Upstream morphological effects of a sequential check dam adjustment process
Sediment flushing and the morphological responses to the procedure of check dam removal are still unclear. Following laboratory experiments that revealed three stages (deepening, widening, and volume release) of check dam adjustment, a check dam built in 2007 at Landao Creek in central Taiwan was ad...
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Veröffentlicht in: | Earth surface processes and landforms 2021-10, Vol.46 (13), p.2527-2539 |
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creator | Chiu, Yu‐Fang Tfwala, Samkele S. Hsu, Yung‐Ching Chiu, Yen‐Yu Lee, Chen‐Yang Chen, Su‐Chin |
description | Sediment flushing and the morphological responses to the procedure of check dam removal are still unclear. Following laboratory experiments that revealed three stages (deepening, widening, and volume release) of check dam adjustment, a check dam built in 2007 at Landao Creek in central Taiwan was adjusted in 2015 by removing central bars and cutting 2.5 m from the middle two piers (stage 1 + 2), with the purpose of regulating sediment transfer and keeping the thalweg at the center of the channel, while also preventing hill slope toe erosion. In 2019, four central piers were removed (stage 3) to increase the volume of sediment released. Annual surveys were conducted after the initial adjustment in 2015 through to 2020 using unmanned aerial vehicles (UAVs). The check dam adjustments revealed that the channel had narrowed and stabilized as indicated by regenerating riparian vegetation. Additionally, distinct terraces had formed on the hill slope toes of the creek channel in proximity to the check dam. The meander upstream weakened following the dam adjustments. This study combining laboratory experiments with actual field observation contributed immensely to check dam decommissioning. Additionally, this study illustrated how an adjustable check dam may aid regulation of sediment transport and thereby sediment balance. It can be adjusted accordingly based on the prevailing channel condition.
The check dam removal guide consists of three stages.
Stage 1: cutting the central portion deeper.
Stage 2: widens the opening.
Stage 3: complete removal. While the adjustable check dam can be adjusted freely in each stage according to the demand of the sediment budget. |
doi_str_mv | 10.1002/esp.5178 |
format | Article |
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The check dam removal guide consists of three stages.
Stage 1: cutting the central portion deeper.
Stage 2: widens the opening.
Stage 3: complete removal. While the adjustable check dam can be adjusted freely in each stage according to the demand of the sediment budget.</description><identifier>ISSN: 0197-9337</identifier><identifier>EISSN: 1096-9837</identifier><identifier>DOI: 10.1002/esp.5178</identifier><language>eng</language><publisher>Bognor Regis: Wiley Subscription Services, Inc</publisher><subject>adjustable check dam ; Check dams ; Coastal inlets ; Creeks ; Dam construction ; Dam effects ; dam removal ; floods ; Laboratories ; Laboratory experiments ; morphodynamics ; Morphology ; Piers ; Riparian vegetation ; Sediment ; sediment continuity ; Sediment transport ; Sediments ; Slopes ; Surveys ; Terraces ; Thalweg ; Unmanned aerial vehicles ; Upstream</subject><ispartof>Earth surface processes and landforms, 2021-10, Vol.46 (13), p.2527-2539</ispartof><rights>2021 John Wiley & Sons, Ltd.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3168-806ebd7f1c4cde0242a6004875a0ed25a514c59220206e832cfdd07d2373ee873</citedby><cites>FETCH-LOGICAL-a3168-806ebd7f1c4cde0242a6004875a0ed25a514c59220206e832cfdd07d2373ee873</cites><orcidid>0000-0003-4796-5435 ; 0000-0003-0662-4044 ; 0000-0002-6927-1402</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fesp.5178$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fesp.5178$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,27901,27902,45550,45551</link.rule.ids></links><search><creatorcontrib>Chiu, Yu‐Fang</creatorcontrib><creatorcontrib>Tfwala, Samkele S.</creatorcontrib><creatorcontrib>Hsu, Yung‐Ching</creatorcontrib><creatorcontrib>Chiu, Yen‐Yu</creatorcontrib><creatorcontrib>Lee, Chen‐Yang</creatorcontrib><creatorcontrib>Chen, Su‐Chin</creatorcontrib><title>Upstream morphological effects of a sequential check dam adjustment process</title><title>Earth surface processes and landforms</title><description>Sediment flushing and the morphological responses to the procedure of check dam removal are still unclear. Following laboratory experiments that revealed three stages (deepening, widening, and volume release) of check dam adjustment, a check dam built in 2007 at Landao Creek in central Taiwan was adjusted in 2015 by removing central bars and cutting 2.5 m from the middle two piers (stage 1 + 2), with the purpose of regulating sediment transfer and keeping the thalweg at the center of the channel, while also preventing hill slope toe erosion. In 2019, four central piers were removed (stage 3) to increase the volume of sediment released. Annual surveys were conducted after the initial adjustment in 2015 through to 2020 using unmanned aerial vehicles (UAVs). The check dam adjustments revealed that the channel had narrowed and stabilized as indicated by regenerating riparian vegetation. Additionally, distinct terraces had formed on the hill slope toes of the creek channel in proximity to the check dam. The meander upstream weakened following the dam adjustments. This study combining laboratory experiments with actual field observation contributed immensely to check dam decommissioning. Additionally, this study illustrated how an adjustable check dam may aid regulation of sediment transport and thereby sediment balance. It can be adjusted accordingly based on the prevailing channel condition.
The check dam removal guide consists of three stages.
Stage 1: cutting the central portion deeper.
Stage 2: widens the opening.
Stage 3: complete removal. While the adjustable check dam can be adjusted freely in each stage according to the demand of the sediment budget.</description><subject>adjustable check dam</subject><subject>Check dams</subject><subject>Coastal inlets</subject><subject>Creeks</subject><subject>Dam construction</subject><subject>Dam effects</subject><subject>dam removal</subject><subject>floods</subject><subject>Laboratories</subject><subject>Laboratory experiments</subject><subject>morphodynamics</subject><subject>Morphology</subject><subject>Piers</subject><subject>Riparian vegetation</subject><subject>Sediment</subject><subject>sediment continuity</subject><subject>Sediment transport</subject><subject>Sediments</subject><subject>Slopes</subject><subject>Surveys</subject><subject>Terraces</subject><subject>Thalweg</subject><subject>Unmanned aerial vehicles</subject><subject>Upstream</subject><issn>0197-9337</issn><issn>1096-9837</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp10E1LAzEQBuAgCq5V8CcsePGydZLsbpKjlPqBBQXtOcRkYrfudtdki_Tfm1qvngZeHmaGl5BLClMKwG4wDtOKCnlEMgqqLpTk4phkQJUoFOfilJzFuAagtJQqI0_LIY4BTZd3fRhWfdt_NNa0OXqPdox573OTR_za4mZsUm5XaD9zl7xx620cu5TnQ-gtxnhOTrxpI178zQlZ3s3fZg_F4vn-cXa7KAyntSwk1PjuhKe2tA6BlczUAKUUlQF0rDIVLW2lGAOWpOTMeudAOMYFR5SCT8jVYW-6mx6Lo17327BJJzWrhGKKlQKSuj4oG_oYA3o9hKYzYacp6H1VOlWl91UlWhzod9Pi7l-n568vv_4HssFp-w</recordid><startdate>202110</startdate><enddate>202110</enddate><creator>Chiu, Yu‐Fang</creator><creator>Tfwala, Samkele S.</creator><creator>Hsu, Yung‐Ching</creator><creator>Chiu, Yen‐Yu</creator><creator>Lee, Chen‐Yang</creator><creator>Chen, Su‐Chin</creator><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0003-4796-5435</orcidid><orcidid>https://orcid.org/0000-0003-0662-4044</orcidid><orcidid>https://orcid.org/0000-0002-6927-1402</orcidid></search><sort><creationdate>202110</creationdate><title>Upstream morphological effects of a sequential check dam adjustment process</title><author>Chiu, Yu‐Fang ; Tfwala, Samkele S. ; Hsu, Yung‐Ching ; Chiu, Yen‐Yu ; Lee, Chen‐Yang ; Chen, Su‐Chin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3168-806ebd7f1c4cde0242a6004875a0ed25a514c59220206e832cfdd07d2373ee873</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>adjustable check dam</topic><topic>Check dams</topic><topic>Coastal inlets</topic><topic>Creeks</topic><topic>Dam construction</topic><topic>Dam effects</topic><topic>dam removal</topic><topic>floods</topic><topic>Laboratories</topic><topic>Laboratory experiments</topic><topic>morphodynamics</topic><topic>Morphology</topic><topic>Piers</topic><topic>Riparian vegetation</topic><topic>Sediment</topic><topic>sediment continuity</topic><topic>Sediment transport</topic><topic>Sediments</topic><topic>Slopes</topic><topic>Surveys</topic><topic>Terraces</topic><topic>Thalweg</topic><topic>Unmanned aerial vehicles</topic><topic>Upstream</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Chiu, Yu‐Fang</creatorcontrib><creatorcontrib>Tfwala, Samkele S.</creatorcontrib><creatorcontrib>Hsu, Yung‐Ching</creatorcontrib><creatorcontrib>Chiu, Yen‐Yu</creatorcontrib><creatorcontrib>Lee, Chen‐Yang</creatorcontrib><creatorcontrib>Chen, Su‐Chin</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Earth surface processes and landforms</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Chiu, Yu‐Fang</au><au>Tfwala, Samkele S.</au><au>Hsu, Yung‐Ching</au><au>Chiu, Yen‐Yu</au><au>Lee, Chen‐Yang</au><au>Chen, Su‐Chin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Upstream morphological effects of a sequential check dam adjustment process</atitle><jtitle>Earth surface processes and landforms</jtitle><date>2021-10</date><risdate>2021</risdate><volume>46</volume><issue>13</issue><spage>2527</spage><epage>2539</epage><pages>2527-2539</pages><issn>0197-9337</issn><eissn>1096-9837</eissn><abstract>Sediment flushing and the morphological responses to the procedure of check dam removal are still unclear. Following laboratory experiments that revealed three stages (deepening, widening, and volume release) of check dam adjustment, a check dam built in 2007 at Landao Creek in central Taiwan was adjusted in 2015 by removing central bars and cutting 2.5 m from the middle two piers (stage 1 + 2), with the purpose of regulating sediment transfer and keeping the thalweg at the center of the channel, while also preventing hill slope toe erosion. In 2019, four central piers were removed (stage 3) to increase the volume of sediment released. Annual surveys were conducted after the initial adjustment in 2015 through to 2020 using unmanned aerial vehicles (UAVs). The check dam adjustments revealed that the channel had narrowed and stabilized as indicated by regenerating riparian vegetation. Additionally, distinct terraces had formed on the hill slope toes of the creek channel in proximity to the check dam. The meander upstream weakened following the dam adjustments. This study combining laboratory experiments with actual field observation contributed immensely to check dam decommissioning. Additionally, this study illustrated how an adjustable check dam may aid regulation of sediment transport and thereby sediment balance. It can be adjusted accordingly based on the prevailing channel condition.
The check dam removal guide consists of three stages.
Stage 1: cutting the central portion deeper.
Stage 2: widens the opening.
Stage 3: complete removal. While the adjustable check dam can be adjusted freely in each stage according to the demand of the sediment budget.</abstract><cop>Bognor Regis</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1002/esp.5178</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0003-4796-5435</orcidid><orcidid>https://orcid.org/0000-0003-0662-4044</orcidid><orcidid>https://orcid.org/0000-0002-6927-1402</orcidid></addata></record> |
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subjects | adjustable check dam Check dams Coastal inlets Creeks Dam construction Dam effects dam removal floods Laboratories Laboratory experiments morphodynamics Morphology Piers Riparian vegetation Sediment sediment continuity Sediment transport Sediments Slopes Surveys Terraces Thalweg Unmanned aerial vehicles Upstream |
title | Upstream morphological effects of a sequential check dam adjustment process |
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