Loading…

Linear-stability analysis of plane beds under flows with suspended loads

Plane beds develop under flows in fluvial and marine environments; they are recorded as parallel lamination in sandstone beds, such as those found in turbidites. However, whereas turbidites typically exhibit parallel lamination, they rarely feature dune-scale cross-lamination. Although the reason fo...

Full description

Saved in:
Bibliographic Details
Published in:Earth surface dynamics 2023-10, Vol.11 (5), p.961-977
Main Authors: Ohata, Koji, Naruse, Hajime, Izumi, Norihiro
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by
cites cdi_FETCH-LOGICAL-a458t-907ef3dfccc54540683453e048f65a3dad42e16f182efcf3e967d938364c88c23
container_end_page 977
container_issue 5
container_start_page 961
container_title Earth surface dynamics
container_volume 11
creator Ohata, Koji
Naruse, Hajime
Izumi, Norihiro
description Plane beds develop under flows in fluvial and marine environments; they are recorded as parallel lamination in sandstone beds, such as those found in turbidites. However, whereas turbidites typically exhibit parallel lamination, they rarely feature dune-scale cross-lamination. Although the reason for the scarcity of dune-scale cross-lamination in turbidites is still debated, the formation of dunes may be dampened by suspended loads. Here, we perform, for the first time, linear-stability analysis to show that flows with suspended loads facilitate the formation of plane beds. For a fine-grained bed, a suspended load can promote the formation of plane beds and dampen the formation of dunes. These results of theoretical analysis were verified with observational data of plane beds under open-channel flows. Our theoretical analysis found that suspended loads promote the formation of plane beds, which suggests that the development of dunes under turbidity currents is suppressed by the presence of suspended loads.
doi_str_mv 10.5194/esurf-11-961-2023
format article
fullrecord <record><control><sourceid>gale_doaj_</sourceid><recordid>TN_cdi_doaj_primary_oai_doaj_org_article_d4a93806cc844c2191d299bed88079ee</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><galeid>A767987567</galeid><doaj_id>oai_doaj_org_article_d4a93806cc844c2191d299bed88079ee</doaj_id><sourcerecordid>A767987567</sourcerecordid><originalsourceid>FETCH-LOGICAL-a458t-907ef3dfccc54540683453e048f65a3dad42e16f182efcf3e967d938364c88c23</originalsourceid><addsrcrecordid>eNptkl1rFDEYhQdRsNT-AO8CXnkxNV-TSS5LUbuwIFQF70KavFmzzE7WvBnq_vumXVEXSi4SDs85cMLpureMXg7MyA-AS4k9Y71RrOeUixfdGWdG9UrwHy__e7_uLhC3lFIm-CCEOetu1mkGV3qs7i5NqR6Im910wIQkR7Kf3AzkDgKSZQ5QSJzyPZL7VH8SXHAPTQxkyi7gm-5VdBPCxZ_7vPv-6eO365t-_eXz6vpq3Ts56NobOkIUIXrvBzlIqrSQgwAqdVSDE8EFyYGpyDSH6KMAo8ZghBZKeq09F-fd6pgbstvafUk7Vw42u2SfhFw21pWa_AQ2SNecVHmvpfTtE1jgxrQ2WtPRALSsd8esfcm_FsBqt3kprT9arkfBjBkl_0dtXAtNc8y1OL9L6O3VqEajx0GNjbp8hmonwC75PENMTT8xvD8xNKbC77pxC6Jdfb09ZdmR9SUjFoh_izNqHydgnyZgGbNtAvZxAuIBzXaidA</addsrcrecordid><sourcetype>Open Website</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>2873199742</pqid></control><display><type>article</type><title>Linear-stability analysis of plane beds under flows with suspended loads</title><source>Publicly Available Content Database</source><creator>Ohata, Koji ; Naruse, Hajime ; Izumi, Norihiro</creator><creatorcontrib>Ohata, Koji ; Naruse, Hajime ; Izumi, Norihiro</creatorcontrib><description>Plane beds develop under flows in fluvial and marine environments; they are recorded as parallel lamination in sandstone beds, such as those found in turbidites. However, whereas turbidites typically exhibit parallel lamination, they rarely feature dune-scale cross-lamination. Although the reason for the scarcity of dune-scale cross-lamination in turbidites is still debated, the formation of dunes may be dampened by suspended loads. Here, we perform, for the first time, linear-stability analysis to show that flows with suspended loads facilitate the formation of plane beds. For a fine-grained bed, a suspended load can promote the formation of plane beds and dampen the formation of dunes. These results of theoretical analysis were verified with observational data of plane beds under open-channel flows. Our theoretical analysis found that suspended loads promote the formation of plane beds, which suggests that the development of dunes under turbidity currents is suppressed by the presence of suspended loads.</description><identifier>ISSN: 2196-632X</identifier><identifier>ISSN: 2196-6311</identifier><identifier>EISSN: 2196-632X</identifier><identifier>DOI: 10.5194/esurf-11-961-2023</identifier><language>eng</language><publisher>Gottingen: Copernicus GmbH</publisher><subject>Analysis ; Bed load ; Channel flow ; Cross laminating ; Dunes ; Flow control ; Flow velocity ; Geomorphology ; Laminated materials ; Lamination ; Loads (forces) ; Marine environment ; Open channel flow ; Reynolds number ; Sandstone ; Sediment transport ; Sedimentary rocks ; Stability analysis ; Suspended load ; Theoretical analysis ; Turbidites ; Turbidity ; Turbidity currents ; Viscosity</subject><ispartof>Earth surface dynamics, 2023-10, Vol.11 (5), p.961-977</ispartof><rights>COPYRIGHT 2023 Copernicus GmbH</rights><rights>2023. This work is published under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-a458t-907ef3dfccc54540683453e048f65a3dad42e16f182efcf3e967d938364c88c23</cites><orcidid>0000-0003-0739-4308 ; 0000-0003-3863-3404</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2873199742/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2873199742?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,25731,27901,27902,36989,44566,75096</link.rule.ids></links><search><creatorcontrib>Ohata, Koji</creatorcontrib><creatorcontrib>Naruse, Hajime</creatorcontrib><creatorcontrib>Izumi, Norihiro</creatorcontrib><title>Linear-stability analysis of plane beds under flows with suspended loads</title><title>Earth surface dynamics</title><description>Plane beds develop under flows in fluvial and marine environments; they are recorded as parallel lamination in sandstone beds, such as those found in turbidites. However, whereas turbidites typically exhibit parallel lamination, they rarely feature dune-scale cross-lamination. Although the reason for the scarcity of dune-scale cross-lamination in turbidites is still debated, the formation of dunes may be dampened by suspended loads. Here, we perform, for the first time, linear-stability analysis to show that flows with suspended loads facilitate the formation of plane beds. For a fine-grained bed, a suspended load can promote the formation of plane beds and dampen the formation of dunes. These results of theoretical analysis were verified with observational data of plane beds under open-channel flows. Our theoretical analysis found that suspended loads promote the formation of plane beds, which suggests that the development of dunes under turbidity currents is suppressed by the presence of suspended loads.</description><subject>Analysis</subject><subject>Bed load</subject><subject>Channel flow</subject><subject>Cross laminating</subject><subject>Dunes</subject><subject>Flow control</subject><subject>Flow velocity</subject><subject>Geomorphology</subject><subject>Laminated materials</subject><subject>Lamination</subject><subject>Loads (forces)</subject><subject>Marine environment</subject><subject>Open channel flow</subject><subject>Reynolds number</subject><subject>Sandstone</subject><subject>Sediment transport</subject><subject>Sedimentary rocks</subject><subject>Stability analysis</subject><subject>Suspended load</subject><subject>Theoretical analysis</subject><subject>Turbidites</subject><subject>Turbidity</subject><subject>Turbidity currents</subject><subject>Viscosity</subject><issn>2196-632X</issn><issn>2196-6311</issn><issn>2196-632X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNptkl1rFDEYhQdRsNT-AO8CXnkxNV-TSS5LUbuwIFQF70KavFmzzE7WvBnq_vumXVEXSi4SDs85cMLpureMXg7MyA-AS4k9Y71RrOeUixfdGWdG9UrwHy__e7_uLhC3lFIm-CCEOetu1mkGV3qs7i5NqR6Im910wIQkR7Kf3AzkDgKSZQ5QSJzyPZL7VH8SXHAPTQxkyi7gm-5VdBPCxZ_7vPv-6eO365t-_eXz6vpq3Ts56NobOkIUIXrvBzlIqrSQgwAqdVSDE8EFyYGpyDSH6KMAo8ZghBZKeq09F-fd6pgbstvafUk7Vw42u2SfhFw21pWa_AQ2SNecVHmvpfTtE1jgxrQ2WtPRALSsd8esfcm_FsBqt3kprT9arkfBjBkl_0dtXAtNc8y1OL9L6O3VqEajx0GNjbp8hmonwC75PENMTT8xvD8xNKbC77pxC6Jdfb09ZdmR9SUjFoh_izNqHydgnyZgGbNtAvZxAuIBzXaidA</recordid><startdate>20231006</startdate><enddate>20231006</enddate><creator>Ohata, Koji</creator><creator>Naruse, Hajime</creator><creator>Izumi, Norihiro</creator><general>Copernicus GmbH</general><general>Copernicus Publications</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ISR</scope><scope>7QH</scope><scope>7TN</scope><scope>7UA</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>PCBAR</scope><scope>PHGZM</scope><scope>PHGZT</scope><scope>PIMPY</scope><scope>PKEHL</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0003-0739-4308</orcidid><orcidid>https://orcid.org/0000-0003-3863-3404</orcidid></search><sort><creationdate>20231006</creationdate><title>Linear-stability analysis of plane beds under flows with suspended loads</title><author>Ohata, Koji ; Naruse, Hajime ; Izumi, Norihiro</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a458t-907ef3dfccc54540683453e048f65a3dad42e16f182efcf3e967d938364c88c23</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Analysis</topic><topic>Bed load</topic><topic>Channel flow</topic><topic>Cross laminating</topic><topic>Dunes</topic><topic>Flow control</topic><topic>Flow velocity</topic><topic>Geomorphology</topic><topic>Laminated materials</topic><topic>Lamination</topic><topic>Loads (forces)</topic><topic>Marine environment</topic><topic>Open channel flow</topic><topic>Reynolds number</topic><topic>Sandstone</topic><topic>Sediment transport</topic><topic>Sedimentary rocks</topic><topic>Stability analysis</topic><topic>Suspended load</topic><topic>Theoretical analysis</topic><topic>Turbidites</topic><topic>Turbidity</topic><topic>Turbidity currents</topic><topic>Viscosity</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ohata, Koji</creatorcontrib><creatorcontrib>Naruse, Hajime</creatorcontrib><creatorcontrib>Izumi, Norihiro</creatorcontrib><collection>CrossRef</collection><collection>Gale In Context: Science</collection><collection>Aqualine</collection><collection>Oceanic Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest Central (New)</collection><collection>ProQuest One Academic (New)</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Middle East (New)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>Directory of Open Access Journals</collection><jtitle>Earth surface dynamics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ohata, Koji</au><au>Naruse, Hajime</au><au>Izumi, Norihiro</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Linear-stability analysis of plane beds under flows with suspended loads</atitle><jtitle>Earth surface dynamics</jtitle><date>2023-10-06</date><risdate>2023</risdate><volume>11</volume><issue>5</issue><spage>961</spage><epage>977</epage><pages>961-977</pages><issn>2196-632X</issn><issn>2196-6311</issn><eissn>2196-632X</eissn><abstract>Plane beds develop under flows in fluvial and marine environments; they are recorded as parallel lamination in sandstone beds, such as those found in turbidites. However, whereas turbidites typically exhibit parallel lamination, they rarely feature dune-scale cross-lamination. Although the reason for the scarcity of dune-scale cross-lamination in turbidites is still debated, the formation of dunes may be dampened by suspended loads. Here, we perform, for the first time, linear-stability analysis to show that flows with suspended loads facilitate the formation of plane beds. For a fine-grained bed, a suspended load can promote the formation of plane beds and dampen the formation of dunes. These results of theoretical analysis were verified with observational data of plane beds under open-channel flows. Our theoretical analysis found that suspended loads promote the formation of plane beds, which suggests that the development of dunes under turbidity currents is suppressed by the presence of suspended loads.</abstract><cop>Gottingen</cop><pub>Copernicus GmbH</pub><doi>10.5194/esurf-11-961-2023</doi><tpages>17</tpages><orcidid>https://orcid.org/0000-0003-0739-4308</orcidid><orcidid>https://orcid.org/0000-0003-3863-3404</orcidid><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 2196-632X
ispartof Earth surface dynamics, 2023-10, Vol.11 (5), p.961-977
issn 2196-632X
2196-6311
2196-632X
language eng
recordid cdi_doaj_primary_oai_doaj_org_article_d4a93806cc844c2191d299bed88079ee
source Publicly Available Content Database
subjects Analysis
Bed load
Channel flow
Cross laminating
Dunes
Flow control
Flow velocity
Geomorphology
Laminated materials
Lamination
Loads (forces)
Marine environment
Open channel flow
Reynolds number
Sandstone
Sediment transport
Sedimentary rocks
Stability analysis
Suspended load
Theoretical analysis
Turbidites
Turbidity
Turbidity currents
Viscosity
title Linear-stability analysis of plane beds under flows with suspended loads
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-21T04%3A18%3A22IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-gale_doaj_&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Linear-stability%20analysis%20of%20plane%20beds%20under%20flows%20with%20suspended%20loads&rft.jtitle=Earth%20surface%20dynamics&rft.au=Ohata,%20Koji&rft.date=2023-10-06&rft.volume=11&rft.issue=5&rft.spage=961&rft.epage=977&rft.pages=961-977&rft.issn=2196-632X&rft.eissn=2196-632X&rft_id=info:doi/10.5194/esurf-11-961-2023&rft_dat=%3Cgale_doaj_%3EA767987567%3C/gale_doaj_%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a458t-907ef3dfccc54540683453e048f65a3dad42e16f182efcf3e967d938364c88c23%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=2873199742&rft_id=info:pmid/&rft_galeid=A767987567&rfr_iscdi=true