Sentence examples for behaviour of sediments from inspiring English sources

A specific application relating to the formation of silica aggregates is described from which the behaviour of sediments containing these materials can be predicted on the basis of a bench-top test and the use of a Lattice Boltzmann simulation.

These methods are unable to understand the behaviour of sediment transport in rivers due to the complexity, noise, non-stationarity, and dynamism of the sediment pattern.

The behaviour of compressible sediments and filter cakes is of significant fundamental interest and widespread practical importance; for example, in the area of solid liquid separation engineering.

Results from tests performed with variable strain rates suggest that the time-dependent (viscous) behaviour of the sediments may be governed by their mineralogy, in particular the presence of plastic fines.

From the graphs and statistics it is apparent that MLPs capture the complex non-linear behaviour of the sediment series relatively better than the conventional models.

The complex processes of the suspension, resettling and consolidation behaviour of deep-sea sediments caused by deep-ocean mining were investigated on board the German RV Sonne and in the laboratory using sediment from the uppermost semi-liquid layer of the Peru Basin.

To evaluate the sorption capacity and desorption behaviour of the biofilm-sediment system, batch experiments were conducted with 8 g sediment and their corresponding formed biofilm.

Behaviour of invertebrates inside sediment showed impairments of body movements in worms exposed to CdS NPs.

Laboratory experiments to simulate landscapes and stratigraphy often suffer from scale effects, because reducing length- and time scales leads to different behaviour of water and sediment.

The results indicate that NTA is a complementary method to existing approaches to characterise the fate and behaviour of ENPs in natural sediment.

Trace elements are particularly useful as indicators of palaeoenvironmental condition of sediments because of differential geochemical behaviour at different oxidation states of the elements (Tribovillard et al. 2006).