Watercourse


Reshaping

Updated on 26/10/2022
Définition
Sens technique
Modification and homogenization of the longitudinal profile of the river (slope), always to increase its discharge capacity. Reshaping consists in equalizing the slope of the stream, changing the zoning of the longitudinal profile. This operation requires the removal of riparian vegetation and
Source
According to OFB

Longitudinal profile

Updated on 13/07/2018
Définition
Sens technique
Profile that characterizes the slope of the watercourse or more generally the thalweg. This slope tends to decrease downstream (concave profile) and different river features are succeeding from upstream to downstream.
Source
According to IGN

Equilibrium profile

Updated on 04/07/2018
Définition
Sens technique
Longitudinal profile of a river whose erosive power is not sufficient.
Source
According to MNHN

Floodplain

Updated on 04/07/2018
Définition
Sens commun
Valley bottom adjacent to a stream which is (or, in the past, was) periodically flooded.
Source
According to AFNOR

Specific power of a river

Updated on 13/07/2018
Définition
Sens technique
Power calculated as the product of the slope and flow rate that characterizes the dynamic potential of the river. The adjustment capacity of the river is largely a function of the specific power.
Source
According to Seine-Normandy Water Agency

Morphology

Updated on 26/10/2022
Définition
Sens commun
Science that studies the characteristics, configuration and evolution of forms of grounds and rocks. The main elements that characterize it are: the cross section profile, longitudinal profile, meanderings, river styles, flow velocity, succession of facies, grain size variations, riparian corridor, and the relationship with the alluvial groundwater sheet.
Source
According to OFB

Spawning run

Updated on 04/07/2018
Définition
Sens commun
Action of migratory fish going up a river to reach its spawning or growth area.
Source
According to Rhone-Alps Regional Council

Meander

Updated on 13/07/2018
Définition
Sens commun

Section between two successive turning points. On the outside of the curve (or extrados) the concave river bank is eroded, steep, and conducive to lateral erosion. On the inside of the curve (or intrados) the convex river bank is sloping gently, suitable for sedimentation of alluvial benches. There are two main types of meanders, incised meanders and free meanders, and an intermediate type, forced cut meanders.

Source
According to Cemagref

Minor bed

Updated on 26/10/2022
Définition
Sens commun

Part of the bed between well-marked river banks in which water entirely flows outside periods of very high-flow and overflowing. The minor bed includes the low-water channel. Its limit is the bankfull discharge channel. In the case of a braided bed, there may be several flow channels. The minor bed is home to varied flora and fauna (fish, invertebrates, crayfish, mussels, diatoms, macrophytes, etc) whose population status is closely linked to the heterogeneity of the bed and to connections with the floodplain and

Source
According to OFB