Bibliografías temáticas / River processes

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Literatura académica sobre el tema "River processes"

Autor: Grafiati
Publicado: 10 de marzo de 2023
Última modificación: 31 de julio de 2025

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Artículos de revistas sobre el tema "River processes"

1

Vandenberghe, Jef, and Ming-ko Woo. "Modern and ancient periglacial river types." Progress in Physical Geography: Earth and Environment 26, no. 4 (2002): 479–506. http://dx.doi.org/10.1191/0309133302pp349ra.

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Climate has been proposed conventionally as the primary factor that determines periglacial river activity (aggradation) and pattern (braided). This concept does not explain the rich diversity in river patterns and morphological processes in both the present and past periglacial environments: besides braided rivers and sandur, meandering, anabranching, transitional and deltaic rivers also occur. A first attempt is made to combine past and present periglacial river types with regard to their morphology, processes and environments. The processes that control river energy and morphology are discus
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2

Delina, Aija, Alise Babre, Konrads Popovs, Juris Sennikovs, and Baiba Grinberga. "Effects of karst processes on surface water and groundwater hydrology at Skaistkalne Vicinity, Latvia." Hydrology Research 43, no. 4 (2012): 445–59. http://dx.doi.org/10.2166/nh.2012.123.

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The Skaistkalne area in Latvia is one of the places where karst processes in gypsum strata occurs. The Iecava and Memele rivers border the area with extensive surface karst features such as sinkholes and karst lakes. Earlier investigations suggested a hydraulic connection between the Iecava and Memele rivers exists via the karst conduits due to the water level (WL) difference in the rivers. A set of methods was performed to study the possible connection: dye tracer was applied in the Iecava river and its occurrence was visually observed at the karst lakes and Memele river; the current velocity
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3

Ou, Haidong, Shirong Cai, Wei Fan, et al. "Sustaining the Pearl River: A Critical Review of Changes in Fluvial Geomorphological Processes and the Driving Forces in the Pearl River Basin." Water 16, no. 7 (2024): 1001. http://dx.doi.org/10.3390/w16071001.

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The Pearl River is one of China’s large rivers, the second-largest river and the fourth-longest river in China. Its unique geography, landform, and climate conditions create unique fluvial geomorphological processes. Affected by human activities and climate change, the fluvial geomorphological processes in the Pearl River Basin have undergone significant changes in recent decades, seriously affecting the river’s sustainable development. This paper critically reviews changes in fluvial geomorphological processes and analyzes influencing factors in the Pearl River Basin with a focus on possibili
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4

Lefebvre, Mario, and Fatima Bensalma. "An Application of Filtered Renewal Processes in Hydrology." International Journal of Engineering Mathematics 2014 (May 5, 2014): 1–9. http://dx.doi.org/10.1155/2014/593243.

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Filtered renewal processes are used to forecast daily river flows. For these processes, contrary to filtered Poisson processes, the time between consecutive events is not necessarily exponentially distributed, which is more realistic. The model is applied to obtain one- and two-day-ahead forecasts of the flows of the Delaware and Hudson Rivers, both located in the United States. Better results are obtained than with filtered Poisson processes, which are often used to model river flows.
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5

Yakhno, Oleg, Ihor Hnativ, and Roman Hnativ. "Influence of cavitation processes on river water purification of mountain streams." Mechanics and Advanced Technologies 6, no. 1 (2022): 62–69. http://dx.doi.org/10.20535/2521-1943.2022.6.1.254613.

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Problems: The article considers the study of the influence of cavitation phenomena in hydrodynamically active areas of mountain rivers on the processes of natural self-purification of water. The paper considers the experimental results of determining the change in seasonal indicators of the hydrochemical composition of surface waters in the Stryi river basin.
 Objective: to determine the impact of hydrodynamically active areas (HAA) of mountain rivers on the processes of natural self-purification and to develop methods of laboratory modeling of these areas to determine the hydrochemical p
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6

Timuhins, Andrejs, Valērijs Rodinovs, and Māris Kļaviņš. "Wavelet analysis of the Baltic region river runoff longh-term trends and fluctuations." Proceedings of the Latvian Academy of Sciences. Section B. Natural, Exact, and Applied Sciences. 64, no. 5-6 (2010): 229–35. http://dx.doi.org/10.2478/v10046-011-0009-1.

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Wavelet analysis of the Baltic region river runoff longh-term trends and fluctuations The study of changes in river discharge and flood regime can provide important information on climate change and its impacts. Wavelet analysis offers new possibilities to study changes of river discharge patterns in regard to periodical processes on a background of climate change. In this study wavelet analysis was used to study long-term changes of river discharge in the Baltic region. Periodic oscillations of discharge intensity, and low- and high-water flow years are common for the major rivers in the East
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7

Ghimire, Motilal, and Puspa Sharma. "Geomorphic assessment of morphology of Siwalik origin rivers in Far-west Nepal." Journal of Nepal Hydrogeological Association 1 (September 1, 2024): 16–42. https://doi.org/10.3126/jnha.v1i1.78220.

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Geology, tectonics, topography, climate, land use, and human activity impact river morphology significantly, affecting downstream morphology and hydrology. In Nepal, rivers traversing complex geology and active tectonics are subjected to intense weathering and erosion, resulting in a high sediment yield and substantial impacts on river morphology. Despite the importance of understanding river morphology, studies on Himalayan rivers remain limited. This study investigates the characteristics of basin and river morphonology of the Siwalik origin river in far-west Nepal using GIS, remote sensing,
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Tsaryk, Petro, Lyubomyr Tsaryk, and Ihor Vitenko. "CARTOGRAPHIC SUPPORT OF TRANSFORMATIONAL GEOECOLOGICAL PROCESSES IN THE DZHURYN RIVER BASIN." SCIENTIFIC ISSUES OF TERNOPIL VOLODYMYR HNATIUK NATIONAL PEDAGOGICAL UNIVERSITY. SERIES: GEOGRAPHY 59, no. 2 (2025): 89–98. https://doi.org/10.25128/2519-4577.25.2.10.

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The growth of anthropogenic impact on the natural environment of basin systems in the context of global climate change causes significant changes in the state of the constituent geosystems, reduces the quality of water, biotic and land resources, creates a danger to the existence of ecosystems and humanity. In this context, there is a need to create new tools for nature management and nature conservation. This function can be performed by cartographic research of the river basin system. The scientific foundations of the development of a comprehensive cartographic research of the river basin sy
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Wohl, Ellen. "Geomorphic context in rivers." Progress in Physical Geography: Earth and Environment 42, no. 6 (2018): 841–57. http://dx.doi.org/10.1177/0309133318776488.

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Geomorphic context refers to the geomorphic setting of a river reach, which is defined as a length of river with consistent valley and channel geometry. Context includes spatial dimensions of geometry, location within a drainage basin, and location within a global context. Context also includes temporal dimensions of the frequency and duration of specific processes influencing the river reach and the historical sequence of natural and human-induced processes that continue to influence process and form in the river reach. These spatial and temporal characteristics interact to create a geomorphi
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10

Li, Pushuang, Dan Li, Xiaoqing Sun, Zhaosheng Chu, Ting Xia, and Binghui Zheng. "Application of Ecological Restoration Technologies for the Improvement of Biodiversity and Ecosystem in the River." Water 14, no. 9 (2022): 1402. http://dx.doi.org/10.3390/w14091402.

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With global warming, urbanization, and the intensification of human activities, great pressures on river ecosystems have caused ecosystem degradation, the decline in habitats and biodiversity, and the loss of function. Ecological restoration technologies (ERTs) in rivers are effective measures for improving habitat and biodiversity, which has the advantage of recovering ecosystems and biodiversity and promoting the formation of healthy rivers. Several applications of ERTs, including ecological water transfer, fish passage construction, dam removal/retrofit, channel reconfiguration, river geomo
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Tesis sobre el tema "River processes"

1

Tassi, Pablo. "Numerical modelling of river processes: flow and river bed deformation." Enschede : University of Twente [Host], 2007. http://doc.utwente.nl/57998.

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VISCONTI, FRANCESCO. "Disclose river morphodynamics processes through experiments." Doctoral thesis, Politecnico di Torino, 2012. http://hdl.handle.net/11583/2502647.

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Rivers’ behavior is increasingly of interest to wide engineering and scientific communities. In fact, fluvial dynamics have an impact on infrastructure and anthropic environments as well as on natural habitats. In addition, the economic values of river as routes of commerce is great, as is the importance of precious minerals deriving from fluvial sedimentary structures. One of the more fascinating river’s peculiarity is the wide range of space and time scales that impact on the overall fluvial dynamics: from the small scales typical of turbulence that are responsible for the motion of s
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3

Pernik, Maribeth. "Mixing processes in a river-floodplain system." Thesis, Georgia Institute of Technology, 1985. http://hdl.handle.net/1853/19514.

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Dong, Na. "Border ice processes on the Saint Lawrence River." Thesis, Université Laval, 2011. http://www.theses.ulaval.ca/2011/28450/28450.pdf.

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Border ice is one of many ice freeze-up processes, but it is discussed only to a limited extent in the literature. Border ice formation can be a precursor for ice jam formation that may restrict navigation and lead to flooding. This master’s thesis is mainly devoted to the research on the border ice on the Saint Lawrence River from Montréal to Québec City. This reach stays artificially open all winter because commercial ships are continuously preventing a full ice cover to form. The traffic also limits the extent of border ice. This study provides key information on ice formation and
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5

Trieu, Hai Q. "Bank erosion processes along the lower Mekong River." Thesis, University of Southampton, 2012. https://eprints.soton.ac.uk/340011/.

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This project conducts an analysis of bank erosion processes on a large, monsoonaffected river, the Lower Mekong River in Laos. The methodological approach taken was to build integrated models of bank erosion processes at three study sites on the Lower Mekong River in Laos (Friendship Bridge, Ang Nyay and Pakse) to simulate processes of (i) groundwater seepage and pore water pressure evolution, (ii) the effect of this on mass-wasting (using the Geo-slope model) and, (iii) fluvial erosion (using a model adapted from Kean and Smith, 2006ab). In all cases the models were parameterised using measur
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6

Headey, Jonathan Mark. "Modelling of river corridors : modelling urban particulate transport processes." Thesis, University of Birmingham, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.289714.

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Markham, Andrew James. "Flow and sediment processes in gravel-bed river bends." Thesis, Queen Mary, University of London, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.308275.

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Phillips, Zachary Rockford. "Holocene Postglacial Fluvial Processes and Landforms in Low Relief Landscapes." Diss., North Dakota State University, 2020. https://hdl.handle.net/10365/32036.

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Postglacial rivers are part of the relatively young low-relief landscape system left behind by glaciers. Over time, postglacial rivers are susceptible to both minor and major channel planform changes as the Earth and its newly exposed rivers adjust to new isostatic and geomorphic equilibriums. Those planform changes result in topographic features that are well preserved among the largely unaltered landscape and offer opportunities to learn about the processes that create them. This work focuses on those minor and major planform changes and the resulting landforms, with a focus on processes eff
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Allread, Tyler M. "Channel Narrowing of the Green River near Green River, Utah: History, Rates, and Processes of Narrowing." DigitalCommons@USU, 1997. https://digitalcommons.usu.edu/etd/6525.

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Previous scientific research has documented channel narrowing on the Green River near Green River, Utah, but the exact timing, rates, and causal mechanisms of that narrowing have been the source of disagreement in the scientific literature. This thesis demonstrates that the Green River has narrowed in two separate periods during the last 100 years. The narrowing is driven primarily by changes in the hydrologic regime and not by the invasion of saltcedar. The channel narrowed between 1930 and 1938, when a shift from wetter than normal conditions to a period of draught led to a reduction in rive
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Moretto, J. "Linking River Channel Forms and Processes in Gravel Bed Rivers: Time, Space, Remote Sensing and Uncertainty." Doctoral thesis, Università degli studi di Padova, 2014. http://hdl.handle.net/11577/3423802.

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The “modern” fluvial morphology, is the results of a series of events characterized by both natural and human dynamics. Recognizing the process responsible for particular morphology is not a simple analysis, it can be more difficult or impossible if the data collected have too low resolution or too high uncertainty in relation to the spatial and temporal scale assessed. This work aims to analyse and optimize different data and collection methods, derived from different time, space and resolution scales, with a good equilibrium between time-consuming and results at low uncertainty. Different
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Libros sobre el tema "River processes"

1

1942-, Tinkler K. J., and Wohl Ellen E. 1962-, eds. Rivers over rock: Fluvial processes in Bedrock channels. American Geophysical Union, 1998.

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2

Chang, Howard H. Fluvial processes in river engineering. Krieger Publishing Co., 1992.

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3

H, Chang Howard. Fluvial processes in river engineering. Wiley, 1988.

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4

Toth, Peterpaul G. Vermilion River: Meandering and alluvial processes. Laurentian University, Department of Earth Sciences, 1991.

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Graf, William L. Fluvial processes in dryland rivers. Springer-Verlag, 1988.

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6

Lindenschmidt, Karl-Erich. River Ice Processes and Ice Flood Forecasting. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-28679-8.

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Brilly, Mitja, ed. Hydrological Processes of the Danube River Basin. Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-3423-6.

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Lindenschmidt, Karl-Erich. River Ice Processes and Ice Flood Forecasting. Springer International Publishing, 2024. http://dx.doi.org/10.1007/978-3-031-49088-0.

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E, Darby Stephen, and Simon Andrew, eds. Incised river channels: Processes, forms, engineering, and management. J. Wiley, 1999.

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J, Batalla Ramon, Garcia Celso, and International Conference on River and Catchment Dynamics: Natural Processes and Human Impacts (2004 : Solsona, Spain), eds. Geomorphological processes and human impacts in river basins. IAHS, 2005.

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Capítulos de libros sobre el tema "River processes"

1

Wang, Zhao-Yin, Joseph H. W. Lee, and Charles S. Melching. "Estuary Processes and Managment." In River Dynamics and Integrated River Management. Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-25652-3_9.

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Shen, Hung Tao. "River Ice Processes." In Advances in Water Resources Management. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-22924-9_9.

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Montgomery, David R., and John M. Buffington. "Channel Processes, Classification, and Response." In River Ecology and Management. Springer New York, 1998. http://dx.doi.org/10.1007/978-1-4612-1652-0_2.

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McClimans, T. A. "Estuarine Fronts and River Plumes." In Physical Processes in Estuaries. Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73691-9_4.

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Edmonds, Douglas A., and Rebecca L. Caldwell. "River Delta Processes and Shapes." In Wetlands and Habitats. CRC Press, 2020. http://dx.doi.org/10.1201/9780429445507-9.

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Starosolszky, Odon. "Runoff and River Flow Measurements." In Land Surface Processes in Hydrology. Springer Berlin Heidelberg, 1997. http://dx.doi.org/10.1007/978-3-642-60567-3_23.

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Nestler, John M., Claudio Baigún, and Ian Maddock. "Achieving the aquatic ecosystem perspective: integrating interdisciplinary approaches to describe instream ecohydraulic processes." In River Science. John Wiley & Sons, Ltd, 2016. http://dx.doi.org/10.1002/9781118643525.ch5.

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Brilly, Mitja. "Danube River Basin Coding." In Hydrological Processes of the Danube River Basin. Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-3423-6_4.

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Dai, Zhijun. "Changjiang River Basin Overview." In Changjiang Riverine and Estuarine Hydro-morphodynamic Processes. Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-16-3771-1_1.

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Richards, Keith. "River channel pattern: processes, forms and sedimentology." In Rivers. Routledge, 2024. http://dx.doi.org/10.4324/9781003465799-7.

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Actas de conferencias sobre el tema "River processes"

1

Chandler, J. R., T. C. Hsu, D. T. Hobbs, N. C. Iyer, J. E. Marra, and P. E. Zapp. "Waste Tank Corrosion Program at Savannah River Site." In CORROSION 1994. NACE International, 1994. https://doi.org/10.5006/c1994-94161.

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Abstract The Savannah River Site (SRS) has approximately 35 million gallons of high level radioactive waste stored in 51 underground tanks. For the last 25 years SRS has maintained an active corrosion research and corrosion control and monitoring program for nuclear waste storage tanks. This program is largely responsible for the successful waste storage experience at SRS. The program has consisted of extensive monitoring of the tanks and surrounding environment for evidence of leaks, extensive research to understand the potential corrosion processes, and development and implementation of corr
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2

Duarte, A. A. L. S., and J. M. P. Vieira. "Mitigation of estuarine eutrophication processes by controlling freshwater inflows." In RIVER BASIN MANAGEMENT 2009. WIT Press, 2009. http://dx.doi.org/10.2495/rm090311.

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"River flow and transport processes." In The International Conference On Fluvial Hydraulics (River Flow 2016). CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-9.

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Barros, M. L. C., P. C. C. Rosman, and J. C. F. Telles. "Water quality modelling in tidal wetlands considering flooding and drying processes." In RIVER BASIN MANAGEMENT 2013. WIT Press, 2013. http://dx.doi.org/10.2495/rbm130351.

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Astaraki, A., and F. Fallah. "Connecting river to sea by a 2-D mathematical model." In Coastal Processes 2011. WIT Press, 2011. http://dx.doi.org/10.2495/cp110191.

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Stankevičienė, Rasa, and Oksana Survilė. "Land Drainage Development Processes and Changes in the Context of Runoff Change in Northern Lithuania." In 11th International Conference “Environmental Engineering”. VGTU Technika, 2020. http://dx.doi.org/10.3846/enviro.2020.807.

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The impact of the drainage of excessively wet land on river runoff has so far been assessed differently and very carefully because of its complexity and diversity. The article analyses changes of drained land areas and runoff in the river basins of Mūša, Lėvuo Tatula and Nemunėlis. Wet land areas in the Mūša, Lėvuo and Nemunėlis rivers basins account for more than 70% from the total basins area and in the Tatula about 90%. Increase of drained land areas in the studied river basins has no significant influence on the change of river runoff. Studies have shown that the change in drained land are
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Bernard, Jerry M., and Ronald W. Tuttle. "Stream Corridor Restoration: Principles, Processes, and Practices." In Wetlands Engineering and River Restoration Conference 1998. American Society of Civil Engineers, 1998. http://dx.doi.org/10.1061/40382(1998)55.

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Holste, N. "Restoring natural river processes through channel realignment." In The International Conference On Fluvial Hydraulics (River Flow 2016). CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-324.

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Visescu, Erika. "RIVER BED PROCESSES MODELLING. STUDY CASE � MODELLING ON CRASNA RIVER SECTOR." In 17th International Multidisciplinary Scientific GeoConference SGEM2017. Stef92 Technology, 2017. http://dx.doi.org/10.5593/sgem2017/31/s12.069.

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Nico, Peter, Dipankar Dwivedi, Patricia Fox, et al. "River Corridor Processes Across Scales in the East River of Colorado." In Goldschmidt2022. European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12282.

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Informes sobre el tema "River processes"

1

Day, T. J. River Processes [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131644.

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Ashmore, P., and M. Church. The impact of climate change on rivers and river processes in Canada. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/211891.

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Field, John, Susannah Erwin, Christina Leonard, et al. Best practices for managing bank erosion within the National Park Service and National Wild and Scenic River System. National Park Service, 2025. https://doi.org/10.36967/2306106.

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Riverbank erosion is a natural process that occurs as rivers adjust to disturbance events and to changes in water and sediment delivery over time. The resulting lateral movement of river channels is fundamental to building complex, dynamic, and resilient landscapes. In this sense, bank erosion is crucial to creating healthy rivers and should be preserved whenever possible. However, river managers may deem protection from bank erosion necessary if bank retreat threatens infrastructure, developed land, or other valuable natural and cultural resources. The National Park Service manages over 220,0
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Conway, K. W., B. D. Bornhold, and J. V. Barrie. Surficial geology and sedimentary processes, Skeena River delta, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207870.

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Orebaugh, E. Adaptation of U(IV) reductant to Savannah River Plant Purex processes. Office of Scientific and Technical Information (OSTI), 1986. http://dx.doi.org/10.2172/5620962.

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Huntley, D., and A. Duk-Rodkin. Landslide processes in the south-central Mackenzie River valley region, Northwest Territories. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2006. http://dx.doi.org/10.4095/222392.

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Kostaschuk, R. A., and 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.

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Biedenharn, David S., and Maureen K. Corcoran. A Literature Review of Processes for Gravel Deposit Identification in the Lower Mississippi River. Defense Technical Information Center, 2010. http://dx.doi.org/10.21236/ada526307.

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Figueroa, Steven, and Minwoo Son. Estuarine dams and weirs : global analysis and synthesis. Engineer Research and Development Center (U.S.), 2025. https://doi.org/10.21079/11681/49804.

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Estuarine dams and weirs are constructed in estuaries for blocking the salt intrusion, securing freshwater, and stabilizing upstream water levels. While they can provide many social benefits, they also alter physical and sedimentary processes. To address this, we perform and extensive remote sensing and literature analysis. Remote sensing was conducted based on a global river database of 1531 rivers representing the largest rivers cumulatively draining 85 % of the landmass discharging into the global ocean. It was found that 9.7 % of global estuaries and deltas are currently affected by estuar
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Smith, S. Jarrell, David W. Perkey, and Kelsey A. Fall. Cohesive Sediment Field Study : James River, Virginia. U.S. Army Engineer Research and Development Center, 2021. http://dx.doi.org/10.21079/11681/41640.

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Estuaries trap much of the fine sediment delivered to them by rivers. This phenomenon presents challenges to the US Army Corps of Engineers (USACE) navigation mission, which maintains navigable waterways for waterborne commerce through estuarine regions. The USACE Regional Sediment Management Program and the USACE Norfolk District are conducting a regional sediment transport modeling study to identify cost-effective sediment management schemes in the James River, a tributary estuary of Chesapeake Bay. A key element of the sediment transport modeling study is the definition of cohesive sediment
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