EXPERIMENTAL STUDIES OF WETTING FRONT INSTABILITY INDUCED BY GRADUAL CHANGE OF PRESSURE GRADIENT AND BY HETEROGENEOUS POROUS MEDIA.

Simple item page
dc.contributor.authorWhite, I.en
dc.contributor.authorColombera, P. M.en
dc.contributor.authorPhilip, J. R.en
dc.date.accessioned2026-01-05T21:42:14Z
dc.date.available2026-01-05T21:42:14Z
dc.date.issued1977en
dc.description.abstractExperimental observations on the onset of instabilities and the wavelengths of disturbances formed in infiltration flows, when the pressure gradient was gradually increased through zero, were compared with the stability analysis of J. R. Philip. For this case and for that of step-increase in conductivity with depth the theory gave a satisfactory account of the onset and development of instability in Hele-Shaw cells.en
dc.description.statusPeer-revieweden
dc.format.extent7en
dc.identifier.issn0361-5995en
dc.identifier.otherORCID:/0000-0002-5455-4514/work/177449076en
dc.identifier.scopus0017485131en
dc.identifier.urihttps://hdl.handle.net/1885/733803774
dc.language.isoenen
dc.sourceSoil Science Society of America Journalen
dc.titleEXPERIMENTAL STUDIES OF WETTING FRONT INSTABILITY INDUCED BY GRADUAL CHANGE OF PRESSURE GRADIENT AND BY HETEROGENEOUS POROUS MEDIA.en
dc.typeJournal articleen
dspace.entity.typePublicationen
local.bibliographicCitation.lastpage489en
local.bibliographicCitation.startpage483en
local.contributor.affiliationWhite, I.; Fenner School of Environment & Society Academic, Fenner School of Environment & Society, ANU College of Systems and Society, The Australian National Universityen
local.identifier.citationvolume41en
local.identifier.doi10.2136/sssaj1977.03615995004100030010xen
local.identifier.pure8103e6cd-0e8e-4814-bb7a-ee54e773f49den
local.identifier.urlhttps://www.scopus.com/pages/publications/0017485131en
local.type.statusPublisheden

Downloads

Collections

ANU Research Publications

DSpace software copyright © 2002-2026 LYRASIS