Experimental and numerical study of wave-induced backfilling beneath submarine pipelines

Deniz Bayraktar, Joseph Ahmad, Bjarke Eltard Larsen, Stefan Carstensen, David R. Fuhrman*

*Bu çalışma için yazışmadan sorumlu yazar

Araştırma sonucu: ???type-name???Makalebilirkişi

21 Atıf (Scopus)

Özet

This paper presents results of complementary experimental and numerical studies involving wave-induced backfilling of current-generated scour holes beneath submarine pipelines. The laboratory experiments are conducted in a wave-plus-current flume, utilizing Laser Doppler Anemometry to measure velocities, synchronized flow visualizations using digital image technology, along with live-bed scour and backfilling measurements. Each experiment is based on a two-stage process: (1) initial scour induced by a pure current, followed by: (2) backfilling induced by pure waves (either regular or irregular). The time series of scour depths are closely monitored through video recordings. Systematic analysis of these has resulted in a closed form expression for the backfilling time scale, which is demonstrated to be a full order of magnitude greater than the well-known time scale of scour (with both governed primarily by the Shields parameter). The developed expression is strictly valid for the current-to-wave backfilling scenarios considered, while likely serving as an upper limit for more general wave-induced backfilling circumstances. The experiments are complemented by similar backfilling simulations utilizing a fully-coupled hydrodynamic and morphodynamic CFD model. The numerical simulations demonstrate the ability of the model to predict backfilling towards expected equilibrium scour depths based on the new wave climate, with time scales reasonably in line with experimental expectations.

Orijinal dilİngilizce
Sayfa (başlangıç-bitiş)63-75
Sayfa sayısı13
DergiCoastal Engineering
Hacim118
DOI'lar
Yayın durumuYayınlandı - 1 Ara 2016

Bibliyografik not

Publisher Copyright:
© 2016 Elsevier B.V.

Finansman

The first author acknowledges the support of a postdoctoral grant from The Scientific and Technical Research Council of Turkey (TUBITAK, grant no. 2219 ). The third and last authors additionally acknowledge support from the FP7-ENV-2013.604-3 European Union project ASTARTE (Assessment, STrategy And Risk Reduction for Tsunamis in Europe), grant no. 603839 .

FinansörlerFinansör numarası
FP7-ENV-2013603839
TUBITAK2219
Türkiye Bilimsel ve Teknolojik Araştirma Kurumu

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