Centrifuge Model Study of SCR Motion in Touchdown Zone

Author(s):  
Her Jia Eddie Hu ◽  
Chun Fai Leung ◽  
Yean Khow Chow ◽  
Andrew Clennel Palmer

Steel catenary risers (SCRs) connect seabed pipelines and flow lines to floating structures used for oil and gas production in deep water. Waves and currents induce motions of the structure and the risers. Repeated horizontal and vertical interactions of SCR at the touchdown zone would induce loads on the seabed soil, and would eventually cause fatigue damage to the risers as the number of load cycle increases. The analysis of SCR fatigue damage is heavily dependent on the soil model. Soil behaviour at touchdown zone such as soil remolding, stiffness degradation and deformation of the seabed at the touchdown zone further complicate the accurate assessment of SCR fatigue damage, which is not appropriately quantified in existing design methods. This paper presents model tests simulating the repeated vertical movement of a length of riser on a geotechnical beam centrifuge at the National University of Singapore. During the tests, the pipe was subject to cyclic motion over fixed vertical displacement amplitude from an invert embedment of 0.5 pipe diameter to 3 pipe diameters into the soil. The results from centrifuge model tests show a significant progressive degradation of soil strength and diminution of excess pore water pressure as the number of load cycle increases. The increased soil strength degradation and diminishing excess negative pore water pressure during cyclic motion of the SCR reduce fatigue damage. In view of different types of environment loadings experienced by the floating platform, test results obtained from parametric studies on the effect of cyclic displacement amplitude on soil stiffness degradation will also be presented in this paper. Lastly, a simple upper bound plasticity solution will be presented and compared with the experimental result.

1988 ◽  
Vol 110 (1) ◽  
pp. 17-23 ◽  
Author(s):  
N. Mori ◽  
Y. Ishikawa ◽  
A. Hirayama ◽  
K. Tamaoki ◽  
H. Kobayashi

Offshore structures are subjected to repeated loads from earthquakes and waves which may cause softening of the clayey seabed foundation. Carrying out a series of model tests on a shaking table, the following results are obtained. Settlement and inclination of a model of the base-part of the structure occur when the excess pore water pressure beneath the model rises to about 5 percent of the initial confining pressure. The earthquake response analysis even taking the nonlinearity of the soil into account cannot predict the results of the model test when the pore water pressure does generate and accumulate. Model tests show that the values of the pore water pressure are about twice as large as those predicted by calculation. From these results, rough evaluation of earthquake stability of the clayey seabed under offshore structures are obtained.


Author(s):  
Trần Thanh Nhàn

In order to observe the end of primary consolidation (EOP) of cohesive soils with and without subjecting to cyclic loading, reconstituted specimens of clayey soils at various Atterberg’s limits were used for oedometer test at different loading increments and undrained cyclic shear test followed by drainage with various cyclic shear directions and a wide range of shear strain amplitudes. The pore water pressure and settlement of the soils were measured with time and the time to EOP was then determined by different methods. It is shown from observed results that the time to EOP determined by 3-t method agrees well with the time required for full dissipation of the pore water pressure and being considerably larger than those determined by Log Time method. These observations were then further evaluated in connection with effects of the Atterberg’s limit and the cyclic loading history.


1981 ◽  
Vol 27 (97) ◽  
pp. 503-505 ◽  
Author(s):  
Ian J. Smalley

AbstractRecent investigations have shown that various factors may affect the shear strength of glacial till and that these factors may be involved in the drumlin-forming process. The presence of frozen till in the deforming zone, variation in pore-water pressure in the till, and the occurrence of random patches of dense stony-till texture have been considered. The occurrence of dense stony till may relate to the dilatancy hypothesis and can be considered a likely drumlin-forming factor within the region of critical stress levels. The up-glacier stress level now appears to be the more important, and to provide a sharper division between drumlin-forming and non-drumlin-forming conditions.


2018 ◽  
Vol 35 (2) ◽  
pp. 111
Author(s):  
Kun ZHANG ◽  
Ze ZHANG ◽  
Xiangyang SHI ◽  
Sihai LI ◽  
Donghui XIAO

Sign in / Sign up

Export Citation Format

Share Document