Simulation of reservoir sedimentation in mountain regions

If a catastrophic landslide occurs in mountain regions, the influence upon sediment transportation remains so great for a long time that the reservoir sedimentation will become a more serious problem. In such a case, the sediment discharge into the reservoir will change remarkably with erosion of th...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Hauptverfasser: Fujita, Masaharu, Michiue, Masanori, Ashida, Kazuo
Format: Buchkapitel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 222
container_issue
container_start_page 209
container_title
container_volume
creator Fujita, Masaharu
Michiue, Masanori
Ashida, Kazuo
description If a catastrophic landslide occurs in mountain regions, the influence upon sediment transportation remains so great for a long time that the reservoir sedimentation will become a more serious problem. In such a case, the sediment discharge into the reservoir will change remarkably with erosion of the sediment deposited in the valleys. So, the way to determine the boundary condition on sediment discharge is discussed by using the field data in the case of “Ontake landslide (1984)”. Then a method to predict the reservoir sedimentation in one dimension is developed on the basis of consideration of the changes of the boundary condition on sediment discharge into the reservoir. This method is applied to the reservoir sedimentation in a field and its applicability is very good.
doi_str_mv 10.1007/BFb0011192
format Book Chapter
fullrecord <record><control><sourceid>springer</sourceid><recordid>TN_cdi_springer_books_10_1007_BFb0011192</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>springer_books_10_1007_BFb0011192</sourcerecordid><originalsourceid>FETCH-springer_books_10_1007_BFb00111923</originalsourceid><addsrcrecordid>eNqVjjsPgjAUha-vRFAXf0FHF_ReWixdNRJ33RuI1VSFmlb9_WI0cXY6j-8MB2BKOCdEuVgVFSIRqbQDEyVzngnkuSBcdiGiJfEkzXLsQfwGmRCKZB8iVBwT5CSHEIdwRkwzwVUEamfrx7W8W9cwd2TeBOOfznoWzMHWprl_kG1Y7R5tao03p7YKYxgcy2swk6-OYFZs9uttEm7eNifjdeXcJWhC_f6tf7_5H9MXeKZCww</addsrcrecordid><sourcetype>Publisher</sourcetype><iscdi>true</iscdi><recordtype>book_chapter</recordtype></control><display><type>book_chapter</type><title>Simulation of reservoir sedimentation in mountain regions</title><source>Springer Books</source><creator>Fujita, Masaharu ; Michiue, Masanori ; Ashida, Kazuo</creator><contributor>Armanini, Aronne ; Di Silvio, Giampaolo</contributor><creatorcontrib>Fujita, Masaharu ; Michiue, Masanori ; Ashida, Kazuo ; Armanini, Aronne ; Di Silvio, Giampaolo</creatorcontrib><description>If a catastrophic landslide occurs in mountain regions, the influence upon sediment transportation remains so great for a long time that the reservoir sedimentation will become a more serious problem. In such a case, the sediment discharge into the reservoir will change remarkably with erosion of the sediment deposited in the valleys. So, the way to determine the boundary condition on sediment discharge is discussed by using the field data in the case of “Ontake landslide (1984)”. Then a method to predict the reservoir sedimentation in one dimension is developed on the basis of consideration of the changes of the boundary condition on sediment discharge into the reservoir. This method is applied to the reservoir sedimentation in a field and its applicability is very good.</description><identifier>ISSN: 0930-0317</identifier><identifier>ISBN: 3540544917</identifier><identifier>ISBN: 9783540544913</identifier><identifier>EISSN: 1613-2580</identifier><identifier>EISBN: 9783540384106</identifier><identifier>EISBN: 3540384103</identifier><identifier>DOI: 10.1007/BFb0011192</identifier><language>eng</language><publisher>Berlin, Heidelberg: Springer Berlin Heidelberg</publisher><subject>Debris Flow ; Grain Size Distribution ; Mountain Region ; Sediment Discharge ; Sediment Transport Rate</subject><ispartof>Fluvial Hydraulics of Mountain Regions, 2005, p.209-222</ispartof><rights>Springer-Verlag 1991</rights><woscitedreferencessubscribed>false</woscitedreferencessubscribed><relation>Lecture Notes in Earth Sciences</relation></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/BFb0011192$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/BFb0011192$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>779,780,784,793,27925,38255,41442,42511</link.rule.ids></links><search><contributor>Armanini, Aronne</contributor><contributor>Di Silvio, Giampaolo</contributor><creatorcontrib>Fujita, Masaharu</creatorcontrib><creatorcontrib>Michiue, Masanori</creatorcontrib><creatorcontrib>Ashida, Kazuo</creatorcontrib><title>Simulation of reservoir sedimentation in mountain regions</title><title>Fluvial Hydraulics of Mountain Regions</title><description>If a catastrophic landslide occurs in mountain regions, the influence upon sediment transportation remains so great for a long time that the reservoir sedimentation will become a more serious problem. In such a case, the sediment discharge into the reservoir will change remarkably with erosion of the sediment deposited in the valleys. So, the way to determine the boundary condition on sediment discharge is discussed by using the field data in the case of “Ontake landslide (1984)”. Then a method to predict the reservoir sedimentation in one dimension is developed on the basis of consideration of the changes of the boundary condition on sediment discharge into the reservoir. This method is applied to the reservoir sedimentation in a field and its applicability is very good.</description><subject>Debris Flow</subject><subject>Grain Size Distribution</subject><subject>Mountain Region</subject><subject>Sediment Discharge</subject><subject>Sediment Transport Rate</subject><issn>0930-0317</issn><issn>1613-2580</issn><isbn>3540544917</isbn><isbn>9783540544913</isbn><isbn>9783540384106</isbn><isbn>3540384103</isbn><fulltext>true</fulltext><rsrctype>book_chapter</rsrctype><creationdate>2005</creationdate><recordtype>book_chapter</recordtype><sourceid/><recordid>eNqVjjsPgjAUha-vRFAXf0FHF_ReWixdNRJ33RuI1VSFmlb9_WI0cXY6j-8MB2BKOCdEuVgVFSIRqbQDEyVzngnkuSBcdiGiJfEkzXLsQfwGmRCKZB8iVBwT5CSHEIdwRkwzwVUEamfrx7W8W9cwd2TeBOOfznoWzMHWprl_kG1Y7R5tao03p7YKYxgcy2swk6-OYFZs9uttEm7eNifjdeXcJWhC_f6tf7_5H9MXeKZCww</recordid><startdate>20051020</startdate><enddate>20051020</enddate><creator>Fujita, Masaharu</creator><creator>Michiue, Masanori</creator><creator>Ashida, Kazuo</creator><general>Springer Berlin Heidelberg</general><scope/></search><sort><creationdate>20051020</creationdate><title>Simulation of reservoir sedimentation in mountain regions</title><author>Fujita, Masaharu ; Michiue, Masanori ; Ashida, Kazuo</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-springer_books_10_1007_BFb00111923</frbrgroupid><rsrctype>book_chapters</rsrctype><prefilter>book_chapters</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Debris Flow</topic><topic>Grain Size Distribution</topic><topic>Mountain Region</topic><topic>Sediment Discharge</topic><topic>Sediment Transport Rate</topic><toplevel>online_resources</toplevel><creatorcontrib>Fujita, Masaharu</creatorcontrib><creatorcontrib>Michiue, Masanori</creatorcontrib><creatorcontrib>Ashida, Kazuo</creatorcontrib></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Fujita, Masaharu</au><au>Michiue, Masanori</au><au>Ashida, Kazuo</au><au>Armanini, Aronne</au><au>Di Silvio, Giampaolo</au><format>book</format><genre>bookitem</genre><ristype>CHAP</ristype><atitle>Simulation of reservoir sedimentation in mountain regions</atitle><btitle>Fluvial Hydraulics of Mountain Regions</btitle><seriestitle>Lecture Notes in Earth Sciences</seriestitle><date>2005-10-20</date><risdate>2005</risdate><spage>209</spage><epage>222</epage><pages>209-222</pages><issn>0930-0317</issn><eissn>1613-2580</eissn><isbn>3540544917</isbn><isbn>9783540544913</isbn><eisbn>9783540384106</eisbn><eisbn>3540384103</eisbn><abstract>If a catastrophic landslide occurs in mountain regions, the influence upon sediment transportation remains so great for a long time that the reservoir sedimentation will become a more serious problem. In such a case, the sediment discharge into the reservoir will change remarkably with erosion of the sediment deposited in the valleys. So, the way to determine the boundary condition on sediment discharge is discussed by using the field data in the case of “Ontake landslide (1984)”. Then a method to predict the reservoir sedimentation in one dimension is developed on the basis of consideration of the changes of the boundary condition on sediment discharge into the reservoir. This method is applied to the reservoir sedimentation in a field and its applicability is very good.</abstract><cop>Berlin, Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/BFb0011192</doi></addata></record>
fulltext fulltext
identifier ISSN: 0930-0317
ispartof Fluvial Hydraulics of Mountain Regions, 2005, p.209-222
issn 0930-0317
1613-2580
language eng
recordid cdi_springer_books_10_1007_BFb0011192
source Springer Books
subjects Debris Flow
Grain Size Distribution
Mountain Region
Sediment Discharge
Sediment Transport Rate
title Simulation of reservoir sedimentation in mountain regions
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-06T16%3A51%3A15IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-springer&rft_val_fmt=info:ofi/fmt:kev:mtx:book&rft.genre=bookitem&rft.atitle=Simulation%20of%20reservoir%20sedimentation%20in%20mountain%20regions&rft.btitle=Fluvial%20Hydraulics%20of%20Mountain%20Regions&rft.au=Fujita,%20Masaharu&rft.date=2005-10-20&rft.spage=209&rft.epage=222&rft.pages=209-222&rft.issn=0930-0317&rft.eissn=1613-2580&rft.isbn=3540544917&rft.isbn_list=9783540544913&rft_id=info:doi/10.1007/BFb0011192&rft_dat=%3Cspringer%3Espringer_books_10_1007_BFb0011192%3C/springer%3E%3Curl%3E%3C/url%3E&rft.eisbn=9783540384106&rft.eisbn_list=3540384103&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rfr_iscdi=true