subject:(bank erosion fluvial geomorphology resources restoration river water)

University of Florida

1. Horan, Andrew M. Streambank Erosion on the Restored Lower Kissimmee River, Florida What Site Factors Influence Rates?.

Degree: MS, Geography, 2012, University of Florida

URL: https://ufdc.ufl.edu/UFE0044170

► The initial purpose of this investigation was to evaluate how different vegetative, sedimentologic, and geomorphic site factors influence erosion rates in an18-km stretch of the… (more)

Subjects/Keywords: Bank erosion; Human geography; Radius of curvature; Riverbanks; Rivers; Sediments; Soils; Stream erosion; Vegetation; Water erosion; bank – erosion – fluvial – geomorphology – resources – restoration – river – water; Kissimmee River ( local )

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APA (6^th Edition):

Horan, A. M. (2012). Streambank Erosion on the Restored Lower Kissimmee River, Florida What Site Factors Influence Rates?. (Masters Thesis). University of Florida. Retrieved from https://ufdc.ufl.edu/UFE0044170

Chicago Manual of Style (16^th Edition):

Horan, Andrew M. “Streambank Erosion on the Restored Lower Kissimmee River, Florida What Site Factors Influence Rates?.” 2012. Masters Thesis, University of Florida. Accessed April 22, 2021. https://ufdc.ufl.edu/UFE0044170.

MLA Handbook (7^th Edition):

Horan, Andrew M. “Streambank Erosion on the Restored Lower Kissimmee River, Florida What Site Factors Influence Rates?.” 2012. Web. 22 Apr 2021.

Vancouver:

Horan AM. Streambank Erosion on the Restored Lower Kissimmee River, Florida What Site Factors Influence Rates?. [Internet] [Masters thesis]. University of Florida; 2012. [cited 2021 Apr 22]. Available from: https://ufdc.ufl.edu/UFE0044170.

Council of Science Editors:

Horan AM. Streambank Erosion on the Restored Lower Kissimmee River, Florida What Site Factors Influence Rates?. [Masters Thesis]. University of Florida; 2012. Available from: https://ufdc.ufl.edu/UFE0044170

University of Kansas

2. Shelley, John Edwin. Geomorphic Equations and Methods for Natural Channel Design.

Degree: PhD, Civil, Environmental, & Architectural Engineering, 2012, University of Kansas

URL: http://hdl.handle.net/1808/9836

► Natural channel design in river engineering is the philosophy and practice of designing stream channels by copying or mimicking the geomorphology of stable, self-formed streams.… (more)

▼ Natural channel design in river engineering is the philosophy and practice of designing stream channels by copying or mimicking the geomorphology of stable, self-formed streams. This dissertation presents methods and equations for incorporating the principals of natural channel design into river and stream engineering in Kansas. Data from 123 reference reaches in Kansas are used to develop these methods and equations. An analysis of 46 gaged reference reaches indicates that the return period of bankfull flow (annual maximum series), ranges from 1.01 to 1.7 years, with an average of 1.2 years. This is significantly lower than the 2-year flow commonly used by engineers in naturalistic river designs. An equation is developed that predicts the 1.2-year flow as a function of watershed drainage area, mean annual precipitation, and the length of the longest flow path in the watershed. This equation is developed using data from 67 gaged streams with drainage areas less than 30 sq miles. Geomorphic measurements from the reference reaches are used to verify previously published relationships between bankfull discharge and bankfull width for streams with sand and gravel beds. A new relationship is developed demonstrating the relationship between bankfull discharge and bankfull width for streams with beds of cohesive clay. Equations are provided to predict the average meander wavelength from the bankfull width, and the pool depth from the depth at the adjacent riffle. Three stream design methods are presented: the Kansas Analytical Method (KAM), the Analytical Reference Reach Method (ARRM), and the Scaled Geomorphic Method (SGM). All three methods are based on natural stream processes and geomorphology. All three methods incorporate the Manning equation for flow resistance and the Meyer-Peter and Muller equation for sediment transport but differ in their use of geomorphic measurements from reference reaches. KAM uses a hydraulic geometry width equation which was developed from many reference reaches. ARRM uses the sinuosity, pool-depth ratio, and meander-width ratio from a single reference reach. SGM calculates a scaling factor that can be used to copy and scale additional cross-sections (pools, runs, and glides, as well as riffles) and planform features from the reference reach. The development of KAM and ARRM is presented in previously published reports. This dissertation presents the development of SGM in detail. KAM, ARRM, and SGM make a common assumption that the median size of sediment in the channel bed is an adequate surrogate for the entire gradation of bed sediments. The reasonableness of this assumption is verified by calculating the bankfull sediment transport capacity for seven ARRM designs. It is found that a channel designed for equilibrium transport of the median sediment size is reasonably designed for transport of the entire gradation of sediment sizes. The exception is when the median sediment size found on the bed is among the largest that are mobile at bankfull flow. These geomorphic relationships,… Advisors/Committee Members: McEnroe, Bruce (advisor), Young, Bryan (advisor), Parr, David (cmtemember), Parsons, Robert L. (cmtemember), Devlin, Frederick (cmtemember).

Subjects/Keywords: Civil engineering; Geomorphology; Water resource management; Fluvial geomorphology; Natural channel design; River engineering; River restoration; Stream realignment

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APA (6^th Edition):

Shelley, J. E. (2012). Geomorphic Equations and Methods for Natural Channel Design. (Doctoral Dissertation). University of Kansas. Retrieved from http://hdl.handle.net/1808/9836

Chicago Manual of Style (16^th Edition):

Shelley, John Edwin. “Geomorphic Equations and Methods for Natural Channel Design.” 2012. Doctoral Dissertation, University of Kansas. Accessed April 22, 2021. http://hdl.handle.net/1808/9836.

MLA Handbook (7^th Edition):

Shelley, John Edwin. “Geomorphic Equations and Methods for Natural Channel Design.” 2012. Web. 22 Apr 2021.

Vancouver:

Shelley JE. Geomorphic Equations and Methods for Natural Channel Design. [Internet] [Doctoral dissertation]. University of Kansas; 2012. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/1808/9836.

Council of Science Editors:

Shelley JE. Geomorphic Equations and Methods for Natural Channel Design. [Doctoral Dissertation]. University of Kansas; 2012. Available from: http://hdl.handle.net/1808/9836

Montana Tech

3. Sawyer, April M. Flood duration and chute cutoff formation in a wandering gravel-bed river.

Degree: MS, 2015, Montana Tech

URL: https://scholarworks.umt.edu/etd/4536

► Chute cutoffs occur when a bypass or “chute” channel incises across a bar or low floodplain area, redistributing water and sediment. Cutoffs result from… (more)

Subjects/Keywords: chute cutoffs; fluvial geomorphology; floods; duration; hydraulic modeling; river restoration; Geomorphology

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APA (6^th Edition):

Sawyer, A. M. (2015). Flood duration and chute cutoff formation in a wandering gravel-bed river. (Masters Thesis). Montana Tech. Retrieved from https://scholarworks.umt.edu/etd/4536

Chicago Manual of Style (16^th Edition):

Sawyer, April M. “Flood duration and chute cutoff formation in a wandering gravel-bed river.” 2015. Masters Thesis, Montana Tech. Accessed April 22, 2021. https://scholarworks.umt.edu/etd/4536.

MLA Handbook (7^th Edition):

Sawyer, April M. “Flood duration and chute cutoff formation in a wandering gravel-bed river.” 2015. Web. 22 Apr 2021.

Vancouver:

Sawyer AM. Flood duration and chute cutoff formation in a wandering gravel-bed river. [Internet] [Masters thesis]. Montana Tech; 2015. [cited 2021 Apr 22]. Available from: https://scholarworks.umt.edu/etd/4536.

Council of Science Editors:

Sawyer AM. Flood duration and chute cutoff formation in a wandering gravel-bed river. [Masters Thesis]. Montana Tech; 2015. Available from: https://scholarworks.umt.edu/etd/4536

4. Kuehn, Ezekiel Allen. Stream Bank Erosion Trends and Sediment Contributions in a Southwestern Missouri River.

Degree: Master of Natural and Applied Science in Geography, Geology, and Planning, Geography, Geology, and Planning, 2015, Missouri State University

URL: https://bearworks.missouristate.edu/theses/2076

► Bank erosion can be a significant source of in-stream sediment that negatively affects water quality and aquatic habitat. However, assessments of the role that… (more)

Subjects/Keywords: stream bank erosion; sediment transport; geographic information system; fluvial geomorphology; Geology; Geomorphology; Sedimentology

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APA (6^th Edition):

Kuehn, E. A. (2015). Stream Bank Erosion Trends and Sediment Contributions in a Southwestern Missouri River. (Masters Thesis). Missouri State University. Retrieved from https://bearworks.missouristate.edu/theses/2076

Chicago Manual of Style (16^th Edition):

Kuehn, Ezekiel Allen. “Stream Bank Erosion Trends and Sediment Contributions in a Southwestern Missouri River.” 2015. Masters Thesis, Missouri State University. Accessed April 22, 2021. https://bearworks.missouristate.edu/theses/2076.

MLA Handbook (7^th Edition):

Kuehn, Ezekiel Allen. “Stream Bank Erosion Trends and Sediment Contributions in a Southwestern Missouri River.” 2015. Web. 22 Apr 2021.

Vancouver:

Kuehn EA. Stream Bank Erosion Trends and Sediment Contributions in a Southwestern Missouri River. [Internet] [Masters thesis]. Missouri State University; 2015. [cited 2021 Apr 22]. Available from: https://bearworks.missouristate.edu/theses/2076.

Council of Science Editors:

Kuehn EA. Stream Bank Erosion Trends and Sediment Contributions in a Southwestern Missouri River. [Masters Thesis]. Missouri State University; 2015. Available from: https://bearworks.missouristate.edu/theses/2076

University of Oregon

5. Baldwin, Daniel. Monitoring Aquatic Habitat Restoration using High-Resolution Multispectral Remote Sensing.

Degree: MS, Department of Geography, 2019, University of Oregon

URL: https://scholarsbank.uoregon.edu/xmlui/handle/1794/24951

► The restoration of riverine habitats is a widespread industry valued at millions of dollars annually. Quantifying the success of river restoration projects is an important… (more)

Subjects/Keywords: Effectiveness Monitoring; Fluvial Geomorphology; High resolution; Multispectral; Riparian; River restoration

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APA (6^th Edition):

Baldwin, D. (2019). Monitoring Aquatic Habitat Restoration using High-Resolution Multispectral Remote Sensing. (Masters Thesis). University of Oregon. Retrieved from https://scholarsbank.uoregon.edu/xmlui/handle/1794/24951

Chicago Manual of Style (16^th Edition):

Baldwin, Daniel. “Monitoring Aquatic Habitat Restoration using High-Resolution Multispectral Remote Sensing.” 2019. Masters Thesis, University of Oregon. Accessed April 22, 2021. https://scholarsbank.uoregon.edu/xmlui/handle/1794/24951.

MLA Handbook (7^th Edition):

Baldwin, Daniel. “Monitoring Aquatic Habitat Restoration using High-Resolution Multispectral Remote Sensing.” 2019. Web. 22 Apr 2021.

Vancouver:

Baldwin D. Monitoring Aquatic Habitat Restoration using High-Resolution Multispectral Remote Sensing. [Internet] [Masters thesis]. University of Oregon; 2019. [cited 2021 Apr 22]. Available from: https://scholarsbank.uoregon.edu/xmlui/handle/1794/24951.

Council of Science Editors:

Baldwin D. Monitoring Aquatic Habitat Restoration using High-Resolution Multispectral Remote Sensing. [Masters Thesis]. University of Oregon; 2019. Available from: https://scholarsbank.uoregon.edu/xmlui/handle/1794/24951

6. Beauchamp, Axel. Impact des aménagements hydrauliques sur les systèmes fluviaux bas-normands depuis 2000 ans : approche géomorphologique et géoarchéologique : Impacts of river management on Normandy rivers over 2000 years : an geomorphologic and geoarchaeologic approach.

Degree: Docteur es, Géographie, 2018, Normandie

URL: http://www.theses.fr/2018NORMC024

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La connaissance de la dynamique hydrosédimentaire des rivières avant et pendant l’installation des nombreux aménagements hydrauliques depuis l’Antiquité restaient très fragmentaire en Basse-Normandie et plus… (more)

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La connaissance de la dynamique hydrosédimentaire des rivières avant et pendant l’installation des nombreux aménagements hydrauliques depuis l’Antiquité restaient très fragmentaire en Basse-Normandie et plus largement en Europe de l’Ouest. On savait encore peu de choses sur les processus d’érosion et de sédimentation qui se sont succédés au sein des rivières normandes au cours des deux derniers millénaires et la part des forçages anthropiques et climatiques qui ont influencé ces processus. L’objectif de la thèse est donc de comprendre et de mesurer la part des héritages dans le fonctionnement actuel des rivières afin de contribuer à leur gestion contemporaine. A cette fin, des recherches géomorphologiques et géoarchéologiques ont été menées dans plusieurs vallées bas-normandes. Ces études ont mis en évidence le poids des installations hydrauliques et en particulier le développement des moulins à eau dans la modification des chenaux d’écoulement mais aussi la construction des plaines alluviales. En effet, la structuration complète du cours d’eau depuis le Moyen Âge a fortement artificialisé les formes en plan et les pentes des cours d’eau et complètement cloisonné leur linéaire. Ces transformations ont favorisé la stabilité latérale des cours d’eau et la sédimentation limoneuse par débordement au sein des plaines alluviales. L’installation de moulins s’accompagne très souvent d’une simplification du tracé en plan de la rivière. Lors de l’équipement maximal des cours d’eau normands on trouvait un moulin tous les 2500 mètres de linéaires hydrographiques. Ces transformations signifient qu’une grande partie des cours actuels sont artificiels. En effet, ces aménagements et l’accélération de la sédimentation limoneuse depuis 1000 ans sont à l’origine de la mise en place d’un équilibre dynamique aboutissant aux formes hydrosédimentaires des rivières actuelles. L’abandon de la gestion des ouvrages hydrauliques et leur destruction au cours des cinquante dernières années viennent remettre en cause cet équilibre.

In Lower Normandy, knowledge of the hydrosedimentary dynamics of rivers before and during the installation of the numerous hydraulic installations since the Roman period remains very fragmentary. Little was known about the rates of erosion and sedimentation that have occurred over the last two millennia and how climatic and anthropogenic controls have influenced these processes. Thus, the challenge of this phD is to understand and measure the role of the inherited structures and operating in the current functioning of the rivers of Lower Normandy in order to help with their contemporary management. To provide answers, geomorphological and geoarchaeological researches has been carried out in several valleys. These studies make it possible to highlight the weight of the hydraulic installations and in particular the developments related to the mills in the setting up of floodplains. Indeed, the complete structuring and management of the watercourse since the Middle Ages artificialized riverbed forms and slopes, and…

Advisors/Committee Members: Delahaye géographe, Daniel (thesis director), Lespez, Laurent (thesis director).

Subjects/Keywords: Dynamique fluviale; Holocène; Sédimentation; Moulin; Fluvial dynamic; Holocene; Fluvial geomorphology; Geoarchaeology; Normandy; Sedimentation; Fluvial engineering; Watermill; River restoration

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Beauchamp, A. (2018). Impact des aménagements hydrauliques sur les systèmes fluviaux bas-normands depuis 2000 ans : approche géomorphologique et géoarchéologique : Impacts of river management on Normandy rivers over 2000 years : an geomorphologic and geoarchaeologic approach. (Doctoral Dissertation). Normandie. Retrieved from http://www.theses.fr/2018NORMC024

Chicago Manual of Style (16^th Edition):

Beauchamp, Axel. “Impact des aménagements hydrauliques sur les systèmes fluviaux bas-normands depuis 2000 ans : approche géomorphologique et géoarchéologique : Impacts of river management on Normandy rivers over 2000 years : an geomorphologic and geoarchaeologic approach.” 2018. Doctoral Dissertation, Normandie. Accessed April 22, 2021. http://www.theses.fr/2018NORMC024.

MLA Handbook (7^th Edition):

Beauchamp, Axel. “Impact des aménagements hydrauliques sur les systèmes fluviaux bas-normands depuis 2000 ans : approche géomorphologique et géoarchéologique : Impacts of river management on Normandy rivers over 2000 years : an geomorphologic and geoarchaeologic approach.” 2018. Web. 22 Apr 2021.

Vancouver:

Beauchamp A. Impact des aménagements hydrauliques sur les systèmes fluviaux bas-normands depuis 2000 ans : approche géomorphologique et géoarchéologique : Impacts of river management on Normandy rivers over 2000 years : an geomorphologic and geoarchaeologic approach. [Internet] [Doctoral dissertation]. Normandie; 2018. [cited 2021 Apr 22]. Available from: http://www.theses.fr/2018NORMC024.

Council of Science Editors:

Beauchamp A. Impact des aménagements hydrauliques sur les systèmes fluviaux bas-normands depuis 2000 ans : approche géomorphologique et géoarchéologique : Impacts of river management on Normandy rivers over 2000 years : an geomorphologic and geoarchaeologic approach. [Doctoral Dissertation]. Normandie; 2018. Available from: http://www.theses.fr/2018NORMC024

Portland State University

7. Anthony, Lowell Henry. Detecting Geomorphic Change and Stream Channel Evolution on the Sandy River, Oregon, Using Lidar Following Dam Removal in 2007.

Degree: MS(M.S.) in Geography, Geography, 2020, Portland State University

URL: https://pdxscholar.library.pdx.edu/open_access_etds/4844

► Following the removal of Marmot Dam on the Sandy River, Oregon, several Lidar flights were flown over the area of the former reservoir. The… (more)

▼ Following the removal of Marmot Dam on the Sandy River, Oregon, several Lidar flights were flown over the area of the former reservoir. The resultant sequential DEMs permitted calculation of reach-scale volumetric erosion and aggradation following dam removal. This allows for change detection across the entire affected reach of the former impoundment rather than just at several cross sections. In the first year there was a net loss of blank sediment in the dewatered reach. Subsequent flights show continued degradation of 145,649 m³ as well as aggradation of 6,232 m³. Sediment transport reached quasi-equilibrium in 2012 with a net change of 65 m³. In addition, this technique allows the extraction of cross-section information which shows that the channel continues to be actively migrating in some areas while also being constrained by bedrock features from past volcanism in some reaches. This study further shows the capability of lidar to measure rates of aggradation and degradation for an entire river system instead of reach specific extrapolations and that repeat lidar flights can more than adequately assess the changing nature of entire stream reaches more rapidly and more cost effectively than traditional field techniques. In addition: The utility of Lidar to do river management with repeat returns, having successive lidar acquisitions run on the watershed level will help us to gain insight into the correlation to precipitation events and geomorphological change in a given reach. Lidar can be used to assess the validity of channel evolution models. Sequential runs of lidar can be used to adjust the overall effectiveness of current CEM's and create new ones that consider reach specific geomorphology. Dam removal projects should incorporate initial lidar flights prior to removal and follow acquisitions based on known CEM's for the region and overall region-specific physiography. Sequential lidar should be used for hazard mitigation and geohazards analysis with an acquisition timeframe that is appropriate for the region's physiography, geology, geomorphology and the return interval of the hazard being monitored. Advisors/Committee Members: Martin Lafrenz.

Subjects/Keywords: Optical radar; Fluvial geomorphology – Oregon – Sandy River Watershed; Dam retirement – Oregon – Sandy River Watershed; Erosion – Measurement; Sedimentation and deposition – Measurement; Geomorphology

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APA (6^th Edition):

Anthony, L. H. (2020). Detecting Geomorphic Change and Stream Channel Evolution on the Sandy River, Oregon, Using Lidar Following Dam Removal in 2007. (Masters Thesis). Portland State University. Retrieved from https://pdxscholar.library.pdx.edu/open_access_etds/4844

Chicago Manual of Style (16^th Edition):

Anthony, Lowell Henry. “Detecting Geomorphic Change and Stream Channel Evolution on the Sandy River, Oregon, Using Lidar Following Dam Removal in 2007.” 2020. Masters Thesis, Portland State University. Accessed April 22, 2021. https://pdxscholar.library.pdx.edu/open_access_etds/4844.

MLA Handbook (7^th Edition):

Anthony, Lowell Henry. “Detecting Geomorphic Change and Stream Channel Evolution on the Sandy River, Oregon, Using Lidar Following Dam Removal in 2007.” 2020. Web. 22 Apr 2021.

Vancouver:

Anthony LH. Detecting Geomorphic Change and Stream Channel Evolution on the Sandy River, Oregon, Using Lidar Following Dam Removal in 2007. [Internet] [Masters thesis]. Portland State University; 2020. [cited 2021 Apr 22]. Available from: https://pdxscholar.library.pdx.edu/open_access_etds/4844.

Council of Science Editors:

Anthony LH. Detecting Geomorphic Change and Stream Channel Evolution on the Sandy River, Oregon, Using Lidar Following Dam Removal in 2007. [Masters Thesis]. Portland State University; 2020. Available from: https://pdxscholar.library.pdx.edu/open_access_etds/4844

8. Castro, Wallas de Souza. Migração dos meandros do baixo curso do rio Claro, Goiás: processos e fatores controladores.

Degree: 2015, Universidade Federal de Goiás; Programa de Pós-graduação em Geografia (IESA); UFG; Brasil; Instituto de Estudos Socioambientais – IESA (RG)

URL: http://repositorio.bc.ufg.br/tede/handle/tede/4979

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Meanders rivers have sinuous channel with singular dynamic of lateral migration by eroding its concave bank and depositing on its convex bank. This dynamic is able to expand and restore fluvial environments when creates a sedimentary environments complex linked to development of floodplain. The nature of preexistent deposits on floodplain, which are remobilized by lateral migration, is important to interpret deposicional dynamics, being central to the identification evolution of meanders. Heterogeneity of the facies is formed by several cycles of sedimentary evolution through channel migration, generating a succession of deposits with different degree cohesion. These depositional environments affect the continuity migration and the evolution of meanders. It was researched the current evolution of meander and riparian vegetation influence and theirs deposit about lateral migration process on downstream Claro river. It was used aerial photographs, satellite images, facies analysis and pin set on the banks to identify the influences of vegetation and material in the migration processes of meanders. The channel showed high mobility verified by the high amount of migration process in 47 years, due to the planforms diffusion and oxbow lakes and by deposits and paleochannel sedimentary facies. The vegetation has not shown attenuating effect against the bank erosion in the two curves analyzed meanders, erosion rates for the segments with vegetation cover were up to 1,3m ahead of the environments of floodplain. It was found that the intensity of channel migration differs between the curves. Migration advances with little resistance from unconsolidated deposits of the current floodplain, whereas in older deposits, pedogenesis and consistent terraces have hindered lateral advance, due to theirs material.

Rios meandrantes possuem canais fluviais sinuosos com dinâmica particular de migração lateral ao erodir suas margens côncavas e depositar nas margens convexas. Esta dinâmica é capaz de ampliar e renovar os ambientes fluviais ao criar um complexo ambiente sedimentar ligado ao desenvolvimento das planícies fluviais. A…

Advisors/Committee Members: Campos, Alfredo Borges de, Zancopé, Márcio Henrique de Campos, Campos, Alfredo Borges de, Bayer, Maximiliano, Rocha, Paulo Cézar.

Subjects/Keywords: Geomorfologia fluvial; Erosão marginal e associação de fácies sedimentares; Fluvial geomorphology; Bank erosion; Analysis sedimentary facies; CIENCIAS HUMANAS::GEOGRAFIA

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APA (6^th Edition):

Castro, W. d. S. (2015). Migração dos meandros do baixo curso do rio Claro, Goiás: processos e fatores controladores. (Masters Thesis). Universidade Federal de Goiás; Programa de Pós-graduação em Geografia (IESA); UFG; Brasil; Instituto de Estudos Socioambientais – IESA (RG). Retrieved from http://repositorio.bc.ufg.br/tede/handle/tede/4979

Chicago Manual of Style (16^th Edition):

Castro, Wallas de Souza. “Migração dos meandros do baixo curso do rio Claro, Goiás: processos e fatores controladores.” 2015. Masters Thesis, Universidade Federal de Goiás; Programa de Pós-graduação em Geografia (IESA); UFG; Brasil; Instituto de Estudos Socioambientais – IESA (RG). Accessed April 22, 2021. http://repositorio.bc.ufg.br/tede/handle/tede/4979.

MLA Handbook (7^th Edition):

Castro, Wallas de Souza. “Migração dos meandros do baixo curso do rio Claro, Goiás: processos e fatores controladores.” 2015. Web. 22 Apr 2021.

Vancouver:

Castro WdS. Migração dos meandros do baixo curso do rio Claro, Goiás: processos e fatores controladores. [Internet] [Masters thesis]. Universidade Federal de Goiás; Programa de Pós-graduação em Geografia (IESA); UFG; Brasil; Instituto de Estudos Socioambientais – IESA (RG); 2015. [cited 2021 Apr 22]. Available from: http://repositorio.bc.ufg.br/tede/handle/tede/4979.

Council of Science Editors:

Castro WdS. Migração dos meandros do baixo curso do rio Claro, Goiás: processos e fatores controladores. [Masters Thesis]. Universidade Federal de Goiás; Programa de Pós-graduação em Geografia (IESA); UFG; Brasil; Instituto de Estudos Socioambientais – IESA (RG); 2015. Available from: http://repositorio.bc.ufg.br/tede/handle/tede/4979

9. Klein, Talia A. Quantifying the Effectiveness of Cedar Revetment in Mitigating Bank Erosion in Riceford Creek, Minnesota.

Degree: MSin Geospatial Sciences, Geography, Geology, and Planning, 2019, Missouri State University

URL: https://bearworks.missouristate.edu/theses/3464

► Southeastern Minnesota has incised streams that are susceptible to bank erosion. Previously, efforts have been made to identify sections of Riceford Creek that have… (more)

Subjects/Keywords: Minnesota; cedar revetment; rivers; stream bank erosion; fluvial geomorphology; revetment failure; revetment success; Rosgen’s BEHI; Geomorphology; Hydrology

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APA (6^th Edition):

Klein, T. A. (2019). Quantifying the Effectiveness of Cedar Revetment in Mitigating Bank Erosion in Riceford Creek, Minnesota. (Masters Thesis). Missouri State University. Retrieved from https://bearworks.missouristate.edu/theses/3464

Chicago Manual of Style (16^th Edition):

Klein, Talia A. “Quantifying the Effectiveness of Cedar Revetment in Mitigating Bank Erosion in Riceford Creek, Minnesota.” 2019. Masters Thesis, Missouri State University. Accessed April 22, 2021. https://bearworks.missouristate.edu/theses/3464.

MLA Handbook (7^th Edition):

Klein, Talia A. “Quantifying the Effectiveness of Cedar Revetment in Mitigating Bank Erosion in Riceford Creek, Minnesota.” 2019. Web. 22 Apr 2021.

Vancouver:

Klein TA. Quantifying the Effectiveness of Cedar Revetment in Mitigating Bank Erosion in Riceford Creek, Minnesota. [Internet] [Masters thesis]. Missouri State University; 2019. [cited 2021 Apr 22]. Available from: https://bearworks.missouristate.edu/theses/3464.

Council of Science Editors:

Klein TA. Quantifying the Effectiveness of Cedar Revetment in Mitigating Bank Erosion in Riceford Creek, Minnesota. [Masters Thesis]. Missouri State University; 2019. Available from: https://bearworks.missouristate.edu/theses/3464

Portland State University

10. Keith, Mackenzie Karli. Reservoir Evolution Following the Removal of Marmot Dam on the Sandy River, Oregon.

Degree: MS(M.S.) in Geology, Geology, 2012, Portland State University

URL: https://pdxscholar.library.pdx.edu/open_access_etds/532

► The October 2007 removal of Marmot Dam, a 14.3-m-tall dam on the Sandy River in northwestern Oregon storing approximately 730,000 m3 of impounded sediment,… (more)

▼ The October 2007 removal of Marmot Dam, a 14.3-m-tall dam on the Sandy River in northwestern Oregon storing approximately 730,000 m3 of impounded sediment, provided an opportunity to study short- and long-term geomorphic effects of dam removal. Monitoring reservoir morphology during the two years following dam decommissioning yields a timeline of reservoir channel change. Comparison of a pre-dam survey in 1911 with post-removal surveys provides a basis from which to gage the Reservoir Reach evolution in the context of pre-dam conditions. Analyses of time-lapse photography, topographic surveys, and repeat LiDAR data sets provide detailed spatial and temporal documentation of a release of sediment from the reservoir following dam removal. The majority of morphologic changes to the reservoir largely took place during the first few days and weeks following removal. Channel incision and widening, along with gradient changes through the Reservoir Reach, exhibit diminishing changes with time. Channel incision rates of up to 13 m/hr and widening rates of up to 26 m/hr occurred within the first 24 hours following breaching of the coffer dam. Although channel position through the Reservoir Reach has remained relatively stable due to valley confinement, its width increased substantially. The channel reached an average width of 45 m within two weeks of breaching, but then erosion rates slowed and the channel width reached about 70 to 80 m after one and two years, respectively. Diminishing volumes of evacuated sediment were measured over time through quantitative analysis of survey datasets. About 15 percent of the initial impounded sediment was eroded from the Reservoir Reach within 60 hours of breaching; after one and two years, 50 and 58 percent was eroded, respectively. Grain-size analysis of terraces cut into reservoir fill following dam removal show that bed material coarsened over time at fixed elevations and vertically downward as the channel incised. Overall, these findings indicate valley morphology and local in-channel bedrock topography controlled the spatial distribution of sediment within the reservoir reach while variability in river discharge determined the timing of episodic sediment release. Changes within the Reservoir Reach shortly after dam removal and subsequent evolution over the two years following removal are likely attributable to 1) the timing and intensity of flow events, 2) the longitudinal and stratigraphic spatial variations in deposit grain-size distributions initially and over time, and 3) the pre-dam topography and existing valley morphology. Advisors/Committee Members: Andrew Fountain.

Subjects/Keywords: Dam removal; Erosion; Sediment; Fluvial geomorphology – Oregon – Sandy River Watershed; Dam retirement – Oregon – Sandy River; Reservoir sedimentation – Oregon – Sandy River Watershed

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APA (6^th Edition):

Keith, M. K. (2012). Reservoir Evolution Following the Removal of Marmot Dam on the Sandy River, Oregon. (Masters Thesis). Portland State University. Retrieved from https://pdxscholar.library.pdx.edu/open_access_etds/532

Chicago Manual of Style (16^th Edition):

Keith, Mackenzie Karli. “Reservoir Evolution Following the Removal of Marmot Dam on the Sandy River, Oregon.” 2012. Masters Thesis, Portland State University. Accessed April 22, 2021. https://pdxscholar.library.pdx.edu/open_access_etds/532.

MLA Handbook (7^th Edition):

Keith, Mackenzie Karli. “Reservoir Evolution Following the Removal of Marmot Dam on the Sandy River, Oregon.” 2012. Web. 22 Apr 2021.

Vancouver:

Keith MK. Reservoir Evolution Following the Removal of Marmot Dam on the Sandy River, Oregon. [Internet] [Masters thesis]. Portland State University; 2012. [cited 2021 Apr 22]. Available from: https://pdxscholar.library.pdx.edu/open_access_etds/532.

Council of Science Editors:

Keith MK. Reservoir Evolution Following the Removal of Marmot Dam on the Sandy River, Oregon. [Masters Thesis]. Portland State University; 2012. Available from: https://pdxscholar.library.pdx.edu/open_access_etds/532

University of Texas – Austin

11. Leitch, Maraigh Brianna 1984-. Oxbow Lake sedimentation along the lower Guadalupe River, Texas.

Degree: MA, Geography, 2011, University of Texas – Austin

URL: http://hdl.handle.net/2152/43597

► Texas Gulf Coastal Plain Rivers are subject to a dynamic climatic and hydrologic regime. A common feature of Gulf Coast meandering rivers in this region… (more)

Subjects/Keywords: Geomorphology; Fluvial geomorphology; Oxbow; Guadalupe River

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APA (6^th Edition):

Leitch, M. B. 1. (2011). Oxbow Lake sedimentation along the lower Guadalupe River, Texas. (Masters Thesis). University of Texas – Austin. Retrieved from http://hdl.handle.net/2152/43597

Chicago Manual of Style (16^th Edition):

Leitch, Maraigh Brianna 1984-. “Oxbow Lake sedimentation along the lower Guadalupe River, Texas.” 2011. Masters Thesis, University of Texas – Austin. Accessed April 22, 2021. http://hdl.handle.net/2152/43597.

MLA Handbook (7^th Edition):

Leitch, Maraigh Brianna 1984-. “Oxbow Lake sedimentation along the lower Guadalupe River, Texas.” 2011. Web. 22 Apr 2021.

Vancouver:

Leitch MB1. Oxbow Lake sedimentation along the lower Guadalupe River, Texas. [Internet] [Masters thesis]. University of Texas – Austin; 2011. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/2152/43597.

Council of Science Editors:

Leitch MB1. Oxbow Lake sedimentation along the lower Guadalupe River, Texas. [Masters Thesis]. University of Texas – Austin; 2011. Available from: http://hdl.handle.net/2152/43597

University of Oregon

12. Appleby, Christina. Modeling Historical Meander Bends Reconnection on the lower Long Tom River in Lane Co. and Benton Co., OR.

Degree: MS, Department of Geography, 2016, University of Oregon

URL: http://hdl.handle.net/1794/20717

► Since the damming and channelization of the lower Long Tom River in the 1940s and 1950s, the quality and quantity of habitat for coastal cutthroat… (more)

Subjects/Keywords: 2D HEC-RAS; Fluvial geomorphology; Geographic Information Systems (GIS); Hydraulic modeling; Long Tom River; River restoration

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APA (6^th Edition):

Appleby, C. (2016). Modeling Historical Meander Bends Reconnection on the lower Long Tom River in Lane Co. and Benton Co., OR. (Masters Thesis). University of Oregon. Retrieved from http://hdl.handle.net/1794/20717

Chicago Manual of Style (16^th Edition):

Appleby, Christina. “Modeling Historical Meander Bends Reconnection on the lower Long Tom River in Lane Co. and Benton Co., OR.” 2016. Masters Thesis, University of Oregon. Accessed April 22, 2021. http://hdl.handle.net/1794/20717.

MLA Handbook (7^th Edition):

Appleby, Christina. “Modeling Historical Meander Bends Reconnection on the lower Long Tom River in Lane Co. and Benton Co., OR.” 2016. Web. 22 Apr 2021.

Vancouver:

Appleby C. Modeling Historical Meander Bends Reconnection on the lower Long Tom River in Lane Co. and Benton Co., OR. [Internet] [Masters thesis]. University of Oregon; 2016. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/1794/20717.

Council of Science Editors:

Appleby C. Modeling Historical Meander Bends Reconnection on the lower Long Tom River in Lane Co. and Benton Co., OR. [Masters Thesis]. University of Oregon; 2016. Available from: http://hdl.handle.net/1794/20717

13. Engel, Frank. The fluvial dynamics of compound meander bends.

Degree: PhD, 0341, 2014, University of Illinois – Urbana-Champaign

URL: http://hdl.handle.net/2142/49644

► The dynamic evolution of the planform of meandering rivers often leads to the development of compound loops with multiple lobes of maximum curvature, also known… (more)

▼ The dynamic evolution of the planform of meandering rivers often leads to the development of compound loops with multiple lobes of maximum curvature, also known as compound meander bends. At present, the interaction among spatial patterns of mean flow, turbulence, bed morphology, bank failures and channel migration in compound loops is poorly understood. In particular, field studies of this interaction over the timescale of planform evolution are lacking. The research presented here examines the co-evolution of flow, bed morphology, and channel planform in two compound meander bends. Careful study is given to the interaction of processes over differing spatial and temporal timescales. Results suggest that patterns of flow, sediment entrainment, and planform evolution in compound meander bends are more complex than in simple meander bends. Moreover, interactions among local influences on the flow, such as outer bank blocks, local topographic steering, and locally high curvature, tend to cause compound loops to evolve toward increasing planform complexity over time rather than stable configurations. The research is comprised of three field investigations. The first study examines the co-evolution of flow, bed morphology, and channel planform in a compound meander loop and relates patterns of near-bank velocity and turbulence to planform change within the loop. Data consist of repeat surveys of channel change in a compound loop over an 11-year period, coupled with Acoustic Doppler Velocimeter (ADV) measurements of 3-D instantaneous velocities for similar magnitude flows at the beginning and end of this period. Results confirm that this compound loop is highly dynamic with major changes in planform occurring over the 11-year period. Spatial patterns of near-bank velocity and turbulence correspond to patterns of bank erosion and channel migration within the loop; however, these patterns are not strictly a function of planform curvature. Instead, local factors, including deflection of the flow by point bars and failed bank blocks, can enhance or inhibit the development of high near-bank velocities and turbulence kinetic energy. The loop has elongated and become more asymmetric over time—a pattern of development consistent with patterns of near-bank velocities and turbulence at the beginning of the study period. The pattern of near-bank velocities and turbulence for measurements at the end of the period indicate that the loop will continue to elongate in the near future, supporting the hypothesis that compound loops change progressively over time rather than evolving into a stable configuration. In the second study, Acoustic Doppler Current Profiler (ADCP) measurements of the time-averaged flow structure are examined to evaluate the influence of channel curvature and hydrologic variability (i.e., stage) on the structure of flow within a compound loop and to relate changes in bed morphology to flow structure at various flow stages. Local increases in centerline curvature (or decreases in dimensionless radius of curvature)… Advisors/Committee Members: Rhoads, Bruce L. (advisor), Rhoads, Bruce L. (Committee Chair), Best, James L. (committee member), Parker, Gary (committee member), Garcia, Marcelo H. (committee member).

Subjects/Keywords: River meander; Acoustic Doppler Current Profiler (ADCP); Turbulence; Acoustic Doppler Velocimeter (ADV); Bank Erosion; Fluvial geomorphology

…19 2.7 Bank Erosion Mechanisms… …119 5.2 Turbulence in Meandering Rivers: Implications for Bank Erosion… …data computed from bank erosion and curvature changes during the study period, whereas filled… …water surface elevation, and the shaded area denotes estimated bank geometry… …lines denote the water surface elevation, and the shaded area denotes estimated bank geometry…

11 more images…

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APA (6^th Edition):

Engel, F. (2014). The fluvial dynamics of compound meander bends. (Doctoral Dissertation). University of Illinois – Urbana-Champaign. Retrieved from http://hdl.handle.net/2142/49644

Chicago Manual of Style (16^th Edition):

Engel, Frank. “The fluvial dynamics of compound meander bends.” 2014. Doctoral Dissertation, University of Illinois – Urbana-Champaign. Accessed April 22, 2021. http://hdl.handle.net/2142/49644.

MLA Handbook (7^th Edition):

Engel, Frank. “The fluvial dynamics of compound meander bends.” 2014. Web. 22 Apr 2021.

Vancouver:

Engel F. The fluvial dynamics of compound meander bends. [Internet] [Doctoral dissertation]. University of Illinois – Urbana-Champaign; 2014. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/2142/49644.

Council of Science Editors:

Engel F. The fluvial dynamics of compound meander bends. [Doctoral Dissertation]. University of Illinois – Urbana-Champaign; 2014. Available from: http://hdl.handle.net/2142/49644

University of Florida

14. Black, Megan Mary. Post-Restoration Analysis of the Planform and Bed Morphology of the Lower Kissimmee River, Florida.

Degree: MS, Geography, 2019, University of Florida

URL: https://ufdc.ufl.edu/UFE0055947

The Lower Kissimmee River is one of the most heavily altered rivers in the world. It was first completely channelized from Lake Kissimmee to Lake Okeechobee in the Advisors/Committee Members: Mossa,Joann (committee chair), Walker,Robert T (committee member).

Subjects/Keywords: channelization – connectivity – everglades – floodplain – florida – fluvial – geomorphology – hydrology – kissimmee – morphology – nutrients – okeechobee – planform – river – water

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APA (6^th Edition):

Black, M. M. (2019). Post-Restoration Analysis of the Planform and Bed Morphology of the Lower Kissimmee River, Florida. (Masters Thesis). University of Florida. Retrieved from https://ufdc.ufl.edu/UFE0055947

Chicago Manual of Style (16^th Edition):

Black, Megan Mary. “Post-Restoration Analysis of the Planform and Bed Morphology of the Lower Kissimmee River, Florida.” 2019. Masters Thesis, University of Florida. Accessed April 22, 2021. https://ufdc.ufl.edu/UFE0055947.

MLA Handbook (7^th Edition):

Black, Megan Mary. “Post-Restoration Analysis of the Planform and Bed Morphology of the Lower Kissimmee River, Florida.” 2019. Web. 22 Apr 2021.

Vancouver:

Black MM. Post-Restoration Analysis of the Planform and Bed Morphology of the Lower Kissimmee River, Florida. [Internet] [Masters thesis]. University of Florida; 2019. [cited 2021 Apr 22]. Available from: https://ufdc.ufl.edu/UFE0055947.

Council of Science Editors:

Black MM. Post-Restoration Analysis of the Planform and Bed Morphology of the Lower Kissimmee River, Florida. [Masters Thesis]. University of Florida; 2019. Available from: https://ufdc.ufl.edu/UFE0055947

University of Ghana

15. Kusimi, J.M. Sediment Yield and Bank Erosion Assessment of Pra River Basin .

Degree: 2014, University of Ghana

URL: http://ugspace.ug.edu.gh/handle/123456789/5467

► The Pra River Basin has been engulfed by certain anthropogenic activities particularly illegal small scale mining (popularly called galamsey) and serious concerns have been raised… (more)

Subjects/Keywords: Bank Erosion; Anthropogenic Activities; Water Resources; Ecosystems; Ghana

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APA (6^th Edition):

Kusimi, J. M. (2014). Sediment Yield and Bank Erosion Assessment of Pra River Basin . (Doctoral Dissertation). University of Ghana. Retrieved from http://ugspace.ug.edu.gh/handle/123456789/5467

Chicago Manual of Style (16^th Edition):

Kusimi, J M. “Sediment Yield and Bank Erosion Assessment of Pra River Basin .” 2014. Doctoral Dissertation, University of Ghana. Accessed April 22, 2021. http://ugspace.ug.edu.gh/handle/123456789/5467.

MLA Handbook (7^th Edition):

Kusimi, J M. “Sediment Yield and Bank Erosion Assessment of Pra River Basin .” 2014. Web. 22 Apr 2021.

Vancouver:

Kusimi JM. Sediment Yield and Bank Erosion Assessment of Pra River Basin . [Internet] [Doctoral dissertation]. University of Ghana; 2014. [cited 2021 Apr 22]. Available from: http://ugspace.ug.edu.gh/handle/123456789/5467.

Council of Science Editors:

Kusimi JM. Sediment Yield and Bank Erosion Assessment of Pra River Basin . [Doctoral Dissertation]. University of Ghana; 2014. Available from: http://ugspace.ug.edu.gh/handle/123456789/5467

Kansas State University

16. Marston, Bryce Kendrick. Influence of the Mountain Pine Beetle disturbance on large wood dynamics and channel morphology in mountain streams.

Degree: PhD, Department of Geography, 2017, Kansas State University

URL: http://hdl.handle.net/2097/35499

► Disturbance regimes are important determinants of both terrestrial and aquatic ecosystem structure and function. Disturbances may linger in the landscape and lag temporally, influencing stream… (more)

Subjects/Keywords: Geography; Fluvial geomorphology; Geomorphology; Water resource management

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APA (6^th Edition):

Marston, B. K. (2017). Influence of the Mountain Pine Beetle disturbance on large wood dynamics and channel morphology in mountain streams. (Doctoral Dissertation). Kansas State University. Retrieved from http://hdl.handle.net/2097/35499

Chicago Manual of Style (16^th Edition):

Marston, Bryce Kendrick. “Influence of the Mountain Pine Beetle disturbance on large wood dynamics and channel morphology in mountain streams.” 2017. Doctoral Dissertation, Kansas State University. Accessed April 22, 2021. http://hdl.handle.net/2097/35499.

MLA Handbook (7^th Edition):

Marston, Bryce Kendrick. “Influence of the Mountain Pine Beetle disturbance on large wood dynamics and channel morphology in mountain streams.” 2017. Web. 22 Apr 2021.

Vancouver:

Marston BK. Influence of the Mountain Pine Beetle disturbance on large wood dynamics and channel morphology in mountain streams. [Internet] [Doctoral dissertation]. Kansas State University; 2017. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/2097/35499.

Council of Science Editors:

Marston BK. Influence of the Mountain Pine Beetle disturbance on large wood dynamics and channel morphology in mountain streams. [Doctoral Dissertation]. Kansas State University; 2017. Available from: http://hdl.handle.net/2097/35499

University of California – Berkeley

17. Butler, Nathaniel L. Water temperature modeling in streams to support ecological restoration.

Degree: Civil and Environmental Engineering, 2015, University of California – Berkeley

URL: http://www.escholarship.org/uc/item/2nj2h119

► Water temperature is a critical water quality parameter that affects salmonid survival by influencing its metabolism and growth at all life stages. Stream temperature is… (more)

▼ Water temperature is a critical water quality parameter that affects salmonid survival by influencing its metabolism and growth at all life stages. Stream temperature is an especially important parameter in California rivers where it frequently limits the range of salmonids. Anthropogenic activities have increased stream temperature and degraded spawning, holding, and rearing habitats, and this has contributed to declines in salmonid populations in California. Fisheries managers have a range of analytical and empirical tools available to assess and quantify elevated stream temperature conditions, but many of these tools do not focus on water temperature conditions at the spatial and temporal scales important to salmonids. My research focuses on assessing water temperature at the watershed and upwelling hyporheic scale which are critical to salmonid survival as stream temperature approaches thermal tolerances.I developed a model to calculate water temperature at locations throughout a watershed to provide a method to evaluate the availability and connectivity of suitable thermal habitat throughout a stream network. The model used a linear weighted average of the maximum and minimum air temperatures of the current and 4 prior days. The weighting parameter is dependent upon upstream drainage area enabling the application of the model to both small tributaries and large mainstem streams. I used historical data from the Sonoma Creek, Napa River, and Russian River watersheds to develop, test, calibrate, and partially validate the model. Model results from Sonoma Creek and Napa River indicated it was generally able to estimate daily average water temperature within 1.5 degrees C of the observed water temperature. Data from the Russian River highlighted the model was limited to streams without significant hydrologic modifications or geologic constraints that forced groundwater to the surface.A 1-D advection dispersion heat transport model was developed to quantify the upwelling hyporheic temperature that provides cold water thermal refugia along a streambed for salmonids. I analyzed hyporheic temperature measured at five sites in a previous research program across sixteen kilometers of Deer Creek near Vina, California, to test, calibrate, and partially validate the model. At three sites, I found the 1-D advection and dispersion were the dominant heat transport mechanisms with model root mean square error less than 0.6 degrees C. At two sites, the model was not applicable because modeling results indicated that surface flow rate variations, solar radiation, and multi-day flow paths also influenced the upwelling hyporheic temperature. Modeling was valuable for highlighting the contribution of these additional processes from that of 1-D advection dispersion. The availability of monitoring data over the summer-fall period was essential for modeling upwelling temperature dynamics along a semi-natural channel.

Subjects/Keywords: Environmental engineering; Water resources management; hyporheic; river restoration; salmon; water temperature

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APA (6^th Edition):

Butler, N. L. (2015). Water temperature modeling in streams to support ecological restoration. (Thesis). University of California – Berkeley. Retrieved from http://www.escholarship.org/uc/item/2nj2h119

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16^th Edition):

Butler, Nathaniel L. “Water temperature modeling in streams to support ecological restoration.” 2015. Thesis, University of California – Berkeley. Accessed April 22, 2021. http://www.escholarship.org/uc/item/2nj2h119.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7^th Edition):

Butler, Nathaniel L. “Water temperature modeling in streams to support ecological restoration.” 2015. Web. 22 Apr 2021.

Vancouver:

Butler NL. Water temperature modeling in streams to support ecological restoration. [Internet] [Thesis]. University of California – Berkeley; 2015. [cited 2021 Apr 22]. Available from: http://www.escholarship.org/uc/item/2nj2h119.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Butler NL. Water temperature modeling in streams to support ecological restoration. [Thesis]. University of California – Berkeley; 2015. Available from: http://www.escholarship.org/uc/item/2nj2h119

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Delft University of Technology

18. Duro, G. Bank erosion in regulated navigable rivers.

Degree: 2021, Delft University of Technology

URL: http://resolver.tudelft.nl/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; urn:NBN:nl:ui:24-uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; 805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; 10.4233/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; urn:isbn:978-94-6366-352-6 ; urn:NBN:nl:ui:24-uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; http://resolver.tudelft.nl/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5

► Banks constitute important areas for the river ecology since they provide a multitude of favourable conditions for flora and fauna. The hydromorphological diversity typical of… (more)

Subjects/Keywords: river morphodynamics; bank erosion; navigation; retreat modelling; river restoration

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APA (6^th Edition):

Duro, G. (2021). Bank erosion in regulated navigable rivers. (Doctoral Dissertation). Delft University of Technology. Retrieved from http://resolver.tudelft.nl/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; urn:NBN:nl:ui:24-uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; 805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; 10.4233/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; urn:isbn:978-94-6366-352-6 ; urn:NBN:nl:ui:24-uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; http://resolver.tudelft.nl/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5

Chicago Manual of Style (16^th Edition):

Duro, G. “Bank erosion in regulated navigable rivers.” 2021. Doctoral Dissertation, Delft University of Technology. Accessed April 22, 2021. http://resolver.tudelft.nl/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; urn:NBN:nl:ui:24-uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; 805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; 10.4233/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; urn:isbn:978-94-6366-352-6 ; urn:NBN:nl:ui:24-uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; http://resolver.tudelft.nl/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5.

MLA Handbook (7^th Edition):

Duro, G. “Bank erosion in regulated navigable rivers.” 2021. Web. 22 Apr 2021.

Vancouver:

Duro G. Bank erosion in regulated navigable rivers. [Internet] [Doctoral dissertation]. Delft University of Technology; 2021. [cited 2021 Apr 22]. Available from: http://resolver.tudelft.nl/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; urn:NBN:nl:ui:24-uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; 805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; 10.4233/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; urn:isbn:978-94-6366-352-6 ; urn:NBN:nl:ui:24-uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; http://resolver.tudelft.nl/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5.

Council of Science Editors:

Duro G. Bank erosion in regulated navigable rivers. [Doctoral Dissertation]. Delft University of Technology; 2021. Available from: http://resolver.tudelft.nl/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; urn:NBN:nl:ui:24-uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; 805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; 10.4233/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; urn:isbn:978-94-6366-352-6 ; urn:NBN:nl:ui:24-uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5 ; http://resolver.tudelft.nl/uuid:805eaec5-3b87-4bd6-bbe3-fa896da3b1c5

University of Melbourne

19. Teo, Elisha Anne Pei Yi. The geomorphological evolution of Corryong Creek, Victoria.

Degree: 2013, University of Melbourne

URL: http://hdl.handle.net/11343/56789

► The present morphology of a river is the outcome of past and present conditions. To understand a fluvial system, the history of a river must… (more)

▼ The present morphology of a river is the outcome of past and present conditions. To understand a fluvial system, the history of a river must therefore be known. Once established, river management activities will be better informed, as a model for channel response is now available. Moreover, using variable-specific studies sometimes creates a bias in attributing geomorphic significance to variables. An integrated approach avoids the underestimation or overestimation of influences because variables are considered collectively. This thesis is driven by this principle. Presented here is an investigation on Corryong Creek, to determine and explain its geomorphological evolution in the period since European settlement. To do so, its history of channel change was first reconstructed, followed by the reconstruction of main geomorphic variables including hydro-climate, catchment land cover, riparian vegetation cover, and river management. Spatiotemporal trends for each parameter were identified, and then compared to decipher interrelationships. Since European settlement, Corryong Creek has become increasingly unstable, exhibiting an overall pattern of straightening, widening and increased sediment deposition. A change in catchment hydrology is evident, which is due to a combination of severe land clearing and an increase in average rainfall since the mid-20th century. Because climate is a significant influence on flow, periodicities in channel stability are observable through climatic phase shifts between wet and dry years dictated by the El Nino Southern Oscillation and the Indian Ocean dipole. Flood regimes were not observed in the rainfall data. While general patterns in channel stability were observed over longer time periods and larger areas, rates of channel change have not necessarily been consistent across smaller spatial and temporal scales. This revealed the influence of river management and riparian willow cover. Severe channel straightening, bank stabilisation and willow growth have distorted the capacity for channel change to occur. In general, channel straightening has increased channel instability by increasing flow velocities (in addition to directly affecting channel planform), bank stabilisation has stunted erosion rates, and willows enhance channel widening and sediment deposition (but their effect reduces as channels widen). This thesis demonstrates that despite complexity, fluvial systems can still be better understood through an analysis of spatiotemporal trends.

Subjects/Keywords: Fluvial geomorphology; River management; Channel development

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APA (6^th Edition):

Teo, E. A. P. Y. (2013). The geomorphological evolution of Corryong Creek, Victoria. (Masters Thesis). University of Melbourne. Retrieved from http://hdl.handle.net/11343/56789

Chicago Manual of Style (16^th Edition):

Teo, Elisha Anne Pei Yi. “The geomorphological evolution of Corryong Creek, Victoria.” 2013. Masters Thesis, University of Melbourne. Accessed April 22, 2021. http://hdl.handle.net/11343/56789.

MLA Handbook (7^th Edition):

Teo, Elisha Anne Pei Yi. “The geomorphological evolution of Corryong Creek, Victoria.” 2013. Web. 22 Apr 2021.

Vancouver:

Teo EAPY. The geomorphological evolution of Corryong Creek, Victoria. [Internet] [Masters thesis]. University of Melbourne; 2013. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/11343/56789.

Council of Science Editors:

Teo EAPY. The geomorphological evolution of Corryong Creek, Victoria. [Masters Thesis]. University of Melbourne; 2013. Available from: http://hdl.handle.net/11343/56789

University of Guelph

20. Good, Ryan. Effects of Skewness on the Morphological Response of Unconfined Alluvial Meandering Streams in a Laboratory Flume.

Degree: Master of Applied Science, School of Engineering, 2018, University of Guelph

URL: https://atrium.lib.uoguelph.ca/xmlui/handle/10214/14099

► Rivers typically follow a meandering pattern where, over time, the river adjusts its morphology to minimize the channel slope. The purpose of the research is… (more)

Subjects/Keywords: river; sediment transport; fluvial geomorphology; flume; meandering

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APA (6^th Edition):

Good, R. (2018). Effects of Skewness on the Morphological Response of Unconfined Alluvial Meandering Streams in a Laboratory Flume. (Masters Thesis). University of Guelph. Retrieved from https://atrium.lib.uoguelph.ca/xmlui/handle/10214/14099

Chicago Manual of Style (16^th Edition):

Good, Ryan. “Effects of Skewness on the Morphological Response of Unconfined Alluvial Meandering Streams in a Laboratory Flume.” 2018. Masters Thesis, University of Guelph. Accessed April 22, 2021. https://atrium.lib.uoguelph.ca/xmlui/handle/10214/14099.

MLA Handbook (7^th Edition):

Good, Ryan. “Effects of Skewness on the Morphological Response of Unconfined Alluvial Meandering Streams in a Laboratory Flume.” 2018. Web. 22 Apr 2021.

Vancouver:

Good R. Effects of Skewness on the Morphological Response of Unconfined Alluvial Meandering Streams in a Laboratory Flume. [Internet] [Masters thesis]. University of Guelph; 2018. [cited 2021 Apr 22]. Available from: https://atrium.lib.uoguelph.ca/xmlui/handle/10214/14099.

Council of Science Editors:

Good R. Effects of Skewness on the Morphological Response of Unconfined Alluvial Meandering Streams in a Laboratory Flume. [Masters Thesis]. University of Guelph; 2018. Available from: https://atrium.lib.uoguelph.ca/xmlui/handle/10214/14099

University of New Brunswick

21. Wojda, Mark. Bank Erosion in the Petitcodiac River Estuary.

Degree: 2011, University of New Brunswick

URL: http://hdl.handle.net/1882/35384

► To further understand bank undercutting processes that occur in the Petitcodiac River estuary (New Brunswick, Canada), the erosion of sediment cores obtained at the base… (more)

Subjects/Keywords: Petitcodiac; estuary erosion; river erosion; bank erosion; bank undercutting

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APA (6^th Edition):

Wojda, M. (2011). Bank Erosion in the Petitcodiac River Estuary. (Thesis). University of New Brunswick. Retrieved from http://hdl.handle.net/1882/35384

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16^th Edition):

Wojda, Mark. “Bank Erosion in the Petitcodiac River Estuary.” 2011. Thesis, University of New Brunswick. Accessed April 22, 2021. http://hdl.handle.net/1882/35384.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7^th Edition):

Wojda, Mark. “Bank Erosion in the Petitcodiac River Estuary.” 2011. Web. 22 Apr 2021.

Vancouver:

Wojda M. Bank Erosion in the Petitcodiac River Estuary. [Internet] [Thesis]. University of New Brunswick; 2011. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/1882/35384.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Wojda M. Bank Erosion in the Petitcodiac River Estuary. [Thesis]. University of New Brunswick; 2011. Available from: http://hdl.handle.net/1882/35384

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

University of Minnesota

22. Wick, Molly Jane. Identifying erosional hotspots in streams along the North Shore of Lake Superior, Minnesota using high-resolution elevation and soils data.

Degree: MS, Water Resources Science, 2013, University of Minnesota

URL: http://hdl.handle.net/11299/162413

► Many streams on the North Shore of Lake Superior, Minnesota, USA, are impaired for turbidity driven by excess fine sediment loading. The goal of this… (more)

▼ Many streams on the North Shore of Lake Superior, Minnesota, USA, are impaired for turbidity driven by excess fine sediment loading. The goal of this project was to develop a GIS-based model using new, openly-available, high-resolution remote datasets to predict erosional hotspots at a reach scale, based on three study watersheds: Amity Creek, the Talmadge River, and the French River. The ability to identify erosional hotspots, or locations that are highly susceptible to erosion, using remote data would be helpful for watershed managers in implementing practices to reduce turbidity in these streams. Erosion in streams is a balance between driving forces, largely controlled by topography; and resisting forces, controlled by the materials that make up a channel's bed and banks. New high-resolution topography and soils datasets for the North Shore provide the opportunity to extract these driving and resisting forces from remote datasets and possibly predict erosion potential and identify erosional hotspots. We used 3-meter LiDAR-derived DEMs to calculate a stream power-based erosion index, to identify stream reaches with high radius of curvature, and to identify stream reaches proximal to high bluffs. We used the Soil Survey Geographic (SSURGO) Database to investigate changes in erodibility along the channel. Because bedrock exposure significantly limits erodibility, we investigated bedrock exposure using bedrock outcrop maps made available by the Minnesota Geological Survey (MGS, Hobbs, 2002; Hobbs, 2009), and by using a feature extraction tool to remotely map bedrock exposure using high-resolution air photos and LiDAR data. Predictions based on remote data were compared with two datasets. Bank Erosion Hazard Index surveys, which are surveys designed to evaluate erosion susceptibility of banks, were collected along the three streams. In addition, a 500-year flood event during our field season gave us the opportunity to collect erosion data after a major event and validate our erosion hotspot predictions. Regressions between predictors and field datasets indicate that the most significant variables are bedrock exposure, the stream power-based erosion index, and bluff proximity. A logistic model developed using the three successful predictors for Amity Creek watershed was largely unsuccessful. A threshold-based model including the three successful predictors (stream power-based erosion index, bluff proximity, and bedrock exposure) was 70% accurate for predicting erosion hotspots along Amity Creek. The limited predictive power of the models stemmed in part from differences in locations of erosion hotspots in a single large-scale flood event and long-term erosion hotspots. The inability to predict site-specific characteristics like large woody debris or vegetation patterns makes predicting erosion hotspots in a given event very difficult. A field dataset including long-term erosion data may improve the model significantly. This model also requires high resolution bedrock exposure data which may limit its application to…

Subjects/Keywords: Erosion; fluvial; Hotspot; LiDAR; River; Stream

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APA (6^th Edition):

Wick, M. J. (2013). Identifying erosional hotspots in streams along the North Shore of Lake Superior, Minnesota using high-resolution elevation and soils data. (Masters Thesis). University of Minnesota. Retrieved from http://hdl.handle.net/11299/162413

Chicago Manual of Style (16^th Edition):

Wick, Molly Jane. “Identifying erosional hotspots in streams along the North Shore of Lake Superior, Minnesota using high-resolution elevation and soils data.” 2013. Masters Thesis, University of Minnesota. Accessed April 22, 2021. http://hdl.handle.net/11299/162413.

MLA Handbook (7^th Edition):

Wick, Molly Jane. “Identifying erosional hotspots in streams along the North Shore of Lake Superior, Minnesota using high-resolution elevation and soils data.” 2013. Web. 22 Apr 2021.

Vancouver:

Wick MJ. Identifying erosional hotspots in streams along the North Shore of Lake Superior, Minnesota using high-resolution elevation and soils data. [Internet] [Masters thesis]. University of Minnesota; 2013. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/11299/162413.

Council of Science Editors:

Wick MJ. Identifying erosional hotspots in streams along the North Shore of Lake Superior, Minnesota using high-resolution elevation and soils data. [Masters Thesis]. University of Minnesota; 2013. Available from: http://hdl.handle.net/11299/162413

University of Kansas

23. Andrzejewski, Kolbe D. HISTORICAL METAMORPHOSIS OF THE ARKANSAS RIVER ON THE KANSAS HIGH PLAINS.

Degree: MS, Geography, 2015, University of Kansas

URL: http://hdl.handle.net/1808/20669

► River metamorphosis is a well-documented global phenomenon, particularly for the historic period. The Arkansas River in western Kansas is an example of a river channel… (more)

▼ River metamorphosis is a well-documented global phenomenon, particularly for the historic period. The Arkansas River in western Kansas is an example of a river channel that has undergone a major historical metamorphosis: the pre-1900’s channel was wide, shallow and braided, but subsequently transformed into a narrow, sinuous meandering system. This study establishes the relationship between the hydrology and dynamics of channel morphology, determined the period in which the metamorphosis occurred, and quantified the channel change. In order to document channel change along a reach of the Arkansas River within the Kansas High Plains this study used ArcGIS to evaluate aerial photography for seven discrete years within the past 75 years, USGS stream gages to document the historical decrease in discharge, Public Land Survey records to characterize early settlement channel widths, and lesser sources such as historical ground-based images and bridge construction plans to further document historical changes in channel morphology. Channel width and sinuosity were measured and recorded for each year of aerial photography to quantitatively determine the magnitude of change and to characterize progression of the historical metamorphosis. The river channel has narrowed by about 145 meters and increased in sinuosity from 1.22 to 1.46 since the acquisition of the first aerial photography (1939). Historical changes in the channel morphology have occurred because of many anthropogenic modifications including a dam, irrigation diversion canals, and groundwater pumping for center pivot irrigation systems. These anthropogenic influences have directly altered the hydrology of the river by decreasing mean annual discharge, reducing peak annual flows, and lowering the water table. The upstream part of the study reach, near the Colorado-Kansas border experiences sporadic flows and has a narrow sinuous channel, where the discharge is actively building and stabilizing the floodplain and channel banks. The downstream reach, below irrigation diversions, channel width increases and sinuosity decreases, where the surface flow is extremely rare, resulting in little or no channel change. Upstream reaches, near Syracuse, have high sinuosity values from riparian vegetation stabilizing point bars and cutbanks, whereas downstream reaches, near Garden City, have low sinuosity values due to minimal riparian vegetation. The character of the Arkansas River channel within the Kansas High Plains may continue its present trajectory as long as the present-day hydrologic regime is maintained and the prevailing climate is unchanged. Advisors/Committee Members: Johnson, William C (advisor), Egbert, Stephen L (cmtemember), Juracek, Kyle E (cmtemember), Halfen, Alan F (cmtemember), Johnson, William C (cmtemember).

Subjects/Keywords: Geomorphology; Geography; Geology; Arkansas River; Fluvial Geomorphology; River Channel Change; River Channel Morphology; River Metamorphosis

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APA (6^th Edition):

Andrzejewski, K. D. (2015). HISTORICAL METAMORPHOSIS OF THE ARKANSAS RIVER ON THE KANSAS HIGH PLAINS. (Masters Thesis). University of Kansas. Retrieved from http://hdl.handle.net/1808/20669

Chicago Manual of Style (16^th Edition):

Andrzejewski, Kolbe D. “HISTORICAL METAMORPHOSIS OF THE ARKANSAS RIVER ON THE KANSAS HIGH PLAINS.” 2015. Masters Thesis, University of Kansas. Accessed April 22, 2021. http://hdl.handle.net/1808/20669.

MLA Handbook (7^th Edition):

Andrzejewski, Kolbe D. “HISTORICAL METAMORPHOSIS OF THE ARKANSAS RIVER ON THE KANSAS HIGH PLAINS.” 2015. Web. 22 Apr 2021.

Vancouver:

Andrzejewski KD. HISTORICAL METAMORPHOSIS OF THE ARKANSAS RIVER ON THE KANSAS HIGH PLAINS. [Internet] [Masters thesis]. University of Kansas; 2015. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/1808/20669.

Council of Science Editors:

Andrzejewski KD. HISTORICAL METAMORPHOSIS OF THE ARKANSAS RIVER ON THE KANSAS HIGH PLAINS. [Masters Thesis]. University of Kansas; 2015. Available from: http://hdl.handle.net/1808/20669

Utah State University

24. Neenan, Johnathan. Evaluation of Stream Bank Restoration to Improve Water Quality in a Semi-Arid Stream.

Degree: MS, Watershed Sciences, 2019, Utah State University

URL: https://digitalcommons.usu.edu/etd/7687

► Human watershed activities such as converting land cover to agriculture and livestock grazing have negatively impacted stream water quality worldwide. One such case is… (more)

Subjects/Keywords: river restoration; water quality; streambank erosion; historical aerial photo analysis; restoration decision making; Water Resource Management

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APA (6^th Edition):

Neenan, J. (2019). Evaluation of Stream Bank Restoration to Improve Water Quality in a Semi-Arid Stream. (Masters Thesis). Utah State University. Retrieved from https://digitalcommons.usu.edu/etd/7687

Chicago Manual of Style (16^th Edition):

Neenan, Johnathan. “Evaluation of Stream Bank Restoration to Improve Water Quality in a Semi-Arid Stream.” 2019. Masters Thesis, Utah State University. Accessed April 22, 2021. https://digitalcommons.usu.edu/etd/7687.

MLA Handbook (7^th Edition):

Neenan, Johnathan. “Evaluation of Stream Bank Restoration to Improve Water Quality in a Semi-Arid Stream.” 2019. Web. 22 Apr 2021.

Vancouver:

Neenan J. Evaluation of Stream Bank Restoration to Improve Water Quality in a Semi-Arid Stream. [Internet] [Masters thesis]. Utah State University; 2019. [cited 2021 Apr 22]. Available from: https://digitalcommons.usu.edu/etd/7687.

Council of Science Editors:

Neenan J. Evaluation of Stream Bank Restoration to Improve Water Quality in a Semi-Arid Stream. [Masters Thesis]. Utah State University; 2019. Available from: https://digitalcommons.usu.edu/etd/7687

University of Oregon

25. Duffin, Jenna. Effects of Engineered Log Jams on Channel Morphology, Middle Fork of the John Day River, Oregon.

Degree: MS, Department of Geography, 2015, University of Oregon

URL: http://hdl.handle.net/1794/19338

► Engineered log jams (ELJs) were constructed on the Middle Fork of the John Day River in eastern Oregon as part of a large restoration project.… (more)

Subjects/Keywords: Engineered log jams; Fluvial; River restoration

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APA (6^th Edition):

Duffin, J. (2015). Effects of Engineered Log Jams on Channel Morphology, Middle Fork of the John Day River, Oregon. (Masters Thesis). University of Oregon. Retrieved from http://hdl.handle.net/1794/19338

Chicago Manual of Style (16^th Edition):

Duffin, Jenna. “Effects of Engineered Log Jams on Channel Morphology, Middle Fork of the John Day River, Oregon.” 2015. Masters Thesis, University of Oregon. Accessed April 22, 2021. http://hdl.handle.net/1794/19338.

MLA Handbook (7^th Edition):

Duffin, Jenna. “Effects of Engineered Log Jams on Channel Morphology, Middle Fork of the John Day River, Oregon.” 2015. Web. 22 Apr 2021.

Vancouver:

Duffin J. Effects of Engineered Log Jams on Channel Morphology, Middle Fork of the John Day River, Oregon. [Internet] [Masters thesis]. University of Oregon; 2015. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/1794/19338.

Council of Science Editors:

Duffin J. Effects of Engineered Log Jams on Channel Morphology, Middle Fork of the John Day River, Oregon. [Masters Thesis]. University of Oregon; 2015. Available from: http://hdl.handle.net/1794/19338

University of Connecticut

26. Belliveau, Lindsey C. Investigating Unit Stream Power and Drainage Capture in the Upper Dajia River, Taiwan using Geomorphic Indices.

Degree: MS, Geological Sciences, 2016, University of Connecticut

URL: https://opencommons.uconn.edu/gs_theses/987

Subjects/Keywords: geology; geomorphology; fluvial; rivers; Taiwan; Dajia River; watersheds; erosion; river incision; meanders

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APA (6^th Edition):

Belliveau, L. C. (2016). Investigating Unit Stream Power and Drainage Capture in the Upper Dajia River, Taiwan using Geomorphic Indices. (Masters Thesis). University of Connecticut. Retrieved from https://opencommons.uconn.edu/gs_theses/987

Chicago Manual of Style (16^th Edition):

Belliveau, Lindsey C. “Investigating Unit Stream Power and Drainage Capture in the Upper Dajia River, Taiwan using Geomorphic Indices.” 2016. Masters Thesis, University of Connecticut. Accessed April 22, 2021. https://opencommons.uconn.edu/gs_theses/987.

MLA Handbook (7^th Edition):

Belliveau, Lindsey C. “Investigating Unit Stream Power and Drainage Capture in the Upper Dajia River, Taiwan using Geomorphic Indices.” 2016. Web. 22 Apr 2021.

Vancouver:

Belliveau LC. Investigating Unit Stream Power and Drainage Capture in the Upper Dajia River, Taiwan using Geomorphic Indices. [Internet] [Masters thesis]. University of Connecticut; 2016. [cited 2021 Apr 22]. Available from: https://opencommons.uconn.edu/gs_theses/987.

Council of Science Editors:

Belliveau LC. Investigating Unit Stream Power and Drainage Capture in the Upper Dajia River, Taiwan using Geomorphic Indices. [Masters Thesis]. University of Connecticut; 2016. Available from: https://opencommons.uconn.edu/gs_theses/987

Vanderbilt University

27. Pickering, Jennifer Lynne. Response of the Brahmaputra River to Tectonic Deformation and Paleohydrological Events in the Foreland Bengal Basin.

Degree: PhD, Environmental Engineering, 2016, Vanderbilt University

URL: http://hdl.handle.net/1803/13467

► The Brahmaputra River has constructed an upland fluvial fan delta with an estimated volume of >5 million km³; of riverine sediments. Much of this stratigraphy… (more)

Subjects/Keywords: allogenic influences on river course; fluvial geomorphology; valley formation; fluvial sedimentology

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APA (6^th Edition):

Pickering, J. L. (2016). Response of the Brahmaputra River to Tectonic Deformation and Paleohydrological Events in the Foreland Bengal Basin. (Doctoral Dissertation). Vanderbilt University. Retrieved from http://hdl.handle.net/1803/13467

Chicago Manual of Style (16^th Edition):

Pickering, Jennifer Lynne. “Response of the Brahmaputra River to Tectonic Deformation and Paleohydrological Events in the Foreland Bengal Basin.” 2016. Doctoral Dissertation, Vanderbilt University. Accessed April 22, 2021. http://hdl.handle.net/1803/13467.

MLA Handbook (7^th Edition):

Pickering, Jennifer Lynne. “Response of the Brahmaputra River to Tectonic Deformation and Paleohydrological Events in the Foreland Bengal Basin.” 2016. Web. 22 Apr 2021.

Vancouver:

Pickering JL. Response of the Brahmaputra River to Tectonic Deformation and Paleohydrological Events in the Foreland Bengal Basin. [Internet] [Doctoral dissertation]. Vanderbilt University; 2016. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/1803/13467.

Council of Science Editors:

Pickering JL. Response of the Brahmaputra River to Tectonic Deformation and Paleohydrological Events in the Foreland Bengal Basin. [Doctoral Dissertation]. Vanderbilt University; 2016. Available from: http://hdl.handle.net/1803/13467

28. Primo, Kristiane Ramos [UNESP]. Avaliação ambiental de trechos urbanos de córregos de leito concretado após intervenções one-off visando a revitalização.

Degree: 2020, Universidade Estadual Paulista (UNESP)

URL: http://hdl.handle.net/11449/191976

►

Submitted by Kristiane Ramos Primo ([email protected]) on 2020-03-16T12:41:07Z No. of bitstreams: 1 tese_versao20_corrigida_comataeficha.pdf: 19266514 bytes, checksum: efc50845791f3360b32eeb5dc1218965 (MD5)

Submitted by Kristiane Ramos Primo ([email protected]) on… (more)

▼

Submitted by Kristiane Ramos Primo ([email protected]) on 2020-03-16T12:41:07Z No. of bitstreams: 1 tese_versao20_corrigida_comataeficha.pdf: 19266514 bytes, checksum: efc50845791f3360b32eeb5dc1218965 (MD5)

Rejected by Luana Priscila Costa ([email protected]), reason: Solicitamos que realize correções na submissão seguindo as orientações abaixo: -O preenchimento no campo “Número do processo/financiamento” é obrigatório para pesquisas financiadas pela Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP). Você assinalou que não obteve financiamento, porém em seu agradecimento aparece menção de financiamento da FAPESP. Nesse sentido, questiono se a tese está ou não vinculada ao referido projeto financiado pela FAPESP. Atenciosamente on 2020-03-24T13:42:22Z (GMT)

Submitted by Kristiane Ramos Primo ([email protected]) on 2020-03-16T12:41:07Z No. of bitstreams: 1 tese_versao20_corrigida_comataeficha.pdf: 19266514 bytes, checksum: efc50845791f3360b32eeb5dc1218965 (MD5)

Submitted by Kristiane Ramos Primo ([email protected]) on 2020-03-24T14:01:46Z No. of bitstreams: 1 tese_versao20_corrigida_comataeficha.pdf: 19266514 bytes, checksum: efc50845791f3360b32eeb5dc1218965 (MD5)

Rejected by Luana Priscila Costa ([email protected]), reason: Solicitamos que realize correções na submissão seguindo as orientações abaixo: -O preenchimento no campo “Número do processo/financiamento” é obrigatório para pesquisas financiadas pela Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP). Você assinalou que não obteve financiamento, porém em seu agradecimento aparece menção de financiamento da FAPESP. Nesse sentido, questiono se a tese está ou não vinculada ao referido projeto financiado pela FAPESP. Atenciosamente on 2020-03-24T13:42:22Z (GMT)

Submitted by Kristiane Ramos Primo ([email protected]) on 2020-03-24T14:01:46Z No. of bitstreams: 1 tese_versao20_corrigida_comataeficha.pdf: 19266514 bytes, checksum: efc50845791f3360b32eeb5dc1218965 (MD5)

Approved for entry into archive by Luana Priscila Costa ([email protected]) on 2020-03-24T14:54:32Z (GMT) No. of bitstreams: 1 tese_versao20_corrigida_comataeficha.pdf: 19266514 bytes, checksum: efc50845791f3360b32eeb5dc1218965 (MD5)

Submitted by Kristiane Ramos Primo ([email protected]) on 2020-03-24T14:01:46Z No. of…

Advisors/Committee Members: Universidade Estadual Paulista (UNESP), Silva, Alexandre Marco da [UNESP].

Subjects/Keywords: Saneamento; Desenvolvimento de recursos hídricos; Sucessão ecológica; River restoration; Sanitation; Water resources development; River restoration; Ecological succession

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APA (6^th Edition):

Primo, K. R. [. (2020). Avaliação ambiental de trechos urbanos de córregos de leito concretado após intervenções one-off visando a revitalização. (Doctoral Dissertation). Universidade Estadual Paulista (UNESP). Retrieved from http://hdl.handle.net/11449/191976

Chicago Manual of Style (16^th Edition):

Primo, Kristiane Ramos [UNESP]. “Avaliação ambiental de trechos urbanos de córregos de leito concretado após intervenções one-off visando a revitalização.” 2020. Doctoral Dissertation, Universidade Estadual Paulista (UNESP). Accessed April 22, 2021. http://hdl.handle.net/11449/191976.

MLA Handbook (7^th Edition):

Primo, Kristiane Ramos [UNESP]. “Avaliação ambiental de trechos urbanos de córregos de leito concretado após intervenções one-off visando a revitalização.” 2020. Web. 22 Apr 2021.

Vancouver:

Primo KR[. Avaliação ambiental de trechos urbanos de córregos de leito concretado após intervenções one-off visando a revitalização. [Internet] [Doctoral dissertation]. Universidade Estadual Paulista (UNESP); 2020. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/11449/191976.

Council of Science Editors:

Primo KR[. Avaliação ambiental de trechos urbanos de córregos de leito concretado após intervenções one-off visando a revitalização. [Doctoral Dissertation]. Universidade Estadual Paulista (UNESP); 2020. Available from: http://hdl.handle.net/11449/191976

Lincoln University

29. Healey, Mark O. Investigation of flood risk & erosion mitigation on the Rangitata River at Klondyke.

Degree: 1997, Lincoln University

URL: http://hdl.handle.net/10182/2499

► Risks to operational integrity of the Rangitata Diversion Race (RDR) presented by bank erosion and extreme discharges in the Rangitata River are investigated. Specific investigations… (more)

Subjects/Keywords: Rangitata River; Klondyke; Rangitata Diversion Race (RDR); Canterbury; New Zealand; river bank erosion; physical hydraulic modelling; computational hydraulics; fluvial geomorphology; river engineering; hydrology; flood frequency analysis; flood control

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Healey, M. O. (1997). Investigation of flood risk & erosion mitigation on the Rangitata River at Klondyke. (Thesis). Lincoln University. Retrieved from http://hdl.handle.net/10182/2499

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16^th Edition):

Healey, Mark O. “Investigation of flood risk & erosion mitigation on the Rangitata River at Klondyke.” 1997. Thesis, Lincoln University. Accessed April 22, 2021. http://hdl.handle.net/10182/2499.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7^th Edition):

Healey, Mark O. “Investigation of flood risk & erosion mitigation on the Rangitata River at Klondyke.” 1997. Web. 22 Apr 2021.

Vancouver:

Healey MO. Investigation of flood risk & erosion mitigation on the Rangitata River at Klondyke. [Internet] [Thesis]. Lincoln University; 1997. [cited 2021 Apr 22]. Available from: http://hdl.handle.net/10182/2499.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Healey MO. Investigation of flood risk & erosion mitigation on the Rangitata River at Klondyke. [Thesis]. Lincoln University; 1997. Available from: http://hdl.handle.net/10182/2499

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

30. Noonan, Brian John. Stream channel erosion as a source of sediment and phosphorus in a central Iowa stream.

Degree: 2016, Iowa State University

URL: https://lib.dr.iastate.edu/etd/15096

► A growing body of evidence suggests that a substantial portion of the sediment and phosphorus delivered to surface waters from agricultural landscapes originates from stream… (more)

Subjects/Keywords: Environmental Science; Midwest; phosphorus; sediment; storm flow; stream bank erosion; transport; Environmental Sciences; Geomorphology; Water Resource Management

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Record Details Similar Records Cite « Share

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Noonan, B. J. (2016). Stream channel erosion as a source of sediment and phosphorus in a central Iowa stream. (Thesis). Iowa State University. Retrieved from https://lib.dr.iastate.edu/etd/15096

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16^th Edition):

Noonan, Brian John. “Stream channel erosion as a source of sediment and phosphorus in a central Iowa stream.” 2016. Thesis, Iowa State University. Accessed April 22, 2021. https://lib.dr.iastate.edu/etd/15096.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7^th Edition):

Noonan, Brian John. “Stream channel erosion as a source of sediment and phosphorus in a central Iowa stream.” 2016. Web. 22 Apr 2021.

Vancouver:

Noonan BJ. Stream channel erosion as a source of sediment and phosphorus in a central Iowa stream. [Internet] [Thesis]. Iowa State University; 2016. [cited 2021 Apr 22]. Available from: https://lib.dr.iastate.edu/etd/15096.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Noonan BJ. Stream channel erosion as a source of sediment and phosphorus in a central Iowa stream. [Thesis]. Iowa State University; 2016. Available from: https://lib.dr.iastate.edu/etd/15096

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

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