Relevant bibliographies by topics / Deep water flow

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Deep water flow'

Author: Grafiati
Published: 4 June 2021
Last updated: 11 February 2022

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Journal articles on the topic "Deep water flow"

1

Timmermans, M.-L., P. Winsor, and J. A. Whitehead. "Deep-Water Flow over the Lomonosov Ridge in the Arctic Ocean." Journal of Physical Oceanography 35, no. 8 (2005): 1489–93. http://dx.doi.org/10.1175/jpo2765.1.

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Abstract The Arctic Ocean likely impacts global climate through its effect on the rate of deep-water formation and the subsequent influence on global thermohaline circulation. Here, the renewal of the deep waters in the isolated Canadian Basin is quanitified. Using hydraulic theory and hydrographic observations, the authors calculate the magnitude of this renewal where circumstances have thus far prevented direct measurements. A volume flow rate of Q = 0.25 ± 0.15 Sv (Sv ≡ 106 m3 s−1) from the Eurasian Basin to the Canadian Basin via a deep gap in the dividing Lomonosov Ridge is estimated. Dee
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Bensi, Manuel, Vedrana Kovačević, Leonardo Langone, et al. "Deep Flow Variability Offshore South-West Svalbard (Fram Strait)." Water 11, no. 4 (2019): 683. http://dx.doi.org/10.3390/w11040683.

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Water mass generation and mixing in the eastern Fram Strait are strongly influenced by the interaction between Atlantic and Arctic waters and by the local atmospheric forcing, which produce dense water that substantially contributes to maintaining the global thermohaline circulation. The West Spitsbergen margin is an ideal area to study such processes. Hence, in order to investigate the deep flow variability on short-term, seasonal, and multiannual timescales, two moorings were deployed at ~1040 m depth on the southwest Spitsbergen continental slope. We present and discuss time series data col
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Dong, Changming, James C. McWilliams, and Alexander F. Shchepetkin. "Island Wakes in Deep Water." Journal of Physical Oceanography 37, no. 4 (2007): 962–81. http://dx.doi.org/10.1175/jpo3047.1.

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Abstract Density stratification and planetary rotation distinguish three-dimensional island wakes significantly from a classical fluid dynamical flow around an obstacle. A numerical model is used to study the formation and evolution of flow around an idealized island in deep water (i.e., with vertical island sides and surface-intensified stratification and upstream flow), focusing on wake instability, coherent vortex formation, and mesoscale and submesoscale eddy activity. In a baseline experiment with strong vorticity generation at the island, three types of instability are evident: centrifug
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Fieux, M., and J. C. Swallow. "Flow of deep water into the Somali Basin." Deep Sea Research Part A. Oceanographic Research Papers 35, no. 2 (1988): 303–9. http://dx.doi.org/10.1016/0198-0149(88)90041-6.

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张, 雨晴. "Flume Experiment Research Progress of Deep Water Gravity Flow." Advances in Geosciences 10, no. 11 (2020): 1062–74. http://dx.doi.org/10.12677/ag.2020.1011105.

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Liu, Ko-Fei. "Tide-Induced Ground-Water Flow in Deep Confined Aquifer." Journal of Hydraulic Engineering 122, no. 2 (1996): 104–10. http://dx.doi.org/10.1061/(asce)0733-9429(1996)122:2(104).

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Siedler, Gerold, Jürgen Holfort, Walter Zenk, Thomas J. Müller, and Tiberiu Csernok. "Deep-Water Flow in the Mariana and Caroline Basins*." Journal of Physical Oceanography 34, no. 3 (2004): 566–81. http://dx.doi.org/10.1175/2511.1.

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Abstract Two major water masses dominate the deep layers in the Mariana and Caroline Basins: the Lower Circumpolar Water (LCPW), arriving from the Southern Ocean along the slopes north of the Marshall Islands, and the North Pacific Deep Water (NPDW) reaching the region from the northeastern Pacific Ocean. Hydrographic and moored observations and multibeam echosounding were performed in the East Mariana and the East Caroline Basins to detail watermass distributions and flow paths in the area. The LCPW enters the East Mariana Basin from the east. At about 13°N, however, in the southern part of t
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Kouskoulas, David M., and Yaron Toledo. "Deep water gravity wave triad resonances on uniform flow." Physics of Fluids 32, no. 7 (2020): 076603. http://dx.doi.org/10.1063/5.0012631.

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McCave, I. N., T. Kiefer, D. J. R. Thornalley, and H. Elderfield. "Deep flow in the Madagascar–Mascarene Basin over the last 150000 years." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 363, no. 1826 (2005): 81–99. http://dx.doi.org/10.1098/rsta.2004.1480.

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The SW Indian Ocean contains at least four layers of water masses with different sources: deep Antarctic (Lower Circumpolar Deep Water) flow to the north, midwater North Indian Deep Water flow to the south and Upper Circumpolar Deep Water to the north, meridional convergence of intermediate waters at 500–1500 m, and the shallow South Equatorial Current flowing west. Sedimentation rates in the area are rather low, being less than 1 cm ka −1 on Madagascar Ridge, but up to 4 cm ka −1 at Amirante Passage. Bottom flow through the Madagascar–Mascarene Basin into Amirante Passage varies slightly on g
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Burckel, Pierre, Claire Waelbroeck, Yiming Luo, et al. "Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka)." Climate of the Past 12, no. 11 (2016): 2061–75. http://dx.doi.org/10.5194/cp-12-2061-2016.

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Abstract. We reconstruct the geometry and strength of the Atlantic meridional overturning circulation during the Heinrich stadial 2 and three Greenland interstadials of the 20–50 ka period based on the comparison of new and published sedimentary 231Pa / 230Th data with simulated sedimentary 231Pa / 230Th. We show that the deep Atlantic circulation during these interstadials was very different from that of the Holocene. Northern-sourced waters likely circulated above 2500 m depth, with a flow rate lower than that of the present-day North Atlantic deep water (NADW). Southern-sourced deep waters
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Dissertations / Theses on the topic "Deep water flow"

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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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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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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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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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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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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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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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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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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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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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Books on the topic "Deep water flow"

1

O'Reilly, Andrew M. A method for simulating transient ground-water recharge in deep water-table settings in central Florida by using a simple water-balance/transfer-function model. U.S. Geological Survey, 2004.

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O'Reilly, Andrew M. A method for simulating transient ground-water recharge in deep water-table settings in central Florida by using a simple water-balance/transfer-function model. U.S. Geological Survey, 2004.

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Barker, René A. Regional hydrology and simulation of deep ground-water flow in the southeastern coastal plain aquifer system in Mississippi, Alabama, Georgia, and South Carolina. U.S. G.P.O., 1992.

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Wirojanagud, Prakob. Numerical modeling of regional ground-water flow in the Deep-Basin Brine aquifer of the Palo Duro Basin, Texas Panhandle. Bureau of the Economic Geology, University of Texas at Austin, 1986.

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Division, Alberta Fisheries Management. Report on Red Deer River instream flow needs study. Golder Associates, 1999.

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D, Crevello Paul, and Harris Paul M. 1931-, eds. Deep-water carbonates: Buildups, turbidites, debris flows and chalks : a core workshop. SEPM, 1985.

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Goater, Lori. Aquatic environment impact ratings a method for evaluating SSRB flow scenarios: Red Deer River case study. 4th ed. Alberta Environment, 2008.

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Wolfe, William J. Recent sedimentation and surface-water flow patterns on the flood plain of the North Fork Forked Deer River, Dyer County, Tennessee. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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J, Wolfe William. Recent sedimentation and surface-water flow patterns on the flood plain of the North Fork Forked Deer River, Dyer County, Tennessee. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Wolfe, William J. Recent sedimentation and surface-water flow patterns on the flood plain of the North Fork Forked Deer River, Dyer County, Tennessee. U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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Book chapters on the topic "Deep water flow"

1

Assem, Haytham, Salem Ghariba, Gabor Makrai, Paul Johnston, Laurence Gill, and Francesco Pilla. "Urban Water Flow and Water Level Prediction Based on Deep Learning." In Machine Learning and Knowledge Discovery in Databases. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-71273-4_26.

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Toxopeus, Serge L. "Viscous-Flow Calculations for KVLCC2 in Deep and Shallow Water." In Computational Methods in Applied Sciences. Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6143-8_9.

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Bogdevicius, Marijonas, Jolanta Janutėnienė, Rimantas Didžiokas, and Vytautas Barzdaitis. "Numerical simulation of geothermal water flow in a deep multistage centrifugal pump." In Advances in Mechanism and Machine Science. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-20131-9_361.

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Morgan, Lynette. "Hydroponic System - Solution Culture." In Hydroponics and protected cultivation: a practical guide. CABI, 2021. http://dx.doi.org/10.1079/9781789244830.0061.

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Abstract This paper discusses about the solution culture or 'hydroculture' systems, which are methods of crop production which do not employ the use of substrates to contain the root system and hold moisture between irrigations. It includes NFT or the nutrient film technique, deep water culture/deep flow technique - float, raft or pond systems, aeroponics, aquaponics, organic solution culture, hydroponic fodder systems, and automation for solution culture systems.
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Morgan, Lynette. "Hydroponic System - Solution Culture." In Hydroponics and protected cultivation: a practical guide. CABI, 2021. http://dx.doi.org/10.1079/9781789244830.0005.

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Abstract This paper discusses about the solution culture or 'hydroculture' systems, which are methods of crop production which do not employ the use of substrates to contain the root system and hold moisture between irrigations. It includes NFT or the nutrient film technique, deep water culture/deep flow technique - float, raft or pond systems, aeroponics, aquaponics, organic solution culture, hydroponic fodder systems, and automation for solution culture systems.
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Chen, Jian-yang, Hui Wang, Da-wang Liu, and Tuo Zou. "Evolution Process Characteristics of and Differential Enrichment of Oil and Gas in Deep Water Gravity Flow Sandstone." In Springer Series in Geomechanics and Geoengineering. Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-2485-1_305.

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Stickley, Catherine E., Lionel Carter, I. Nick Mccave, and Phil P. E. Weaver. "Lower Circumpolar Deep Water Flow Through the SW Pacific Gateway for the Last 190 Ky: Evidence from Antarctic Diatoms." In Geophysical Monograph Series. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm126p0101.

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LOUCKS, R. G., A. A. BROWN, C. W. ACHAUER, and D. A. BUDD. "CARBONATE GRAVITY-FLOW SEDIMENTATION ON LOW-ANGLE SLOPES OFF THE WOLFCAMPIAN NORTHWEST SHELF OF THE DELAWARE BASIN." In Deep-Water Carbonates. SEPM (Society for Sedimentary Geology), 1985. http://dx.doi.org/10.2110/cor.85.06.0056.

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ARMENTROUT, JOHN M. "GRAVITY-FLOW DEPOSITS OF A SLOPE VALLEY SYSTEM, HIGH ISLAND A-537 FIELD, GULF OF MEXICO." In Turbidites and Associated Deep-Water Facies. SEPM (Society for Sedimentary Geology), 1995. http://dx.doi.org/10.2110/cor.95.20.0165.

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Zavala, Carlos, Mariano Arcuri, Mariano Di Meglio, Helena Gamero Diaz, and Carmen Contreras. "A Genetic Facies Tract for the Analysis of Sustained Hyperpycnal Flow Deposits." In Sediment Transfer from Shelf to Deep Water—Revisiting the Delivery System. American Association of Petroleum Geologists, 2012. http://dx.doi.org/10.1306/13271349st613438.

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Conference papers on the topic "Deep water flow"

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Kristiansen, P., D. Dangle, E. P. Andren, and N. Cockrell. "Deep Water Sparse OBN Surveys - Processing Flow and QC." In 77th EAGE Conference and Exhibition 2015. EAGE Publications BV, 2015. http://dx.doi.org/10.3997/2214-4609.201413183.

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Singh, Sunil Kumar. "Flow Assurance Challenges- FPSO Based Development of MA Deep Water Field." In SPE Oil and Gas India Conference and Exhibition. Society of Petroleum Engineers, 2012. http://dx.doi.org/10.2118/153831-ms.

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Deka, Barasha, Rohit Sharma, Vikas Mahto, and Subhash Polara. "Quantum Dots: Low-Dosage Hydrate Inhibitors for Deep Water Flow Assurance." In Offshore Technology Conference. Offshore Technology Conference, 2020. http://dx.doi.org/10.4043/30654-ms.

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Monahan, Peter. "Flow Assurance Challenge for Offshore Deep Water in Republic of Congo." In Offshore Technology Conference. Offshore Technology Conference, 2009. http://dx.doi.org/10.4043/20279-ms.

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Soetikno, Darmadi, Isti Rodiah, Muhammad Islahuddin, et al. "Heat loss model for flow assurance in a deep water riser." In 4TH INTERNATIONAL CONFERENCE ON MATHEMATICS AND NATURAL SCIENCES (ICMNS 2012): Science for Health, Food and Sustainable Energy. AIP Publishing LLC, 2014. http://dx.doi.org/10.1063/1.4868856.

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Gong, Zhiwu, Shaoran Ren, Liang Zhang, Guodong Cui, Yanmin Liu, and Yanyong Wang. "Shallow Gas and Shallow Water Flow Induced by Natural Gas Hydrate Dissociation in Deep Water Sediments." In Offshore Technology Conference. Offshore Technology Conference, 2017. http://dx.doi.org/10.4043/27624-ms.

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Giraldo, Diego Garcia, and Ronald W. Yeung. "The Deep-Water-Horizon Spill: Flow-Rate Estimation Based on Satellite Images." In ASME 2012 31st International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/omae2012-84153.

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The “Deep Water Horizon” Mobil Offshore Drilling Unit (MODU) is one of several classes of floatable drilling machines. As a consequence of the accident on April 20, 2010, the worst ecological disaster with regard to oil spills in the US history was generated in the Gulf of Mexico, causing extensive damage to marine and wildlife habitats, as well as the Gulf’s fishing and tourism industries. Since that moment, experts are trying to estimate the total amount of oil being lost into the sea. The objective of this presentation is to report a procedure developed in the first author’s thesis1 an inde
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Xiangyang, Niu, Gao Yiyang, Wang Runna, and Du Meng. "Vertical Oil-in-Water Flow Pattern Identification with Deep CNN-LSTM Network." In 2020 International Conference on Intelligent Computing and Human-Computer Interaction (ICHCI). IEEE, 2020. http://dx.doi.org/10.1109/ichci51889.2020.00088.

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He, Zhiguo, Weiming Wu, Yongping Yuan, and Sam S. Y. Wang. "Simulation of Rainfall-Runoff in the Deep Hollow Lake Watershed Using an Integrated Surface-Subsurface Flow Model." In World Environmental and Water Resources Congress 2007. American Society of Civil Engineers, 2007. http://dx.doi.org/10.1061/40927(243)176.

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Hasan, A. Rashid, Rayhana N. Sohel, and Xiaowei Wang. "Estimating Zonal Flow Contributions in Deep Water Assets From Pressure and Temperature Data." In ASME 2017 36th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/omae2017-62537.

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Producing hydrocarbon from deep water assets is extremely challenging and expensive. A good estimate of rates from multiple pay zones is essential for well monitoring, surveillance, and workover decisions. Such information can be gleaned from flowing fluid pressure and temperature; deep-water wells are often well instrumented that offers such data on a continuous basis. In this study a model is presented that estimates zonal flow contributions based on energy and momentum balances. Kinetic and heat energy coming from the reservoir fluid to the production tubing is accounted for in the model. T
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Reports on the topic "Deep water flow"

1

Recent sedimentation and surface-water flow patterns on the flood plain of the North Fork Forked Deer River, Dyer County, Tennessee. US Geological Survey, 1993. http://dx.doi.org/10.3133/wri924082.

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