Flow modelling to estimate suspended sediment travel times for two Canadian Deltas

The approximate travel times for suspended sediment transport through two multi-channel networks are estimated using flow modelling. The focus is on the movement of high sediment concentrations that travel rapidly downstream. Since suspended sediment transport through river confluences and bifurcati...

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Bibliographic Details
Main Author: S. R. Fassnacht
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2000
Subjects:
T
G
Online Access:https://doaj.org/article/6e6721e5ffaa4191b0b8f93eb9d6a885
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spelling ftdoajarticles:oai:doaj.org/article:6e6721e5ffaa4191b0b8f93eb9d6a885 2023-05-15T17:09:30+02:00 Flow modelling to estimate suspended sediment travel times for two Canadian Deltas S. R. Fassnacht 2000-01-01T00:00:00Z https://doaj.org/article/6e6721e5ffaa4191b0b8f93eb9d6a885 EN eng Copernicus Publications http://www.hydrol-earth-syst-sci.net/4/425/2000/hess-4-425-2000.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 1027-5606 1607-7938 https://doaj.org/article/6e6721e5ffaa4191b0b8f93eb9d6a885 Hydrology and Earth System Sciences, Vol 4, Iss 3, Pp 425-438 (2000) Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2000 ftdoajarticles 2022-12-31T07:23:27Z The approximate travel times for suspended sediment transport through two multi-channel networks are estimated using flow modelling. The focus is on the movement of high sediment concentrations that travel rapidly downstream. Since suspended sediment transport through river confluences and bifurcation movement is poorly understood, it is assumed that the sediment moves at approximately the average channel velocity during periods of high sediment load movement. Calibration of the flow model is discussed, with an emphasis on the incorporation of cross-section data, that are not referenced to a datum, using a continuous water surface profile. Various flow regimes are examined for the Mackenzie and the Slave River Deltas in the Northwest Territories, Canada, and a significant variation in travel times is illustrated. One set of continuous daily sediment measurements throughout the Mackenzie Delta is used to demonstrate that the travel time estimates are reasonable. Keywords: suspended sediment; multi-channel river systems; flow modelling; sediment transport Article in Journal/Newspaper Mackenzie Delta Northwest Territories Slave River Directory of Open Access Journals: DOAJ Articles Northwest Territories Canada Mackenzie Delta ENVELOPE(-136.672,-136.672,68.833,68.833)
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
spellingShingle Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
S. R. Fassnacht
Flow modelling to estimate suspended sediment travel times for two Canadian Deltas
topic_facet Technology
T
Environmental technology. Sanitary engineering
TD1-1066
Geography. Anthropology. Recreation
G
Environmental sciences
GE1-350
description The approximate travel times for suspended sediment transport through two multi-channel networks are estimated using flow modelling. The focus is on the movement of high sediment concentrations that travel rapidly downstream. Since suspended sediment transport through river confluences and bifurcation movement is poorly understood, it is assumed that the sediment moves at approximately the average channel velocity during periods of high sediment load movement. Calibration of the flow model is discussed, with an emphasis on the incorporation of cross-section data, that are not referenced to a datum, using a continuous water surface profile. Various flow regimes are examined for the Mackenzie and the Slave River Deltas in the Northwest Territories, Canada, and a significant variation in travel times is illustrated. One set of continuous daily sediment measurements throughout the Mackenzie Delta is used to demonstrate that the travel time estimates are reasonable. Keywords: suspended sediment; multi-channel river systems; flow modelling; sediment transport
format Article in Journal/Newspaper
author S. R. Fassnacht
author_facet S. R. Fassnacht
author_sort S. R. Fassnacht
title Flow modelling to estimate suspended sediment travel times for two Canadian Deltas
title_short Flow modelling to estimate suspended sediment travel times for two Canadian Deltas
title_full Flow modelling to estimate suspended sediment travel times for two Canadian Deltas
title_fullStr Flow modelling to estimate suspended sediment travel times for two Canadian Deltas
title_full_unstemmed Flow modelling to estimate suspended sediment travel times for two Canadian Deltas
title_sort flow modelling to estimate suspended sediment travel times for two canadian deltas
publisher Copernicus Publications
publishDate 2000
url https://doaj.org/article/6e6721e5ffaa4191b0b8f93eb9d6a885
long_lat ENVELOPE(-136.672,-136.672,68.833,68.833)
geographic Northwest Territories
Canada
Mackenzie Delta
geographic_facet Northwest Territories
Canada
Mackenzie Delta
genre Mackenzie Delta
Northwest Territories
Slave River
genre_facet Mackenzie Delta
Northwest Territories
Slave River
op_source Hydrology and Earth System Sciences, Vol 4, Iss 3, Pp 425-438 (2000)
op_relation http://www.hydrol-earth-syst-sci.net/4/425/2000/hess-4-425-2000.pdf
https://doaj.org/toc/1027-5606
https://doaj.org/toc/1607-7938
1027-5606
1607-7938
https://doaj.org/article/6e6721e5ffaa4191b0b8f93eb9d6a885
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