Littérature scientifique sur le sujet « Sediment transport direction »
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Articles de revues sur le sujet "Sediment transport direction"
Abrantes, João R. C. B., Nuno E. Simões, João L. M. P. de Lima et Abelardo A. A. Montenegro. « Two-dimensional (2D) numerical modelling of rainfall induced overland flow, infiltration and soil erosion : comparison with laboratory rainfall-runoff simulations on a two-directional slope soil flume ». Journal of Hydrology and Hydromechanics 69, no 2 (21 mai 2021) : 140–50. http://dx.doi.org/10.2478/johh-2021-0003.
Texte intégralAl-Salem, K., et A. Al-Rashed. « Modeling of Sediment Transport Using Wave Height action in Fialaka Marina ». IOP Conference Series : Earth and Environmental Science 958, no 1 (1 décembre 2021) : 012023. http://dx.doi.org/10.1088/1755-1315/958/1/012023.
Texte intégralCheng, Wufeng, Shenliang Chen, Jun Zhu, Xiaojing Zhong, Jin Hu et Junli Guo. « Identification of the Sediment Movement Mechanism via Grain Size and Shape : A Case Study of a Beach in Eastern Hainan Island in South China ». Water 15, no 20 (17 octobre 2023) : 3637. http://dx.doi.org/10.3390/w15203637.
Texte intégralABO ZED, ABO BAKER I. « Effects of waves and currents on the siltation problem of Damietta harbour, Nile Delta coast, Egypt ». Mediterranean Marine Science 8, no 2 (3 décembre 2007) : 33. http://dx.doi.org/10.12681/mms.152.
Texte intégralShen, Jian, Dianci Chi et Bingrou Xi. « Sediment distributions and transport patterns in the Pearl River Estuary and its adjacent coastal ocean ». Advances in Engineering Technology Research 8, no 1 (19 octobre 2023) : 398. http://dx.doi.org/10.56028/aetr.8.1.398.2023.
Texte intégralAdel, Mnaf, et Ali N. Hilo. « The Effects of submerged vanes inclination angle on sediment transport into sub-channel ». Wasit Journal of Engineering Sciences 11, no 1 (1 avril 2023) : 105–15. http://dx.doi.org/10.31185/ejuow.vol11.iss1.414.
Texte intégralWalstra, Dirk-Jan, J. De Vroeg, J. Van Thiel de Vries, C. Swinkels, A. Luijendijk, W. De Boer, R. Hoekstra et al. « A COMPREHENSIVE SEDIMENT BUDGET FOR THE MISSISSIPPI BARRIER ISLANDS ». Coastal Engineering Proceedings 1, no 33 (25 octobre 2012) : 81. http://dx.doi.org/10.9753/icce.v33.sediment.81.
Texte intégralWang, Hongbing, Yuxi Wu, Xiaoming Wan, Lu Xia et Si Wang. « Grain Size Characteristics of Surface Sediments and Their Migration Trends in the Nearshore Waters of East Guangdong ». Sustainability 15, no 14 (15 juillet 2023) : 11069. http://dx.doi.org/10.3390/su151411069.
Texte intégralAnokhin, V. M., O. M. Vinogradova, I. M. Pyatov et D. S. Dudakova. « Longshore Sediment Transport in Lake Ladoga Based on Analyses of the Heavy Mineral Fraction of Sand in Coastal Sediments ». Известия Русского географического общества 155, no 3-4 (1 décembre 2023) : 3–16. http://dx.doi.org/10.31857/s0869607123030023.
Texte intégralRachman, Cyril, et Yuyun Qomariyah. « INVESTIGATING THE LITTORAL TRANSPORT OF SEDIMENT ALONG THE NASESE COASTLINE, SUVA, FIJI ISLANDS ». Coastal Engineering Proceedings, no 36v (28 décembre 2020) : 48. http://dx.doi.org/10.9753/icce.v36v.sediment.48.
Texte intégralThèses sur le sujet "Sediment transport direction"
Baville, Paul. « Stratigraphic correlation uncertainty : On the impact of the sediment transport direction in computer-assisted multi-well correlation ». Electronic Thesis or Diss., Université de Lorraine, 2022. http://www.theses.fr/2022LORR0111.
Texte intégralSubsurface modeling is a way to predict the structure and the connectivity of stratigraphic units by honoring subsurface observations. These observations are commonly be sampled along wells at a large and sparse horizontal scale (kilometer-scale) but at a fine vertical scale (meter-scale). There are two types of well data: (1) well logs, corresponding to quasi-continuous (regular sampling) geophysical measurements along the well path (e.g., gamma ray, sonic, neutron porosity), and (2) regions, corresponding to categorical reservoir properties and defined by their top and bottom depths along the well path (e.g., biozones, structural zones, sedimentary facies). Markers are interpreted along the well path and can be associated in order to generate a consistent set of marker associations called well correlations. These well correlations may be generated manually (deterministic approach) by experts, but this may be prone to biases and does not ensure reproducibility. Well correlations may also be generated automatically (deterministic or probabilistic approach) by computing with an algorithm a large number of consistent well correlations and by ranking these realizations according to their likelihood. The likelihood of these computer-assisted well correlations are directly linked to the principle of correlation used to associate markers. This work introduces two principles of correlation, which tend to reproduce the chronostratigraphy and the depositional processes at the parasequence scale: (1) "a marker (described by facies and distality taken at the center of an interval having a constant facies and a constant distality) cannot be associated with another marker described by a depositionally deeper facies at a more proximal position, or a depositionally shallower facies at a more distal position", and (2) "the lower the difference between a chronostratigraphic interpolation (in between markers) and a conceptual depositional profile, the higher the likelihood of the marker association". These two principles of correlation are first benchmarked with analytical solutions and applied on synthetic cases. They have then been used (1) to predict the connectivity of stratigraphic units from well data without strong knowledge on depositional environments by inferring the correlation parameters, or (2) to evaluate the likelihood of a hypothetical depositional environment by generating stochastic realizations and assessing the uncertainties. The methods are applied on a siliciclastic coastal deltaic system targeting a Middle Jurassic reservoir in the South Viking Graben in the North Sea.This work enables (1) to define two specific principles of correlation defined by a few parameters that can be used to generate stochastically well correlations within coastal deltaic systems, and (2) to open the path towards a simple combination of specific principles of correlation to obtain a better characterization of coastal deltaic systems by assessing the uncertainties
van, Gaalen Joseph F. « Longshore Sediment Transport From Northern Maine To Tampa Bay, Florida : A Comparison Of Longshore Field Studies To Relative Potential Sediment Transport Rates Derived From Wave Information Study Hindcast Data ». Scholar Commons, 2004. https://scholarcommons.usf.edu/etd/1280.
Texte intégralXu, Tongtong. « Wave transformation and alongshore sediment transport due to obliquely oriented shoreface-connected ridges ». Thesis, Georgia Institute of Technology, 2015. http://hdl.handle.net/1853/54466.
Texte intégralVilches, Thanira Thammy Bastos. « Relação entre reflectâncias de imagens orbitais e transporte de sedimentos em suspensão no Rio Doce ». Universidade Federal do Espírito Santo, 2013. http://repositorio.ufes.br/handle/10/6134.
Texte intégralSuspended solids transport excess, caused by erosion, may limit water use and cause rivers siltation. Suspended solids concentration may be assessed by remote sensing because the reflectance of the scenes, in the visible and infrared ranges, is positively influenced. This work aims at the understanding of the variability of suspended sediments concentrations in a Doce river stretch located in Espírito Santo state, Brazil, through spectral analysis of satellite images data and analysis of field measurements results. There were analyzed suspended solids concentrations for samples collected in Regência and Colatina Doce river sections and images captured by LANDSAT 5 TM satellite. To obtain reflectance values, the following operations were performed: geometric correction, conversion of DN values to apparent FRB values, atmospheric correction, using the 6S model (FRB surface), and transformation of NCs values.The results showed that, for the images corrected from atmospheric effects, the values of the ND curve related to the apparent FRB are higher than the values of the surface s FRB curve in the visible region, due to the electromagnetic radiation scattering phenomenon. In the near-infrared regions, the reverse was observed, because of the absorption of electromagnetic radiation by the atmosphere. It was observed positive correlation between reflectance and suspended solids concentration, despite the difficulties in obtaining data from same satellite images and field sample collection dates. For Regência data, the best correlation was obtained for band 1, located in the visible range of the surface s FRB curve, suggesting less suspended sediment transport. For Colatina, the best correlation occurred for band 4, located in the near-infrared range of the same surface s FRB curve, indicating greater sediment transport in this part of the Doce river during the sampling dates. It was concluded that the surface reflectance best represents the water spectral curve and that the correlated data showed the following pattern: smaller reflectance corresponds to lower water suspended solids concentration
O transporte de sólidos em suspensão, causado por erosão, é um dos problemas que limitam o uso da água, podendo causar assoreamento nos rios. A concentração de sólidos suspensos pode ser avaliada através do sensoriamento remoto, pois a reflectância da cena, na faixa do visível e do infravermelho, é positivamente influenciada. Desta forma, este trabalho visa o conhecimento da variabilidade das concentrações de sedimentos em suspensão no trecho do rio Doce localizada no ES, através de análises de dados espectrais contidos nas imagens orbitais e de resultados de medições em campo. Para tanto, foram avaliados dados concentrações de sólidos suspensos em amostras coletadas em Regência e Colatina, e imagens TM do satélite LANDSAT 5. Para obtenção dos valores de reflectância, foram realizadas as seguintes operações: correção geométrica, conversão dos NDs para valores de FRB aparente, correção atmosférica com uso do modelo 6S (FRB superfície), e transformação de NCs em valores de reflectância. Os resultados mostraram que nas imagens corrigidas dos efeitos atmosféricos, os valores da curva de ND referentes aos FRBs aparentes são superiores aos valores da curva FRB de superfície na região do visível, devido ao fenômeno de espalhamento da radiação eletromagnética. Nas regiões do infravermelho próximo, ocorreu o inverso, uma vez que há absorção da radiação eletromagnética pela atmosfera. Quanto aos sólidos suspensos, foram encontradas correlações positivas entre a reflectância e a concentração dos sólidos suspensos, apesar das dificuldades de obtenção de dados concomitantes das datas de imagens orbitais com datas da coleta de campo. Para os dados de Regência, a melhor correlação ocorreu para banda 1, que se localiza na faixa do visível, da curva dos FRB de superfície, sugerindo menor transporte de sedimentos suspensos. Para Colatina, ocorreu para banda 4, que se encontra na faixa do infravermelho próximo, também para curva dos FRB de superfície, sugerindo maior transporte de sedimentos nesse trecho do rio Doce, para as datas de amostragem. Conclui-se que a reflectância que melhor representa a curva espectral da água é de superfície e os dados correlacionados seguiram o padrão de quanto menores as reflectâncias, menores as concentrações de sólidos suspensos na água
Heald, J., I. K. McEwan et Simon J. Tait. « Sediment transport over a flat bed in a uni-directional flow : simulations and validation ». 2004. http://hdl.handle.net/10454/3619.
Texte intégralA discrete particle model is described which simulates bedload transport over a flat bed of a unimodal mixed-sized distribution of particles. Simple physical rules are applied to large numbers of discrete sediment grains moving within a unidirectional flow. The modelling assumptions and main algorithms of the bedload transport model are presented and discussed. Sediment particles are represented by smooth spheres, which move under the drag forces of a simulated fluid flow. Bedload mass-transport rates calculated by the model exhibit a low sensitivity to chosen model parameters. Comparisons of the calculated mass-transport rates with well-established empirical relationships are good, strongly suggesting that the discrete particle model has captured the essential elements of the system physics. This performance provides strong justification for future interrogation of the model to investigate details of the small-scale constituent processes which have hitherto been outside the reach of previous experimental and modelling investigations.
Livres sur le sujet "Sediment transport direction"
Passchier, Sandra. Sediment supply and transport directions in the Gulf of Gdańsk as observed from SEM analysis of quartz grain surface textures = : Geneza osadów dennych i źródła materiału osadowego w Zatoce Gdańskiej w świetle analizy SEM powierzchni ziarn kwarcu. Warszawa : Polish Geological Institute, 1997.
Trouver le texte intégralMofjeld, Harold O. Formulas for velocity, sediment concentration and suspended sediment flux for steady uni-directional pressure-driven flow. Seattle, Wash : U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, 1988.
Trouver le texte intégralChapitres de livres sur le sujet "Sediment transport direction"
Kawamura, Kiichiro, Kazumasa Oguri, Mutsuo Inoue, Kan-Hsi Hsiung, Taishi Kudaka et Ken Takai. « Ongoing Persistent Slope Failures at the Toe of a Giant Submarine Slide in the Ryukyu Trench that Generated the AD 1771 Meiwa Tsunami ». Dans Progress in Landslide Research and Technology, Volume 1 Issue 2, 2022, 63–74. Cham : Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-18471-0_5.
Texte intégralYang, Shu-Qing. « Formulae of Sediment Transport in Unsteady Flows (Part 2) ». Dans Sediment Transport - Recent Advances [Working Title]. IntechOpen, 2020. http://dx.doi.org/10.5772/intechopen.94761.
Texte intégralBianchi, Thomas S. « Sources and Distribution of Sediments ». Dans Biogeochemistry of Estuaries. Oxford University Press, 2006. http://dx.doi.org/10.1093/oso/9780195160826.003.0014.
Texte intégralUda, Takaaki, Susumu Onaka et Tomohiro Mori. « Beach Changes Triggered by Ground Subsidence and Waves Generated by Easterly Trade Wind near Pekalongan on North Shore of Java Island ». Dans Sediment Transport Research - Further Recent Advances [Working Title]. IntechOpen, 2024. http://dx.doi.org/10.5772/intechopen.1004907.
Texte intégralKroon, Aart. « Marine and Coastal Environments ». Dans The Physical Geography of Western Europe. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199277759.003.0016.
Texte intégralSakhvadze, David, Gigo Jandieri, Besik Saralidze et Giorgi Sakhvadze. « A novel method of hydro-vacuum dispersion of metallurgical melts : research and implementation ». Dans Sediment Transport Research - Further Recent Advances [Working Title]. IntechOpen, 2024. http://dx.doi.org/10.5772/intechopen.1004129.
Texte intégral« Anadromous Sturgeons : Habitats, Threats, and Management ». Dans Anadromous Sturgeons : Habitats, Threats, and Management, sous la direction de Pierre Nellis, Simon Senneville, Jean Munro, Georges Drapeau, Daniel Hatin, Gaston Desrosiers et François J. Saucier. American Fisheries Society, 2007. http://dx.doi.org/10.47886/9781888569919.ch12.
Texte intégralArmentrout, John M. « Tectonics and paleogeography of a post-accretionary forearc basin, Coos Bay area, SW Oregon, USA ». Dans From Terranes to Terrains : Geologic Field Guides on the Construction and Destruction of the Pacific Northwest, 187–243. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.0062(06).
Texte intégralTrenhaile, A. S. « Tide-Dominated Environments ». Dans Coastal Dynamics and Landforms, 190–211. Oxford University PressOxford, 1997. http://dx.doi.org/10.1093/oso/9780198233534.003.0008.
Texte intégralWelch, J. L., B. Z. Foreman, D. Malone et J. Craddock. « Provenance of early Paleogene strata in the Bighorn Basin (Wyoming, USA) : Implications for Laramide tectonism and basin-scale stratigraphic patterns ». Dans Tectonic Evolution of the Sevier-Laramide Hinterland, Thrust Belt, and Foreland, and Postorogenic Slab Rollback (180–20 Ma). Geological Society of America, 2022. http://dx.doi.org/10.1130/2022.2555(09).
Texte intégralActes de conférences sur le sujet "Sediment transport direction"
Dorokhova, Evgenia, Evgenia Dorokhova, Dmitry Dorokhov et Dmitry Dorokhov. « SEDIMENT MAPPING AND TRANSPORT PATHWAYS IN THE NEARSHORE ZONE OF THE RUSSIAN PART OF THE SOUTH-EASTERN BALTIC SEA ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b9489e8deb2.41910928.
Texte intégralDorokhova, Evgenia, Evgenia Dorokhova, Dmitry Dorokhov et Dmitry Dorokhov. « SEDIMENT MAPPING AND TRANSPORT PATHWAYS IN THE NEARSHORE ZONE OF THE RUSSIAN PART OF THE SOUTH-EASTERN BALTIC SEA ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b43152071d3.
Texte intégralBabakov, Alexander, Alexander Babakov, Boris Chubarenko et Boris Chubarenko. « SEDIMENT TRANSPORT NEAR THE VISTULA SPIT (BALTIC SEA) ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b93751e4b25.42106675.
Texte intégralBabakov, Alexander, Alexander Babakov, Boris Chubarenko et Boris Chubarenko. « SEDIMENT TRANSPORT NEAR THE VISTULA SPIT (BALTIC SEA) ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4315e36e45.
Texte intégralHao, Jialing, Xiaoxin Jiang et Juan Yang. « Three-Dimensional Numerical Model of Wind-Driven Current in a Lake Based on POM Model ». Dans ASME 2009 28th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/omae2009-79898.
Texte intégralJangir, Pramod Kumar, Kevin C. Ewans et Ian R. Young. « Comparison of Ocean Wave Direction Spectra Estimated Using an Array of Three Optech Laser Sensors and a Directional Waverider Buoy ». Dans ASME 2023 42nd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2023. http://dx.doi.org/10.1115/omae2023-101196.
Texte intégralNOSHI, YASUHITO, TAKAAKI UDA, AKIO KOBAYASHI et TAKAYUKI YOSHINO. « UPCOAST EXPANSION OF EROSION OPPOSITE TO DIRECTION OF PREDOMINANT LONGSHORE SAND TRANSPORT OBSERVED IN FUTTSU POINT ». Dans Coastal Sediments 2015. WORLD SCIENTIFIC, 2015. http://dx.doi.org/10.1142/9789814689977_0038.
Texte intégralHan, Xiao, et Ning Zhang. « Coastal Hydrodynamic and Sediment-Salinity Transport Simulations for Southwest Louisiana Using Measured Vegetation Data ». Dans ASME 2015 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2015. http://dx.doi.org/10.1115/imece2015-51571.
Texte intégralBobykina, Valentina, Valentina Bobykina, Boris Chubarenko, Boris Chubarenko, Konstantin Karmanov et Konstantin Karmanov. « MORPHODYNAMICS OF THE SHORES OF THE VISTULA SPIT (THE BALTIC SEA) IN A PERIOD OF 2002-2015 BY RESULTS OF IN-SITU MEASUREMENTS ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b943e73f9e6.07698800.
Texte intégralBobykina, Valentina, Valentina Bobykina, Boris Chubarenko, Boris Chubarenko, Konstantin Karmanov et Konstantin Karmanov. « MORPHODYNAMICS OF THE SHORES OF THE VISTULA SPIT (THE BALTIC SEA) IN A PERIOD OF 2002-2015 BY RESULTS OF IN-SITU MEASUREMENTS ». Dans Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4315ec153d.
Texte intégralRapports d'organisations sur le sujet "Sediment transport direction"
Rice, J. M., M. Ross, H E Campbell, R. C. Paulen et M. B. McClenaghan. Net evolution of subglacial sediment transport in the Quebec-Labrador Sector of the Laurentide Ice Sheet, Quebec and Newfoundland and Labrador. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/332151.
Texte intégralZiegler, Nancy, Nicholas Webb, Adrian Chappell et Sandra LeGrand. Scale invariance of albedo-based wind friction velocity. Engineer Research and Development Center (U.S.), mai 2021. http://dx.doi.org/10.21079/11681/40499.
Texte intégralLi, Honghai, Grace Maze, Kevin Conner et John Hazelton. Sediment transport modeling at Stono Inlet and adjacent beaches, South Carolina. Engineer Research and Development Center (U.S.), décembre 2021. http://dx.doi.org/10.21079/11681/42501.
Texte intégralPtsuty, Norbert, Andrea Habeck et Christopher Menke. Shoreline position and coastal topographical change monitoring at Gateway National Recreation Area : 2017–2022 and 2007–2022 trend report. National Park Service, août 2023. http://dx.doi.org/10.36967/2299536.
Texte intégralPsuty, Norbert, Christopher Menke, Katherine Ames, Andrea Aabeck et Casey Jones. Shoreline position and coastal topographical change monitoring at Assateague Island National Seashore : 2005–2020 trend report. National Park Service, avril 2022. http://dx.doi.org/10.36967/nrr-2293154.
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