Sentence examples for point of flow from inspiring English sources
The size of the LSB is defined by the expanse between the point of flow separation and reattachment (Figs. 1, 2) and is generally expressed in terms of the airfoil chord length (x/C) (measured in meter).
Their method is based on the determination of the vanishing point of flow from the lane mark lines and calculating the optical flow along straight lines drawn from the vanishing point.
As RAP decreases, venous return increases until the point of flow limitation.
Hagen Pousille's law clearly shows that flow depends on the pressure gradient from the initial to the distal point of flow and on the length and size of the vessels (i.e. resistances).
Numerical simulation provides the pressure and velocity values at all nodal points of flow domain around the rotating blades.
Ice-blocks ground at points of flow deceleration, generating distinctive patterns of scour and deposition scaled to the obstacle size.
The paper deals with the method intended for determining installation points of flow meters and reducing valves.
They collected 1158 data points of flow boiling heat transfer of R134a in minichannels and reviewed 18 flow boiling heat transfer correlations.
The fahrboschung was defined by (Heim 1932) as the inclination of the line connecting the crest of the landslide source with the toe of the deposits and can be evaluated by the ratio between the elevation difference of the highest and lowest points of flow (H) and the corresponding horizontal distance (L): mathit{tan}alpha =frac{H}{L} (9).
On gently sloping terrain, wetlands occur at broad hollows and points of flow convergence with organic soils and dense vegetation atop permafrost, both of which make soils resistant to initiation of channelized flow.
Locations of trail braiding often occur at stream crossings or other distinct points of flow concentration, such as hollows or groundwater-fed wetlands that are more prone to soil erosion and permafrost degradation, potentially initiating surface-water channels susceptible to headward erosion and the local expansion of drainage density (Dietrich and Dunne 1993); (Knighton 1998).
