Sentence examples for motion and sediment from inspiring English sources

Classically, scaling proceeded from dimensional analysis of the equations of motion and sediment transport, and minor concessions, such as vertical length scale distortion, led to acceptable results.

Light, water motion and sediment transport might influence the distribution of the two morphotypes.

Light, water motion and sediment transport are determining factors in the distribution of gorgonians [ 49].

In E. flexuosa, the differences of the two morphotypes are related to depth profiles, water motion and sediment transport.

The distribution of the species spans through several environmental gradients (e.g., depth, light, water motion and sediment transport) [ 90] and display an unusual amount of morphological variability.

In this study, first, the morphological variation of 14 traits of E. flexuosa was evaluated in seven reefs (from protected to exposed areas to water motion) at two depths (< 5 m and >17 m) and the correlation of morphology with light, water motion and sediment patterns was inferred.

The two morphotypes found in two depth habitats (hereafter deep and shallow indicating the depth of habitat) are exposed to different water motion, light, and sediment transport regimes.

Since 80% of the variation was explained by the first two principal components, environmental gradients related to depth, water motion, light and sediment transport could probably explain a portion of the morphological differences.

It firstly provides a critical appraisal of prevailing conceptual models of proglacial systems, and uses this to justify compiling data on rates of landform change in terms of planform, horizontal motion, elevation changes and sediment budgets.

This velocity (Vt) is added to the vertical velocity of fluid motion at every time step, until the marker particle ceases its motion and settles as sediment when they reach the ground surface.

With respect to strong motion data, Takai et al. (2016) observed clear differences in the ground motions between the rock and sediment sites in the Kathmandu valley.