Water/Sediment Two-Phase Flow Relating to Natural Disaster
Multi-Phase flow is often related to natural disasters. Especially large flows cause drastic geomorphic changes and can lead to catastrophy in downstream areas. Debris flow is a typical two-phase flow in such phenomena. In this paper, the authors explain the behaviour of debris flow obtained by obse...
Gespeichert in:
Veröffentlicht in: | Japanese journal of multiphase flow 1991-07, Vol.5 (3), p.186-203 |
---|---|
Hauptverfasser: | , |
Format: | Artikel |
Sprache: | eng |
Online-Zugang: | Volltext |
Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
container_end_page | 203 |
---|---|
container_issue | 3 |
container_start_page | 186 |
container_title | Japanese journal of multiphase flow |
container_volume | 5 |
creator | ASHIDA, Kazuo EGASHIRA, Shinji |
description | Multi-Phase flow is often related to natural disasters. Especially large flows cause drastic geomorphic changes and can lead to catastrophy in downstream areas. Debris flow is a typical two-phase flow in such phenomena. In this paper, the authors explain the behaviour of debris flow obtained by observations and experiments. A consititutive equation for debris flow is developed by considering the mechanism of energy dissipation in the flow of the mixture of water and sand particles. The consititutive equation is applied to discuss the distributions of velocity and particle concentration in uniform debris flow. The authors describe the characteristics of two-phase flow in catastrophic events by taking such examples as the Mt. St. Helens eruption, Mt. Asama's eruption and the Mt. Ontake land slide. |
doi_str_mv | 10.3811/jjmf.5.186 |
format | Article |
fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1476183463</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>3176827641</sourcerecordid><originalsourceid>FETCH-LOGICAL-c996-82a86814d8f500ca14f36952322add8313011a30392865d86d2c68fbdb2a6dc33</originalsourceid><addsrcrecordid>eNotkE1Lw0AURQdRMNRu_AUBd0LSeTPJ9I07qVaFoqIBl8NrZqIp-agzCcV_35a6uptz74XD2DXwVCLAbLNpqzRPAdUZiwARknyu-TmLuIYsEZjJSzYNoV5zzrUCBTpid180OD_7dLZuXTfExa5P3n8ouHjZ9Lv4wzU01N13PPTxKw2jpyZ-qAOFQ-mKXVTUBDf9zwkrlo_F4jlZvT29LO5XSam1SlAQKoTMYpVzXhJklVQ6F1IIshYlSA5AkkstUOUWlRWlwmpt14KULaWcsJvT7Nb3v6MLg9n0o-8OjwayuQKUmTpStyeq9H0I3lVm6-uW_J8Bbo52zNGOyc3BjtwD71RVxg</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1476183463</pqid></control><display><type>article</type><title>Water/Sediment Two-Phase Flow Relating to Natural Disaster</title><source>J-STAGE Free</source><source>EZB-FREE-00999 freely available EZB journals</source><creator>ASHIDA, Kazuo ; EGASHIRA, Shinji</creator><creatorcontrib>ASHIDA, Kazuo ; EGASHIRA, Shinji</creatorcontrib><description>Multi-Phase flow is often related to natural disasters. Especially large flows cause drastic geomorphic changes and can lead to catastrophy in downstream areas. Debris flow is a typical two-phase flow in such phenomena. In this paper, the authors explain the behaviour of debris flow obtained by observations and experiments. A consititutive equation for debris flow is developed by considering the mechanism of energy dissipation in the flow of the mixture of water and sand particles. The consititutive equation is applied to discuss the distributions of velocity and particle concentration in uniform debris flow. The authors describe the characteristics of two-phase flow in catastrophic events by taking such examples as the Mt. St. Helens eruption, Mt. Asama's eruption and the Mt. Ontake land slide.</description><identifier>ISSN: 0914-2843</identifier><identifier>EISSN: 1881-5790</identifier><identifier>DOI: 10.3811/jjmf.5.186</identifier><language>eng</language><publisher>Osaka City: Japan Science and Technology Agency</publisher><ispartof>Japanese journal of multiphase flow, 1991-07, Vol.5 (3), p.186-203</ispartof><rights>Copyright Japan Science and Technology Agency 1991</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27901,27902</link.rule.ids></links><search><creatorcontrib>ASHIDA, Kazuo</creatorcontrib><creatorcontrib>EGASHIRA, Shinji</creatorcontrib><title>Water/Sediment Two-Phase Flow Relating to Natural Disaster</title><title>Japanese journal of multiphase flow</title><description>Multi-Phase flow is often related to natural disasters. Especially large flows cause drastic geomorphic changes and can lead to catastrophy in downstream areas. Debris flow is a typical two-phase flow in such phenomena. In this paper, the authors explain the behaviour of debris flow obtained by observations and experiments. A consititutive equation for debris flow is developed by considering the mechanism of energy dissipation in the flow of the mixture of water and sand particles. The consititutive equation is applied to discuss the distributions of velocity and particle concentration in uniform debris flow. The authors describe the characteristics of two-phase flow in catastrophic events by taking such examples as the Mt. St. Helens eruption, Mt. Asama's eruption and the Mt. Ontake land slide.</description><issn>0914-2843</issn><issn>1881-5790</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1991</creationdate><recordtype>article</recordtype><recordid>eNotkE1Lw0AURQdRMNRu_AUBd0LSeTPJ9I07qVaFoqIBl8NrZqIp-agzCcV_35a6uptz74XD2DXwVCLAbLNpqzRPAdUZiwARknyu-TmLuIYsEZjJSzYNoV5zzrUCBTpid180OD_7dLZuXTfExa5P3n8ouHjZ9Lv4wzU01N13PPTxKw2jpyZ-qAOFQ-mKXVTUBDf9zwkrlo_F4jlZvT29LO5XSam1SlAQKoTMYpVzXhJklVQ6F1IIshYlSA5AkkstUOUWlRWlwmpt14KULaWcsJvT7Nb3v6MLg9n0o-8OjwayuQKUmTpStyeq9H0I3lVm6-uW_J8Bbo52zNGOyc3BjtwD71RVxg</recordid><startdate>19910701</startdate><enddate>19910701</enddate><creator>ASHIDA, Kazuo</creator><creator>EGASHIRA, Shinji</creator><general>Japan Science and Technology Agency</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TB</scope><scope>8FD</scope><scope>FR3</scope><scope>KR7</scope></search><sort><creationdate>19910701</creationdate><title>Water/Sediment Two-Phase Flow Relating to Natural Disaster</title><author>ASHIDA, Kazuo ; EGASHIRA, Shinji</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c996-82a86814d8f500ca14f36952322add8313011a30392865d86d2c68fbdb2a6dc33</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1991</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>ASHIDA, Kazuo</creatorcontrib><creatorcontrib>EGASHIRA, Shinji</creatorcontrib><collection>CrossRef</collection><collection>Mechanical & Transportation Engineering Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Civil Engineering Abstracts</collection><jtitle>Japanese journal of multiphase flow</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>ASHIDA, Kazuo</au><au>EGASHIRA, Shinji</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Water/Sediment Two-Phase Flow Relating to Natural Disaster</atitle><jtitle>Japanese journal of multiphase flow</jtitle><date>1991-07-01</date><risdate>1991</risdate><volume>5</volume><issue>3</issue><spage>186</spage><epage>203</epage><pages>186-203</pages><issn>0914-2843</issn><eissn>1881-5790</eissn><abstract>Multi-Phase flow is often related to natural disasters. Especially large flows cause drastic geomorphic changes and can lead to catastrophy in downstream areas. Debris flow is a typical two-phase flow in such phenomena. In this paper, the authors explain the behaviour of debris flow obtained by observations and experiments. A consititutive equation for debris flow is developed by considering the mechanism of energy dissipation in the flow of the mixture of water and sand particles. The consititutive equation is applied to discuss the distributions of velocity and particle concentration in uniform debris flow. The authors describe the characteristics of two-phase flow in catastrophic events by taking such examples as the Mt. St. Helens eruption, Mt. Asama's eruption and the Mt. Ontake land slide.</abstract><cop>Osaka City</cop><pub>Japan Science and Technology Agency</pub><doi>10.3811/jjmf.5.186</doi><tpages>18</tpages><oa>free_for_read</oa></addata></record> |
fulltext | fulltext |
identifier | ISSN: 0914-2843 |
ispartof | Japanese journal of multiphase flow, 1991-07, Vol.5 (3), p.186-203 |
issn | 0914-2843 1881-5790 |
language | eng |
recordid | cdi_proquest_journals_1476183463 |
source | J-STAGE Free; EZB-FREE-00999 freely available EZB journals |
title | Water/Sediment Two-Phase Flow Relating to Natural Disaster |
url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-29T05%3A05%3A32IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Water/Sediment%20Two-Phase%20Flow%20Relating%20to%20Natural%20Disaster&rft.jtitle=Japanese%20journal%20of%20multiphase%20flow&rft.au=ASHIDA,%20Kazuo&rft.date=1991-07-01&rft.volume=5&rft.issue=3&rft.spage=186&rft.epage=203&rft.pages=186-203&rft.issn=0914-2843&rft.eissn=1881-5790&rft_id=info:doi/10.3811/jjmf.5.186&rft_dat=%3Cproquest_cross%3E3176827641%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1476183463&rft_id=info:pmid/&rfr_iscdi=true |