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...
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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 |
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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> |
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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 |
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