An anaytical solution of the vertically one-dimensional convection-diffusion equation
DC Field | Value | Language |
---|---|---|
dc.contributor.author | 정경태 | - |
dc.contributor.author | 김창식 | - |
dc.contributor.author | 이종찬 | - |
dc.contributor.author | 강현우 | - |
dc.contributor.author | 진재율 | - |
dc.contributor.author | 김미경 | - |
dc.contributor.author | 존노이 | - |
dc.date.accessioned | 2020-07-17T12:51:12Z | - |
dc.date.available | 2020-07-17T12:51:12Z | - |
dc.date.created | 2020-02-11 | - |
dc.date.issued | 2003-05-24 | - |
dc.identifier.uri | https://sciwatch.kiost.ac.kr/handle/2020.kiost/32278 | - |
dc.description.abstract | The vertically one-dimensional diffusion equation has been solved analytically in the presence of downward convective velocity and boundary fluxes. The convection-diffusion equation has been transformed into a simple fiffusion equation amd the Galerkin eigenfunction method has been applied. Applications have been made on two problems, the determination of the time-varying vertical structure of suspended sediment associated with erosion and deposition processes, and the calculation of sea water temperature under surface heat flux. | - |
dc.description.uri | 2 | - |
dc.language | English | - |
dc.publisher | 한국해양환경공학회 | - |
dc.relation.isPartOf | 연직1차원 이송확산식의 이론해 | - |
dc.title | An anaytical solution of the vertically one-dimensional convection-diffusion equation | - |
dc.type | Conference | - |
dc.citation.conferencePlace | KO | - |
dc.citation.endPage | 258 | - |
dc.citation.startPage | 251 | - |
dc.citation.title | 연직1차원 이송확산식의 이론해 | - |
dc.contributor.alternativeName | 정경태 | - |
dc.contributor.alternativeName | 김창식 | - |
dc.contributor.alternativeName | 이종찬 | - |
dc.contributor.alternativeName | 강현우 | - |
dc.contributor.alternativeName | 진재율 | - |
dc.contributor.alternativeName | 김미경 | - |
dc.identifier.bibliographicCitation | 연직1차원 이송확산식의 이론해, pp.251 - 258 | - |
dc.description.journalClass | 2 | - |