Littérature scientifique sur le sujet « FLUVIAL CHARACTERISTICS »
Créez une référence correcte selon les styles APA, MLA, Chicago, Harvard et plusieurs autres
Sommaire
Consultez les listes thématiques d’articles de revues, de livres, de thèses, de rapports de conférences et d’autres sources académiques sur le sujet « FLUVIAL CHARACTERISTICS ».
À côté de chaque source dans la liste de références il y a un bouton « Ajouter à la bibliographie ». Cliquez sur ce bouton, et nous générerons automatiquement la référence bibliographique pour la source choisie selon votre style de citation préféré : APA, MLA, Harvard, Vancouver, Chicago, etc.
Vous pouvez aussi télécharger le texte intégral de la publication scolaire au format pdf et consulter son résumé en ligne lorsque ces informations sont inclues dans les métadonnées.
Articles de revues sur le sujet "FLUVIAL CHARACTERISTICS"
Woronko, Barbara, Paweł Zieliński et Robert Jan Sokołowski. « Climate evolution during the Pleniglacial and Late Glacial as recorded in quartz grain morphoscopy of fluvial to aeolian successions of the European Sand Belt ». Geologos 21, no 2 (1 juin 2015) : 89–103. http://dx.doi.org/10.1515/logos-2015-0005.
Texte intégralLin, Zhipeng, Le Chen, Jingfu Shan, Tan Zhang, Qianjun Sun et Yiwu Wang. « A New Sequence Stratigraphic Framework of Terrestrial Fluvial ». Studies in Engineering and Technology 4, no 1 (30 juillet 2017) : 85. http://dx.doi.org/10.11114/set.v4i1.2521.
Texte intégralHassan, Marwan A., Hal Voepel, Rina Schumer, Gary Parker et Luigi Fraccarollo. « Displacement characteristics of coarse fluvial bed sediment ». Journal of Geophysical Research : Earth Surface 118, no 1 (25 février 2013) : 155–65. http://dx.doi.org/10.1029/2012jf002374.
Texte intégralPayenberg, T. H. D., et S. C. Lang. « RESERVOIR GEOMETRY OF FLUVIAL DISTRIBUTARY CHANNELS—IMPLICATIONS FOR NORTHWEST SHELF, AUSTRALIA, DELTAIC SUCCESSIONS ». APPEA Journal 43, no 1 (2003) : 325. http://dx.doi.org/10.1071/aj02017.
Texte intégralHuang, Kai, Chunsheng Shen, Kai Kang, Libing Wang, Zhongbo Xu et Lin Li. « Characteristics of Mudstone in Complex Fluvial Sedimentary System in Bohai L Oilfield ». Earth Science Research 7, no 2 (8 juillet 2018) : 79. http://dx.doi.org/10.5539/esr.v7n2p79.
Texte intégralZHANG, Yuanfu, Xin DAI, Min WANG et Xinxin LI. « The concept, characteristics and significance of fluvial fans ». Petroleum Exploration and Development 47, no 5 (octobre 2020) : 1014–26. http://dx.doi.org/10.1016/s1876-3804(20)60113-6.
Texte intégralFerreira, Cesar Cardoso, Paulo César Rocha, Arnaldo Yoso Sakamoto et Heloissa Gabriela Silva Sokolowski. « Análise Temporal da Dinâmica de Aspectos Físicos Fluviais no Rio Abobral-Pantanal-MS-BR ». Revista Brasileira de Geografia Física 12, no 7 (29 février 2020) : 2672. http://dx.doi.org/10.26848/rbgf.v12.7.p2672-2684.
Texte intégralGuo, Shao Lei, et Xuan Ying Guo. « The Fluvial Process of Wandering Reach in the Lower Yellow River ». Applied Mechanics and Materials 438-439 (octobre 2013) : 1309–13. http://dx.doi.org/10.4028/www.scientific.net/amm.438-439.1309.
Texte intégralZheng, Dong-Yu, et Si-Xuan Wu. « Principal component analysis of textural characteristics of fluvio-lacustrine sandstones and controlling factors of sandstone textures ». Geological Magazine 158, no 10 (21 mai 2021) : 1847–61. http://dx.doi.org/10.1017/s0016756821000418.
Texte intégralAlexouli - Livaditi, A., K. Vouvalidis, G. Livaditis et S. Pechlivanidou. « Drainage network characteristics of Athens plain at the end of the 19th century ». Bulletin of the Geological Society of Greece 40, no 4 (1 janvier 2007) : 1513. http://dx.doi.org/10.12681/bgsg.17054.
Texte intégralThèses sur le sujet "FLUVIAL CHARACTERISTICS"
Phillips, John Mansell. « The effective particle size characteristics of fluvial suspended sediment ». Thesis, University of Exeter, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.296287.
Texte intégralTamang, Lakpa. « EFFECTS OF BOULDER LIFTING ON THE FLUVIAL CHARACTERISTICS OF LOWER BALASON BASIN IN DARJEELING DISTRICT, WEST BENGAL ». Thesis, University of North Bengal, 2013. http://ir.nbu.ac.in/handle/123456789/949.
Texte intégralLanders, Mark Newton. « Fluvial suspended sediment characteristics by high-resolution, surrogate metrics of turbidity, laser-diffraction, acoustic backscatter, and acoustic attenuation ». Diss., Georgia Institute of Technology, 2011. http://hdl.handle.net/1853/43747.
Texte intégralRieck, Leslie O. « Associations between hydrogeomorphic characteristics and biotic community dynamics in urban streams of Columbus, Ohio, USA ». The Ohio State University, 2019. http://rave.ohiolink.edu/etdc/view?acc_num=osu1563042221041466.
Texte intégralAbouessa, Ashour. « Sedimentological and ichnological characteristics of Dur At Tallah siliciclastic rock sequence, and their significance in the depositional environment interpretation of tidal-fluvial system (Upper Eocene, Sirt Basin, Libya) ». Phd thesis, Université de Strasbourg, 2013. http://tel.archives-ouvertes.fr/tel-00985603.
Texte intégralJohnson, Arvee Sujil. « Yielding characteristics of an overconsolidated fluvio-glacial clay from the Belfast region ». Thesis, Queen's University Belfast, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.263399.
Texte intégralDe, Wilde Mélissa. « Conséquences des exondations pour les communautés végétales aquatiques et le fonctionnement des zones humides fluviales ». Thesis, Lyon 1, 2014. http://www.theses.fr/2014LYO10275/document.
Texte intégralThe objective of this thesis was to measure how changes in hydrological regimes, particularly dewatering govern 1) aspects of the functioning of wetlands, 2) the organization and short-term dynamics of aquatic plant communities and 3 ) survival and plastic response of aquatic plants. This thesis addresses issues at different spatial and temporal scales. First, at the decade scale, I measured the effect of water-level decreases in riverine wetlands on their physico-chemistry characteristics. Second, at the season scale, I measured the influence of sedimentary characteristics of wetlands on short-term response of plant communities to dewatering. Finally, at the scale of a few weeks, I was interested in the ability of aquatic angiosperm species to develop a plastic adjustment to dewatering, in experimental laboratory conditions and in situ, and I looked determinism of this response (ecological, morphological, phylogenetic). In terms of physico-chemical characteristics of surface waters, the 15- year study of the dynamics of riverine wetlands undergoing dewatering, not reached, as is usually described in the literature, with an increase of water body nutrient contents, but rather changes suggesting variations of the hydrogeological functioning of wetlands in favor of a greater influence of the hillslope groundwater table in their water supply. In situ response of plant communities to dewatering differs according to sediment type. Both, resistance and resilience of communities decrease with the sediment water retention capacity. The ability of aquatic plants to tolerate dewatering, in experimental conditions, seems to differ according to their phylogenetic position, but not according to their growth form (rosettes or caulescentes). Species tolerating dewatering show phenotypic adjustments such as denser aerial organs and high plasticity of the leaves, which may explain the maintenance of a similar growth rate in terrestrial and aquatic conditions in these species
Gardes, Thomas. « Reconstruction temporelle des contaminations métalliques et organiques particulaires dans le bassin versant de l'Eure et devenir des sédiments suite à l'arasement d'un barrage. Reconstruction of anthropogenic activities in legacy sediments from the Eure River, a major tributary of the Seine Estuary (France) Flux estimation, temporal trends and source determination of trace metal contamination in a major tributary of the Seine estuary, France Temporal trends, sources, and relationships between sediment characteristics and polycyclic aromatic hydrocarbons (PAHs) and polychlorinated biphenyls (PCBs) in sediment cores from the major Seine estuary tributary, France Impacts à court-terme de l’arasement d’un barrage sur la morphologie du cours d’eau et la remobilisation de sédiments contaminés par les métaux traces Bioaccessibility of polycyclic aromatic compounds (PAHs, PCBs) and trace elements : Influencing factors and determination in a river sediment core ». Thesis, Normandie, 2020. http://www.theses.fr/2020NORMR038.
Texte intégralThe anthropogenic impact on rivers has significantly increased following the industrial revolutioninitiated by Western countries. Thus, changes in the geomorphology of rivers for water storage andnavigation, the conversion of land for agricultural, industrial and urbanization purposes illustrate thisenvironmental pressure, which results, among other things, in an increase in discharges of variouscontaminants into environmental compartments, particularly rivers. Therefore, part of these dischargescan end up in suspended particulate matter, which is then considered as storage wells, which transit inrivers. River development, particularly the construction of dams, encourages the sedimentation of these contaminated particles over time. These sediments of anthropogenic origin, also called legacy sediments, are therefore witnesses to human activities and make it possible to reconstruct the temporal trajectories of contamination within watersheds. The Eure River, a major tributary of the Seine estuary, has experienced significant anthropogenic pressures since the twentieth century. The temporal reconstruction of anthropogenic pressures has required the combination of different methodological approaches: (i) a diachronic analysis of the morphological modifications of the river was carried out, in conjunction with (ii) an analysis of the sedimentary dynamics and the nature of the sediment deposits by coupling geophysical, sedimentological and geochemical methods, and (iii) the setting up of a network for monitoring the hydro-sedimentary behaviour with continuous sampling of suspended particulate matter. Significant geomorphological changes have occurred in the lower reaches of the watershed, with the main consequences being an outlet moved some ten kilometres in the direction of a dam and the formation of hydraulic annexes favouring the accumulation of sediments as early as the 1940s. These made it possible to show that the Eure River watershed had experienced significant contamination, the consequences of which are still being recorded despite the cessation of activities or uses. The temporal trends of trace metal and metalloid elements showed strong contaminations in As in the 1940s and contaminations of industrial origin in Cr, Co, Ni, Cu, Zn, Ag and Cd in the 1960s and 1970s, as well as contaminations in Sb and Pb in 1990–2000. The latter are still recorded despite the cessation of the activities responsible for the discharges, as evidenced by the results from the suspended particulate matter currently collected in the river. Like most trace metals, organic contaminants such as PAHs showed significant contamination during the 1940–1960s, with signatures indicating a predominantly pyrogenic origin. PCBs showed significant contamination during the period 1950–1970, in connection with the production and national uses of mixtures composed mainly of low chlorinated congeners. Finally, interest in a third family of persistent organic contaminants, organochlorine pesticides, showed the use of lindane and DDT, particularly during the 1940–1970 period, and highlighted the post-ban use of lindane and the presence of a metabolite of DDT several decades after the cessation of its use, in connection with the increase in erosion of cultivated soils
Fambrough, Brooke A. « Controls on fluvial longitudinal profile and sediment characteristics predictions from a morphodynamic model / ». 2008. http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-2546/index.html.
Texte intégralDu, Kuan-Ying, et 杜冠穎. « Neotectonic characteristics of Liuchia fault, southwestern Taiwan, from the analysis of fluvial channel morphology ». Thesis, 2013. http://ndltd.ncl.edu.tw/handle/04255177193576822722.
Texte intégral國立臺灣大學
地質科學研究所
101
The Liuchia fault in southwestern Taiwan has been considered as one of the major active faults in the active Taiwan orogen. It is identified by its clear geomorphic features, and forms a major geologic boundary of Taiwan’s Western Foothills. In the twentieth century, several large earthquakes occurred in southwestern Taiwan and caused significant damages. However, there is no unanimous historical evidence for the activity on the Liuchia fault. Therefore, the Liuchia fault poses large hazard potentials for this populous area. Several previous studies have shown that fluvial channel morphology, such as channel slope and width, is strongly influenced by tectonic activities on the assumption of the rock uplift being balanced by the incision of river channels. Base on these hypotheses, it has been shown previously that the analysis of river channel morphology can successfully estimate the activity of potentially active faults in central Taiwan. As a result, we attempted to obtain information of recent activity of the Liuchia fault by analyzing the channel morphology of the Kueichung River, which flows across the fault. We also attempted to calculate the actual river incision rates from the age of river terraces along the river. Such information would enable us to construct the subsurface geometry of this important active structure. We have obtained a detailed river long profile of the Kueichung River from surveys using RTK-GPS, and the channel width profile from actual field measurements using a Laser Rangefinder. The fluvial channel morphology of the Kueichung River appears to have been affected by active folding in the hanging-wall block of the Liuchia fault. Such active deformation pattern is also evident from river incision rate patterns, calculated from the ages and elevations of river terraces along the channel. From the Liuchia fault toward the east, the uplift rate becomes higher, to a highest of 4.6mm/yr at the axis of the Niushan anticline. The uplift rate then becomes lower toward the Chiendapu syncline. The uplift rate pattern indicates the active folding is the uplift mechanism and the fault tip does not extend to the surface yet. We constructed a model of the subsurface geometry of the Liuchia fault, and obtained the trend of dipping angle for the fault plane underneath. Based on this model, we estimated the activity of the Liuchia fault may cause Mw 6.5 earthquakes in the future, and the recurrence interval is about 140yrs. Our results suggest the Liuchia fault has high hazard potential for this populous area, and we need to pay attention to this structure.
Livres sur le sujet "FLUVIAL CHARACTERISTICS"
Lowham, H. W. Characteristics of fluvial systems in the plains and deserts of Wyoming. Cheyenne, Wyo : U.S. Dept. of the Interior, U.S. Geological Survey, 1993.
Trouver le texte intégralGogoi, Swapnali. Advanced Topics on River Study : Fluvio-geomorphological characteristics. LAP Lambert Academic Publishing, 2011.
Trouver le texte intégralChapitres de livres sur le sujet "FLUVIAL CHARACTERISTICS"
Tal, Michal, Karen Gran, A. Brad Murray, Chris Paola et D. Murray Hicks. « Riparian vegetation as a primary control on channel characteristics in multi-thread rivers ». Dans Riparian Vegetation and Fluvial Geomorphology, 43–58. Washington, D. C. : American Geophysical Union, 2004. http://dx.doi.org/10.1029/008wsa04.
Texte intégralWalling, D. E., et P. W. Moorehead. « The particle size characteristics of fluvial suspended sediment : an overview ». Dans Sediment/Water Interactions, 125–49. Dordrecht : Springer Netherlands, 1989. http://dx.doi.org/10.1007/978-94-009-2376-8_12.
Texte intégralPoulos, S. E. « An insight to the fluvial characteristics of the Mediterranean and Black Sea watersheds ». Dans Advances in the Research of Aquatic Environment, 191–98. Berlin, Heidelberg : Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-19902-8_22.
Texte intégralHuang, Huiming, Xiantao Huang, Yuliang Zhu et Siqi Li. « River Regime Evolution of the South Channel in the Changjiang River Estuary, China, During Past 50 Years ». Dans Lecture Notes in Civil Engineering, 1209–19. Singapore : Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-6138-0_106.
Texte intégralMollah, Swati. « Fluvial Characteristics of Dwarka-Mayurakshi Plain Causing Flood in Kandi Block and Impacts of Manmade Embankments on Riparian Environment ». Dans Anthropogeomorphology, 395–409. Cham : Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-77572-8_20.
Texte intégralWan, Zhaohui, et Zhaoyin Wang. « Characteristics of fluvial processes associated with hyperconcentrated flow ». Dans Hyperconcentrated Flow, 189–212. CRC Press, 2020. http://dx.doi.org/10.1201/9781003077671-9.
Texte intégralOguchi, T., Y. S. Hayakawa et T. Wasklewicz. « Remote Data in Fluvial Geomorphology : Characteristics and Applications ». Dans Reference Module in Earth Systems and Environmental Sciences. Elsevier, 2021. http://dx.doi.org/10.1016/b978-0-12-818234-5.00103-6.
Texte intégralGraf, William L. « Fluvial Sediment, Forms, and Processes ». Dans Plutonium and the Rio Grande. Oxford University Press, 1995. http://dx.doi.org/10.1093/oso/9780195089332.003.0009.
Texte intégralCarr, Michael H. « Valley Networks ». Dans Water On Mars, 71–99. Oxford University PressNew York, NY, 1996. http://dx.doi.org/10.1093/oso/9780195099386.003.0004.
Texte intégral« Characteristics of plunging flows in stepped-channel chutes ». Dans Fluvial, Environmental and Coastal Developments in Hydraulic Engineering, 17–26. CRC Press, 2004. http://dx.doi.org/10.1201/9780203023396-4.
Texte intégralActes de conférences sur le sujet "FLUVIAL CHARACTERISTICS"
Headley, Rachel, Amy Johnston, Jessica M. Orlofkse, Benjamin Sieren et Christopher D. Tyrrell. « LINKING FLUVIAL SEDIMENTATION CHARACTERISTICS TO LARVAL DRAGONFLY HABITAT ». Dans Joint 55th Annual North-Central / 55th Annual South-Central Section Meeting - 2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021nc-362825.
Texte intégralAmirshahi, S., C. Winter et E. Kwoll. « Characteristics of instantaneous turbulent events in southern German Bight ». Dans The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742 : CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-32.
Texte intégralvan, R., R. Schielen, A. Blom, M. Kleinhans et S. Hulscher. « Characteristics of side channels in the River Ain, France ». Dans The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742 : CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-39.
Texte intégralPAN, CUNHONG, AIJU YOU et NINGPING FU. « SOME CHARACTERISTICS OF HILLY AND FLUVIAL MACRO-TIDAL CAO'E ESTUARY ». Dans Proceedings of the 13th IAHRߝ;APD Congress. World Scientific Publishing Company, 2002. http://dx.doi.org/10.1142/9789812776969_0196.
Texte intégralWu, Yihong, Baoligao Bai-Yin, Xiangpeng Mu, Shengzong Xie et Shuang Zheng. « Hydrodynamic characteristics in channel flow with submerged flexible aquatic plants ». Dans The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742 : CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-346.
Texte intégralBassie, Abby. « Image-based instrumentation development for measurement of debris flow characteristics ». Dans The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742 : CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-85.
Texte intégralOkamoto, T., H. Takebayashi, T. Kaneko, Y. Shibayama et K. Toda. « Flood-flow characteristics in a blocked river : Detour flow around a bridge ». Dans The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742 : CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-292.
Texte intégralHeidari, M., V. Roussinova, R. Balachandar et R. Barron. « Experimental study of wake characteristics of shallow flow past a single cylinder ». Dans The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742 : CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-54.
Texte intégralDevi, T., et B. Kumar. « A study on the flow characteristics in a finite vegetation patch with downward seepage ». Dans The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742 : CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-127.
Texte intégralKean, Jonathan, Alan Cuthbertson et Lindsay Beevers. « Near-bed turbulence characteristics in unsteady hydrograph flows over mobile and immobile gravel beds ». Dans The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742 : CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-283.
Texte intégralRapports d'organisations sur le sujet "FLUVIAL CHARACTERISTICS"
Cole, E. L., M. L. Fowler, S. R. Jackson, M. P. Madden, V. Raw-Schatzinger, S. P. Salamy, P. Sarathi et M. A. Young. Reservoir Characterization, Production Characteristics, and Research Needs for Fluvial/Alluvial Reservoirs in the United States. Office of Scientific and Technical Information (OSTI), avril 1999. http://dx.doi.org/10.2172/6081.
Texte intégralDavid, Gabrielle C. L., Patrick H. Trier, Ken M. Fritz, Steven L. Kichefski, Tracie-Lynn Nadeau, L. Allan James, Brian J. Topping, Wohl Ellen E. et Aaron Allen. National Ordinary High Water Mark Field Delineation Manual for Rivers and Streams : Interim Version. U.S. Army Engineer Reseach and Development Center, novembre 2022. http://dx.doi.org/10.21079/11681/46102.
Texte intégralCharacteristics of fluvial systems in the plains and deserts of Wyoming. US Geological Survey, 1993. http://dx.doi.org/10.3133/wri914153.
Texte intégral