River Profile & Flow Flashcards
Gradient: irregularities may arise when
River crosses a boundary, such as between a hard rock and easily erodible rock.
Gradient: can be measured at
Intervals from river source.
Gradient: as the gradient lessens,
The valley widens.
Gradient =
Difference in height (m) / distance (m)
Speed of flow can be estimated by
The manning equation.
Isobel lines are lines that
Connect points of the same water speed in a river.
Longitude profile:
The elevation against distance from the source.
Base level:
The lowest level of the river, cannot go any lower.
Reynolds number: below 500 is
Laminar flow.
Reynolds equation can be rearranged to
Find distance.
Hydraulic radius (m) =
Area of cross section (m2) / wetted perimeter (m)
Wetted perimeter (semi-circle channel) =
π r
Area of cross section (for a semi circle channel) =
1/2 π r2