Non-linear wave-induced transient response of soil around a trenched pipeline
Introduction
Wave-induced forces upon submarine pipelines have attracted extensive attention from coastal engineers, for the ever-increasing engineering activities in offshore and coastal regions. To reduce wave-induced forces and thereby to enhance their stability, offshore pipelines are always trenched into seabed. The trenches are generally backfilled either by in situ sediment or by pouring selected backfill material over the pipeline from bottom-dump barge. When water waves propagate over a porous seabed, cyclic excess pore pressures can be generated within seabed with accompanying decrease in effective stresses, which have been recognized as dominant factors for the instability of a buried pipeline. Thus, a proper evaluation of the wave-induced excess pore pressures around pipeline is important for offshore geotechnical engineers involved with the design of foundations for offshore pipeline.
There have been various analytical investigations of the problem of seabed response to wave loading, based on different assumptions of the rigidity of soil skeleton and compressibility of pore fluid, including Madsen, 1978, Yamamoto et al., 1978, Mei and Foda, 1981, Jeng, 1997. Besides the development of analytical solutions, numerical simulations have been widely applied to examine such a problem in recent years, such as the finite difference method (Zen and Yamazaki, 1990), the finite element method (Thomas, 1989, Gatmiri, 1990, Jeng and Lin, 1996). Most previous investigations of the wave–seabed interaction have been reviewed by Jeng (2003). However, all aforementioned investigations have only examined the soil response under the action of two-dimensional progressive waves in the absence of a marine structure.
The importance of wave–soil–pipeline interaction phenomenon has ever been addressed in the literature (Clukey et al., 1989). To date, this problem has not yet been fully understood because of the complicated behavior of soils and the special geometry of pipeline. Design of marine pipelines regarding their stability is a rather complicated problem. Based on the potential theory, the hydrodynamic uplift forces on the buried pipelines have been studied (MacPherson, 1978, Spierenburg, 1986, MacDougal et al., 1988). However, the potential theory is somewhat far from the realistic conditions of soil as a two-phase medium. Based on Biot's consolidation theory (Biot, 1941), the wave-induced pore pressure around a buried pipeline has been studied through a boundary integral equation method (Cheng and Liu, 1986) and a finite element method (Magda, 1997). Among these, Cheng and Liu (1986) considered a buried pipe in a region that is surrounded by two impermeable walls. Magda (1997) considered a similar case with a wider range of the degree of saturation. Jeng (2001) proposed a 2D FEM model to investigate the wave-induced pore pressure, effective stresses within soil around buried pipeline. However, most previous investigations of the wave–seabed–pipe interaction problem have been concerned only with a single sediment layer and linear wave loading. In engineering practice, pipelines are always trenched and covered with coarser materials, especially in shallow water. Moreover, the actual waves in shallow water zone are always characterized as non-linear. However, the non-linear wave-induced responses of backfill soils around trenched pipeline have not been revealed yet.
This paper is aimed at developing a finite element model for investigating the effects of backfill soil properties on non-linear wave-induced excess pore pressures upon a trenched pipeline, which will be verified with existing experimental results. The effects of non-linear component of wave loading are examined firstly. Moreover, the influences of the physical properties of backfill materials and the geometry profile of trenches are thereafter numerically evaluated, respectively, by varying shear modulus, permeability coefficient of backfill soil, slope angle and depth of trenches, etc.
Section snippets
Governing equations and boundary conditions
In this study, a two-dimensional problem is considered. A pipeline (with outer diameter of D) is fully buried within a trench in a porous seabed of finite thickness h laid upon an impermeable rigid bottom, as depicted in Fig. 1. The geometry profile of the trench is characterized by trench depth S, bottom width B and slope angle ϕ. The wave is assumed to propagate in the positive x-direction, while the z-direction is upward from the interface between porous seabed and impermeable rigid bottom.
Finite element formulations for porous seabed
The second-order non-linear wave-induced oscillatory soil response is periodically fluctuating in the temporal domain. Similar to expression form of wave pressure at the surface of seabed in Eq. (15), the wave-induced excess pore pressure, soil displacements and effective stresses within seabed can be expressed aswhere Qj (j=1,…,6) represents p, us, ws, , and , respectively. Subscripts ‘r’ and ‘c’
Verification of the numerical model
To verify the aforementioned non-linear wave–soil–pipe interaction numerical model, a comparison of the numerical results with the experimental results by Sudhan et al., 2002, Turcotte et al., 1984 is carried out, as shown in Fig. 3. The tests by Sudhan et al. (2002) were conducted in a 30 m long, 2 m wide and 1.7 m deep wave flume. The aluminum pipe 200 mm in diameter, 1.96 m in length with 10 mm thick walls was buried within sand pit 2.0 m×2.0 m×0.6 m in size, where the uniform and fairy homogeneous
Parametric study and discussion
In this study, the above FEM model is used to investigate the transient response of soil around trenched pipeline under non-linear wave loading. The input data for the investigations are listed in Table 1.
Conclusions
A two-dimensional finite element model is developed to investigate the non-linear wave-induced transient response of soil around a trenched pipeline, which is verified with flume test results by Turcotte et al., 1984, Sudhan et al., 2002. The effects of wave non-linearity and backfill soil properties on the distribution of excess pore pressure are examined parametrically. Based on the numerical results, the following conclusions can be drawn:
- (1)
The bottom pressure fluctuations induced by
Acknowledgements
Financial support by ‘Tenth Five-year Plan’ of Chinese Academy of Sciences (Project No. KJCX2-SW-L03) is greatly appreciated. The authors also thank Dr Dong-Sheng Jeng at the University of Sydney for his valuable discussions.
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2022, Ocean EngineeringCitation Excerpt :On the wave-induced dynamics of marine pipeline and its seabed foundation, a few works have been conducted in the past two decades. Most of them were limited to the very dense seabed soil whose behaviour can be nearly modelled by poro-elastic model (Gao and Wu, 2006; Luan et al., 2008; Duan et al., 2017; Zhou et al., 2015; Zhang et al., 2011). In fact, there is another type of seafloor soil widely distributed in the offshore zone worldwide.