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  4. Stability of artificial subaqueous slopes in sandy soils under wave loads

Stability of artificial subaqueous slopes in sandy soils under wave loads

Publikationstyp
Conference Paper
Date Issued
2015-05
Sprache
English
Author(s)
Bubel, Julian
Pick, Marc-André
Grabe, Jürgen
Institut
Geotechnik und Baubetrieb B-5
TORE-URI
http://hdl.handle.net/11420/7250
First published in
Proceedings of the International Conference on Offshore Mechanics and Arctic Engineering - OMAE
Number in series
1-2015
Citation
34th International Conference on Ocean, Offshore and Arctic Engineering, OMAE 2015
Contribution to Conference
34th International Conference on Ocean, Offshore and Arctic Engineering, OMAE 2015
Publisher DOI
10.1115/OMAE201541827
Scopus ID
2-s2.0-84947801610
Publisher
American Society of Mechanical Engineers (ASME)
ISBN of container
978-0-7918-5647-5
Shallow foundation structures in marine environments can rarely be placed on top of the sea floor. Weak soils usually need to be excavated to place the structure on more stable ground. Steep but stable slopes of the resulting pit meet both economic and ecologic aims as they minimise material movement and sediment disturbance. This paper focuses changes of geometry of submarine slopes in non-cohesive soils (erosion, sedimentation, breach failure, liquefaction failure) due to surface waves. After Terzaghi the angle between slope and the horizontal of the ground surface of cohesionless soil is at most equal to the critical state friction angle, as obviously true for dry soil. However, it can be observed that natural submarine slopes of sandy soils are always mildly sloped. During the construction of artificial submarine pits under offshore conditions it should be considered that the long-term slope-inclination is less than onshore due to hydrodynamic actions (e. g. flow, waves, earthquakes). Large surface waves cause excess pore water pressures within the soil body, leading to a reduction of effective stresses and in case of submarine slopes to changes of the slope geometry depending on wave length L, wave height H, water depth h and soil properties (permeability k, relative density Dr). During our preliminary work we investigated such processes based on the coupling of linear wave theory and linear quasistatic consolidation theory (e.g. [1]). With the help of numerical modelling we solved corresponding equations considering also materially nonlinear consolidation. However, deformations were always limited by used Lagrangian-FEM. Recent developments at our Institute enable the use of an Eulerian-FEM approach with an u-p-Formulation for fully saturated soil [2]. This allows larger deformations of the subaqueous slope to be numerically investigated.
DDC Class
600: Technology
Funding(s)
Stabilität von künstlichen Unterwasserböschungen in sandigen Böden
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