Thèses sur le sujet « Bed roughness »
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Robert, Andre. « Statistical modelling of sediment bed profiles and bed roughness properties in alluvial channels ». Thesis, University of Cambridge, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.292244.
Texte intégralSorenson, Kent S. (Kent Soren). « Moveable bed roughness and sediment resuspension in the field ». Thesis, Massachusetts Institute of Technology, 1995. http://hdl.handle.net/1721.1/35047.
Texte intégralWilbers, Antoine. « The development and hydraulic roughness of subaqueous dunes / ». Utrecht : Koninklijk Nederlands Aardrijkskundig Genootschap, 2004. http://www.loc.gov/catdir/toc/fy0708/2004464077.html.
Texte intégralLefebvre, Alice. « Bed roughness over vegetated beds : sonar imaging techniques and effect on unidirectional currents ». Thesis, University of Southampton, 2009. https://eprints.soton.ac.uk/72139/.
Texte intégralRahman, Shikha. « Effect of bed roughness on scalar mixing in turbulent boundary layers ». Diss., Georgia Institute of Technology, 2002. http://hdl.handle.net/1853/32794.
Texte intégralBatt, Rachel Louise. « The influence of bed roughness on the dynamics of gravity currents ». Thesis, University of Leeds, 2008. http://etheses.whiterose.ac.uk/11282/.
Texte intégralHersberger, Daniel S. « Wall roughness effects on flow and scouring in curved channels with gravel bed / ». Lausanne, 2002. http://library.epfl.ch/theses/?display=detail&nr=2632.
Texte intégralKendall, Robert L. « Sand bed roughness in the nearshore, COAST 3D experiment, Egmond aan Zee, the Netherlands ». Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2000. http://handle.dtic.mil/100.2/ADA380327.
Texte intégralThesis advisor(s): Gallagher, Edith L. ; Thornton, Edward B. "June 2000." Includes bibliographical references (p. 75-76). Also available online.
Velioglu, Deniz. « Effects Of Different Bed Roughnesses On The Characteristics Of Hydraulic Jumps ». Master's thesis, METU, 2012. http://etd.lib.metu.edu.tr/upload/12614018/index.pdf.
Texte intégralKhan, Muhammad Ijaz. « The influence of two-dimensional bed roughness on the flow structure of a turbulent boundary layer ». Thesis, University College London (University of London), 2004. http://discovery.ucl.ac.uk/1446901/.
Texte intégralPlott, James Read. « A Generalized Log-Law Formulation For a Wide Range of Boundary Roughness Conditions Encountered in Streams ». Thesis, Virginia Tech, 2011. http://hdl.handle.net/10919/76866.
Texte intégralMaster of Science
Tatman, Eric-Paul Daniel. « The Characterization and Fatigue Life Impact from Surface Roughness on Structurally Relevant Features Produced Using Additive Manufacturing ». Wright State University / OhioLINK, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=wright1564754673356237.
Texte intégralSimsek, Cagdas. « Forced Hydraulic Jump On Artificially Roughened Beds ». Master's thesis, METU, 2007. http://etd.lib.metu.edu.tr/upload/12608038/index.pdf.
Texte intégralThein, Myint. « Experimental investigation of flow resistance and velocity distributions in a rectangular channel with large bed-roughness elements ». Diss., Georgia Institute of Technology, 1993. http://hdl.handle.net/1853/19580.
Texte intégralValentine, Kendall. « Characterization of the bed, critical boundary shear stress, roughness, and bedload transport in the Connecticut River Estuary ». Thesis, Boston College, 2015. http://hdl.handle.net/2345/bc-ir:104550.
Texte intégralThis study characterizes the bed of the Connecticut River estuary in terms of grain size and bedforms, and relates these to river discharge, tidal currents, and sediment transport. Over four field excursions, sediment cores were collected, in addition to bathymetry surveys, and water column measurements. A three-dimensional circulation and sediment transport model calculated boundary shear stress over the same time. The bed of the estuary is composed mostly of sand, with small amounts of fine sediments. Deposition of fine sediments is limited by the landward extent of the salt intrusion. Large bedforms are oriented seaward. The critical shear stress for the median grain size is exceeded each tidal cycle. Bedload transport is dominantly seaward during high discharge conditions, but varies during low discharge. Bathymetry surveys from previous studies and this study show consistent bedform fields over 25 years. Bedforms observed in the field reflect typical conditions rather than extreme events
Thesis (MS) — Boston College, 2015
Submitted to: Boston College. Graduate School of Arts and Sciences
Discipline: Earth and Environmental Sciences
Yee, Irene. « Powder Bed Surface Quality and Particle Size Distribution for Metal Additive Manufacturing and Comparison with Discrete Element Model ». DigitalCommons@CalPoly, 2018. https://digitalcommons.calpoly.edu/theses/1888.
Texte intégralBomminayuni, Sandeep Kumar. « Large eddy simulation of turbulent flow over a rough bed using the immersed boundary method ». Thesis, Georgia Institute of Technology, 2010. http://hdl.handle.net/1853/34821.
Texte intégralWhip, Bo Ryan. « Effect of Process Parameters on the Surface Roughness and Mechanical Performance of Additively Manufactured Alloy 718 ». Wright State University / OhioLINK, 2018. http://rave.ohiolink.edu/etdc/view?acc_num=wright1526993831680976.
Texte intégralSchnur, Christopher. « Electron Beam - Powder Bed Fusion Of Alloy 718 : Influences Of Contour Parameters On Surface And Microstructural Characteristics ». Thesis, Högskolan Väst, Avdelningen för Industriell ekonomi, Elektro- och Maskinteknik, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:hv:diva-14318.
Texte intégralBalachandramurthi, Arun Ramanathan. « Fatigue Properties of Additively Manufactured Alloy 718 ». Licentiate thesis, Högskolan Väst, Avdelningen för avverkande och additativa tillverkningsprocesser (AAT), 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:hv:diva-13186.
Texte intégralCerino, Bastien. « Large-scale flow structures in shallow mixing layers over uniform and spanwise-heterogeneous bed surfaces ». Electronic Thesis or Diss., Lyon 1, 2024. http://www.theses.fr/2024LYO10269.
Texte intégralThis PhD investigates the effect of bed roughness on shallow mixing layers (SML) and the evolution of coherent structures that populate them, such as Kelvin-Helmholtz Coherent Structures (KHCSs), Secondary Currents (SCs), and Large and Very-Large Scale Motions (LSMs and VLSMs respectively). Two bed roughness scenarios are considered: a uniformly rough bed and a lateral transition from a rough bed to a smooth bed. The rough bed is made of artificial dense grass with a height of 5mm, while the smooth bed is made of PVC plate. The experiments are conducted in an 18m × 1.98m laboratory flume. The flow configurations explored include both initially spanwise sheared and uniform flows. First, we explore the flows over the uniformly rough bed, comparing the acquired data to previous measurements conducted in the same flume with a hydraulically smooth bed. The objectives are to validate driving parameters for SML and KHCSs observed in the literature, assess the effect of a rough bed on the turbulent field of SML, and explore the interactions between KHCSs, LSMs, and VLSMs. Second, we investigate the longitudinal evolution of SML, KHCSs, SCs, LSMs and VLSMs over a bed with a lateral roughness transition. We evaluate the mechanisms of lateral momentum exchange and their relative importance, ultimately exploring the interaction between all four types of coherent structures
Lindbäck, Katrin. « Hydrology and Bed Topography of the Greenland Ice Sheet : Last known surroundings ». Doctoral thesis, Uppsala universitet, Luft-, vatten och landskapslära, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-259076.
Texte intégralDe ökade temperaturerna i Arktis påskyndar förlusten av landbaserad is lagrad i glaciärer och permafrost. Grönlands inlandsis är den största ismassan på norra halvklotet och lagrar ca 10% av allt sötvatten på jorden, vilket motsvarar ca 7 meter global havsnivåhöjning. För ett par decennier sedan var inlandsisens massbalans dåligt känd och antogs ha liten inverkan på dagens havsnivåhöjning. Utvecklingen av regionala klimatmodeller och satellitbaserad fjärranalys av inlandsisen har under de senaste decenniet påvisat en betydande massförlust. För att förutse vilken inverkan inlandsisen har på framtida havsnivåhöjningar krävs en förståelse för de fysikaliska processerna som styr dess massbalans och isrörelse. I de sydöstra och centrala västra delarna av inlandsisen domineras massförlusten av dynamiska processer i isströmmar som kalvar ut i havet. Massförlusten i de centrala norra, sydvästra och nordöstra delarna domineras av isytans massbalans. Ytterst lite är känt om hur det hydrologiska systemet ser ut under inlandsisen; hur väl det hydrologiska systemet är utvecklat avgör vattnets påverkan på isrörelsen. I denna doktorsavhandling har jag använt markbaserade radarmätningar för att kartlägga den subglaciala topografin för en del av den västra landbaserade inlandsisen. Denna kunskap är en viktig förutsättning för att kunna modellera den subglaciala hydrologin. Med hjälp av rumsligt högupplöst data över istjockleken och bottentopografin har jag gjort följande specifika studier: Först har jag analyserat de geologiska och glaciologiska förhållandena i regionen genom att jämföra proglacial och subglacial spektralanalys av terrängens ytojämnheter. Sedan har jag analyserat den subglaciala vattenavrinningen och påvisat en potential för att avrinningsområdena kan ändras beroende på vattentryckförhållandena på botten. Slutligen har jag tittat mer i detalj på englaciala radarstrukturer som ofta observerats i radardata från västra Grönland. Sammanfattningsvis belyser avhandlingen behovet av inte bara noggranna rumsligt högupplösta subglaciala digitala höjdmodeller, utan även regionalt optimerad interpolering när detaljerade hydrologiska studier ska utföras på Grönlands inlandsis.
Wahman, Clarence. « Corrosion of additively manufactured magnesium alloy WE43 : An investigation in microstructure and corrosion properties of as built samples manufactured with Powder Bed Fusion-Laser Beam ». Thesis, Uppsala universitet, Tillämpad materialvetenskap, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-448525.
Texte intégralEvcimen, Taylan Ulas. « The Effect Of Prismatic Roughness Elemnts On Hydraulic Jump ». Master's thesis, METU, 2005. http://etd.lib.metu.edu.tr/upload/12605792/index.pdf.
Texte intégralMasiagutova, Elina. « Étude de la génération des topographies de surfaces latérales issues du procédé LPBF pour un alliage d’aluminium AlSi10Mg ». Thesis, Lyon, 2022. http://www.theses.fr/2022LYSEE002.
Texte intégralIn the current study, surface generation during additive manufacturing (AM), especially the laser powder bed fusion (LPBF) process was studied. LPBF is a progressive process that can lead to new opportunities, such as applications that require complex structures (internal channels or lightweight lattice structures). It has therefore attracted considerable attention, which has led to research and development in many industries, particularly in the aerospace industry.A surface generation study to optimize surface roughness and material density by examining the influence of the primary LPBF process parameters was therefore performed. During this study, the relationship between the roughness of the top and side surfaces and the density of the material was established. This made it possible to determine the first window of optimal parameters.An analysis of the roughness dispersion and process reproducibility were then carried out. This analysis revealed a significant roughness dispersion, especially from one side to the other. As a result, recommendations on surface measurements have been proposed.The effect of different process options (secondary parameters) are also studied in order to better understand the generation of the side surface and optimize it. This study showed that compensations and contour settings are key parameters that can help reduce the side surface roughness. Indeed, the geometric positioning of the different weld tracks is an important issue that must be addressed to reduce surface roughness. Based on the results of this study, it is possible to reduce the average surface roughness Sa from 40 to 10 μm.Finally, this thesis presents a new approach to modeling side surfaces roughness (at 0°). The approach is based on the weld track geometry (radii of curvature). It allows to take into account the weld tracks and layers position in relation to each other and thus to predict the roughness for different scanning strategies, compensation parameters
Evcimen, Taylan Ulas. « Effect Of Prismatic Roughness On Hydraulic Jump In Trapezoidal Channels ». Phd thesis, METU, 2012. http://etd.lib.metu.edu.tr/upload/12614467/index.pdf.
Texte intégralHaws, Benjamin B. « Ability of ADV Measurements to Detect Turbulence Differences Between Angular and Rounded Gravel Beds of Intermediate - Roughness Scale ». Diss., CLICK HERE for online access, 2008. http://contentdm.lib.byu.edu/ETD/image/etd2558.pdf.
Texte intégralCILLI, Silvia. « Evaluation of bedload yield in two small sand-bed rivers of the Ravenna province (Italy) ». Doctoral thesis, Università degli studi di Ferrara, 2020. http://hdl.handle.net/11392/2487848.
Texte intégralIl trasporto di sedimenti, e in particolare il trasporto solido (al fondo), è uno dei più dinamici e complessi risultati dei processi idro-climatici, idraulici e geomorfologici che si verificano all’interno di un bacino fluviale. La capacità di produzione sedimentaria dipende strettamente dalla fornitura di sedimenti dal bacino che è altamente controllata da fattori primari quali: clima, area del bacino, geologia e topografia. Ulteriormente influenzato da impatti antropici, il trasporto di sedimenti controlla le risposte geomorfiche dei fiumi che, a loro volta possono essere ulteriormente esacerbati dai cambiamenti climatici. Diversi sono gli strumenti e le tecniche di campionamento utilizzati sul campo per quantificare il trasporto solido. Le difficoltà connesse alla loro efficienza, assieme alla richiesta di grandi risorse umane e finanziarie, hanno dimostrato che il trasporto solido è uno dei processi fluviali più difficili da misurare. Negli ultimi cinquant'anni tali difficoltà hanno spinto gli scienziati a sviluppare modelli empirici per la stima del trasporto solido al fondo. Sono state proposte diverse formule basate fondamentalmente su studi di laboratorio e di campo, pur considerando che le misure dirette di campo sono molto limitate. Nonostante i continui sforzi compiuti, esistono ancora grandi limiti delle equazioni. Comprendere e quantificare il tasso dei sedimenti trasportati sta diventando sempre più importante per una varietà di problemi sia da un punto di vista scientifico che applicativo. Sebbene vi siano alcuni sporadici studi sperimentali sugli apporti solidi fluviali in regione Emilia-Romagna, i dati a disposizione sono estremamente esigui e, sfortunatamente, si riferiscono solo a un numero limitato di fiumi. Data la scarsa conoscenza degli apporti fluviali a scala regionale, questa ricerca mira a quantificare il trasporto solidi dei corsi d’acqua attraverso indagini sul campo e misurazioni dirette svolte su due fiumi rappresentativi con lo scopo di ampliare il dataset attuale a disposizione. Mediante un approccio di tipo idraulico ed idrologico e, soprattutto, mediante campagne di misura diretta del trasporto solido, si è quantificato il trasporto al fondo nei Fiumi Uniti e Savio. Entrambi i fiumi scorrono dall'Appennino settentrionale alla Pianura Padana, sfociando nel mare Adriatico in prossimità della provincia di Ravenna. Concentrandosi in particolare sul trasporto solido fluviale, l'indagine si svolge nei pressi degli ultimi dieci chilometri dei corsi d’acqua, a ridosso delle zone fociali. Le campagne sono state condotte con un approccio di misurazione diretta ( ossia tramite l’utilizzo del campionatore Helley-Smith) iniziato nel 2005-06 da autori precedenti ed esteso dall’autrice nel 2019. Campionamenti ripetuti effettuati in diverse condizioni di piena hanno permesso di calcolare le scale di deflusso degli apporti solidi (e il carico solido al fondo fluviale annuale). Ulteriori indagini batimetriche sono state condotte in prossimità delle sezioni di misura, rivelando la presenza di forme di fondo. Ulteriori approfondimenti sono stati svolti relativamente ai fattori che influenzano il trasporto solido, del quale è stata anche effettuata una stima analizzando alcune classiche equazioni presenti in letteratura. Sono state infatti considerate sia le condizioni di soglia del movimento dei sedimenti sia la componente di rugosità dovuta alla presenza delle forme di fondo, ed in particolare dovuta alle dune. I dati ottenuti indicano che l’apporto solido fluviale dei fiumi studiati è molto variabile ed in particolare il trasporto solido dei Fiumi Uniti è superiore a quello del fiume Savio. Infine, è stato eseguito un confronto tra dati misurati sul campo e quelli ottenuti da criteri ben noti di letteratura allo scopo di definire la migliore equazione utilizzabile a scala regionale per quantificare l’apporto solido fluviale alle spiagge romagnole.
Lorentz, Benoît [Verfasser], et A. [Akademischer Betreuer] Albers. « An approach to investigate surface roughness influence on non-lubricated and lubricated contacts by means of the finite element analysis = Ein Ansatz zur Untersuchung der Oberflächenrauheiteinflüsse bei geschmierten und trockenen Kontakten mittels der Finite Elemente Methode [[Elektronische Ressource]] / Benoît Lorentz. Betreuer : A. Albers ». Karlsruhe : KIT-Bibliothek, 2013. http://d-nb.info/1049730488/34.
Texte intégralNunes, Vasco B. « Survey And Statistical Parameterization Of Bed Roughness Of A Coral Reef ». Thesis, 2005. http://hdl.handle.net/10125/10531.
Texte intégralWu, Chi-shou, et 吳啟碩. « The dynamics of intruders differing in surface roughness in a vertical vibrated granular bed ». Thesis, 2011. http://ndltd.ncl.edu.tw/handle/11661903960165397163.
Texte intégral國立中央大學
能源工程研究所
99
This study investigates experimentally the Brazil-nut effect in a quasi-2D vertical vibrated granular bed, the only difference lying in the surface roughness of the larger disks (or called intruders). The so-called “Brazil nut problem” means the larger particle rises to the top of the container and the smaller particles move to the bottom. The dynamics of the larger disk is recorded by using a high speed camera. The effects of vibration conditions and filling height of the granular bed on the dynamics of intruder are investigated in the study. The results show that the rising velocity decreases with increasing granular bed filling height. It also shows that the rising time becomes faster with the larger dimensionless vibration acceleration and smaller vibration frequency is applied in the granular system. However, the rise time of the rough disks is smaller than the smooth one because of the larger energy dissipation of the rough disks. Additionally, the difference in the rising time between the rough and smooth intruders is more significant with the smaller dimensionless vibration acceleration, higher vibration frequency and higher granular bed filling height.
Zhang, Y., M. Rubinato, E. Kazemi, Jaan H. Pu, Y. Huang et P. Lin. « Numerical and experimental analysis of shallow turbulent flow over complex roughness beds ». 2019. http://hdl.handle.net/10454/17144.
Texte intégralA set of shallow-water equations (SWEs) based on a k-epsilon Reynold stress model is established to simulate the turbulent flows over a complex roughness bed. The fundamental equations are discretized by the second-order finite-difference method (FDM), in which spatial and temporal discretization are conducted by staggered-grid and leap-frog schemes, respectively. The turbulent model in this study stems from the standard k-epsilon model, but is enhanced by replacing the conventional vertical production with a more rigorous and precise generation derived from the energy spectrum and turbulence scales. To verify its effectiveness, the model is applied to compute the turbulence in complex flow surroundings (including a rough bed) in an abrupt bend and in a natural waterway. The comparison of the model results against experimental data and other numerical results shows the robustness and accuracy of the present model in describing hydrodynamic characteristics, especially turbulence features on the complex roughness bottom.
National Key Research and Development Program of China (Grant No: 2016YFE0122500, 2013CB036401 and 2013CB036402), China Postdoctoral Science Foundation (Grant No: 2016M591184) and Programme of Introducing Talents of Discipline to Universities (Grant No: BC2018038)
Research Development Fund Publication Prize Award winner, June 2019.
SINGH, ABHINAV. « STUDY OF THE BEHAVIOUR OF HYDRAULICS JUMP OVER ROUGH HORIZONTAL BED USING DIFFERENT SIZES OF WOODEN BLOCKS ». Thesis, 2016. http://dspace.dtu.ac.in:8080/jspui/handle/repository/14662.
Texte intégralHoroshenkov, Kirill V., Andrew Nichols, Simon J. Tait et G. A. Maximov. « The pattern of surface waves in a shallow free surface flow ». 2013. http://hdl.handle.net/10454/9579.
Texte intégralThis work presents new water surface elevation data including evidence of the spatial correlation of water surface waves generated in shallow water flows over a gravel bed without appreciable bed forms. Careful laboratory experiments have shown that these water surface waves are not well-known gravity or capillary waves but are caused by a different physical phenomenon. In the flow conditions studied, the shear present in shallow flows generates flow structures, which rise and impact on the water-air interface. It is shown that the spatial correlation function observed for these water surface waves can be approximated by the following analytical expression W(rho) = e(-rho 2/2 sigma w2)COS(2 pi L-0(-1)rho). The proposed approximation depends on the spatial correlation radius, sigma(w), characteristic spatial period, L-0, and spatial lag, . This approximation holds for all the hydraulic conditions examined in this study. It is shown that L-0 relates to the depth-averaged flow velocity and carries information on the shape of the vertical velocity profile and bed roughness. It is also shown that sigma(w) is related to the hydraulic roughness and the flow Reynolds number.
Lacey, Ralph William Jay. « The hydrodynamics associated with instream large roughness elements in gravel-bed rivers = L'hydrodynamique associée aux éléments de rugosité dans les rivières à lit de graviers ». Thèse, 2007. http://hdl.handle.net/1866/18281.
Texte intégralMartín, Violeta. « Hydraulic roughness of armoured gravel beds : the role of grain protrusion ». Thesis, 2003. http://hdl.handle.net/2429/14800.
Texte intégralJing, H., C. Li, Yakun Guo, L. Zhu et Y. Li. « Numerical modeling of flow in continuous bends from Daliushu to Shapotou in Yellow River ». 2014. http://hdl.handle.net/10454/10657.
Texte intégralThe upper reach of the Yellow River from Daliushu to Shapotou consists of five bends and has complex topography. A two-dimensional Re-Normalisation Group (RNG) k-ε model was developed to simulate the flow in the reach. In order to take the circulation currents in the bends into account, the momentum equations were improved by adding an additional source term. Comparison of the numerical simulation with field measurements indicates that the improved two-dimensional depth-averaged RNG k-ε model can improve the accuracy of the numerical simulation. A rapid adaptive algorithm was constructed, which can automatically adjust Manning's roughness coefficient in different parts of the study river reach. As a result, not only can the trial computation time be significantly shortened, but the accuracy of the numerical simulation can also be greatly improved. Comparison of the simulated and measured water surface slopes for four typical cases shows that the longitudinal and transverse slopes of the water surface increase with the average velocity upstream. In addition, comparison was made between the positions of the talweg and the main streamline, which coincide for most of the study river reach. However, deviations between the positions of the talweg and the main streamline were found at the junction of two bends, at the position where the river width suddenly decreases or increases.
National Natural Science Foundation of China (Grants No. 11361002 and 91230111), the Natural Science Foundation of Ningxia, China (Grant No. NZ13086), the Project of Beifang University of Nationalities, China (Grant No. 2012XZK05), the Foreign Expert Project of Beifang University of Nationalities, China, and the Visiting Scholar Foundation of State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, China (Grant No. 2013A011).
Grant, Michael. « New modelling and simulation methods to support clean marine propulsion ». Thesis, 2021. http://hdl.handle.net/1828/13308.
Texte intégralGraduate