Investigation of Cobble Bar Morphology and Sediment Texture in an Arctic River

Different methods are widely used to map grain size distributions in rivers, and a comparison of these methods could give better insight into the fluvial geomorphology of Arctic rivers, which are inaccessible to sampling over much of the year. This study focuses on the Miella River near Abisko, Swed...

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Bibliographic Details
Main Author: Shoen, Kyle
Other Authors: Sawyer, Audrey
Format: Thesis
Language:English
Published: The Ohio State University 2024
Subjects:
Online Access:https://kb.osu.edu/handle/1811/104258
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spelling ftohiostateu:oai:kb.osu.edu:1811/104258 2024-05-19T07:27:18+00:00 Investigation of Cobble Bar Morphology and Sediment Texture in an Arctic River Shoen, Kyle Sawyer, Audrey 2024-05 application/pdf https://kb.osu.edu/handle/1811/104258 en_US eng The Ohio State University The Ohio State University. School of Earth Sciences Undergraduate Research Theses https://kb.osu.edu/handle/1811/104258 Earth Science Morphology Sediment Texture Arctic Grain Sizing Thesis 2024 ftohiostateu 2024-04-30T23:30:13Z Different methods are widely used to map grain size distributions in rivers, and a comparison of these methods could give better insight into the fluvial geomorphology of Arctic rivers, which are inaccessible to sampling over much of the year. This study focuses on the Miella River near Abisko, Sweden (latitude 68N), which has ice break-up and flood events. I analyze grain size across six geomorphic zones that were identified along a characteristic cobble bar and adjacent riverbed. As part of this analysis, I compare manual Wolman pebble counts and ground-based photographic analysis of sediment textures. Ten evenly scattered ground-based photographs from each of the six zones were taken approximately 1 m from the surface level and were analyzed using BASEGRAIN, an automatic MATLAB-based object detection software. BASEGRAIN was rapid to implement compared to Wolman pebble counts but challenging to implement in submerged portions of the channel, leading to inaccuracies in grain size estimation underwater. Both BASEGRAIN and Wolman pebble counts identified distinct sediment texture differences between zones. This study contributes to a larger effort to shed new light on geomorphologic and sediment transport processes of the Miella River and will help guide the selection of different grain size analysis techniques in future Arctic river studies. McKenzie-Brecher Undergraduate Research Grant from Byrd Polar and Climate Research Center GSA North Central Section Undergraduate Research Grant No embargo Academic Major: Earth Sciences Thesis Abisko Arctic Ohio State University (OSU): Knowledge Bank
institution Open Polar
collection Ohio State University (OSU): Knowledge Bank
op_collection_id ftohiostateu
language English
topic Earth Science
Morphology
Sediment Texture
Arctic
Grain Sizing
spellingShingle Earth Science
Morphology
Sediment Texture
Arctic
Grain Sizing
Shoen, Kyle
Investigation of Cobble Bar Morphology and Sediment Texture in an Arctic River
topic_facet Earth Science
Morphology
Sediment Texture
Arctic
Grain Sizing
description Different methods are widely used to map grain size distributions in rivers, and a comparison of these methods could give better insight into the fluvial geomorphology of Arctic rivers, which are inaccessible to sampling over much of the year. This study focuses on the Miella River near Abisko, Sweden (latitude 68N), which has ice break-up and flood events. I analyze grain size across six geomorphic zones that were identified along a characteristic cobble bar and adjacent riverbed. As part of this analysis, I compare manual Wolman pebble counts and ground-based photographic analysis of sediment textures. Ten evenly scattered ground-based photographs from each of the six zones were taken approximately 1 m from the surface level and were analyzed using BASEGRAIN, an automatic MATLAB-based object detection software. BASEGRAIN was rapid to implement compared to Wolman pebble counts but challenging to implement in submerged portions of the channel, leading to inaccuracies in grain size estimation underwater. Both BASEGRAIN and Wolman pebble counts identified distinct sediment texture differences between zones. This study contributes to a larger effort to shed new light on geomorphologic and sediment transport processes of the Miella River and will help guide the selection of different grain size analysis techniques in future Arctic river studies. McKenzie-Brecher Undergraduate Research Grant from Byrd Polar and Climate Research Center GSA North Central Section Undergraduate Research Grant No embargo Academic Major: Earth Sciences
author2 Sawyer, Audrey
format Thesis
author Shoen, Kyle
author_facet Shoen, Kyle
author_sort Shoen, Kyle
title Investigation of Cobble Bar Morphology and Sediment Texture in an Arctic River
title_short Investigation of Cobble Bar Morphology and Sediment Texture in an Arctic River
title_full Investigation of Cobble Bar Morphology and Sediment Texture in an Arctic River
title_fullStr Investigation of Cobble Bar Morphology and Sediment Texture in an Arctic River
title_full_unstemmed Investigation of Cobble Bar Morphology and Sediment Texture in an Arctic River
title_sort investigation of cobble bar morphology and sediment texture in an arctic river
publisher The Ohio State University
publishDate 2024
url https://kb.osu.edu/handle/1811/104258
genre Abisko
Arctic
genre_facet Abisko
Arctic
op_relation The Ohio State University. School of Earth Sciences Undergraduate Research Theses
https://kb.osu.edu/handle/1811/104258
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