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Fluid mud layer is close to the sediment hyperconcentrated water between it and the upper body of water has obvious interface, it has great mobility. Foreign fluid mud research began in the 1950s, Inglis and allen (1957) at the time of the thames estuary sediment movement in great britain for the first time using a fluid mud; Then the fluid mud were found in the gironde estuary in france, the mississippi of the united states,Thailand weinan estuaries and other coastal estuary muddy; Migniot (1968) and dutch engineering consulting association (1968) were also used "cremede vase" and "sling mud" other names; Kirby and parker (1983) for a definition of the fluid mud;Parker and hooper (1994) has an alternative fluid mud with "high concentration of water in the sediment layer." Domestic fluid mud research began in the 1960s, which was first discovered in tianjin new harbor back silting studysubsequently found in lianyun port,Shanghai port,and Yellow river estuary, Yangtze river estuary and other mucky ports estuaries;In recent years the three gorges reservoir, Xiaolangdi reservoir have also found that the presence of fluid mud. Fluid mud is widely present in the estary,gulf,inland waterways,lakes and reservoirs; It is closely related to port and waterway silting,sailing depth use,reservoir sediment density current and water pollution problem;Thus causing a large number of researchers on the causes fluid mud,defining and motion characteristics,and aspects of research and exploration,We made a series of scientific research. But being limited field data and experimental conditions, At home and abroad in recent years it has been little progress in their research.

Formation and motion characteristics of summary fluid mud