dc.contributor.author |
Apostolopoulos, G |
en |
dc.contributor.author |
Amolochitis, G |
en |
dc.contributor.author |
Stamataki, S |
en |
dc.date.accessioned |
2014-03-01T02:51:07Z |
|
dc.date.available |
2014-03-01T02:51:07Z |
|
dc.date.issued |
2007 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/35380 |
|
dc.relation.uri |
http://www.scopus.com/inward/record.url?eid=2-s2.0-55849148990&partnerID=40&md5=fbfea0b27ddff0cb92f0b1b354c696d1 |
en |
dc.subject.other |
Bed-rocks |
en |
dc.subject.other |
Electrode configurations |
en |
dc.subject.other |
Electrode distances |
en |
dc.subject.other |
Marine cables |
en |
dc.subject.other |
Port constructions |
en |
dc.subject.other |
Resistivity tomographies |
en |
dc.subject.other |
Resistivity values |
en |
dc.subject.other |
RMS errors |
en |
dc.subject.other |
Schlumberger |
en |
dc.subject.other |
Sea bottoms |
en |
dc.subject.other |
Signal-to-Noise ratios |
en |
dc.subject.other |
Sudden changes |
en |
dc.subject.other |
Well datums |
en |
dc.subject.other |
Diagnostic radiography |
en |
dc.subject.other |
Electrolysis |
en |
dc.subject.other |
Excavation |
en |
dc.subject.other |
Exhibitions |
en |
dc.subject.other |
Medical imaging |
en |
dc.subject.other |
Poles |
en |
dc.subject.other |
Ports and harbors |
en |
dc.subject.other |
Signal to noise ratio |
en |
dc.subject.other |
Tomography |
en |
dc.subject.other |
Ocean structures |
en |
dc.title |
Marine resistivity tomography prior excavation works in port construction |
en |
heal.type |
conferenceItem |
en |
heal.publicationDate |
2007 |
en |
heal.abstract |
The detection of bedrock relief under the sea bottom is of great importance for the excavation works in port construction as well as for the foundation of various installations. Marine resistivity tomography profiles, properly positioned to cover the area under investigation and to avoid various obstacles, can provide this information. Precise knowledge of bathymetry is required in order to give reliable results. Well data for reference are valuable in defining and verifying the sudden changes of resistivity values in the sections. The Schlumberger electrode configuration is preferred with its more efficient signal-to-noise ratio. Pole-Pole can give information which is less accurate in horizontal layering but offers deeper detection. The RMS error in interpretation takes higher values when the sea bottom is deeper. Marine cable with 3m electrode distance and 32 lead takeouts is easily elaborated and effective to detect bedrock relief for depths of sea bottom: 5-15m and depth of investigation for Schlumberger array 20m and polepole 40m. |
en |
heal.journalName |
Society of Petroleum Engineers - 69th European Association of Geoscientists and Engineers Conference and Exhibition 2007 - ""Securing the Future"" |
en |
dc.identifier.volume |
1 |
en |
dc.identifier.spage |
345 |
en |
dc.identifier.epage |
349 |
en |