Abstract
Laboratory experiments show that the propagation and sedimentation patterns of particle‐laden gravity currents are strongly influenced by the size of suspended particles. The main series of experiments consisted of fixed‐volume releases of dilute mixtures containing two sizes of silicon carbide particles (25 μm and 69 μm mean diameter) within a 6‐m flume. Polydisperse experiments involved mixtures of five different particle sizes and variation of the amounts of the finest and coarsest particles. All variables apart from the initial relative proportions of particles were identical in the experiments. The effects of mixing different proportions of fine and coarse particles is markedly non‐linear. Adding small amounts of fine sediment to a coarse‐grained gravity current has a much larger influence on flow velocity, run‐out distance and sedimentation patterns than adding a small amount of coarse sediment to a fine‐grained gravity current. The experiments show that adding small amounts of fine particles to a coarse‐grained current results in enhanced flow velocities because the fine sediment remains suspended and maintains an excess current density for a much longer time. Thus, the distance to which coarse particles are transported increases substantially as the proportion of fines in the flow is increased. Our experiments suggest that sandy turbidity currents containing suspended fines will be much more extensive than turbidity currents composed of clean sand.