Flocculated suspended sediment in a micro-tidal environment
Silt and clay particles are unstable when suspended in saline waters. They coagulate into sediment flocs having settling velocities orders of magnitude higher than the individual particles constituting them. In the Danish Wadden Sea in-situ analyses were carried out to obtain the natural textural co...
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Veröffentlicht in: | Sedimentary geology 1988-06, Vol.57 (3), p.249-256 |
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