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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.
11

Salt intrusion and circulation changes in the Eastmain River estuary, James Bay, subsequent to a large reduction of the fresh water discharge

Lepage, Serge. January 1984 (has links)
No description available.
12

Novel methodology for assessing phytoplankton response to pCO2 enrichment in fresh and saltwater

Gifford, Susan B 21 July 2011 (has links)
Atmospheric CO2 emissions are on the rise and are expected to reach 780 parts per million by the year 2100. Research investigating the impacts of increasing CO2 is a relatively new field and the response of phytoplankton communities is largely unknown, especially in coastal and freshwater ecosystems where no CO2 manipulation studies have completed. The present study attempts to encourage uniformity in methods utilized in CO2 perturbation studies and identifies changes in phytoplankton abundance in freshwater (James River) and coastal ocean (Atlantic, Cape Hatteras) sites. A novel bubbling method to manipulate pCO2 was compared with the classic method of acid addition in conjunction with laboratory and in situ experiments. The novel and classic methods were equally effective at manipulating carbonate chemistry to predicted levels. However, the laboratory experiment saw greater variation in both pCO2 levels and chlorophyll-a concentrations throughout the four-day incubation period. The results from the present study encourage use of the novel methodology in combination with in situ experimental setup to assess changes in phytoplankton communities as a result of pCO2 enrichment. This pairing will allow greater replication of small volume incubations without introducing new abiotic conditions such as temperature and light. Additionally this study found no significant treatment effect on phytoplankton communities in either freshwater James River or coastal Atlantic.
13

Discontinuous Galerkin (DG) methods for variable density groundwater flow and solute transport

Povich, Timothy James 30 January 2013 (has links)
Coastal regions are the most densely populated regions of the world. The populations of these regions continue to grow which has created a high demand for water that stresses existing water resources. Coastal aquifers provide a source of water for coastal populations and are generally part of a larger system where freshwater aquifers are hydraulically connected with a saline surface-water body. They are characterized by salinity variations in space and time, sharp freshwater/saltwater interfaces which can lead to dramatic density differences, and complex groundwater chemistry. Mismanagement of coastal aquifers can lead to saltwater intrusion, the displacement of fresh water by saline water in the freshwater regions of the aquifers, making them unusable as a freshwater source. Saltwater intrusion is of significant interest to water resource managers and efficient simulators are needed to assist them. Numerical simulation of saltwater intrusion requires solving a system of flow and transport equations coupled through a density equation of state. The scale of the problem domain, irregular geometry and heterogeneity can require significant computational resources. Also, modeling sharp transition zones and accurate flow velocities pose numerical challenges. Discontinuous Galerkin (DG) finite element methods (FEM) have been shown to be well suited for modeling flow and transport in porous media but a fully coupled DG formulation has not been applied to the variable density flow and transport model. DG methods have many desirable characteristics in the areas of numerical stability, mesh and polynomial approximation adaptivity and the use of non-conforming meshes. These properties are especially desirable when working with complex geometries over large scales and when coupling multi-physics models (e.g. surface water and groundwater flow models). In this dissertation, we investigate a new combined local discontinuous Galerkin (LDG) and non-symmetric, interior penalty Galerkin (NIPG) formulation for the non-linear coupled flow and solute transport equations that model saltwater intrusion. Our main goal is the formulation and numerical implementation of a robust, efficient, tightly-coupled combined LDG/NIPG formulation within the Department of Defense (DoD) Proteus Computational Mechanics Toolkit modeling framework. We conduct an extensive and systematic code and model verification (using established benchmark problems and proven convergence rates) and model validation (using experimental data) to verify accomplishment of this goal. Lastly, we analyze the accuracy and conservation properties of the numerical model. More specifically, we derive an a priori error estimate for the coupled system and conduct a flow/transport model compatibility analysis to prove conservation properties. / text
14

Hydraulics of duckbill valve jet diffusers

Karandikar, Jaydeep Sharad. January 1997 (has links)
published_or_final_version / Civil and Structural Engineering / Master / Master of Philosophy
15

Geochemical Trends Associated with the seawater-freshwater mixing zone in a Surficial Costal Aquifer, Sapelo Island, GA

Snyder, Matthew Thomas 05 1900 (has links)
No description available.
16

Properties model for aqueous sodium chloride solutions near the critical point of water /

Liu, Bing, January 2005 (has links) (PDF)
Thesis (Ph. D.)--Brigham Young University. Dept. of Chemical Engineering, 2005. / Includes bibliographical references (p. 145-156).
17

Thermodynamic and related studies of aqueous copper (II) sulfate solutions /

Akilan, Chandrika. January 2008 (has links)
Thesis (Ph.D.)--Murdoch University, 2008. / Thesis submitted to the Faculty of Minerals and Energy. Includes bibliographical references (leaves 180-202)
18

A multi-tracer study of saltwater origin, cross-formational flow, and the geochemical evolution of groundwater in the southern High Plains Aquifer along the western caprock escarpment, east-central New Mexico

Langman, Jeff B. January 2008 (has links)
Thesis (Ph. D.)--University of Texas at El Paso, 2008. / Title from title screen. Vita. CD-ROM. Includes bibliographical references. Also available online.
19

The education of an indigenous woman: the pursuit of truth, social justice and healthy relationships in a Coast Salish community context

Underwood, Mavis Kathleen 07 May 2018 (has links)
In 1951 British Columbia public schools opened their doors to First Nations children furthering federal government goals of assimilation. First Nations learners entered provincial public schools as a "billable commodity" while newcomers flooded British Columbia seeking opportunities in a province rich in natural resources in forests, mines, fisheries and land. Sadly the public schools' curricula contained colonization history but no curriculum to describe First Nations existence and history. Locally, there was no recognition of the existence of the Coast Salish people as distinct and prosperous Saltwater People. The indifference to the history of indigenous peoples left newcomers with gaps in their understanding of First Peoples Hostilities and resentments grew as immigration multiplied the numbers and pressure of homesteaders encroaching on traditional indigenous homelands paired with increasing intrusion and restrictions under the Indian Act and shrinking of traditional territories to small contained reserves. / Graduate
20

A review of the configurations, capabilities, and cutting-edge options for multistage solar stills in water desalination

Rashid, F.L., Kaood, A., Al-Obaidi, Mudhar A.A.R., Mohammed, H.I., Alsarayreh, Alanood A., Al-Muhsen, N.F.O., Abbas, A.S., Zubo, R.H.A., Mohammad, A.T., Alsadaie, S., Sowgath, M.T., Abd-Alhameed, Raed, Mujtaba, Iqbal M. 11 June 2023 (has links)
Yes / The desalination of saltwater is a viable option to produce freshwater. All the desalination processes are energy-intensive and can be carried out on a large scale. Therefore, producing freshwater using renewable energy sources is the most desirable option considering the current energy crisis and the effect that fossil-fuel-based energy has on our carbon footprint. In this respect, the tray-type still, one of several solar power desalination still varieties, is popular owing to its straightforward design, economic materials of construction, and minimal maintenance requirements, especially in isolated island regions with restricted energy and natural water supplies. The traditional tray-type solar power has a few drawbacks, such as the inability to recover latent heat from condensation, reduced thermal convection, a large heat capacity, and comparatively minimal driving power through evaporation. Therefore, the improvement of heat and mass transfer capabilities in tray-type stills has been the subject of many studies. However, there is a lack of a comprehensive review in the open literature that covers the design and operational details of multistage solar stills. The purpose of this paper is to present a thorough overview of the past research on multistage solar stills, in terms of configurations, capabilities, and cutting-edge options. In comparison to a unit without a salt-blocking formation, the review indicates that a multistage distillation unit may run continuously at high radiation and generate pure water that is around 1.7 times higher than a unit without a salt-blocking formation. The most effective deign is found to be “V”-shaped solar still trays that attach to four-stage stills, since they are less expensive and more economical than the “floor” (Λ-shape) design, which requires two collectors. Additionally, it can be stated that the unit thermal efficiency, solar percentage, and collected solar energy (over the course of a year) increase by 23%, 18%, and 24%, respectively, when the solar collectors are increased by 26% (at the constant inflow velocity of the water).

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