dc.contributor.author |
Stavropoulou, M |
en |
dc.contributor.author |
Vardoulakis, I |
en |
dc.contributor.author |
Tronvoll, J |
en |
dc.date.accessioned |
2014-03-01T01:45:36Z |
|
dc.date.available |
2014-03-01T01:45:36Z |
|
dc.date.issued |
1997 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/24652 |
|
dc.subject |
Flow Rate |
en |
dc.subject |
Fluid Flow |
en |
dc.subject |
Porous Media |
en |
dc.subject |
Turbulent Flow |
en |
dc.subject |
X-ray Ct |
en |
dc.title |
Hydrodynamic erosion; A potential mechanism of sand production in weak sandstones |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1016/S1365-1609(97)00190-1 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1016/S1365-1609(97)00190-1 |
en |
heal.publicationDate |
1997 |
en |
heal.abstract |
Fluidized column experiments have been performed, where a 10 cm in diameter and 15 cm high cylindrical sand column was subjected to linear upwards flow of water. The tests were monitored by means of an X-ray CT-scanner. The experiments showed that a change in the flow rate gave rise to a propagating density wave starting upstream at the bottom of |
en |
heal.journalName |
International Journal of Rock Mechanics and Mining Sciences |
en |
dc.identifier.doi |
10.1016/S1365-1609(97)00190-1 |
en |