Channel aggradation triggered by dam failure amplifies the damage of outburst flood
Outburst floods generated by dam breaches associated with debris flow may have long-lasting effects on the formation and development landscape and the safety of human beings, increasing the difficulty of disaster prevention and mitigation. However, little was considered about channel aggradation con...
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description | Outburst floods generated by dam breaches associated with debris flow may have long-lasting effects on the formation and development landscape and the safety of human beings, increasing the difficulty of disaster prevention and mitigation. However, little was considered about channel aggradation contributing downstream damage of outburst flood. Therefore, we investigated a debris flow dam’s breaching and flooding process triggered by a 50-year heavy rainfall occurring on 17th June 2020 in Danba, China. The 6-m dam and a concomitant 1.04 × 10
6
m
3
barrier lake were formed by a tributary debris flow blocking the Xiaojin river. We used the dam breach overtopping and two-dimensional hydrodynamic models to simulate the whole process. The dam breach event persisted for 4.5 h with an outburst flood peak discharge of 823.5 m
3
/s, equal to a 20-year flood. It was noted that numerous sediments of approximately 5 × 10
6
m
3
were transported to the downstream channel, elevating the main channel bed and the terrace by 10–15 m and 2–5 m, respectively. Averaged transportation efficiency of an outburst flood is 1269.73 times greater than a 20-year seasonal flood. We simulated representative seasonal floods and outburst floods based on the pre-beach river geometry, which shows that previous channel capacity is sufficient to convey seasonal floods and the outburst flood. However, the outburst flood could easily submerge terraces and living land using after-breach geometry. Due to river aggradation lifting river elevation, deposited riverbed promotes sediment and flood evolute to living land, resulting in amplified damage. Additionally, we collected 59 dam breaches and demonstrated that local riverbed slopes could increase more than 100 times. During dam breaches, the sharp slope plays a key role in high sediment transportation efficiency. This study can promote understanding the formation and development of channel aggradation triggered by outburst flood and provide more reasonable considerations for disaster prevention and mitigation triggered by outburst flood hazard chain. |
doi_str_mv | 10.1007/s10346-023-02026-6 |
format | Article |
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6
m
3
barrier lake were formed by a tributary debris flow blocking the Xiaojin river. We used the dam breach overtopping and two-dimensional hydrodynamic models to simulate the whole process. The dam breach event persisted for 4.5 h with an outburst flood peak discharge of 823.5 m
3
/s, equal to a 20-year flood. It was noted that numerous sediments of approximately 5 × 10
6
m
3
were transported to the downstream channel, elevating the main channel bed and the terrace by 10–15 m and 2–5 m, respectively. Averaged transportation efficiency of an outburst flood is 1269.73 times greater than a 20-year seasonal flood. We simulated representative seasonal floods and outburst floods based on the pre-beach river geometry, which shows that previous channel capacity is sufficient to convey seasonal floods and the outburst flood. However, the outburst flood could easily submerge terraces and living land using after-breach geometry. Due to river aggradation lifting river elevation, deposited riverbed promotes sediment and flood evolute to living land, resulting in amplified damage. Additionally, we collected 59 dam breaches and demonstrated that local riverbed slopes could increase more than 100 times. During dam breaches, the sharp slope plays a key role in high sediment transportation efficiency. This study can promote understanding the formation and development of channel aggradation triggered by outburst flood and provide more reasonable considerations for disaster prevention and mitigation triggered by outburst flood hazard chain.</description><identifier>ISSN: 1612-510X</identifier><identifier>EISSN: 1612-5118</identifier><identifier>DOI: 10.1007/s10346-023-02026-6</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Accretion ; Aggradation ; Agriculture ; Amplification ; Channel capacity ; Civil Engineering ; Dam breaching ; Dam failure ; Dams ; Debris flow ; Detritus ; Disasters ; Downstream ; Earth and Environmental Science ; Earth Sciences ; Emergency preparedness ; Flood damage ; Flood hazards ; Flood peak ; Floods ; Geography ; Heavy rainfall ; Hydrodynamic models ; Lakes ; Mitigation ; Natural Hazards ; Original Paper ; Outbursts ; Overtopping ; Prevention ; Rainfall ; River beds ; River channels ; Riverbeds ; Rivers ; Sediment ; Sediments ; Slopes ; Storm damage ; Terraces ; Transportation ; Tributaries ; Two dimensional models</subject><ispartof>Landslides, 2023-07, Vol.20 (7), p.1343-1362</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a342t-8a22a0ecbaf09d05169d9b8c2bfc1f9832f7acc5d2b844fcb3129c73aa4abc853</citedby><cites>FETCH-LOGICAL-a342t-8a22a0ecbaf09d05169d9b8c2bfc1f9832f7acc5d2b844fcb3129c73aa4abc853</cites><orcidid>0000-0002-9559-5988</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s10346-023-02026-6$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s10346-023-02026-6$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,780,784,27924,27925,41488,42557,51319</link.rule.ids></links><search><creatorcontrib>Liu, Dingzhu</creatorcontrib><creatorcontrib>Cui, Yifei</creatorcontrib><creatorcontrib>Jin, Wen</creatorcontrib><creatorcontrib>Wang, Hao</creatorcontrib><creatorcontrib>Tang, Hui</creatorcontrib><title>Channel aggradation triggered by dam failure amplifies the damage of outburst flood</title><title>Landslides</title><addtitle>Landslides</addtitle><description>Outburst floods generated by dam breaches associated with debris flow may have long-lasting effects on the formation and development landscape and the safety of human beings, increasing the difficulty of disaster prevention and mitigation. However, little was considered about channel aggradation contributing downstream damage of outburst flood. Therefore, we investigated a debris flow dam’s breaching and flooding process triggered by a 50-year heavy rainfall occurring on 17th June 2020 in Danba, China. The 6-m dam and a concomitant 1.04 × 10
6
m
3
barrier lake were formed by a tributary debris flow blocking the Xiaojin river. We used the dam breach overtopping and two-dimensional hydrodynamic models to simulate the whole process. The dam breach event persisted for 4.5 h with an outburst flood peak discharge of 823.5 m
3
/s, equal to a 20-year flood. It was noted that numerous sediments of approximately 5 × 10
6
m
3
were transported to the downstream channel, elevating the main channel bed and the terrace by 10–15 m and 2–5 m, respectively. Averaged transportation efficiency of an outburst flood is 1269.73 times greater than a 20-year seasonal flood. We simulated representative seasonal floods and outburst floods based on the pre-beach river geometry, which shows that previous channel capacity is sufficient to convey seasonal floods and the outburst flood. However, the outburst flood could easily submerge terraces and living land using after-breach geometry. Due to river aggradation lifting river elevation, deposited riverbed promotes sediment and flood evolute to living land, resulting in amplified damage. Additionally, we collected 59 dam breaches and demonstrated that local riverbed slopes could increase more than 100 times. During dam breaches, the sharp slope plays a key role in high sediment transportation efficiency. This study can promote understanding the formation and development of channel aggradation triggered by outburst flood and provide more reasonable considerations for disaster prevention and mitigation triggered by outburst flood hazard chain.</description><subject>Accretion</subject><subject>Aggradation</subject><subject>Agriculture</subject><subject>Amplification</subject><subject>Channel capacity</subject><subject>Civil Engineering</subject><subject>Dam breaching</subject><subject>Dam failure</subject><subject>Dams</subject><subject>Debris flow</subject><subject>Detritus</subject><subject>Disasters</subject><subject>Downstream</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Emergency preparedness</subject><subject>Flood damage</subject><subject>Flood hazards</subject><subject>Flood peak</subject><subject>Floods</subject><subject>Geography</subject><subject>Heavy rainfall</subject><subject>Hydrodynamic models</subject><subject>Lakes</subject><subject>Mitigation</subject><subject>Natural Hazards</subject><subject>Original Paper</subject><subject>Outbursts</subject><subject>Overtopping</subject><subject>Prevention</subject><subject>Rainfall</subject><subject>River beds</subject><subject>River channels</subject><subject>Riverbeds</subject><subject>Rivers</subject><subject>Sediment</subject><subject>Sediments</subject><subject>Slopes</subject><subject>Storm damage</subject><subject>Terraces</subject><subject>Transportation</subject><subject>Tributaries</subject><subject>Two dimensional models</subject><issn>1612-510X</issn><issn>1612-5118</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><recordid>eNp9kEtLxDAQx4MouK5-AU8Bz9W82qZHWXyB4EEFb2Hy6nbpNmuSHvbb27WiNw_DDMz_AT-ELim5poTUN4kSLqqCMD4NYVVRHaEFrSgrSkrl8e9NPk7RWUobQlhDeLNAr6s1DIPrMbRtBAu5CwPOsWtbF53Feo8tbLGHrh-jw7Dd9Z3vXMJ57Q4faB0OHocx6zGmjH0fgj1HJx765C5-9hK939-9rR6L55eHp9XtcwFcsFxIYAyIMxo8aSwpadXYRkvDtDfUN5IzX4MxpWVaCuGN5pQ1puYAArSRJV-iqzl3F8Pn6FJWmzDGYapUTLJaUiEmLEvEZpWJIaXovNrFbgtxryhRB3hqhqcmeOobnqomE59NaRIPE4u_6H9cX2fscwc</recordid><startdate>20230701</startdate><enddate>20230701</enddate><creator>Liu, Dingzhu</creator><creator>Cui, Yifei</creator><creator>Jin, Wen</creator><creator>Wang, Hao</creator><creator>Tang, Hui</creator><general>Springer Berlin 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triggered by dam failure amplifies the damage of outburst flood</title><author>Liu, Dingzhu ; Cui, Yifei ; Jin, Wen ; Wang, Hao ; Tang, Hui</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a342t-8a22a0ecbaf09d05169d9b8c2bfc1f9832f7acc5d2b844fcb3129c73aa4abc853</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Accretion</topic><topic>Aggradation</topic><topic>Agriculture</topic><topic>Amplification</topic><topic>Channel capacity</topic><topic>Civil Engineering</topic><topic>Dam breaching</topic><topic>Dam failure</topic><topic>Dams</topic><topic>Debris flow</topic><topic>Detritus</topic><topic>Disasters</topic><topic>Downstream</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Emergency preparedness</topic><topic>Flood damage</topic><topic>Flood hazards</topic><topic>Flood peak</topic><topic>Floods</topic><topic>Geography</topic><topic>Heavy rainfall</topic><topic>Hydrodynamic models</topic><topic>Lakes</topic><topic>Mitigation</topic><topic>Natural Hazards</topic><topic>Original Paper</topic><topic>Outbursts</topic><topic>Overtopping</topic><topic>Prevention</topic><topic>Rainfall</topic><topic>River beds</topic><topic>River channels</topic><topic>Riverbeds</topic><topic>Rivers</topic><topic>Sediment</topic><topic>Sediments</topic><topic>Slopes</topic><topic>Storm damage</topic><topic>Terraces</topic><topic>Transportation</topic><topic>Tributaries</topic><topic>Two dimensional models</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Liu, Dingzhu</creatorcontrib><creatorcontrib>Cui, Yifei</creatorcontrib><creatorcontrib>Jin, Wen</creatorcontrib><creatorcontrib>Wang, Hao</creatorcontrib><creatorcontrib>Tang, Hui</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central 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Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><jtitle>Landslides</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Liu, Dingzhu</au><au>Cui, Yifei</au><au>Jin, Wen</au><au>Wang, Hao</au><au>Tang, Hui</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Channel aggradation triggered by dam failure amplifies the damage of outburst flood</atitle><jtitle>Landslides</jtitle><stitle>Landslides</stitle><date>2023-07-01</date><risdate>2023</risdate><volume>20</volume><issue>7</issue><spage>1343</spage><epage>1362</epage><pages>1343-1362</pages><issn>1612-510X</issn><eissn>1612-5118</eissn><abstract>Outburst floods generated by dam breaches associated with debris flow may have long-lasting effects on the formation and development landscape and the safety of human beings, increasing the difficulty of disaster prevention and mitigation. However, little was considered about channel aggradation contributing downstream damage of outburst flood. Therefore, we investigated a debris flow dam’s breaching and flooding process triggered by a 50-year heavy rainfall occurring on 17th June 2020 in Danba, China. The 6-m dam and a concomitant 1.04 × 10
6
m
3
barrier lake were formed by a tributary debris flow blocking the Xiaojin river. We used the dam breach overtopping and two-dimensional hydrodynamic models to simulate the whole process. The dam breach event persisted for 4.5 h with an outburst flood peak discharge of 823.5 m
3
/s, equal to a 20-year flood. It was noted that numerous sediments of approximately 5 × 10
6
m
3
were transported to the downstream channel, elevating the main channel bed and the terrace by 10–15 m and 2–5 m, respectively. Averaged transportation efficiency of an outburst flood is 1269.73 times greater than a 20-year seasonal flood. We simulated representative seasonal floods and outburst floods based on the pre-beach river geometry, which shows that previous channel capacity is sufficient to convey seasonal floods and the outburst flood. However, the outburst flood could easily submerge terraces and living land using after-breach geometry. Due to river aggradation lifting river elevation, deposited riverbed promotes sediment and flood evolute to living land, resulting in amplified damage. Additionally, we collected 59 dam breaches and demonstrated that local riverbed slopes could increase more than 100 times. During dam breaches, the sharp slope plays a key role in high sediment transportation efficiency. This study can promote understanding the formation and development of channel aggradation triggered by outburst flood and provide more reasonable considerations for disaster prevention and mitigation triggered by outburst flood hazard chain.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s10346-023-02026-6</doi><tpages>20</tpages><orcidid>https://orcid.org/0000-0002-9559-5988</orcidid></addata></record> |
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subjects | Accretion Aggradation Agriculture Amplification Channel capacity Civil Engineering Dam breaching Dam failure Dams Debris flow Detritus Disasters Downstream Earth and Environmental Science Earth Sciences Emergency preparedness Flood damage Flood hazards Flood peak Floods Geography Heavy rainfall Hydrodynamic models Lakes Mitigation Natural Hazards Original Paper Outbursts Overtopping Prevention Rainfall River beds River channels Riverbeds Rivers Sediment Sediments Slopes Storm damage Terraces Transportation Tributaries Two dimensional models |
title | Channel aggradation triggered by dam failure amplifies the damage of outburst flood |
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