Relevant bibliographies by topics / Fluvial sediments

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Fluvial sediments'

Author: Grafiati
Published: 4 June 2021
Last updated: 26 July 2025

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Journal articles on the topic "Fluvial sediments"

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Rosales-Hoz, L., A. Carranza-Edwards, C. Mendez-Jaime, and M. A. Monreal-Gómez. "Metals in shelf sediments and their association with continental discharges in a tropical zone." Marine and Freshwater Research 50, no. 3 (1999): 189. http://dx.doi.org/10.1071/mf98107.

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Geochemical studies of shelf sediments of the south-eastern Gulf of Mexico were carried out to understand the influence of fluvial and fluvio–lagoonal discharges on sediment geochemistry and to study elemental distribution patterns that could be used together with hydrographic and sedimentological data to assess depth circulation. On the basis of sediment chemical composition, three provinces were identified: fluvial, fluvio–lagoonal and calcareous; their distribution is a function of circulation patterns and fluvio and fluvio–lagoonal discharges. Factor analysis separated the sediments into t
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Woronko, Barbara, Paweł Zieliński, and 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 (2015): 89–103. http://dx.doi.org/10.1515/logos-2015-0005.

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Abstract We present results of research into fluvial to aeolian successions at four sites in the foreland of the Last Glacial Maximum, i.e., the central part of the “European Sand Belt”. These sites include dune fields on higher-lying river terraces and alluvial fans. Sediments were subjected to detailed lithofacies analyses and sampling for morphoscopic assessment of quartz grains. Based on these results, three units were identified in the sedimentary succession: fluvial, fluvio-aeolian and aeolian. Material with traces of aeolian origin predominate in these sediments and this enabled conclus
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Liu, Zhe, Jinsong Yang, Hua Zhao, Lei Song, and Chengmin Wang. "Luminescence Dating of Holocene Fluvial Sediments from the Daluze Area in the North China Plain." Water 17, no. 13 (2025): 1942. https://doi.org/10.3390/w17131942.

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Optically stimulated luminescence (OSL) dating is an important method for determining the ages of late Quaternary sediments. However, partial bleaching of quartz in fluvial sediments remains a challenge, with debates on grain-size effects in different sedimentary environments. The aim of this paper is to explore the bleaching degree and its influencing factors of different grain-size quartz in fluvial sediments from the Yanchi section in the Daluze area, North China Plain. According to sedimentological methods and grain size analysis, lacustrine and fluvial layers were identified, and the ages
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Marinho, Rogério Ribeiro, Antonio Fábio Sabbá Guimarães Vieira, and Feliciano De Souza Maciel. "Análise Montante-Jusante da Granulometria dos Sedimentos de Fundo e Suspenso do Rio Negro e Tributários (Bacia Amazônica, Brasil)." Revista Brasileira de Geografia Física 14, no. 2 (2021): 997. http://dx.doi.org/10.26848/rbgf.v14.2.p997-1008.

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O conhecimento das características físicas de sedimentos transportados por grandes sistemas fluviais possui significativa importância para o entendimento de processos geomorfológicos e hidrológicos. O nível de conhecimento dos grandes sistemas fluviais da Amazônia e sua relação com o transporte de sedimentos ainda é limitado, resultando em lacunas de conhecimento sobre a dinâmica da paisagem nesta complexa região. Este trabalho teve como objetivo avaliar a distribuição espacial da granulometria de sedimentos de fundo e suspenso do Rio Negro e tributários. Realizou-se análise da distribuição do
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Sawakuchi, André Oliveira, Vinicius Ribau Mendes, Fabiano do Nascimento Pupim, et al. "Optically stimulated luminescence and isothermal thermoluminescence dating of high sensitivity and well bleached quartz from Brazilian sediments: from Late Holocene to beyond the Quaternary?" Brazilian Journal of Geology 46, suppl 1 (2016): 209–26. http://dx.doi.org/10.1590/2317-488920160030295.

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ABSTRACT: The development of optically stimulated luminescence (OSL) dating of sediments has led to considerable advance in the geochronology of the Quaternary. OSL dating is a well established technique to determine sediment burial ages from tens of years to few hundred thousand years. Recent studies have shown that Quaternary sediments of Brazil are dominated by quartz grains with high luminescence sensitivity, allowing the determination of precise and reliable OSL burial ages. In this paper, we show examples of OSL dating of quartz aliquots and single grains from different regions in Brazil
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Wang, H., and X. Jia. "Selective deposition response to aeolian-fluvial sediment supply in the desert braided channel of the Upper Yellow River, China." Natural Hazards and Earth System Sciences Discussions 3, no. 2 (2015): 1269–90. http://dx.doi.org/10.5194/nhessd-3-1269-2015.

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Abstract. Rivers flow across aeolian dunes and develop braided stream channels. Both aeolian and fluvial sediment supplies regulate sediment transport and deposition in such a cross-dune braided river. Here we show a significant selective deposition in response to both aeolian and fluvial sediment supplies in the Ulan Buh desert braided channel. This selective deposition developed by the interaction between the flows and the Aeolian-fluvial sediment supplies, making the coarser sediments (> 0.08 mm) from aeolian sand supply and bank erosion to accumulate in the channel center and the finer
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Wang, H., X. Jia, Y. Li, and W. Peng. "Selective deposition response to aeolian–fluvial sediment supply in the desert braided channel of the upper Yellow River, China." Natural Hazards and Earth System Sciences 15, no. 9 (2015): 1955–62. http://dx.doi.org/10.5194/nhess-15-1955-2015.

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Abstract. Rivers flow across aeolian dunes and develop braided stream channels. Both aeolian and fluvial sediment supplies regulate sediment transport and deposition in such cross-dune braided rivers. Here we show a significant selective deposition in response to both aeolian and fluvial sediment supplies in the Ulan Buh desert braided channel. The Ulan Buh desert is the main coarse sediment source for this desert braided channel, and the mean percentage of the coarser (> 0.08 mm) grains on the aeolian dunes surface is 95.34 %. The lateral selective deposition process is developed by the in
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Słowik-Opoka, Ewa, and Anna Michno. "Factors Diversifying the Characteristics of Fluvial Sediments Accumulated in Mountain Stream Channels—A Case Study from the Polish Carpathians." Water 16, no. 23 (2024): 3476. https://doi.org/10.3390/w16233476.

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This paper presents the diversification of fluvial sediments caused by the occurrence of coarse woody debris (CWD), boulder steps (BSs), and mixed structures (MSs), understood as a combination of CWD and BSs in a stream channel in a small forested catchment in the Polish Carpathians. This research is crucial for understanding the role of this kind of threshold present in a stream channel in shaping fluvial sediment characteristics in small forested mountain catchments. Our hypothesis is that the threshold type in a stream channel determines fluvial sediment diversification. This was verified i
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Halifa-Marín, A., P. Pérez-Cutillas, M. Almagro, and C. Boix-Fayos. "Presión antrópica sobre cuencas de drenaje en ecosistemas frágiles: variaciones en las existencias (stock) de carbono orgánico asociadas a cambios morfológicos fluviales." Cuadernos de Investigación Geográfica 45, no. 1 (2019): 245. http://dx.doi.org/10.18172/cig.3690.

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Anthropic changes in the drainage area of catchments can influence dominant erosion processes and sediment sources and mobilize specific carbon pools. It also causes changes in the sedimentary dynamics and thus in the fluvial morphology. At the same time fluvial morphologies can create the conditions for stabilizing organic carbon (OC) in sediments by burial, carbon preservation, slowing down mineralization processes, and terrestrial or aquatic plant colonization. All this might have a significant impact on the fluvial carbon sink or sources. This work explores the impact of changes in the dra
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Galia, Tomáš, and Václav Škarpich. "Coarse Bed Sediments in a Headwater Channel as Indicators of Fluvial Processes and Slope-Channel Coupling: A Case Study from the Carpathian Mountains (Czech Republic)." Moravian Geographical Reports 21, no. 3 (2013): 2–11. http://dx.doi.org/10.2478/mgr-2013-0012.

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Abstract The character of riverbed sediments usually reflects fluvial processes and the dynamics of sediment transport in fluvial systems. The approach in this study was based on the measurement of the largest boulders located within a bankfull channel, and on the observation of changes in their size in the longitudinal profile of a headwater stream in the Moravian-Silesian Beskids Mountains. The resulting trends in a particle-size index reflect the character of sediment delivery into channel segments and the recent channel-forming processes. The largest boulders were observed in channel secti
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Dissertations / Theses on the topic "Fluvial sediments"

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Heim, Sabine. "Geochronology of anthropogenic contaminants in fluvial sediments /." Aachen : Shaker, 2005. http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&doc_number=014779100&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA.

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Taylor, Katherine Sarah. "Ephemeral-fluvial sediments as potential hydrocarbon reservoirs." Thesis, University of Aberdeen, 1994. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=123206.

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Although reservoirs formed from ephemeral-fluvial sandstones have previously been considered relatively simple, unresolved problems of sandbody correlation and production anomalies demonstrate the need for improved understanding of their internal complexity. Ephemeral flows occur in direct response to precipitation, receiving little or no water from springs or other long-continued sources. They consequently predominate in dryland regions where precipitation is high in intensity, short lived and of limited areal extent. Resulting flow is high energy, relatively shallow and also restricted in du
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Heim, Sabine [Verfasser]. "Geochronology of Anthropogenic Contaminants in Fluvial Sediments / Sabine Heim." Aachen : Shaker, 2005. http://d-nb.info/118658825X/34.

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Ewald, Karl Heins. "Caracterização de formas topográficas em fundos de vale no Planalto de Cascavel, Região Oeste do Estado do Paraná." Universidade Estadual do Oeste do Paraná, 2013. http://tede.unioeste.br:8080/tede/handle/tede/1655.

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Made available in DSpace on 2017-07-10T17:51:34Z (GMT). No. of bitstreams: 1 Karl_Heins_Ewald.pdf: 3570741 bytes, checksum: c5bdd80e061dc3f0dc6cf78e808ab2d3 (MD5) Previous issue date: 2013-05-09<br>Coordenação de Aperfeiçoamento de Pessoal de Nível Superior<br>Rivers are important agents working in the sculpturing of relief, through its high transport capacity of sediments originary from slopes and marginal erosion. The modeling occurs through the processes of erosion and deposition of sediments, which depend on variables such as lithological composition, slope, and flooding. The processes
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Evans, Dyfed. "Fluvial dispersal of heavy metals in contaminated soils and sediments." Thesis, University of Bradford, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.334773.

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Saup, Casey Morrisroe. "Biogeochemical Cycling in Pristine and Mining-Impacted Upland Fluvial Sediments." The Ohio State University, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=osu1593664378874682.

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Tofelde, Stefanie [Verfasser], and Taylor [Akademischer Betreuer] Schildgen. "Signals stored in sediment : fluvial sediments as records of landscape evolution / Stefanie Tofelde ; Betreuer: Taylor Schildgen." Potsdam : Universität Potsdam, 2018. http://d-nb.info/1218404566/34.

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Guarch, Ribot Alba. "Dissolved organic matter fluctuations in an intermittent headwater stream: from storm oscillations to decadal hydrological changes = Fluctuacions de la matèria orgànica dissolta en un riu de capçalera intermitent : de crescudes a canvis hidrològics decennals." Doctoral thesis, Universitat de Barcelona, 2017. http://hdl.handle.net/10803/406137.

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Dissolved organic matter (DOM) is an important source of carbon for aquatic microorganisms and it regulates many biogeochemical processes. Therefore, changes in river DOM concentration and properties could notably affect the functioning of fluvial and coastal ecosystems and alter the global carbon cycle. The DOM in headwater streams is strongly influenced by hydrology, as a consequence of the modification of catchment flow paths with high discharges. During storm events, the catchment hillsides are washed and terrigenous DOM is transported to rivers. In the Mediterranean region, the precipitat
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Chandra, Shobhit. "Fluvial landforms and sediments in the north-central Gangetic Plain, India." Thesis, University of Cambridge, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.309855.

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Hu, Mengyu. "Plio-Pleistocene environmental variations inferred from thick sediment sequences in the North China Plain." Thesis, University of Oxford, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.363619.

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Books on the topic "Fluvial sediments"

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Williams, Owen R. Methods for collection and analysis of fluvial-sediment data. U.S. Dept. of Agriculture, Forest Service, Watersshed and Air Management Staff, 1988.

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Edwards, Thomas K. Field methods for measurement of fluvial sediment. Dept. of the Interior, U.S. Geological Survey, 1986.

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Douglas, Glysson G., Guy Harold P, and Geological Survey (U.S.), eds. Field methods for measurement of fluvial sediment. U.S. Geological Survey, 1999.

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Smith, Norman D., and J. Rogers. Fluvial sedimentology VI. Blackwell Science, 1999.

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Marriott, Susan B., Suzanne F. Leclair, and Michael D. Blum. Fluvial sedimentology VII. Blackwell Pub., 2005.

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G, Ethridge Frank, Flores Romeo M, and Harvey Michael D, eds. Recent developments in fluvial sedimentology: Contributions from the Third International Fluvial Sedimentology Conference. Society of Economic Paleontologists and Mineralogists, 1987.

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Stevens, Herbert H. Computer programs for computing particle-size statistics of fluvial sediments. U.S. Dept. of the Interior, Geological Survey, 1986.

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Stevens, Herbert H. Computer programs for computing particle-size statistics of fluvial sediments. U.S. Geological Survey, 1986.

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Stevens, Herbert H. Computer programs for computing particle-size statistics of fluvial sediments. U.S. Dept. of the Interior, Geological Survey, 1986.

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Törnqvist, Torbjörn E. Fluvial sedimentary geology and chronology of the Holocene Rhine-Meuse delta, the Netherlands. Koninklijk Nederlands Aardrijkskundig Genootschap, 1993.

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Book chapters on the topic "Fluvial sediments"

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Keen-Zebert, Amanda. "Luminescence, Fluvial Sediments." In Encyclopedia of Scientific Dating Methods. Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6326-5_3-1.

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Keen-Zebert, Amanda. "Luminescence, Fluvial Sediments." In Encyclopedia of Scientific Dating Methods. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6304-3_3.

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Rivard, Lambert A. "Section 7 Fluvial System Sediments." In Satellite Geology and Photogeomorphology. Springer Berlin Heidelberg, 2011. http://dx.doi.org/10.1007/978-3-642-20608-5_8.

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Westrich, Bernd. "Hydromechanic Aspects of Contaminated Sediment Transport in Fluvial Systems." In Sediments and Water Interactions. Springer New York, 1986. http://dx.doi.org/10.1007/978-1-4612-4932-0_6.

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Ebinghaus, R., and R. D. Wilken. "Mercury Distribution and Speciation in a Polluted Fluvial System." In Sediments and Toxic Substances. Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-642-79890-0_9.

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Douglas, Audrey R., Paul A. Montagna, and Timothy Dellapenna. "Influence of Inflows on Estuary Sediments." In Estuaries of the World. Springer Nature Switzerland, 2025. https://doi.org/10.1007/978-3-031-70882-4_6.

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AbstractRivers deliver sediments, organic matter/carbon, contaminants, and nutrients from watersheds. Sediments form delta, estuarine, marsh, and wetland habitats. Most of the sediments are derived from weathered rocks that are transported by rivers during floods as both bedload (sand and gravel) and suspended load (silts and clays, i.e., mud). Siliciclastic sand can enter the estuary naturally through four mechanisms, which are: (1) shoreline erosion; (2) inflow from rivers; (3) advection into the bay via the flood tide, through tidal inlets and cuts; and (4) barrier island overwash. River-mo
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Stokes, Stephen, and Des E. Walling. "Radiogenic and Isotopic Methods for the Direct Dating of Fluvial Sediments." In Tools in Fluvial Geomorphology. John Wiley & Sons, Ltd, 2005. http://dx.doi.org/10.1002/0470868333.ch9.

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Amsler, Mario L., Edmundo C. Drago, and Aldo R. Paira. "Fluvial Sediments: Main Channel and Floodplain Interrelationships." In The Middle Paraná River. Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-70624-3_5.

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Rivard, Lambert A. "Surficial Deposits Group F · Fluvial System Sediments." In Geohazard-associated Geounits. Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/b93844_9.

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Wehmiller, John F. "Amino Acid Racemization, Fluvial and Lacustrine Sediments (AAR)." In Encyclopedia of Scientific Dating Methods. Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6304-3_114.

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Conference papers on the topic "Fluvial sediments"

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Livanov, Oliver, Alexandru Banescu, Adrian Burada, Paula Pindic, and Ciprian Anore. "THE PARTICLE SIZE OF THE BOTTOM SEDIMENTS IN SOME CANALS OF THE FLUVIAL-MARINE DANUBE DELTA." In 24th SGEM International Multidisciplinary Scientific GeoConference 24. STEF92 Technology, 2024. https://doi.org/10.5593/sgem2024/1.1/s01.17.

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In deltaic environments like the Danube Delta, sedimentary particles can range from clay and silt to sand and gravel. The proximity to the Black Sea introduces marine processes into the deltaic system that can be translated as a mixture of fine-grained sediments derived from the fluvial delta along with marine sediments from the Black Sea. This region is of particular importance for the ecology and hydrology of the Danube Delta due to the presence of sandy deposits that cause a major change in both natural and anthropogenic habitats. The emergence of artificial canals dug in sandy deposits had
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STORLAZZI, C. D., L. H. VAN DER HEIJDEN, O. M. CHERITON, R. T. MCCALL, and G. WINTER. "MODELING FLUVIAL SEDIMENT PLUMES: IMPACTS TO CORAL REEFS." In Coastal Sediments 2023. WORLD SCIENTIFIC, 2023. http://dx.doi.org/10.1142/9789811275135_0151.

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Catianis, Irina, Adriana Maria Constantinescu, Dan-Lucian Vasiliu, Bogdan-Adrian Ispas, and Dumitru Grosu. "PHYSICAL AND CHEMICAL CHARACTERISTICS OF TATARU AND MERHEI LACUSTRINE SEDIMENTS, FROM THE DANUBE DELTA, ROMANIA." In 22nd SGEM International Multidisciplinary Scientific GeoConference 2022. STEF92 Technology, 2022. http://dx.doi.org/10.5593/sgem2022/5.1/s20.042.

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The quality and quantity of delta lakes� sediment depend on fluvial input and in-situ bio-geo-chemical processes. The present study investigates the quality of lacustrine sediments collected from two lakes - Tataru and Merhei, situated in different hydrodynamic environments within the Danube Delta, Romania, but both connected to fluvial input of water and sediment of the Danube. The following physical and chemical analyses have been carried out on several lake-bottom sediment samples: the main lithological components (total organic matter-TOM%, total carbonates-CAR% and siliciclastic fraction-
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Abdullatif, Osman, Mutasim Osman, Mazin Bashri, Ammar Abdlmutalib, and Mohamed Yassin. "Sedimentology and Evolution of the Fluvial-Deltaic System: A Modern Depositional Model Analog from the Red Sea Coastal Region, Saudi Arabia." In SPE Middle East Oil & Gas Show and Conference. SPE, 2021. http://dx.doi.org/10.2118/204558-ms.

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Abstract Siliciclastic sediments represent important lithological unit of the Red Sea coastal plain. Their subsurface equivalents are important targets of groundwater aquifer and hydrocarbon reservoirs in the region. The lithofacies of the modern fluvial deltaic system has several distinct geomorphic units and sub-environments such as alluvial, fluvial, delta plain, aeolian, intertidal, coastal sabkha and eustuarine sediments. This study intends to characterize the lithofacies and the depositional environments and to produce an integrated facies model for this modern fluvial-deltaic system. Th
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DOUCETTE, J., and C. PINILLA. "A TALE OF FIVE HARBOURS: FLUVIAL VS. LONGSHORE SEDIMENT SOURCES IN GREAT LAKES HARBOURS." In Coastal Sediments 2015. WORLD SCIENTIFIC, 2015. http://dx.doi.org/10.1142/9789814689977_0133.

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Dezso, Jozsef. "RANDOMLY LAYERED FLUVIAL SEDIMENTS INFLUENCED GROUNDWATER-SURFACE WATER INTERACTION." In 17th International Multidisciplinary Scientific GeoConference SGEM2017. Stef92 Technology, 2017. http://dx.doi.org/10.5593/sgem2017h/33/s12.041.

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Wallace, Corey D., Audrey H. Sawyer, Mohamad Reza Soltanian, and Rebecca Barnes. "NITRATE REMOVAL WITHIN HETEROGENEOUS FLUVIAL SEDIMENTS UNDER TIDAL INFLUENCE." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-338852.

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Jodeau, M., G. Antoine, M. Cormier, Q. Monnoyer, and N. Gratiot. "Settling velocity of sediments from reservoirs, laboratory measurements and numerical modeling." In The International Conference On Fluvial Hydraulics (River Flow 2016). CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-149.

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HUSSAIN, Mazhar, Daniel LEVACHER, Nathalie LEBLANC, Hafida ZMAMOU, Irini DJERAN-MAIGRE, and Andry RAZAKAMANANTSOA. "Possible recycling of dredged sediments in earth bricks - case studies of marine, fluvial and dam sediments." In Journées Nationales Génie Côtier - Génie Civil. Editions Paralia, 2022. http://dx.doi.org/10.5150/jngcgc.2022.078.

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Lo, Edward, Chris Matocha, Michael McGlue, and Aguinaldo Silva. "CLAY MINERALOGY OF MODERN FLUVIAL SEDIMENTS FROM THE PANTANAL BASIN, BRAZIL." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-371057.

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Reports on the topic "Fluvial sediments"

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Moorman, B. J., A. S. Judge, and D. G. Smith. Examining Fluvial Sediments using Ground Penetrating Radar in British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132493.

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Keller, Stephen, and Emily Perman. OF-23-06 Geologic Map of the Wiggins Quadrangle, Morgan County, Colorado. Colorado Geological Survey, 2024. https://doi.org/10.58783/cgs.of2306.zluy3701.

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Located within the northern Colorado Piedmont, the Wiggins 7.5-minute quadrangle consists of gently sloping topography comprised of eolian-mantled uplands paired with alluvial valleys occupied by ephemeral streams. Kiowa Creek and Bijou Creek, both north-flowing tributaries to the South Platte River, are the dominant fluvial courses in the quadrangle and exhibit seasonal flow corresponding with regional rainfall events. Alluvial deposits ranging from Upper Pleistocene to Upper Holocene in age cover most of the quadrangle, filling the modern fluvial drainages as well as multiple north-south-tre
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Lavoie, D., V. Tremblay, and C. Rivard. Sandstone composition and diagenesis of the Paskapoo Formation and their significance for shallow groundwater aquifer in the Fox Creek area, west-central Alberta. Natural Resources Canada/CMSS/Information Management, 2023. http://dx.doi.org/10.4095/331923.

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The shallow aquifer in the Fox Creek area is hosted by the Paleocene Paskapoo Formation. The formation consists of fluvial deposits with channel-filled high-energy sandstone cutting through fine-grained, low energy overbank sediments. Three internal members are recognized, these members define three hydrostratigraphic units (two aquifers versus one aquitard). In fall 2022, three boreholes were drilled and cored. The succession is slightly dominated by sandstone with subordinate fine-grained sediments and thin coal intervals. The calcareous to non-calcareous sandstone is either tight and well c
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4

Lindsey, Kassandra. OF-23-03 Geologic Map of the Loveland Quadrangle, Larimer County, Colorado. Colorado Geological Survey, 2024. https://doi.org/10.58783/cgs.of2303.lvwf5542.

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The Loveland quadrangle is situated in the northern part of the Colorado Piedmont section of the Great Plains. The Upper Cretaceous Niobrara and Pierre Shale underlie the quadrangle and record some of the final sequences of the Cretaceous Western Interior Seaway. They dip at around 18 to 25 degrees on the western border of the mapped area where the units comprise portions of the characteristic Front Range hogbacks. Dips rapidly decrease to the east. Two faults may exist in the subsurface: one on the west side of the quadrangle associated with structures mapped in the adjacent Masonville quadra
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Humphrey, Neil F. Quantifying Fluvial Sediment Transport by Anchor Ice. Defense Technical Information Center, 1999. http://dx.doi.org/10.21236/ada630378.

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Ielpi, A., R. H. Rainbird, and W. J. Davis. Record of Precambrian orogenic unroofing preserved in fluvial strata of western Nunavut. Natural Resources Canada/CMSS/Information Management, 2024. http://dx.doi.org/10.4095/332496.

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Fluvial sandstone in the Kilohigok and Elu basins of western Nunavut record deposition related to the amalgamation and tenure of the Nuna supercontinent. The ca. 1.9 Ga Burnside River Formation was sourced by erosional unroofing of the nearly coeval Thelon Orogen, about 250 km away, in a regime of crustal flexure. This proximally sourced sandstone contains abundant clustered channel forms that point to high-magnitude discharge and sediment yield in weakly mobile channels. By comparison, the ca. 1.6 Ga Ellice Formation was sourced by the erosional unroofing of the ca. 1.8 Ga Trans-Hudson Orogen
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Budzich, Jeffrey. PR-685-184506-R05 Fluvial Geomorphology Equations and Mechanics. Pipeline Research Council International, Inc. (PRCI), 2020. http://dx.doi.org/10.55274/r0011666.

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Channel hydrology, hydraulics, and sediment composition are key variables to calculating vertical and horizontal channel movement. A variety of methods are available for estimating channel bed scour, bank erosion, and channel migration with fewer available to predict avulsion potential. These methods vary in complexity from simplified empirical and theoretical equations to complex multi-dimensional models that may be used to understand potential hydrotechnical threats to pipelines and other structures. Furthermore, there are a variety of publicly available resources of relevant information to
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Thorne, Colin R., and Kevin S. Skinner. Geomorphic Approach to Regional Sediment Management in Engineered and Restored Fluvial Systems. Defense Technical Information Center, 2001. http://dx.doi.org/10.21236/ada396050.

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Echevarria-Doyle, Waleska, S. McKay, and Susan Bailey. Sensitivity of sediment transport analyses in dam removal applications. Engineer Research and Development Center (U.S.), 2023. http://dx.doi.org/10.21079/11681/47595.

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Dam removal has become a widespread river management practice in the US for a variety of goals including ecosystem restoration, removing aging infrastructure, flood risk management, and recreation. The ability to forecast the sediment impacts of dam removal is critical to evaluating different management alternatives that can minimize adverse consequences for ecosystems and human communities. Tullos et al. (2016) identified seven Common Management Concerns (CMCs) associated with dam removal. Four of these CMCs; degree and rate of reservoir sediment erosion, excessive channel incision upstream o
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Ogston, Andrea S. Processes Controlling Transfer of Fine-Grained Sediment in Tidal Systems Spanning a Range of Fluvial Influence. Defense Technical Information Center, 2012. http://dx.doi.org/10.21236/ada572944.

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