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Relevant bibliographies by topics / Deep water flow / Dissertations / Theses

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Dissertations / Theses on the topic 'Deep water flow'

Author: Grafiati

Published: 4 June 2021

Last updated: 11 February 2022

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1

Han, Jiangchen. "An approach for upscaling the flow effects of multiple deep-water genetic units." Thesis, Heriot-Watt University, 2015. http://hdl.handle.net/10399/3121.

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Developing a deep-water basin raises many issues and challenges; one of the most significant and necessary issues is overpressure prediction. Basin modelling to construct full scale models is an effective way to find out overpressure distribution in many conditions. However, with current modelling and other methods, it is difficult to obtain data about highly heterogeneous complex structures, which involve coupling between hydraulics and geo-mechanics (compaction) in a system with spatial complexity and temporal evolution of geological bodies, termed as genetic units (GUs). The data collection

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2

Reynolds, Ben Christopher. "Neodymium and lead isotope time series from Atlantic ferromanganese crusts." Thesis, University of Oxford, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.342540.

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3

Chung, Shin Fun. "Characterisation of soft soils for deep water developments." University of Western Australia. School of Civil and Resource Engineering, 2005. http://theses.library.uwa.edu.au/adt-WU2005.0079.

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[Truncated abstract] This research has studied the penetration and extraction resistance profiles of different types of penetrometers in soft clay. The penetrometers of interest include the cone, T–bar, ball and plate. Effects of the surface roughness and aspect ratio of the T–bar penetrometer on its resistance have also been investigated. Undrained shear strength, Su, profiles derived from the penetration tests are compared with the shear strengths measured from field vane shear tests and laboratory (triaxial and simple shear) tests. Both in situ and centrifuge model penetration tests were u

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4

Haque, Md Mominul. "Comparison of behaviour of 1520 mm (60 in.) concrete pipe with sidd design under deep cover." Ohio University / OhioLINK, 1998. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1176497142.

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5

Voeckler, Hendrik Maximilian. "Modeling deep groundwater flow through fractured bedrock in a mountainous headwater catchment using a coupled surface water - groundwater model, Okanagan Basin, British Columbia." Thesis, University of British Columbia, 2012. http://hdl.handle.net/2429/43539.

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Quantifying recharge to the mountain block from headwater catchments in snowmelt dominated upland mountainous regions is an important aspect of hydrologic studies. This study contributes to understanding of the interaction between surface water, soil water and deep groundwater flow in headwater catchments. A novel approach was developed for estimating the bedrock hydraulic conductivity of a regional-scale fractured bedrock aquifer using discrete fracture network (DFN) modeling. The methodology was tested in the mountainous Okanagan Basin, British Columbia, Canada. Discrete fractures were mappe

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6

Ryan, Svenja [Verfasser], Torsten [Akademischer Betreuer] Kanzow, Torsten [Gutachter] Kanzow, and Rhein [Gutachter] Monika. "On the Flow of Modified Warm Deep Water toward the Filchner Ronne Ice Shelf, Weddell Sea, Antarctica / Svenja Ryan ; Gutachter: Torsten Kanzow, Rhein Monika ; Betreuer: Torsten Kanzow." Bremen : Staats- und Universitätsbibliothek Bremen, 2018. http://d-nb.info/1171420447/34.

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7

Krienen, Lisa [Verfasser], Thomas R. [Akademischer Betreuer] Rüde, Benavides Antonio [Akademischer Betreuer] Cardona, and Loera Hector [Akademischer Betreuer] Lopez. "Understanding deep groundwater flow systems to contribute to a sustainable use of the water resource in the Mexican Altiplano / Lisa Krienen ; Thomas R. Rüde, Antonio Cardona Benavides, Hector Lopez Loera." Aachen : Universitätsbibliothek der RWTH Aachen, 2018. http://d-nb.info/1195715005/34.

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8

Colombo, Pedro. "Modelling dense water flows through sills in large scale realistic ocean models : demonstrating the potential of a hybrid geopotential/terrain-following vertical coordinate." Thesis, Université Grenoble Alpes (ComUE), 2018. http://www.theses.fr/2018GREAU017/document.

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Dans le jargon de l’océanographie physique, un «overflow » est une masse d’eau dense, formée sur un plateau continental ou dans une mer marginale, qui rejoint l’océan ouvert en s’écoulant par-delà de fortes contraintes topographiques telles que d’étroits détroits, des seuils ou des talus continentaux particulièrement pentus. Ces processus d'overflow jouent un rôle important en distribuant les flux de chaleur et de sel dans l'océan, car ils alimentent les courants profonds et la plus grande partie des eaux profondes de l'océan global. Une représentation irréaliste de ces processus dans les modè

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9

Zhang, Andi. "Numerical investigation of multiphase Darcy-Forchheimer flow and contaminant transport during SO₂ co-injection with CO₂ in deep saline aquifers." Diss., Georgia Institute of Technology, 2013. http://hdl.handle.net/1853/49065.

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Of all the strategies to reduce carbon emissions, carbon dioxide (CO₂) geological sequestration is an immediately available option for removing large amounts of the gas from the atmosphere. However, our understanding of the transition behavior between Forchheimer and Darcy flow through porous media during CO₂ injection is currently very limited. In addition, the kinetic mass transfer of SO₂ and CO₂ from CO₂ stream to the saline and the fully coupling between the changes of porosity and permeability and multiphase flow are two significant dimensions to investigate the brine acidification and th

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10

Clesi, Vincent. "Formation de la Terre et de Mars : étude expérimentale et numérique." Thesis, Clermont-Ferrand 2, 2016. http://www.theses.fr/2016CLF22750/document.

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La formation des noyaux planétaires métalliques est un évènement majeur pour l’évolution des propriétés physico-chimiques des planètes telluriques telles que nous les connaissons aujourd’hui. En effet, l’abondance des éléments sidérophiles (i.e. qui ont des affinités chimiques avec les phases métalliques) dans les manteaux planétaires s’explique par les conditions dans lesquelles se sont séparées les phases métalliques et silicatées. Au premier rang de ces conditions se trouvent la pression, la température et la fugacité d’oxygène. La distribution des éléments dans le noyau et le manteau ne pe

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11

Henderson, Samuel Straker. "Tracking deep-water flow on Eirik drift over the past 160 kyr linking deep-water changes to freshwater fluxes /." 2009. http://hdl.rutgers.edu/1782.2/rucore10001600001.ETD.000051018.

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12

Chao, Wei-Ting, and 趙偉廷. "Flow field measurement of deep water breaking wave impact on a vertical wall." Thesis, 2009. http://ndltd.ncl.edu.tw/handle/04807003799474299761.

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碩士<br>國立臺灣大學<br>工程科學及海洋工程學研究所<br>97<br>Deep water breaking impact on a vertical wall were investigated in this research. The breaking waves were generated by linearly-varying-frequency wave trains. A P.I.V. measurement system was used to record the particle motion in fluids, such that the instantaneous wave flow field can be calculated. Based on the measured results, qualitative descriptions of the variations of flow field around the vertical wall during breaking wave impact process were made in this research. It showed that due to a plunging breaker causes much more violated flow filed than a

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13

Lim, Ho Joon. "Experimental Study on Kinematics and Dynamics of Breaking Waves in Deep Water." Thesis, 2010. http://hdl.handle.net/1969.1/ETD-TAMU-2010-08-8501.

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A new measurement technique called fiber optic reflectometer (FOR) was developed to investigate multiphase flows. The principle and setup of the FOR technique were introduced and applied to various experiments. Based on the coherently mixed signal between the Fresnel reflection off the fiber-liquid interface and the scattered signal off the object, such as a gas bubble, and a solid particle, this single probe technique is capable of simultaneously measuring the velocity of the object with a high accuracy and the phase of the fluid. In addition, bubble diameter, velocity, and void fraction were

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14

Littlepage, John Stanley. "Use of well testing and multiple point statistics in analyzing deep water channel turbidite reservoirs." Thesis, 2011. http://hdl.handle.net/2152/ETD-UT-2011-08-4120.

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Well testing has long been used to determine the dynamic characteristics of a reservoir. However due to the increase in interest in exploring deep offshore reservoirs and the expense associated with performing well tests of sufficient duration, alternative methods for retrieving reservoir specific information from tests of limited duration are necessary. This thesis presents analysis of derivative plots from well tests in different locations along a heterogeneous channelized environment and the information that can be derived the shape of these plots. The viability of calibrating a multiple po

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15

Holder, Rachel. "Studies into the Initial Conditions, Flow Rate, and Containment System of Oil Field Leaks in Deep Water." Thesis, 2013. http://hdl.handle.net/1969.1/151119.

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Oil well blow outs are investigated to determine methods to quickly and accurately respond to an emergency situation. Flow rate is needed to guide containment and dispersal operations. The Stratified Integral Multiphase Plume, SIMP, model was used to investigate the range of initial conditions available to integral modeling. Sensitivity to initial conditions is modest, but without experimental data at the appropriate scale the most accurate condition is unable to be determined. Flow rates are difficult to directly measure in blow out situations, so another method must be determined; therefore,

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16

Zoeller, Khalhela. "Insights into the distribution and mobility of metals in the sheeted dike complex formed at fast-spreading ridges (Pito Deep, EPR)." Thesis, 2014. http://hdl.handle.net/1828/5264.

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Hydrothermal fluid circulation is an important process in the formation and evolution of ocean crust. A tectonic window located at Pit Deep (NE corner Easter Microplate) provides an ideal location to examine a 3-dimensional view of ocean crust formed at the fast-spreading East Pacific Rise. This study focuses on the base metal (Cu, Ni, Mn, Co, Zn, and Pb) content of the bulk rock and mineral components in the sheeted dike complex. There is no observable trend of metal mobility with depth, geographic location, or dominant alteration phase. Secondary mineral analyses (using LA-ICP-MS) show that

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17

Reaume, Jonathan Daniel. "Wave-Cavity Resonator: Experimental Investigation of an Alternative Energy Device." Thesis, 2015. http://hdl.handle.net/1828/6960.

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A wave cavity resonator (WCR) is investigated to determine the suitability of the device as an energy harvester in rivers or tidal flows. The WCR consists of coupling between self-excited oscillations of turbulent flow of water in an open channel along the opening of a rectangular cavity and the standing gravity wave in the cavity. The device was investigated experimentally for a range of inflow velocities, cavity opening lengths, and characteristic depths of the water. Determining appropriate models and empirical relations for the system over a range of depths allows for accuracy when d

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