Thus, agriculture practices can be adapted with respect to sediments through changing the crops and through new cultivation as well in the aggraded land.
Dead fish were counted and removed along with bottom sediments before changing the water about 30% from the rearing volume every 24 h.
Tidally residual suspended sediment flux varied with the changing sediment dynamics.
Throughout deglaciation, deposition within the lake was characterized by abrupt changes in grain size and in the architecture of individual sediment bodies, reflecting changing delivery paths and sediment supply, and by dynamic margin oscillations typical of water-terminating glaciers.
Modelling suggested that these data could only be partially controlled by transport capacity implying an important role for sediment supply and potentially for the influence of changing sediment connectivity.
If the fluid has sediment in it, changing the fluid could cause the sediment to stick to the gears.
In addition, changing sediment supply plays a role in overall sediment architecture, but is only well resolved for the Holocene, with higher rates of fluvial supply recognised in the mid Holocene.
However, further perturbation, for example by glacial advance or extreme climatic events, would likely modify the pattern of suspended sediment yields by changing terrain surface mobilization thresholds and reconfiguring channel sediment stores.
Across-shelf variations in sediment 40Ar/39Ar age reflect changing modes of sediment dispersal on the continental shelf.
The Adriatic Sea is one place where changing sediment pathways and along-strike currents have a major impact on sequence architecture.
