The paper outlines the processes that determine pipeline embedment in soft sediments typical of deep water, and describes quantitative methods for assessing the contribution to pipeline embedment from each process. The main processes considered are: self-weight, force concentration during installation, and cyclic lateral and vertical motion during pipe-laying. For each process, non-dimensionalized solutions are provided to evaluate embedment for given pipeline and soil properties, and different conditions operative during pipe-laying. Methods to establish a penetration resistance profile using modern penetration testing techniques are described, and the up-scaling of these measurements to pipeline behavior is discussed. The important effects of heave and soil self-weight are also quantified, and the effects of remolding and subsequent reconsolidation following a cyclic event are also demonstrated. Finally, the influence of cyclic motion within the touchdown zone during pipe-laying is explored. Examples of numerical and physical modeling of the lay process show that these dynamic effects can have a dominant influence on the as-laid embedment. Approaches for quantifying this aspect of behavior in design are discussed.
OTC 19128and is the parameter that most significantly affects the feasibility of a design [1]. Empirical and theoretical solutions for predicting pipeline embedment are available, but are consistently found to under-estimate the embedment when compared with field survey data, primarily due to additional penetration caused by the static load concentration at the touchdown point, and dynamic oscillations of the pipeline as it is laid [2]. This paper examines recent developments in estimating pipeline penetration, including theoretical studies based on large deformation finite element analysis, and physical model tests to evaluate the effect of cyclic deformations on pipeline penetration.
Seabed CharacterizationImproved reliability in estimating pipeline penetration hinges on accurate measurement of the shear strength profile, particularly in the upper 0.5 m of the seabed. Techniques to achieve this include: (a) in situ testing; (b) ship-based vane or penetrometer tests in box-cores recovered from the seabed; (c) laboratory tests on samples obtained from the seabed. All such measurements become more challenging in very soft sediments, either because of disturbance to the recovered samples or, for the in situ testing, due to minor errors in the depth datum or load cell zero readings, both of which become much more significant at shallow depths and low strength material.Modern techniques for obtaining large diameter piston cores have led to improvement in sample quality over most of the sample length [3,4], but any slight delay in triggering the piston of gravity corers will lead to gross disturbance of the very shallow soils, and also to uncertainty in the depth datum [5]. The development of a static sampler activated from a fixed frame [6] should lead to further improvement, provided the shallow material...