ABSTRACT
A series of flume- and laboratory-based experiments defined and quantified the thresholds of sunken oil transport using No.6 heavy fuel oil mixed with kaolinite clay. When the sunken oil became mobile, the current-induced bed shear stress exceeded a threshold value specific to the oil, known as critical shear stress (CSS). The oil's CSS was evaluated as a function of water velocity, water temperature, oil condition, and sediment size. Based on experimental results, the stages of oil transport were defined and empirical relationships using the oil's kinematic viscosity (vo) and sediment size were developed to predict oil CSS at each transport stage. For vo<2 × 104 cSt, multiple thresholds of movement were observed: (1) gravity dispersion, (2) rope formation, (3) ripple formation, and (4) break-apart/resuspension. When vo> 6 × 104 cSt, transport was more likely to occur as a single event with the oil remaining intact, saltating over the bed in the direction of flow.
