dc.contributor.author |
Marinos, V |
en |
dc.contributor.author |
Fortsakis, P |
en |
dc.contributor.author |
Prountzopoulos, G |
en |
dc.contributor.author |
Marinos, P |
en |
dc.date.accessioned |
2014-03-01T01:36:38Z |
|
dc.date.available |
2014-03-01T01:36:38Z |
|
dc.date.issued |
2011 |
en |
dc.identifier.issn |
1672-6316 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/21367 |
|
dc.subject |
Dams |
en |
dc.subject |
Distribution with depth |
en |
dc.subject |
Flysch |
en |
dc.subject |
Grout curtain |
en |
dc.subject |
Permeability |
en |
dc.subject.classification |
Environmental Sciences |
en |
dc.title |
Permeability in flysch - Distribution decrease with depth and grout curtains under dams |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1007/s11629-011-2108-5 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1007/s11629-011-2108-5 |
en |
heal.language |
English |
en |
heal.publicationDate |
2011 |
en |
heal.abstract |
A considerable number of in situ permeability tests in flysch are processed to a depth of 120m with a good spatial distribution. The distribution of permeability values for the different litho-types of this formation, their comparison and their decrease with depth is discussed. The depth where a permeability of 3 to 5×10-7m/sec can be retained (the limit of a reasonable grouting under a high dam) may be twofold if the geological history of the formation could not contain a compressional tectonic process. This depth may reach 100m in some cases. The differences in the mean values of permeability among the various litho-types are minor, while the presence of siltstones, always present although with varied participation, dramatically controls the global permeability. © 2011 Science Press, Institute of Mountain Hazards and Environment, CAS and Springer-Verlag Berlin Heidelberg. |
en |
heal.publisher |
SCIENCE CHINA PRESS |
en |
heal.journalName |
Journal of Mountain Science |
en |
dc.identifier.doi |
10.1007/s11629-011-2108-5 |
en |
dc.identifier.isi |
ISI:000289004600015 |
en |
dc.identifier.volume |
8 |
en |
dc.identifier.issue |
2 |
en |
dc.identifier.spage |
234 |
en |
dc.identifier.epage |
238 |
en |