compounds that did not undergo appreciable WO, thus indicating that only organic compounds that contain acidic (albeit weakly acidic) hydrogens undergo low temperature (165°C) WO in highly alkaline, high ionic strength solution. Two different reaction mechanisms were identified to occur during low temperature WO in highly alkaline, high ionic strength solution. Malonic and formic acids underwent WO predominantly via a free radical based reaction mechanism, while citric, lactic, malic and tartaric acids underwent WO predominantly via an ionic based reaction mechanism. The six organic compounds that did not undergo appreciable WO in isolation (acetic, propionic, butyric, oxalic, succinic and glutaric acids) all underwent appreciable WO when in the presence of malonic acid undergoing low temperature WO. Hence, low temperature WO of all of the above-mentioned compounds can be initiated by free radical intermediates produced by malonic acid undergoing WO in highly alkaline, high ionic strength solution. The ability of several transition metal oxides to catalyse the WO of the chosen 12 organic compounds was investigated. Of the transition metal oxides studied CuO was clearly the most active. Five of the organic compounds studied (malonic, citric, lactic, malic and tartaric acids) were catalytically wet oxidised by CuO in highly alkaline, high ionic strength solution in isolation. The order of catalytic activity observed was malonic > tartaric> lactic> malic> citric. Two different catalytic reaction mechanisms were identified for CuO catalysed WO in highly alkaline solution for the organic compounds studied. CuO catalysed the WO of malonic acid predominantly by catalysing the formation of free radical intermediates. CuO catalysed the WO of citric, lactic, malic and tartaric acids predominantly via a complexation-based reaction mechanism.
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Vrouefigure in Reza de Wet se drama-oeuvreVan der Wal, Hester Rossly 30 November 2005 (has links)
The central problem of this thesis is the situation of women in Reza De Wet's dramatic-oeuvre, and their yearning to escape from unacceptable circumstances. Chapter 1 deals with the historical background of the changing position of women in South African history, and indicates De Wet's dramatic oeuvre as the climax of this genre in the eighties. Chapters 2 and 3 deal with the female characters of Vrystaat-trilogie and Trits: Mis, Mirakel, Drif. Within the central problem, this study focuses on an ongoing liberation process which reaches its climax in Trits. Chapter 4 (A Russian trilogy) investigates the inner liberation process of female characters before and after the Russian Revolution, and focuses on their yearning for a better future. The conclusion of this thesis is that De Wet, by making use of concepts like intertextuality and fantasy, succeeded in deconstructing the image of a mythical Afrikaans countryside portrayed in earlier literature. Simultaneously the ongoing theme of an inner liberation takes place in the lives of most of the female characters throughout De Wet's dramatic oeuvre / Afrikaans & Theory of Literature / M.A. (Afrikaans)
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Wet/Dry Mapping - Reference Map (36x48)Underwood, Brian 06 1900 (has links)
A poster sized map that shows labeled sections of the Agua Fria River to assist volunteers in collecting data for the annual Wet/Dry Mapping event.
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Wet/Dry Mapping - 2011 Wet/Dry MapUnderwood, Brian 07 1900 (has links)
A map of the wet and dry segments along the Agua Fria River in 2011.
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Wet/Dry Mapping - 2011 Wet/Dry Map (with Isolated Pools)Underwood, Brian 07 1900 (has links)
A map of the wet and dry segments along the Agua Fria River in 2011.
**Note: This map contains point locations of the isolated pools documented along the Agua Fria River in 2011.
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Wet/Dry Mapping - Wet/Dry Comparison Map w/Pie Charts (2008-2011)Underwood, Brian 07 1900 (has links)
An 8.5x11 map showing the wet and dry segments of the Agua Fria River for years 2008-2011. For each year, the map also contains pie charts of the perentage wet and percetage dry portions of the river.
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Wet/Dry Mapping - 2011 Observation MapUnderwood, Brian 07 1900 (has links)
A poster sized map (36"x48") of the wildlife, anthropogenic, and invasive species observations made along the Agua Fria River in 2011.
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Wet/Dry Mapping - Wet/Dry Comparison Map (2008-2010)Underwood, Brian 07 1900 (has links)
A comparison map showing Wet/Dry data along the Agua Fria River for years 2008-2010.
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Wet/Dry Mapping - Wet/Dry Comparison Map w/Pie Charts (2008-2010)Underwood, Brian 07 1900 (has links)
A comparison map showing Wet/Dry data for years 2008-2010. **Note this map includes pie charts to show a numerical percentage of how much of the river area surveyed is wet and how much is dry.
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