A new method for the analytical solution of a degenerate diffusion equation

Certain nonlinear diffusion equations of degenerate parabolic type display a finite speed of propagation of disturbances. This mathematical behavior can be used to describe a wide range of nonlinear phenomena such as the penetration distance of a thermal layer, the boundary of a reaction zone, or a...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Advances in water resources 2005-10, Vol.28 (10), p.1091-1101
Hauptverfasser: Prasad, S.N., Salomon, J.B.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 1101
container_issue 10
container_start_page 1091
container_title Advances in water resources
container_volume 28
creator Prasad, S.N.
Salomon, J.B.
description Certain nonlinear diffusion equations of degenerate parabolic type display a finite speed of propagation of disturbances. This mathematical behavior can be used to describe a wide range of nonlinear phenomena such as the penetration distance of a thermal layer, the boundary of a reaction zone, or a wetting front in unsaturated soil moisture flow. However, there are two main difficulties in obtaining solutions to problems of this class. One is that the location of the interface is not known a priori and must be discovered during the analysis. The other is the fact that the differential equation is singular in the neighborhood of the interface. The solution technique developed and presented in this work overcomes these difficulties by extracting a local solution of the differential equation in the neighborhood of the diffusing front. One profound result is the discovery that the velocity of the front is entirely controlled by the first term of the spectral series expansion. Also, by capturing the critical behavior of the solution in the region of the singularity and incorporating the behavior as a dominant factor, the series expansion is provided a means for very rapid convergence. The versatility of the solution technique is demonstrated by solving various boundary value problems covering a broad range of interest and the solutions are tested against previously published results.
doi_str_mv 10.1016/j.advwatres.2005.04.005
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_17475979</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0309170805000989</els_id><sourcerecordid>17475979</sourcerecordid><originalsourceid>FETCH-LOGICAL-c370t-2d9c2706bf786396b091f234223d56b90aed4f47765051d1d2846c884e5860073</originalsourceid><addsrcrecordid>eNqFkDtPxDAQhC0EEsfjN-CKLmHtOHZSnhAvgUQB1JbPXoNPuRhsB8S_J6dDtFRTzDez2iHkjEHNgMmLdW3c55cpCXPNAdoaRD3LHlmwTvGql63aJwtooK-Ygu6QHOW8BoBOKL4g90s64hfdYHmLjvqYaHlDakYzfJdgzUBzHKYS4kijp4Y6fMURkylIXfB-ylsHPyazRU7IgTdDxtNfPSYv11fPl7fVw-PN3eXyobKNglJx11uuQK686mTTyxX0zPNGcN64Vq56MOiEF0rJFlrmmOOdkLbrBLadBFDNMTnf9b6n-DFhLnoTssVhMCPGKWumhGp71c-g2oE2xZwTev2ewsakb81Ab8fTa_03nt6Op0HoWebk2S7pTdTmNYWsX544sAYYCJjrZ2K5I3D-9DNg0tkGHC26kNAW7WL498oPiFiE7g</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>17475979</pqid></control><display><type>article</type><title>A new method for the analytical solution of a degenerate diffusion equation</title><source>Elsevier ScienceDirect Journals</source><creator>Prasad, S.N. ; Salomon, J.B.</creator><creatorcontrib>Prasad, S.N. ; Salomon, J.B.</creatorcontrib><description>Certain nonlinear diffusion equations of degenerate parabolic type display a finite speed of propagation of disturbances. This mathematical behavior can be used to describe a wide range of nonlinear phenomena such as the penetration distance of a thermal layer, the boundary of a reaction zone, or a wetting front in unsaturated soil moisture flow. However, there are two main difficulties in obtaining solutions to problems of this class. One is that the location of the interface is not known a priori and must be discovered during the analysis. The other is the fact that the differential equation is singular in the neighborhood of the interface. The solution technique developed and presented in this work overcomes these difficulties by extracting a local solution of the differential equation in the neighborhood of the diffusing front. One profound result is the discovery that the velocity of the front is entirely controlled by the first term of the spectral series expansion. Also, by capturing the critical behavior of the solution in the region of the singularity and incorporating the behavior as a dominant factor, the series expansion is provided a means for very rapid convergence. The versatility of the solution technique is demonstrated by solving various boundary value problems covering a broad range of interest and the solutions are tested against previously published results.</description><identifier>ISSN: 0309-1708</identifier><identifier>EISSN: 1872-9657</identifier><identifier>DOI: 10.1016/j.advwatres.2005.04.005</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Analytic methods ; diffusion ; equations ; Heat equation ; mathematical models ; Parabolic partial differential equations of degenerate type ; Singularities ; soil water movement ; unsaturated flow ; wetting front</subject><ispartof>Advances in water resources, 2005-10, Vol.28 (10), p.1091-1101</ispartof><rights>2005 Elsevier Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c370t-2d9c2706bf786396b091f234223d56b90aed4f47765051d1d2846c884e5860073</citedby><cites>FETCH-LOGICAL-c370t-2d9c2706bf786396b091f234223d56b90aed4f47765051d1d2846c884e5860073</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0309170805000989$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3536,27903,27904,65309</link.rule.ids></links><search><creatorcontrib>Prasad, S.N.</creatorcontrib><creatorcontrib>Salomon, J.B.</creatorcontrib><title>A new method for the analytical solution of a degenerate diffusion equation</title><title>Advances in water resources</title><description>Certain nonlinear diffusion equations of degenerate parabolic type display a finite speed of propagation of disturbances. This mathematical behavior can be used to describe a wide range of nonlinear phenomena such as the penetration distance of a thermal layer, the boundary of a reaction zone, or a wetting front in unsaturated soil moisture flow. However, there are two main difficulties in obtaining solutions to problems of this class. One is that the location of the interface is not known a priori and must be discovered during the analysis. The other is the fact that the differential equation is singular in the neighborhood of the interface. The solution technique developed and presented in this work overcomes these difficulties by extracting a local solution of the differential equation in the neighborhood of the diffusing front. One profound result is the discovery that the velocity of the front is entirely controlled by the first term of the spectral series expansion. Also, by capturing the critical behavior of the solution in the region of the singularity and incorporating the behavior as a dominant factor, the series expansion is provided a means for very rapid convergence. The versatility of the solution technique is demonstrated by solving various boundary value problems covering a broad range of interest and the solutions are tested against previously published results.</description><subject>Analytic methods</subject><subject>diffusion</subject><subject>equations</subject><subject>Heat equation</subject><subject>mathematical models</subject><subject>Parabolic partial differential equations of degenerate type</subject><subject>Singularities</subject><subject>soil water movement</subject><subject>unsaturated flow</subject><subject>wetting front</subject><issn>0309-1708</issn><issn>1872-9657</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2005</creationdate><recordtype>article</recordtype><recordid>eNqFkDtPxDAQhC0EEsfjN-CKLmHtOHZSnhAvgUQB1JbPXoNPuRhsB8S_J6dDtFRTzDez2iHkjEHNgMmLdW3c55cpCXPNAdoaRD3LHlmwTvGql63aJwtooK-Ygu6QHOW8BoBOKL4g90s64hfdYHmLjvqYaHlDakYzfJdgzUBzHKYS4kijp4Y6fMURkylIXfB-ylsHPyazRU7IgTdDxtNfPSYv11fPl7fVw-PN3eXyobKNglJx11uuQK686mTTyxX0zPNGcN64Vq56MOiEF0rJFlrmmOOdkLbrBLadBFDNMTnf9b6n-DFhLnoTssVhMCPGKWumhGp71c-g2oE2xZwTev2ewsakb81Ab8fTa_03nt6Op0HoWebk2S7pTdTmNYWsX544sAYYCJjrZ2K5I3D-9DNg0tkGHC26kNAW7WL498oPiFiE7g</recordid><startdate>20051001</startdate><enddate>20051001</enddate><creator>Prasad, S.N.</creator><creator>Salomon, J.B.</creator><general>Elsevier Ltd</general><scope>FBQ</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20051001</creationdate><title>A new method for the analytical solution of a degenerate diffusion equation</title><author>Prasad, S.N. ; Salomon, J.B.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c370t-2d9c2706bf786396b091f234223d56b90aed4f47765051d1d2846c884e5860073</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2005</creationdate><topic>Analytic methods</topic><topic>diffusion</topic><topic>equations</topic><topic>Heat equation</topic><topic>mathematical models</topic><topic>Parabolic partial differential equations of degenerate type</topic><topic>Singularities</topic><topic>soil water movement</topic><topic>unsaturated flow</topic><topic>wetting front</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Prasad, S.N.</creatorcontrib><creatorcontrib>Salomon, J.B.</creatorcontrib><collection>AGRIS</collection><collection>CrossRef</collection><collection>Aqualine</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Advances in water resources</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Prasad, S.N.</au><au>Salomon, J.B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A new method for the analytical solution of a degenerate diffusion equation</atitle><jtitle>Advances in water resources</jtitle><date>2005-10-01</date><risdate>2005</risdate><volume>28</volume><issue>10</issue><spage>1091</spage><epage>1101</epage><pages>1091-1101</pages><issn>0309-1708</issn><eissn>1872-9657</eissn><abstract>Certain nonlinear diffusion equations of degenerate parabolic type display a finite speed of propagation of disturbances. This mathematical behavior can be used to describe a wide range of nonlinear phenomena such as the penetration distance of a thermal layer, the boundary of a reaction zone, or a wetting front in unsaturated soil moisture flow. However, there are two main difficulties in obtaining solutions to problems of this class. One is that the location of the interface is not known a priori and must be discovered during the analysis. The other is the fact that the differential equation is singular in the neighborhood of the interface. The solution technique developed and presented in this work overcomes these difficulties by extracting a local solution of the differential equation in the neighborhood of the diffusing front. One profound result is the discovery that the velocity of the front is entirely controlled by the first term of the spectral series expansion. Also, by capturing the critical behavior of the solution in the region of the singularity and incorporating the behavior as a dominant factor, the series expansion is provided a means for very rapid convergence. The versatility of the solution technique is demonstrated by solving various boundary value problems covering a broad range of interest and the solutions are tested against previously published results.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.advwatres.2005.04.005</doi><tpages>11</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0309-1708
ispartof Advances in water resources, 2005-10, Vol.28 (10), p.1091-1101
issn 0309-1708
1872-9657
language eng
recordid cdi_proquest_miscellaneous_17475979
source Elsevier ScienceDirect Journals
subjects Analytic methods
diffusion
equations
Heat equation
mathematical models
Parabolic partial differential equations of degenerate type
Singularities
soil water movement
unsaturated flow
wetting front
title A new method for the analytical solution of a degenerate diffusion equation
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-25T20%3A03%3A36IST&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=A%20new%20method%20for%20the%20analytical%20solution%20of%20a%20degenerate%20diffusion%20equation&rft.jtitle=Advances%20in%20water%20resources&rft.au=Prasad,%20S.N.&rft.date=2005-10-01&rft.volume=28&rft.issue=10&rft.spage=1091&rft.epage=1101&rft.pages=1091-1101&rft.issn=0309-1708&rft.eissn=1872-9657&rft_id=info:doi/10.1016/j.advwatres.2005.04.005&rft_dat=%3Cproquest_cross%3E17475979%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=17475979&rft_id=info:pmid/&rft_els_id=S0309170805000989&rfr_iscdi=true