Letteratura scientifica selezionata sul tema "Processus estuaire"
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Articoli di riviste sul tema "Processus estuaire":
Drapeau, Georges, e Rémy Morin. "Contribution des vagues au transport des sédiments littoraux dans la région de Trois-Pistoles, estuaire du Saint-Laurent, Québec". Géographie physique et Quaternaire 35, n. 2 (1 febbraio 2011): 245–51. http://dx.doi.org/10.7202/1000441ar.
Dionne, Jean-Claude. "Données quantitatives sur les cailloux à la surface du couvert glaciel, estuaire du Saint-Laurent". Géographie physique et Quaternaire 47, n. 2 (23 novembre 2007): 181–92. http://dx.doi.org/10.7202/032947ar.
Brodeur, Denis, e Michel Allard. "Les plates-formes littorales de l’île aux Coudres, moyen estuaire du Saint-Laurent, Québec". Géographie physique et Quaternaire 37, n. 2 (29 novembre 2007): 179–95. http://dx.doi.org/10.7202/032513ar.
Dinauer, Ashley, e Alfonso Mucci. "Spatial variability in surface-water <i>p</i>CO<sub>2</sub> and gas exchange in the world's largest semi-enclosed estuarine system: St. Lawrence Estuary (Canada)". Biogeosciences 14, n. 13 (6 luglio 2017): 3221–37. http://dx.doi.org/10.5194/bg-14-3221-2017.
Gomes, Vando J. C., Nils E. Asp, Eduardo Siegle, José Diego Gomes, Ariane M. M. Silva, Andrea S. Ogston e Charles A. Nittrouer. "Suspended-Sediment Distribution Patterns in Tide-Dominated Estuaries on the Eastern Amazon Coast: Geomorphic Controls of Turbidity-Maxima Formation". Water 13, n. 11 (1 giugno 2021): 1568. http://dx.doi.org/10.3390/w13111568.
R., Anusiya, e Sukumaran M. "Assessment of Seasonal Variation (2020 to 2021) in Physico-Chemical Parameters of Nandalar Estuary in East Coast of Tamil Nadu, India". International Journal of Zoological Investigations 08, special issue (2022): 254–58. http://dx.doi.org/10.33745/ijzi.2022.v08i0s.030.
Schmidt, Sabine, e Ibrahima Iris Diallo. "Hypoxia also occurs in small highly turbid estuaries: the example of the Charente (Bay of Biscay)". Biogeosciences 21, n. 7 (10 aprile 2024): 1785–800. http://dx.doi.org/10.5194/bg-21-1785-2024.
Braat, Lisanne, Thijs van Kessel, Jasper R. F. W. Leuven e Maarten G. Kleinhans. "Effects of mud supply on large-scale estuary morphology and development over centuries to millennia". Earth Surface Dynamics 5, n. 4 (9 ottobre 2017): 617–52. http://dx.doi.org/10.5194/esurf-5-617-2017.
Conroy, Ted, David A. Sutherland e David K. Ralston. "Estuarine Exchange Flow Variability in a Seasonal, Segmented Estuary". Journal of Physical Oceanography 50, n. 3 (marzo 2020): 595–613. http://dx.doi.org/10.1175/jpo-d-19-0108.1.
Kleinhans, Maarten G., Lonneke Roelofs, Steven A. H. Weisscher, Ivar R. Lokhorst e Lisanne Braat. "Estuarine morphodynamics and development modified by floodplain formation". Earth Surface Dynamics 10, n. 2 (29 aprile 2022): 367–81. http://dx.doi.org/10.5194/esurf-10-367-2022.
Tesi sul tema "Processus estuaire":
Le, Normant Catherine. "Modélisation numérique tridimensionnelle des processus de transport des sédiments cohésifs en environnement estuarien". Toulouse, INPT, 1995. http://www.theses.fr/1995INPT014H.
Voltz, Baptiste. "Dynamique de la matière organique au sein dans les estuaires picards : caractérisation des faciès biosédimentaires et quantification des processus de minéralisation benthique". Thesis, Littoral, 2020. http://www.theses.fr/2020DUNK0579.
Estuaries ensure a high production and transfer a large amount of organic matter (OM) from continent to ocean. To understand OM exchanges at the continent-ocean interface along the eastern English Channel coast, it is primordial to establish a mass balance OM budget in the three main estuaries : the Canche, the Authie and the Somme estuaries. In this frame, the sedimentary OM distribution and origin were studied by coupling a sedimentological description of surficial sediments and an elemental and isotopic characterization of the sedimentary OM. Such approach was carried out from near from subtidal to supratidal stages, along transects transversal to the main river channel, resulting in a sampling of 36, 37 and 39 stations respectively from the Canche, the Authie and the Somme estuaries. Based on this mapping approach, a representative transect was selected in the Canche and the Authie estuaries in order to quantify the sedimentary OM benthic mineralization along the tidal gradient and finally to establish an OM mineralization budget at the estuarine scale. Based on the sedimentological and biological characterization of sediments, the estuarine landscape was described according to four biosedimentary facies : sand flats, mud flats, low and high marshes. This study evidenced that the distribution of OM at the estuary scale is mainly controlled by the distribution of these biosedimentary facies. Indeed, sand flats are subject to intense hydrodynamic conditions in which sedimentary OM deposition is limited. On the other hand, OM is preferentially deposited in fine-grained sediments such as mud flats and salt marshes. Both of these sedimentary environments are subjected to lower hydrodynamic conditions, especially salt marshes, where vegetation enhances deposition and limits the resuspension of sedimentary OM. Indeed, the high quantities of sedimentary OM measured in salt marshes mainly originate from C3 halophytes dominating high marsh areas. Nevertheless, our study also evidenced that the deposition of sedimentary OM along the tidal gradient depends on the contribution of particulate OM from fluvial and marine/estuarine phytoplankton communities. Moreover, this study has demonstrated that various evolutions of the geomorphological features, with a mature salt marsh present in the Cancheestuary, a seaward prograding salt marsh on the north shore of the Authie estuary, a salt marsh retreat on the north shore of the Somme estuary resulting from an advanced sand infilling. The OM benthic mineralization campaigns demonstrated that during immersion and emersion periods, mud flats and salt marshes are the main contributors to total OM mineralization along the tidal gradient in contrast to sand flats. The spatial variation mainly depended on the sedimentological characteristics of each of biosedimentary facies but also on biological factors such as benthic macrofauna, microphytobenthos and root system of halophytes. The OM mineralization budget at the estuarine scale showed a significant contribution of sand flats in the Authie estuary given their wide distribution. This thesis contributes to a better definition of the role of "Picard" estuaries in the OM cycling and allows a first step towards the quantification of a mass balance OM budget in the three main estuaries of the eastern English Channel coast
Lesourd, Sandric. "Processus d'envasement d'un estuaire macrotidal : zoom temporel du siecle a l'heure ; application a l'estuaire de la seine". Caen, 2000. http://www.theses.fr/2000CAEN2049.
Orseau, Sylvain. "Dynamique sédimentaire d'un estuaire tropical sous influence amazonienne : Le cas de l'estuaire du Mahury". Thesis, Littoral, 2016. http://www.theses.fr/2016DUNK0450.
The mud banks migration observed along the Guyanese coastline generates navigating issues, especially for the unique harbor of French Guiana located in the Mahury Estuary. The hydro-sedimentary dynamic of this mesotidal estuary and the influence of the mud banks migration is poorly documented. The main results have brought to light the relative importance of the river discharge and tidal currents on the fine sediment dynamics. Even though the tidal asymmetry is dominated by the flood, the ebb currents are predominant during the wet season and are equivalent to the flood currents during the dry season. The fine sediment dynamics are mainly governed by the resuspension even though some stratification events can highly damp turbulence during the first hours of the ebb. The residual fluxes of sediment are generally landward during the dry season and in the wet season when river discharges are lower than the seasonnal averages. However, the bathymetric evolution over 20 years indicates the stability of the deposits and underlines the estuary's capacity of flushing sediments brought from the mud bank. The interdependence between the Mahury Estuary and the Kaw mudbank will therefore be subject to discussion. It will allow us to evaluate the mud bank influence on the estuarine sedimentology or, inversely, evaluate the capacity of the estuary to interfere with the mud bank migration and slowing down its progression with the currents
Cordier, Mateo. "Ecosystème estuarien et système économique régional: faisabilité d'une intégration par modélisation input-output : application au cas de l'habitat halieutique dans l'estuaire de la Seine". Doctoral thesis, Universite Libre de Bruxelles, 2011. http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/209905.
Doctorat en Sciences agronomiques et ingénierie biologique
info:eu-repo/semantics/nonPublished
Verney, Romaric. "Processus de contrôle de la dynamique des sédiments cohésifs : Mesures in situ, mesures expérimentales et modélisation : Application à l'estuaire de Seine". Rouen, 2006. http://www.theses.fr/2006ROUES032.
Hydrodynamic forcing parameters that influence intertidal ares have been determined in the Seine estuary. These parameters induce sediment erosion, ranging from few millimeters to several centimeters per tide. The knowledge of erosion and deposition mechanisms has led to the development of a semi-empirical 1DV numerical model, simulating the evolution of intertidal areas. Flocculation/deflocculation processes have been studied in lab from natural suspended particulate matter (SPM). Kinetic tests have been carried out with SPM sampled in the Seine estuary. This study has permitted to classify the controlling parameters, representing turbulence, SPM concentration and quality as the predominant parameters. A flocculation numerical model has been developed to simulate the dynamics of natural particles. The comparison of the experimental results and the simulation results allowed evaluating the variability of the collision efficiency as a function of SPM characteristics
Normandeau, Alexandre. "Processus gravitaires tardi-quaternaires dans les canyons et chenaux sous-marins du Saint-Laurent (Est du Canada)". Doctoral thesis, Université Laval, 2015. http://hdl.handle.net/20.500.11794/25907.
Les canyons et chenaux sous-marins sont formés par des courants de densité subaquatiques et sont les principaux conduits par lesquels les sédiments continentaux atteignent les milieux marins profonds. Plusieurs canyons et chenaux sous-marins incisent les marges de l’estuaire et du golfe du Saint-Laurent jusqu’à une profondeur de ≥ 300 m. Des données hydroacoustiques et sédimentologiques récemment acquises ont permis d’analyser en détail la morphologie et les processus sédimentaires tardi-quaternaires qui ont modifié l’architecture de ces systèmes turbiditiques. Quatre types de systèmes turbiditiques ont été identifiés en fonction de leur source respective de sédiments. Un premier type de système, alimenté par la dérive littorale, a été cartographié dans les secteurs de Sept-Îles, Les Escoumins et Tadoussac. La formation et l’évolution de ces trois systèmes semblent être étroitement liées à un apport sédimentaire provenant de l’érosion des rives avoisinantes. Vers la mi-Holocène, alors que la charge sédimentaire provenant des rivières a drastiquement diminué, l’érosion des fronts deltaïques a vraisemblablement contribué à alimenter ces systèmes turbiditiques. L’activité gravitaire est aujourd’hui dominée par des mouvements de masse qui permettent le transfert sédimentaire vers le niveau de base. Un second type de canyon a été découvert dans le secteur de Pointe-des-Monts. Bien qu’il ne reçoive pas d’apport sédimentaire, ce dernier est le seul où des formes en croissant, probablement associées à des courants supercritiques, ont migré récemment. Leur activité holocène peut être expliquée par des mouvements de masse épisodiques et des courants quasi-continus d’origine hydrodynamique se déplaçant sur le plancher marin. Des données sédimentologiques suggèrent que ces courants d’origine hydrodynamique seraient responsables de la formation des canyons. Deux autres types de chenaux et canyons ont été identifiés dans l’estuaire, soit des systèmes reliés aux rivières et aux glaciers. Ces deux types de systèmes ont été actifs majoritairement au début de l’Holocène, alors que la charge sédimentaire transportée vers l’estuaire était plus importante, permettant la génération de courants hyperpycnaux. Ainsi, cette recherche a permis de démontrer la variabilité morphologique des canyons et chenaux de l’estuaire et du golfe du Saint-Laurent ainsi que les différentes phases d’activité et types de processus gravitaires qui ont mené à la formation de systèmes turbiditiques dans un contexte tectonique et climatique similaire.
Submarine canyons and channels are formed by subaqueous sediment density flows and are the main conduits through which continental sediments reach deeper sedimentary basins. Numerous submarine canyons and channels incise the margins of the Estuary and Gulf of St. Lawrence, to a depth of ≥ 300 m. Multibeam bathymetry, acoustic backscatter, seismic reflection and sedimentological analysis have allowed examining in great detail the morphology and the late-Quaternary sedimentary processes within these systems. Four types of submarine fans were identified based on their respective source of sediment. A submarine fan located in ≤ 60 m deep in the Sept-Îles sector has illlustrated the role of longshore drift on the formation and evolution of such systems. Longshore drift, through submarine transverse bars and coastal sand bars, forced the formation of a submarine fan near 5 ka BP. Its activity is now dominated by the passage of low density/intensity flows forming sandwaves on the edge of the coastal shelf and high energy flows (probably slope failures) that allow the accumulation of sediment on the deeper submarine fan. Two other systems fed by longshore drift were identified in the Tadoussac and Les Escoumins sectors, where similar recent episodic activity has been described. A second type of canyon system was discovered in the Pointe-des-Monts sector. These canyons are sediment-starved and yet, they are the only systems in which crescentic bedforms recently migrated upslope. Their short- and long-term activity can be explained by slope failures and quasi-continuous hydrodynamic processes along the seafloor. Sedimentological data suggest that quasi-continuous flows of hydrodynamic origin are responsible for the formation of the canyons. Two other types of channels and canyons were identified in the St. Lawrence: systems fed by rivers and glaciers. Both types of systems were active mainly in the early-Holocene, when sediment supply to the St. Lawrence was greater. When sediment supply drastically diminished during mid-Holocene, erosion of deltaic fronts likely led to an increase in longshore-drift transport and the formation and/or continuated activity of the Sept-Îles and Les Escoumins systems.
Yang, Chengfan. "Li isotope study of Yangtze River sediments : new constraints on climate, weathering and carbon cycle relationships". Electronic Thesis or Diss., Sorbonne université, 2020. https://accesdistant.sorbonne-universite.fr/login?url=https://theses-intra.sorbonne-universite.fr/2020SORUS433.pdf.
In order to better understand the weathering-climate feedback, a series of studies was carried out in the Changjiang (Yangtze) Basin. First, the operation of the Three Gorges Dam (TGD) changed downstream sediment geochemical compositions. Before 2003, large amounts of upstream-derived sediments deposited and experienced further weathering in the mid-lower basin. Since 2003, strong riverbed sediment resuspension changed the roles of the mid-lower reaches from important sinks to major sources of sediments delivered to the sea. As a consequence, an intensified weathering intensity of downstream sediment was observed.Second, dissolved δ7Li exhibit a conservative behavior in the Changjiang Estuary. During the process of SPM transported offshore, weathering product flocculated and deposited, while primary minerals resuspended. The combined effect resulted in the UCC-like SPM δ7Li values. There is a Li isotope fractionation between the dissolved load and exchangeable phase. However, this process shows negligible impact on δ7Li of dissolved load and particulates. Third, weathering response to climate is complex in large river basins. During the Younger Dryas, the positive excursion of clay δ7Li is consistent with enhanced incongruent weathering, in response to temperature cooling. The minor variation of clay δ7Li at 11 – 2 ka likely indicate stable weathering and mile climate variation. Over the last 2 kyr, the fluctuation of clay δ7Li is mostly caused by intensification of human activities. In summary, this thesis sheds new lights on the weathering-climate feedback over geologic past, and provides perspectives on how human activities affect natural processes
Trentesaux, Alain. "Enregistrement de processus sédimentaires pléistocènesExemples de plates-formes détritiques et de bassins profondsMer du Nord et mers de Chine". Habilitation à diriger des recherches, Université des Sciences et Technologie de Lille - Lille I, 2005. http://tel.archives-ouvertes.fr/tel-00140889.
L'objectif des travaux présentés dans ce mémoire est, par une approche sédimentologique, de reconstituer les conditions environnementales, tant sur les continents que sur les plates-formes, ayant conduit aux dépôts étudiés. Sur cette base, nous avons entrepris des études sur des dépôts du Pléistocène en mer du Nord ainsi que dans les mers de Chine de l'Est et du Sud. Cette époque, par sa proximité, permet des études à très haute résolution temporelle tandis qu'elle est caractérisée par des oscillations climatiques et eustatiques importantes et rapides. De plus, les dépôts les plus récents portent la trace de l'Homme.
Sur la plate-forme, l'étude des grands corps sableux, bancs et très grandes dunes, a permis de préciser les mécanismes de leur mise en place. A court terme, même dans les environnements dominés par la marée, l'importance de phénomènes sporadiques tels que les houles de tempêtes, a été démontrée. Ils impriment aux formes et à la structure des fonds marins leur marque tandis que les agents tidaux sont les pourvoyeurs du matériel sédimentaire. A plus long terme, ce ne sont plus les agents dynamiques qui conditionnent la préservation des corps sédimentaires mais la création d'espace disponible et l'importance des apports sédimentaires. Au niveau de l'estuaire de l'Authie, des séries de carottages nous ont aidé à mesurer les conséquences du mouvement vers le nord des divers ensembles sédimentaires sur le type de sédiment rencontré ainsi que sur les modifications d'un espace naturel convoité par l'Homme.
Dans les bassins profonds, en mer de Chine du Sud, nos études ont permis de préciser les sources du matériel sédimentaire et son transport en faisant la part des contributions éolienne, fluviatile et marine. L'étude des caractères sédimentologiques de la fraction détritique a permis également d'étudier la balance ntre l'érosion et l'altération sur les zones émergées ainsi que de voir quelle est la réponse des marqueurs détritiques aux changements climatiques globaux depuis 2 millions d'années.
Webley, James A. C. "The ecology of the mud crab (Scylla serrata): their colonisation of estuaries and role as scavengers in ecosystem processes". Thesis, Griffith University, 2008. http://hdl.handle.net/10072/367091.
Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
School of Environment
Science, Environment, Engineering and Technology
Full Text
Libri sul tema "Processus estuaire":
C, Heip, e Herman P. M. J, a cura di. Major biological processes in European tidal estuaries. Dordrecht: Kluwer Academic Publishers, 1995.
Dronkers, Job, e Wim van Leussen, a cura di. Physical Processes in Estuaries. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73691-9.
Nielsen, Peter. Coastal and estuarine processes. New Jersey: World Scientific, 2009.
J, Dronkers J., Leussen Wim van 1946- e Netherlands. Ministerie van Verkeer en Waterstaat., a cura di. Physical processes in estuaries. Berlin: Springer-Verlag, 1988.
F, Dame Richard, e NATO Advanced Research Workshop on the Role of Bivalve Filter Feeders in Marine Ecosystem Processes (1992 : Renesse, Netherlands), a cura di. Bivalve filter feeders in estuarine and coastal ecosystem processes. Berlin: Springer-Verlag, 1993.
H, McAnally William, Mehta Ashish J e Nearshore and Estuarine Cohesive Sediment Transport Conference (5th : 1998 : Seoul, Korea), a cura di. Coastal and estuarine fine sediment processes. Amsterdam: Elsevier, 2001.
Workshop, on Cohesive Sediment Dynamics with Special Reference to Physical Processes in Estuaries (1984 Tampa Fla ). Estuarine cohesive sediment dynamics: Proceedings of a workshop on cohesive sediment dynamics with special reference to physical processes in estuaries, Tampa, Florida, November 12-14, 1984. Berlin: Springer-Verlag, 1986.
Dai, Zhijun. Changjiang Riverine and Estuarine Hydro-morphodynamic Processes. Singapore: Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-16-3771-1.
Heip, C. H. R., e P. H. J. Herman, a cura di. Major Biological Processes in European Tidal Estuaries. Dordrecht: Springer Netherlands, 1995. http://dx.doi.org/10.1007/978-94-009-0117-9.
Hunt, Simon. Transport processes in the Upper Severn Estuary. Birmingham: University of Birmingham, 1994.
Capitoli di libri sul tema "Processus estuaire":
Semeniuk, Vic, e Margaret Brocx. "Beach Processes". In Encyclopedia of Estuaries, 55–73. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-8801-4_304.
Wiseman, W. J. "Estuarine-shelf interactions". In Baroclinic Processes on Continental Shelves, 109–15. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/co003p0109.
Wollast, R. "Biogeochemical Processes in Estuaries". In Marine Science Frontiers for Europe, 61–77. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-642-55862-7_5.
Wang, Zhao-Yin, Joseph H. W. Lee e Charles S. Melching. "Estuary Processes and Managment". In River Dynamics and Integrated River Management, 467–554. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-25652-3_9.
Simpson, J. H., e I. D. James. "Coastal and estuarine fronts". In Baroclinic Processes on Continental Shelves, 63–93. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/co003p0063.
McClimans, T. A. "Estuarine Fronts and River Plumes". In Physical Processes in Estuaries, 55–69. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73691-9_4.
Mylroie, John E., Michael J. Lace, Patricia N. Kambesis e Joan R. Mylroie. "Karst Processes and Estuarine Coastlines". In Encyclopedia of Estuaries, 373–80. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-017-8801-4_297.
van Leussen, W., e J. Dronkers. "Physical Processes in Estuaries: An Introduction". In Physical Processes in Estuaries, 1–18. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73691-9_1.
Geyer, W. R. "The Advance of a Salt Wedge Front: Observations and Dynamical Model". In Physical Processes in Estuaries, 181–95. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73691-9_10.
West, J. R., e K. Shiono. "The Structure of Turbulence in Partially Mixed Estuaries". In Physical Processes in Estuaries, 196–210. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73691-9_11.
Atti di convegni sul tema "Processus estuaire":
Zhang, Wei, Mingyuan Yang, Xiaolin Zhang e Peipei Dong. "Study on the Characteristics of Temporal and Spatial Variation of Suspended Sediment in the Pearl River Estuary". In ASME 2009 28th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/omae2009-79033.
Yang, Mingyuan, e Wei Zhang. "Study on Salinity Stratification and Distribution in Lingding Yang Estuary". In ASME 2008 27th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2008. http://dx.doi.org/10.1115/omae2008-57123.
Gross, Edward S., Nicholas J. Nidzieko, Michael L. MacWilliams e Mark T. Stacey. "Parameterization of Estuarine Mixing Processes in the San Francisco Estuary Based on Analysis of Three-Dimensional Hydrodynamic Simulations". In 10th International Conference on Estuarine and Coastal Modeling. Reston, VA: American Society of Civil Engineers, 2008. http://dx.doi.org/10.1061/40990(324)20.
Chu, A., Z. B. Wang e H. J. de Vriend. "29. PROCESS-BASED MODELING FOR THE YANGTZE ESTUARY". In Coastal Dynamics 2009 - Impacts of Human Activities on Dynamic Coastal Processes. WORLD SCIENTIFIC, 2009. http://dx.doi.org/10.1142/9789814282475_0032.
Senden, David van, e Douglas Lord. "Estuary Processes Investigation; New South Wales, Australia". In 27th International Conference on Coastal Engineering (ICCE). Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40549(276)288.
Ji, Zhen-Gang, Michael R. Morton e John H. Hamrick. "Modeling Hydrodynamic and Water Quality Processes in a Reservoir". In Eighth International Conference on Estuarine and Coastal Modeling. Reston, VA: American Society of Civil Engineers, 2004. http://dx.doi.org/10.1061/40734(145)38.
Pham Van Bang, Damien, e Patrick Brisset. "Non-Intrusive Devices Applied to Sedimentation and Consolidation". In ASME-JSME-KSME 2011 Joint Fluids Engineering Conference. ASMEDC, 2011. http://dx.doi.org/10.1115/ajk2011-11017.
Pan, Shunqi, Yongping Chen, Yanliang Du, Sam Reed e Judith Wolf. "66. MODELLING OF SEDIMENT TRANSPORT AT EXE ESTUARY, DEVON, UK". In Coastal Dynamics 2009 - Impacts of Human Activities on Dynamic Coastal Processes. WORLD SCIENTIFIC, 2009. http://dx.doi.org/10.1142/9789814282475_0068.
Duarte, A. A. L. S., e J. M. P. Vieira. "Mitigation of estuarine eutrophication processes by controlling freshwater inflows". In RIVER BASIN MANAGEMENT 2009. Southampton, UK: WIT Press, 2009. http://dx.doi.org/10.2495/rm090311.
Iemelianov, V. O., O. M. Ivanik e Т. B. Кulаha. "Estuaries as a component of the Black Sea monitoring system". In XIV International Scientific Conference “Monitoring of Geological Processes and Ecological Condition of the Environment”. European Association of Geoscientists & Engineers, 2020. http://dx.doi.org/10.3997/2214-4609.202056093.
Rapporti di organizzazioni sul tema "Processus estuaire":
Smith, S. Jarrell, David W. Perkey e Kelsey A. Fall. Cohesive Sediment Field Study : James River, Virginia. U.S. Army Engineer Research and Development Center, agosto 2021. http://dx.doi.org/10.21079/11681/41640.
Kastaschuk, R. A., J. L. Luternauer e M. A. Church. Sedimentary processes in the estuary. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1998. http://dx.doi.org/10.4095/210036.
Kostaschuk, R. A., e J. L. Luternauer. Sedimentary processes and their environmental significance: lower main channel, Fraser River estuary. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2004. http://dx.doi.org/10.4095/215799.
Bryan, Frank, John Dennis, Parker MacCready e Michael Whitney. Collaborative Project: Improving the Representation of Coastal and Estuarine Processes in Earth System Models. Office of Scientific and Technical Information (OSTI), ottobre 2016. http://dx.doi.org/10.2172/1329376.
Eisemann, Eve, Catherine Thomas, Matthew Balazik, Damarys Acevedo-Mackey e Safra Altman. Environmental factors affecting coastal and estuarine submerged aquatic vegetation (SAV). Engineer Research and Development Center (U.S.), ottobre 2021. http://dx.doi.org/10.21079/11681/42185.
Bryan, Frank, John Dennis, Parker MacCready e Michael Whitney. Final Report Collaborative Project. Improving the Representation of Coastal and Estuarine Processes in Earth System Models. Office of Scientific and Technical Information (OSTI), novembre 2015. http://dx.doi.org/10.2172/1226494.
Bryan, Frank, John Dennis, Parker MacCready e Michael M. Whitney. Final Report Collaborative Project: Improving the Representation of Coastal and Estuarine Processes in Earth System Models. Office of Scientific and Technical Information (OSTI), settembre 2016. http://dx.doi.org/10.2172/1356337.
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