dc.contributor.author |
Christodoulou George, C |
en |
dc.date.accessioned |
2014-03-01T01:08:19Z |
|
dc.date.available |
2014-03-01T01:08:19Z |
|
dc.date.issued |
1991 |
en |
dc.identifier.issn |
0022-1686 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/10411 |
|
dc.relation.uri |
http://www.scopus.com/inward/record.url?eid=2-s2.0-0026360530&partnerID=40&md5=5d1a8d559beb5f3cc1329ab9a789a76d |
en |
dc.subject.classification |
Engineering, Civil |
en |
dc.subject.classification |
Water Resources |
en |
dc.subject.other |
Fluid Mechanics--Mathematical Models |
en |
dc.subject.other |
Fluids--Concentration |
en |
dc.subject.other |
Fluids--Density |
en |
dc.subject.other |
Dilution |
en |
dc.subject.other |
Sloping Bottoms |
en |
dc.subject.other |
Flow of Water |
en |
dc.subject.other |
Dense |
en |
dc.subject.other |
Effluent Dispersal |
en |
dc.title |
Dilution of dense effluents on a sloping bottom |
en |
heal.type |
journalArticle |
en |
heal.language |
English |
en |
heal.publicationDate |
1991 |
en |
heal.abstract |
A simple model is proposed for evaluating the dilution and other main characteristics of a dense boundary-attached 3-D plume, created by the disposal of heavier effluent into a quiescent homogeneous ambient. It is based on matching requirements between the near-and intermediate field, which allow the calculation of necessary quantities at the initiation of the bottom plume in terms of the initial discharge parameters. The subsequent spreading is described through a generalization of available data. |
en |
heal.publisher |
INT ASSN HYDRAULIC RESEARCH |
en |
heal.journalName |
Journal of Hydraulic Research |
en |
dc.identifier.isi |
ISI:A1991FT83400003 |
en |
dc.identifier.volume |
29 |
en |
dc.identifier.issue |
3 |
en |
dc.identifier.spage |
329 |
en |
dc.identifier.epage |
339 |
en |